\r\n\tHydroxyapatite (HA) is an important member of the calcium phosphate chemical family. It has been used in several medical applications for the past decades, due to its chemical similarity to the mineral phase of bone and high biocompatibility. Several studies demonstrated that bone mineral presents several ion substitutions, so in order to prepare a synthetic material with an even closer composition to bone mineral, HA has been prepared with the incorporation of several ions like, silicon or fluoride. These ions induced not only structural changes on HA lattice, but also on its biocompatibility. \r\n\tSignificant advances in nanotechnologies resulted in the preparation of HA in different forms, with a wider range of applications, from support to drug and gene delivery. \r\n\tThis book aims to collect the most relevant information regarding HA properties, modifications and its application in the biomedical field.
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1. Introduction
The tooth is a complex organ that consists of enamel, dentin, cementum, and pulp. Missing teeth is frequently occurring problem in aging populations. To treat these defects, the current approach involves prostheses, autotransplantation, and dental implants. The exploration of new strategies for tooth replacement has become a hot topic. Using the foundations of experimental embryology, developmental and molecular biology, tooth regeneration is becoming realistic possibility. Several different methods have been proposed to achieve biological tooth replacement. These include scaffold-based tooth regeneration, cell pellet engineering, stimulation of the formation of a third dentition, and gene-manipulated tooth regeneration. The idea that a third dentition might be locally induced to replace missing teeth is an attractive concept (Young et al., 2005; Edward & Mason, 2006; Takahashi et al., 2008, 2013). This approach is generally presented in terms of adding molecules to induce de novo tooth initiation in the mouth. Tooth development is the result of reciprocal and reiterative signaling between oral ectoderm-derived dental epithelium and cranial neural crest cell-derived dental mesenchyme under genetic control (Thesleff, 2006). More than 200 genes are known to be expressed during tooth development (http://bite-it.helsinki.fi/). A number of mouse mutants are now starting to provide some insights into the mechanisms of supernumerary tooth formation. Multiple supernumerary teeth may have genetic components in their etiology and partially represent the third dentition in humans. Such candidate molecules might be those that are involved in embryonic tooth induction, in successional tooth formation, or in the control of the number of teeth. This means that it may be possible to induce de novo tooth formation by the in situ repression or activation of a single candidate molecule. In this review, we provide an overview of the collective knowledge of tooth regeneration, especially regarding the control of the number of teeth for molecularly targeted therapy by the stimulation of a third dentition.
2. The third dentition
It has been suggested that, in humans, a “third dentition” with one or more supernumerary teeth can occur in addition to the permanent dentition, and supernumerary teeth are sometimes thought to represent a partial post-permanent dentition (Ooe, 1969). The deciduous teeth are, ontogenetically, the first generation of teeth. The permanent teeth (except molar) belong to the second dentition. The term “third dentition” refers to the opinion that one more set of teeth can occur in addition to the permanent teeth (Figure 1). Human teeth are diphyodont excepting the permanent molars. The normal mouse dentition is monophyodont and composed of one incisor and three molars in each quadrant. The number of teeth is usually strictly determined. It was initially reported that there is an anlagen of the third dentition in some mammals (Leche, 1893). The presence of an epithelial anlagen of the third dentition was also noticed in humans (Ooe, 1969). The teeth and anlagen that appear in third dentition in serial sections of infant jaws and some fetuses have been analysed. The epithelium which is considered as the anlagen of the third dentition develops lingual to all permanent tooth germs (Ooe, 1969). Furthermore, when it appears, the predecessor (permanent tooth germ) is in the bell-shaped stage (Ooe, 1969). The timing of appearance of the third dentition seems to be after birth (Table 1). This means that we have a chance to access the formation of the third dentition in the mouth.
Detailed histological analysis of the tooth replacement in these models indicates that the successional teeth are initiated from the dental lamina epithelium, which grows from the lingual side of the deciduous tooth enamel organ, and it later elongates and buds into the jaw mesenchyme, forming successional teeth. Jarvien et al. showed that, in the ferret, Usag-1(also known as Sostdc1, Ectodin, and Wise) is expressed in the elongating successional dental lamina at the interface between the lamina and deciduous tooth, as well as the buccal side of the dental lamina, suggesting that Sostdc1 plays a role in defining the identity of the dental lamina(Jarvinen et al., 2009). Handrigan et al. analysed successional tooth formation in the snake and in lizard, and proposed that dental epithelium stem cells are responsible for the formation of successional lamina, and Wnt signaling may regulate the dental eithelial stem cell fate in these cells (Handrigan et al., 2010). Maintenance or reactivation of component dental lamina is thus pivotal for the replacement tooth and supernumerary formation.
3. Human syndromes associated with supernumerary teeth
Supernumerary teeth can be associated with a syndrome or they can be found in non-syndromic patients. Only 1% of non-syndromic cases have multiple supernumerary teeth, which occur most frequently in the mandibular premolar area, followed by the molar and anterior regions, respectively (Yusof, 1990; Yague-Garcia et al., 2009). Genetic mutations have been associated with the presence or absence of individual types of teeth.
Supernumerary teeth are associated with 8 syndromes and developmental abnormalities in which the resposible genes already have been isolated (Takahashi et al., 2013). The percentage occurrence in CCD is 22% in the maxillary incisor region and 5% in the molar region (Shafer, 1983). CCD is a dominantly inherited skeletal dysplasia caused by mutations in RUNX2 (Mundlos et al., 1997). There is a wide spectrum of phenotypic variability ranging from the full-blown phenotype to an isolated dental phenotype characterized by supernumerary tooth formation and/or the delayed eruption of permanent teeth in CCD (Takahashi et al., 2008). Runx2-deficient mice were found to exhibit lingual buds in front of the upper molars, and these were much more prominent than in wild-type mice (Aberg et al., 2004). These buds presumably represent the mouse secondary dentition, and it is likely that RUNX2 acts to prevent the formation of these buds. Runx2 regulates the proliferation of cells and may exert specific control on the dental lamina and formation of successive dentitions. Runx2 heterozygous mutant mice mostly phenocopied the skeletal defects of CCD in humans, but with no supernumerary tooth formation (Otto et al., 1997). Notably, in Runx2 homozygous and heterozygous mouse upper molars, a prominent epithelial bud regularly presents. This epithelial bud protrudes lingually with active Shh signaling, and it may represent the extension of the dental lamina for successional tooth formation in mice. Hence, although Runx2 is required for primary tooth development, it prevents the growth of the dental lamina and successional tooth formation (Otto et al., 1997).
Familial adenomatous polyposis (FAP), also named adenomatous polyposis of the colon (APC), is an autosomal dominant hereditary disorder characterized by the development of many precancerous colorectal adenomatous polyps. In addition to colorectal neoplasm, individuals can develop variable extracolonic lesions, including upper gastrointestinal polyposis, osteomas and dental anomalies (Wijn et al., 2007). Dental abnormalities include impacted teeth, congenital absence of one or more teeth, supernumerary teeth and odontomas (Wijn et al., 2007). Gardner syndrome is a variant of FAP characterized by multiple adenomas of the colon and rectum typical of FAP together with osteomas and soft tissue tumors (Chimenos-Kustner et al., 2005). Supernumerary teeth and osteomas were originally described as a part of Gardner syndrome, but they can also occur in FAP patients with or without other extracolonic lesions (Chimenos-Kustner et al., 2005; Wijn et al., 2007). FAP and Gardner syndrome are caused by a large number of germinal mutations in the Apc gene (Groden et al., 1991). Apc is a tumor suppressor gene involved in the down-regulation of free intracellular ß-catenin, the major signal transducer of the canonical Wnt signaling pathway (Groden et al., 1991). Approximately 11-27% of patients have supernumerary teeth, but, so far, no specific codon mutation of the Apc gene has been found to correlate with supernumerary teeth.
The identification of mutations in RUNX2 causing an isolated dental phenotype in CCD and in Apc causing FAP has attracted attention as a possible route towards inducing de novo tooth formation.
4. Supernumerary tooth formation in a mouse model
A number of mouse mutants provide insights into the supernumerary tooth formation (Takahashi et al., 2013). Several mechanisms by which supernumerary tooth might arise in mice have been proposed (Murashima-Suginami et al., 2008; Wang et al., 2009). One plausible explanation for supernumerary tooth formation is the rescue of tooth rudiments such as within the diastema region or maxillary deciduous incisor (Yamamoto et al., 2005; Murashima-Suginami et al., 2007; Lagronova-Churava et al., 2013). During early stages of mouse tooth development transient vestigial tooth buds develop in the diastema area; developing to the bud stage yet later regressing and disappear by apoptosis, or merge with the mesial crown of the adjacent first molar tooth organ (Yamamoto et al., 2005; Lagronova-Churava et al., 2013). The rudimentary maxillary incisor regressed by apoptotic elimination of mesenchymal cells (Murashima-Suginami et al., 2007). We demonstrated that USAG-1-deficient mouse model has supernumerary incisors in the maxillary and mandible, a fused tooth in the maxillary and mandibular molar regions, and a supernumerary tooth was also located in front of the first mandibular molar (Figure 2). Increased BMP signaling results in supernumerary teeth in the Usag-1-deficient mouse model (Murashima-Suginami et al., 2008). Recently, we claimed that gene interactions between BMP-7 and USAG-1 regulate the supernumerary maxillary incisor formation (Kiso et al., 2014). BMP-7 was co-localized with USAG-1 in the area of the maxillary rudiment incisor tooth germ in addition to the regular maxillary incisor tooth organ. USAG-1 abrogation rescued the apoptotic elimination of mesenchymal cells in the rudimentary maxillary incisor tooth primordia at E15, whereas the tooth sizes were comparable (Murashima-Suginami et al., 2007, 2008). The apoptotic mesenchymal cells in USAG-1-/-/BMP-7-/-are similar to USAG-1+/+/BMP-7+/+in contrast to that of USAG-1-/-/BMP-7+/+. These results support our interpretation that USAG-1 functions as a novel BMP-7 antagonist in the maxilla. We confirmed that increased BMP signaling in supernumerary teeth of the USAG-1 deficient mice could be prohibited by BMP-7 abrogation. In the contrast, to test whether BMP-7 has the potential to induce supernumerary tooth formation, we performed explant culture and subsequent subrenal kidney capsule culture. The incisor explants supplemented with BMP-7 in USAG-1+/-as well as USAG-1-/-have supernumerary tooth in similar numbers after 20 days culture, while these cultured explants in USAG-1+/+retained normal tooth number (Figure 2). These results demonstrated that BMP-7 can induce supernumerary tooth formation, however it is impossible to induce extra tooth by only BMP-7 (Kiso et al., 2014). While we showed that enhanced BMP signaling resulted in supernumerary teeth, we also demonstarated that BMP signaling was modulated by Wnt signaling in the Usag-1-deficient mouse model (Figure 3) (Murashima-Suginami et al., 2008). Canonical Wnt/β-catenin signaling and its down-stream molecule Lef-1 are essential for tooth development. Overexpression of Lef-1 under the control of the K14 promoter in transgenic mice leads to the development abnormal invaginations of the dental epithelium in the mesenchyme and formation of a tooth-like structure (Zhou et al., 1995). De novo supernumerary teeth arising directly from the primary tooth germ or dental lamima have been reported in Apc loss-of-function or β-catenin gain-of-function mic. It was demonstrated that mouse tooth buds expressing stabilized β-catenin give rise to extra teeth (Jarvinen et al., 2006). Conditional knockout of the Apc-gene resulted in supernumerary teeth in mice (Wang et al., 2009). Notably, adult oral tissues, especially young adult tissues, are still responsive to the loss of Apc (Wang et al., 2009). In old adult mice, supernumerary teeth can be induced on both labial and lingual sides of the incisors, which contain adult stem cells supporting the continuous growth of mouse incisors (Huysseune et al., 2004). In young mice, supernumerary tooth germs were induced in multiple regions of the jaw in both incisor and molar regions. They can form directly from the oral epithelium, in the dental lamina connecting the developing molar or incisor tooth germ to the oral epithelium, in the crown region, as well as in the elongating and furcation area of the developing root (Wang et al., 2009). Wnt/BMP signaling seems to be essential in supernumerary tooth formation (Figure 3).
We also demonstrated that Cebpb deficiency was related to the formation of supernumerary teeth(Figure 2). A total of 66.7% of Cebpb-/-12-month-olds sustained supernumerary teeth and/or odontomas in the diastema between the incisor and the first molar (Huang et al., 2012). Furthermore, it was suggested that the dental epitheilal stem cells might be contributated to supernumerary tooth formation in mice (Figure 2).
These mouse models clearly demonstrated that it was possible to induce de novo tooth formation by the in situ inhibition or activation of single molecule such as USAG-1, BMP7 or CEBPB.
5. Molecularly targeted therapy
Molecularly targeted therapy is a type of treatment that uses drugs or other substances to identify and attack specific types of cells by interfering with specific targeted molecules.
Most targeted therapies are either small moleclule or monoclonal antibodies. Small molecules are typically able to diffuse into cells and can act on target that are found inside the cells. Monoclonal antibodies usually can not penetorate the surface membrane and are directed against targets that are outside cells or on the surface of cells. Candidates for small molecules are identified in screeing the effect of thousands of test compounds on a specific target. The best candidates are then chemically modified to produce many closely related versions. Monoclonal antibody are prepared first by immunized animals such as mice with purified target moleclules.They are humanized by replacing the animal portion of the antibody with human portion. More than 40 molecularly targeted cancer therapy have been approved by the U.S Food and Drug Administration for the treatment of specific type of cancer. Many more are in clinical trials or preclinical testing (Forscher et al., 2014). Recent molecularly targeted therapy also has successfully been introduced into the treatment of several inflammatory rheumatic diseases such as rheumatoid arthritis (Mocsai et al., 2014).
Molecularly targeted therapy provides a unique tool for the delivery of previously identified signaling molecules in both time and space that may significantly augment our progress toward clinical tooth regeneration. Stimulation of the formation of a third dentition comprises an attractive concept (Figure 4). This approach is generally presented in terms of adding molecules to induce de novo tooth initiation in the mouth. We have a chance to access the formation of the third dentition in the mouth, because the time of appearance of the third dentition seems to be after birth. Advances in our understanding of signal transduction by Wnt/BMP signalling in the supernumerary teeth formation offer numerous opportunities for devising new targeted therapies (Figure 3).This led to a new approach of drug development whereby targeted therapy are developed by directly targeting molecules thought to be involved in the the formation of a third dentition. A mojor approach for the development targeted therapeutics has been the application of monoclonal antibody for targeting molecules such as USAG-1.
Molecularly targeted therapy seems to be a suitable approach in tooth regeneration by stimulation of the third dentition.
Figure 1.
Multiple impacted supernumerary teeth (the third dentition) in a 13-year-old non-syndromic patient.
The third dentition develops lingual to the permanent tooth germ (D). All impacted supernumerary teeth in this patient are located to the lingual side of the permanent teeth (white arrow) (A-C). These multiple supernumerary teeth seem to be post-permanent dentition (“third dentition”). (Takahahsi et al., 2013, copy right, In Tech)
\n\t\t
\n\t\t
\n\t\t\t
\n\t\t\t\t\n\t\t\t
\n\t\t
\n\t
Table 1.
Timing of appearance of the third dentition (Takahahsi et al., 2013, copy right, In Tech)
Figure 2.
Supernumerary teeth formation in mouse model
Usag-1 deficient mice (A-C) A: Oblique view of the maxillary incisors. B: Occlusal view of the mandibular incisors. C: Occlusal view of the mandibular molars. Micro-CT images of Cebpb dificient mice (D-F) A frontal view (D), a sagittal view (E) and a horizontal view (F) BMP-7 has potential to partially induce the formation of maxillary supernumerary incisors formation in vitro. The incisor explants supplemented with (H)/without (G) BMP-7 in USAG-1+/− (G, H) sagittal sections of explant. (I) Sox2 positive detal epithelial stem cells in sagittal sections of the rudimentary maxillary incisor tooth primordia at E15.
Figure 3.
Wnt/BMP signaling in supernumerary tooth formation.
Underlined molecules are responsible genes for human syndromes or mutant mouse associated with supernumerary teeth
Figure 4.
Molecularly targeted therapy for the tooth regeneration by stimulation of a third dentition
6. Conclusion
We have a chance to access the formation of the third dentition in the mouth, because the timing of the appearance of the third dentition seems to be after birth. The identification of mutations in RUNX2 causing an isolated dental phenotype in CCD and supernumerary tooth formation in the mouse model clearly demonstrated that it was possible to induce de novo tooth formation by the in situ inhibition or activation of a single candidate molecule. These results support the idea that the de novo inhbition or activation of candidate molecules such as RUNX2 or USAG-1 might be used to stimulate the third dentition in order to induce new tooth formation in the mouse (Figure 4). Molecularly targeted therapy seems to be a suitable approach in tooth regeneration by stimulation of the third dentition.
Acknowledgments
This work was supported by Grant-in-Aid for Scientific Research(C):22592213 and 25463081 and A-STEP (Adaptable & Seamless Technology Transfer Program through Target-driven R&D) FS stage: AS231Z01061G and AS242Z02645Q.
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Introduction",level:"1"},{id:"sec_2",title:"2. The third dentition",level:"1"},{id:"sec_3",title:"3. Human syndromes associated with supernumerary teeth",level:"1"},{id:"sec_4",title:"4. Supernumerary tooth formation in a mouse model",level:"1"},{id:"sec_5",title:"5. Molecularly targeted therapy",level:"1"},{id:"sec_6",title:"6. Conclusion",level:"1"},{id:"sec_7",title:"Acknowledgments",level:"1"}],chapterReferences:[{id:"B1",body:'AbergTCavenderAGaikwadJ. SBronckersA. LWangXWaltimo-sirénJThesleffIDSouzaRN. Phenotypic changes in dentition of Runx2 homozygote-null mutant mice. J Histochem Cytochem 2004521131139Aberg T, Cavender A, Gaikwad JS, Bronckers AL, Wang X, Waltimo-Sirén J, Thesleff I, D\'Souza RN. Phenotypic changes in dentition of Runx2 homozygote-null mutant mice. 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Proc Natl Acad Sci U S A 2006103491862718632Järvinen E, Salazar-Ciudad I, Birchmeier W, Taketo MM, Jernvall J, Thesleff I. Continuous tooth generation in mouse is induced by activated epithelial Wnt/beta-catenin signaling. Proc Natl Acad Sci U S A 2006;103(49):18627-18632.'},{id:"B10",body:'JärvinenETummersMThesleffIThe role of the dental lamina in mammalian tooth replacement. J Exp Zool B Mol Dev Evol 2009B(4):281-291.Järvinen E, Tummers M, Thesleff I. The role of the dental lamina in mammalian tooth replacement. J Exp Zool B Mol Dev Evol 2009 ;312B(4):281-291.'},{id:"B11",body:'KisoHTakahashiKSaitoKTogoYTsukamotoHHuangBSugaiMShimizuATabataYEconomidesA. NSlavkinH. CBesshoKInteractions between BMP-7 and USAG-1 (uterine sensitization-associated gene-1) regulate supernumerary organ formations. PLoS ONE. 20149, e96938, 2014Kiso, H., Takahashi, K., Saito, K., Togo, Y., Tsukamoto, H., Huang, B., Sugai, M., Shimizu, A., Tabata, Y., Economides, AN., Slavkin, HC., Bessho, K. Interactions between BMP-7 and USAG-1 (uterine sensitization-associated gene-1) regulate supernumerary organ formations. PLoS ONE. 2014, 9, e96938, 2014'},{id:"B12",body:'KratochwilKDullMFarinasIGalceranJGrosschedlRLef1 expression is activated by BMP-4 and regulates inductive tissue interactions in tooth and hair development. Genes Dev 1996101113821394Kratochwil K, Dull M, Farinas I, Galceran J, Grosschedl R. Lef1 expression is activated by BMP-4 and regulates inductive tissue interactions in tooth and hair development. Genes Dev 1996;10(11):1382-1394.'},{id:"B13",body:'LecheWStudien uber die Entwicklung des Zahnsstemsbei den Saugetieren. Morph Jb 189319502574Leche W. Studien uber die Entwicklung des Zahnsstemsbei den Saugetieren. Morph Jb 1893;19: 502-574.'},{id:"B14",body:'MócsaiAKovácsLGergelyPWhat is the future of targeted therapy in rheumatology: biologics or small molecules? BMC Med. 2014Mócsai A, Kovács L, Gergely P. What is the future of targeted therapy in rheumatology: biologics or small molecules? BMC Med. 2014;12:43.'},{id:"B15",body:'MundlosSOttoFMundlosCMullikenJ. BAylsworthA. SAlbrightSLindhoutDColeW. GHennWKnollJ. HOwenM. JMertelsmannRZabelB. UOlsenB. RMutations involving the transcription factor CBFA1 cause cleidocranial dysplasia. Cell 1997895773779Mundlos S, Otto F, Mundlos C, Mulliken JB, Aylsworth AS, Albright S, Lindhout D, Cole WG, Henn W, Knoll JH, Owen MJ, Mertelsmann R, Zabel BU, Olsen BR. Mutations involving the transcription factor CBFA1 cause cleidocranial dysplasia. Cell 1997; 89(5): 773-779.'},{id:"B16",body:'Murashima-suginamiATakahashiKKawabataTSakataTTsukamotoHSugaiMYanagitaMShimizuASakuraiTSlavkinH. CBesshoKRudiment incisors survive and erupt as supernumerary teeth as a result of USAG-1 abrogation. Biochem. Biophys. Res. Commun 20073593549555Murashima-Suginami A, Takahashi K, Kawabata T, Sakata T, Tsukamoto H, Sugai M, Yanagita M, Shimizu A, Sakurai T, Slavkin HC, Bessho K. Rudiment incisors survive and erupt as supernumerary teeth as a result of USAG-1 abrogation. Biochem. Biophys. Res. Commun 2007;359(3):549-555.'},{id:"B17",body:'Murashima-suginamiATakahashiKSakataTTsukamotoHSugaiMYanagitaMShimizuASakuraiTSlavkinH. CBesshoKEnhanced BMP signaling results in supernumerary tooth formation in USAG-1 deficient mouse. Biochem Biophys Res Commun 2008369410121016Murashima-Suginami A, Takahashi K, Sakata T, Tsukamoto H, Sugai M, Yanagita M, Shimizu A, Sakurai T, Slavkin HC, Bessho K. Enhanced BMP signaling results in supernumerary tooth formation in USAG-1 deficient mouse. Biochem Biophys Res Commun 2008;369(4):1012-1016.'},{id:"B18",body:'OoëTEpithelial anlagen of human third dentition and their migrations in the mandible and maxilla. Okajimas Fol Anat Jap 1969465243251Ooë T. Epithelial anlagen of human third dentition and their migrations in the mandible and maxilla. Okajimas Fol Anat Jap 1969; 46(5):243-251.'},{id:"B19",body:'OttoFThornellA. PCromptonTDenzelAGilmourK. CRosewellI. RStampG. WBeddingtonR. SMundlosSOlsenB. RSelbyP. BOwenM. JCbfa1, a candidate gene for cleidocranial dysplasia syndrome, is essential for osteoblast differentiation and bone development. Cell 1997895765771Otto F, Thornell AP, Crompton T, Denzel A, Gilmour KC, Rosewell IR, Stamp GW, Beddington RS, Mundlos S, Olsen BR, Selby PB, Owen MJ. Cbfa1, a candidate gene for cleidocranial dysplasia syndrome, is essential for osteoblast differentiation and bone development. Cell 1997;89(5):765-771.'},{id:"B20",body:'ShaferW. GHineM. Kand LeviB. MTextbook of oral pathology 4th Ed. Philadelphia:WB Saunders Co;1983Shafer, W. G., Hine, M. K., and Levi, B. M. Textbook of oral pathology 4th Ed. Philadelphia:WB Saunders Co;1983.'},{id:"B21",body:'TakahashiKSakataTMurashima-suginamiATsukamotoHKisoHand BesshoKTooth regeneration: Potential for stimulation of the formation of a third dentition by one gene. Current Topics in Genetics 200837782Takahashi, K., Sakata, T., Murashima-Suginami, A., Tsukamoto, H., Kiso, H. and Bessho, K. Tooth regeneration: Potential for stimulation of the formation of a third dentition by one gene. Current Topics in Genetics 2008;3: 77-82.'},{id:"B22",body:'TakahashiKKisoHSaitoKTogoYTsukamotoHHuangBand BesshoK2013Feasibility of gene therapy for tooth regeneration by stimulation of a third dentition: Gene Therapy-Tools and Potential Applications, In Tech, Rijeka, Croatia, 30727744Takahashi, K., Kiso, H., Saito, K., Togo, Y., Tsukamoto, H., Huang, B. and Bessho, K. (2013) Feasibility of gene therapy for tooth regeneration by stimulation of a third dentition: Gene Therapy-Tools and Potential Applications, In Tech, Rijeka, Croatia, 30, 727-744'},{id:"B23",body:'ThesleffIThe genetic basis of tooth development and dental defects. Am J Med Genet A 20061402325302535Thesleff I. The genetic basis of tooth development and dental defects. Am J Med Genet A 2006;140(23):2530-2535.'},{id:"B24",body:'WangX. POConnellD. JLundJ. JSaadiIKuraguchiMTurbe-doanACavallescoRKimHParkP. JHaradaHKucherlapatiRMaasRL. Apc inhibition of Wnt signaling regulates supernumerary tooth formation during embryogenesis and throughout adulthood. Development 20091361119391949Wang XP, O\'Connell DJ, Lund JJ, Saadi I, Kuraguchi M, Turbe-Doan A, Cavallesco R, Kim H, Park PJ, Harada H, Kucherlapati R, Maas RL. Apc inhibition of Wnt signaling regulates supernumerary tooth formation during embryogenesis and throughout adulthood. Development 2009;136(11):1939-1949.'},{id:"B25",body:'WijnM. AKellerJ. JGiardielloF. MBrandH. SOral and maxillofacial manifestations of familial adenomatous polyposis. Oral Dis 2007134360365Wijn MA, Keller JJ, Giardiello FM, Brand HS. Oral and maxillofacial manifestations of familial adenomatous polyposis. Oral Dis 2007;13(4):360-365.'},{id:"B26",body:'Yagüe-garcíaJBerini-aytésLGay-escodaCMultiple supernumerary teeth not associated with complex syndromes: a retrospective study. Med Oral Patol Oral Cir Bucal 2009E331336Yagüe-García J, Berini-Aytés L, Gay-Escoda C. Multiple supernumerary teeth not associated with complex syndromes: a retrospective study. Med Oral Patol Oral Cir Bucal 2009;14(7):E331-336'},{id:"B27",body:'YamamotoHChoS. WSongS. JHwangH. JLeeM. Jet al2005Characteristic tissue interaction of the diastema region in mice. Archives of oral biology 50189198Yamamoto H, Cho SW, Song SJ, Hwang HJ, Lee MJ, et al. (2005) Characteristic tissue interaction of the diastema region in mice. Archives of oral biology 50: 189-198.'},{id:"B28",body:'YoungC. SAbukawaHAsricanRRavensMTroulisM. JKabanL. BVacantiJ. PYelickP. CTissue-engineered hybrid tooth and bone. Tissue Eng 2005Young CS, Abukawa H, Asrican R, Ravens M, Troulis MJ, Kaban LB, Vacanti JP, Yelick PC. Tissue-engineered hybrid tooth and bone. Tissue Eng 2005;11(9-10):1599-1610.'},{id:"B29",body:'YusofW. ZNon-syndrome multiple supernumerary teeth: literature review. J Can Dent Assoc 1990562147149Yusof WZ. Non-syndrome multiple supernumerary teeth: literature review. J Can Dent Assoc 1990;56(2):147-149.'},{id:"B30",body:'ZhouPByrneCJacobsJFuchsELymphoid enhancer factor 1 directs hair follicle patterning and epithelial cell fate. Genes Dev199596700713Zhou P, Byrne C, Jacobs J, Fuchs E. Lymphoid enhancer factor 1 directs hair follicle patterning and epithelial cell fate. Genes Dev1995;9(6):700-713.'}],footnotes:[],contributors:[{corresp:null,contributorFullName:"Katsu Takahashi",address:null,affiliation:'
Department of Oral and Maxillofacial Surgery, Graduate School of Medicine, Kyoto University, Japan
Quantitative risk assessment of natural hazards serves nowadays as the basis for a targeted risk management, respectively allows a risk-based classification and communication of the considered hazardous event in society [1, 2] (see also chapter [3] of this book). One of the most important and pervasive problems in this context concerns the investigation of time-scale properties and complex relationships between process activity, social development (exposure, protective measures, land use, etc.) and climate change. The correct understanding of the correlation structures governing observational time series might provide useful information on the dynamical features of natural hazard processes and on the dynamical mechanisms involved [4].
Steep headwater catchments typically provide the setting for such natural hazardous events because they are, besides being a drainage area for precipitation (see chapter [5] of this book), also sediment source zones of river systems, delivering significant volumes of sediment to the valley floor in highly dissected and coupled landscapes. As stated by [6], headwater catchments differ from down-stream reaches by their close coupling to hillslope processes, more temporal and spatial variation, and their need for different means of protection from land use. Especially processes, which are capable to relocate a considerable quantity of sediments, like bedload transport processes, debris floods or debris flows, often have tragic consequences on human settlements and infrastructures. Thus, for such hydrogeomorphic hazards the probability of occurrence and magnitude is beside the occurrence of critical rainfall events essentially a function of runoff and erosion which is, however, directly coupled to the protective effects of forested landscapes. In connection with frequently occurring natural hazard processes, protective forests, even if they currently only fulfill indirect protective effects, represent an essential factor in the risk reduction of natural hazard processes over long periods of time – on large potential natural hazard disposition areas. Today, about 30% of the forest area in Austria is assigned a protective function to avoid serious natural hazards, and according to the interim evaluation of the Austrian Forest Inventory, this share is increasing [7]. However, the same inventory data show that only half of such classified protective forests have a stable structure. The reasons for this are a significant aging of the Austrian protective forest stands due to a lack of natural regeneration and a lack of resistance to natural disturbances. This concerns climate-related forest disturbances such as forest fires, wind, and insect outbreaks, which will likely increase in the coming decades. Here, climate change can alter the frequency, intensity, duration and timing of such natural disturbances [8, 9]. Based on data of more than 10,000 torrent catchment areas in Austria [10], showed that natural disturbances increased the probability of torrential events in the last 32 years. With the expected increase of the global average surface temperature of 3–5°C by 2100, compared to the first decade of the 20th century, the spatial and temporal impact of climate change on forests represents an additional threat to the desired protective forest structures and thus to natural hazard management.
The aim of this research was to investigate the effects of climate-induced natural disturbance regimes (bark beetle or storm damage) on hydrogeological processes in forested alpine torrent catchments. Combining methods from forestry, hydrology and geotechnical engineering, an integral approach was chosen to analyze possible effects of natural disturbances on hydrogeomorphic hazards in the perspective of future protective forest developments. This work was carried out in the course of the project “PROTECTED” funded by the Austrian Climate Research Program. The chapter presents hydrological findings as well as a brief summary of geotechnical findings as described in [11].
2. Runoff and landslide simulations in forested headwater catchments affected by canopy disturbances
To analyze the impact of future change, an ensemble of forest landscape simulations has been conducted in two steep headwater catchments located in the Stubai valley, Tyrol, Austria. With the “Innerer Lehnertalbach” (IL) and the “Äußere Lehnertalbach” (AL) two typical torrential catchments with high relief energy (Melton ratio for IL = 1.3; Melton ratio for AL = 1.2, cf. [12]) have been chosen. Both catchments are situated in ecoregion 1.2 (Subkontinentale Innenalpen-West), dominated by metamorphic lithologies (mainly Gneiss). They are a typical example of mountain forest ecosystems of the central Alps, dominated by Norway spruce (Picea abies (L.) Karst.), European larch (Larix decidua L.) and Swiss stone pine (Pinus cembra L.). An overview of the catchment area characteristics is shown in Table 1.
Parameters
“Innerer Lehnertalbach”
“Äußerer Lehnertalbach”
Area [km2]
4.8
1.3
Min. elevation [m a.s.l]
1,043
1,037
Max. elevation [m a.s.l]
2,094
2,480
Mean slope gradient [°]
34
36
Forest cover [%]
83
36
Table 1.
Catchment area characteristics of the “Innere-” and “Äußere Lehnertalbach”.
Duration [min]
Precipitation intensities [mm/h]
“Innerer Lehnertalbach”
“Äußerer Lehnertalbach”
60
88.85
94.65
240
130.10
138.39
720
178.56
180.26
Table 2.
eHYD design precipitation values based on a 100-year recurrence interval for the selected catchments.
2.1 Climate and precipitation scenarios
In order to cover the widest possible range of future climate scenarios, four different climate forecasts have been selected, based on three global models from the Irish Center for High-End Computing (ichec), the Pierre Simon Laplace Institute (ipsl) and the MetOffice Hadley Center (mohc). All three global models (ichec, ipsl, mohc) have been operated with the RCP 8.5 scenario – assuming a very high gain of energy (8.5 W/m2) caused by future climate change. The global model ichec, however, was additionally operated with a moderate, RCP 4.5, climate perspective (4.5 W/m2). The temperature and precipitation differences of the Eur-11 dataset for the period 2071–2100 compared to 1981–2010 are shown in Figure 1. All mean air temperatures increase in comparison to 1981–2010. Of the climate predictions used, only mohc8.5 shows negative precipitation trends. In addition to the climate forecast scenarios, forest landscape simulations are further driven by assuming no climate change and a future climate development aligned with historic climate data. This climate scenario is denoted as historic and results for the period from 1961 to 2015 from combined 1x1 km INCA and SPARTACUS, grid data of the Central Institute for Meteorology and Geodynamics (ZAMG) and observation series of ZAMG weather stations, as well as locally installed monitoring stations.
Figure 1.
Used climate forecasts based on the EUR-11 dataset as average temperature and precipitation difference of the period 2071–2100 compared to 1981–2010 (summer).
For each of the climate forecast scenarios, forest landscape development was simulated for 200 years with the individual-based forest landscape and disturbance model (iLand) [13]. Disturbance events have been stochastically considered based on 20 replicates, while we considered the non-disturbance landscape to be based on one replicate. Further, all iLand simulations were additionally conducted with and without considering forest management activities. Thus, in total 210 landscape simulations have been performed.
Three precipitation events of varying duration (60 min, 240 min and 720 min) with a recurrence interval of 100 years have been defined, covering a wide range of information about the hydrological response of disturbances in forests. The design precipitation events result from the area-averaged, maximized precipitation (MaxModN, eHYD) of grid points close to the selected torrential catchments. Design precipitation probabilities of MaxMod are based on a simulation model calibrated with measured data and accounting for the topography. MaxModN gives precipitation values that are usually higher than those observed (Table 2).
2.2 Runoff simulations
The runoff simulations in the study area were performed with two, conceptually different, hydrological modeling approaches.
For the selected torrential catchments, like for nearly 96% of all torrential catchments in Austria, no information about past rainfall-runoff events exists. This is mainly because of the lack of continuous discharge measurements devices (water gauges). For this reason, runoff simulations have been performed with the precipitation/runoff (P/R) model ZEMOKOST [14] – an easy to apply event-based concept-model, specially developed for the application in small to medium-sized (< 100 km2) ungauged torrential catchments. The semi distributed model is based on a two-layer concept with a surface and a subsurface runoff module. ZEMOKOST needs the portions of surface runoff classes (RCconst) and surface roughness (c) classes for each sub-catchment (see chapter [5] of this book). The main parameters, runoff coefficient (RCconst) and surface roughness (c), have been investigated, following the code of practice developed by [15]. Actual site characteristics (vegetation, soil) were mapped in the field to ensure realistic assessment of runoff characteristics. In this context, vegetation in ZEMOKOST is primarily considered on the basis of its hydrologic vegetation characteristics, i.e., forest vegetation and dwarf shrub cover versus woody free vegetation. ZEMOKOST was then calibrated and checked for plausibility for the test-catchments using the existing precipitation and discharge time series and data from historic events.
Runoff simulations have additionally been carried out with the physically based, grid-distributed hydrological program GEOtop 2.1. Such models account beside surface flow also for subsurface (or inter) flow and groundwater related effects, important phenomena when simulating soil erosion activity. In GEOtop, land use is made up of vegetation classes consisting of a non-arable and differently forested groups. The individual groups do not represent any particular tree species, but result from units of similar vegetation height, leaf area, canopy coverage and root depth, directly determined by iLand simulations. Surface runoff in the channel and along the hillslopes are determined by Manning’s empirical hydraulic approach. Since the runoff regime in forests is determined primarily by forest soil conditions, the interaction with the lithosphere is of high importance, described by soil physical parameters. In addition to the topographical data, pedological data add differences in depth, so-called horizons. Each type of soil consists of different soil horizons. Each soil horizon is characterized by its physical properties (soil texture data). The storage and conductivity of the individual horizons is given by the water content at wilting point, field capacity and saturation, as well as the conductivity at saturation and determined by means of pedotransfer functions proposed by [16] on their sand and clay content. The conductivity in the unsaturated soil matrix is calculated by van Genuchten values (α, n). Those values can be determined according to [17] by classifying the soil texture according to United States Department of Agriculture (USDA).
Finally, GEOtop runoff results have been validated with the runoff results proposed by ZEMOKOST, where it has been found that the drainage roughness has a significant impact. Figure 2 shows a calibration example of the “Äußere Lehnertalbach” for GEOtop simulations based on a sensitivity analyses of varying hydraulic roughness parameters (40 simulations), compared to ZEMOKOST simulations for a 100-year precipitation event of the duration levels 60, 240 and 720 min. The solid line corresponds to the calibrated GEOtop simulation.
Figure 2.
Validation of GEOtop based on ZEMOKOST simulations for a 100-year precipitation event of the duration levels 60, 240 and 720 min at the “Äußere Lehnertalbach”. While the shaded area contains all simulated hydrographs, the solid line represents the hydrograph of the calibrated model.
For future runoff predictions of peak discharges, simulated with both hydrological models, varying land use conditions were provided by the pre-conducted number of iLand simulations of the selected catchments – resulting in multiple runoff simulation scenarios.
For future ZEMOKOST simulations the parameters RCconst and c are calculated from iLand outputs. In order to derive RCconst, pedohydrological reaction units were mapped in the field. Six different units have been characterized. Considering the iLand outputs canopy cover, ground cover and soil water content, RCconst is given as an output for the different reaction units. Each c value is assigned a range of iLand output values per parameter on basis of [15]. For an iLand output parameter set the best fit c value is selected.
GEOtop simulations have been based on the biosphere mapped via land use parameters. The land use is formed by vegetation classes, consisting of non-vegetated and differently forested groups. The individual groups do not represent a specific tree species, but result from units of similar vegetation height, soil roughness, leaf area, canopy cover and root depth, which were determined via iLand.
2.3 Slope stability simulations
Simulations of the effect of forest disturbances on hillslope erosion processes are based on the results from the distributed runoff simulations of GEOtop in combination with an extended version of the Mohr-Coulomb soil stability model. The stability of each soil column – 1 m in depth with an area of 100 m2 – i.e. each cell in the study area, was subsequently estimated for each layer l for simulation i at time t according to Eq. (1).
FSilt=B+A−∑k=1lhk∗mikt∗tanϕltanβAE1
where FSilt is the factor of safety for a specific soil column in the study area under simulation i for its layer l, with values below 1 indicating that the soil column is instable at the depth of layer l and time t. ℎ(k) is the depth of layer k, mikt the saturation of layer k at time t, as given by Eq. (3), ϕ(l) is the internal angle of friction of layer l in rad and β is the slope angle of the soil column in rad. In Eq. (1), A equals to the normal stress resulting from the soil and plant weight reduced by the pore water pressure and was derived by means of Eq. (2).
A=γw−1∗qi+∑k=1lhk∗mikt∗γsatk−γk+γkE2
where γw is the specific weight of water in kNm−3, qi is the additional pressure due to the weight of the vegetation in Pa, hk is the depth of layer k in m, mikt is the saturation of layer k for simulation i given by Eq. (3):
mikt=θiktθsatkE3
where θikt is the soil water content of layer k at the time t for simulation i and θk is the saturated water content of layer k, γsatk is the specific weight of the saturated soil of layer k in kNm−3, γk and is the specific weight of the dry soil of layer k in kNm−3.
The cohesion component of the resisting forces was estimated according to Eq. (4).
B=2∗Csl+Cr,ilγwsin2βE4
where Csl is the soil cohesion of layer l in Pa, Cr,il is the root cohesion of layer l for simulation i in Pa, γw is the specific weight of water in kNm−3 and β is the slope angle of the soil column in rad.
A detailed description of the geotechnical parameterization as well as the parametrization of root cohesion and vegetation weight can be found in [11].
3. Future possible tendencies of canopy disturbances show no significant influence on runoff after heavy rainfall events
The variability of the peak discharge, resulting from the presence of natural disturbances within the forested area, is given by the relative peak discharge change ΔQjtd for each climate scenario j, with specific precipitation duration d and time frame t. Accounting for disturbance effects per applied climate scenario, ΔQj,itd is estimated based on the ratio between the peak discharge of the i-th replicant of the climate change scenario j considering disturbance effects Qj,i1td, with the peak discharge of the climate change scenario j without considering disturbance effects Qj0td, for each precipitation duration and time slice.
∆Qj,itd=Qj,i1tdQj0tdE5
From the 20 relative peak discharge change observations per climate scenarios, precipitation duration and time slices, the median ΔQ∼jtd is derived, and the 95% confidence interval is estimated based on 2,500 bootstrap samples. To account for epistemic uncertainty, ∆Qj,itd values are based on the pooled model results (ZEMOKOST and GEOtop).
Figure 3 shows the relative peak discharge change for 50, 100, 150 and 200 years after simulation begin – stratified by the selected torrential catchments, historical based –, wettest (ipsl85) –, and driest (mohc85) climate scenarios as well as management and no management.
Figure 3.
In each figure, the upper panel shows the change in peak discharge relative to the peak discharge without disturbances stratified by management and no management for 50, 100, 150 and 200 years after simulation begin. All discharge values are based on the pooled model results (ZEMOKOST and GEOtop). The symbol is located at the median, while the lower and upper end of the bar represent the 25. And 75. Percentile estimated from 20 repetitions. The lower panel shows the disturbed area relative to the total area occupied by forest for each year.
The results (Figure 3) do not permit any significant influence of natural disturbances on the runoff behavior in torrent catchment areas. Neither could a significant change in soil water content be observed for any of the future climate scenarios and disturbance induced simulated landscapes (c.f. Figure 4). However, positive trends describing an increase in runoff due to an increase in the disturbed forest area cannot be completely ruled out visually, i.e.: times with a high number of disturbances (supposing a critical size of disturbed area) apparently also cause an increase in runoff behavior during heavy precipitation events.
Figure 4.
The influence on climate change scenarios on modeled slope stability criteria and the corresponding mobilized volume. Canopy disturbances influence the development of tree species and thus the existing apparent cohesion through the root system.
4. Climate change and climate-driven development of canopy disturbances are directly related to the disposition of landslides
The results given refer to the mobilized volume, which is calculated for each cell and all climate scenarios individually as the cell-area times the unstable soil depth. The latter is defined as the height from the surface, of the considered cell, to the first soil layer whose factor of safety (FSi,eq.1) is simulated below one. A detailed presentation and discussion of all results can be found in [11]. However, this chapter provides a brief summary of the main findings that summarize the influence of natural disturbances on slope stability criteria (amount of mobilized volume) by i) the influence of soil water content, ii) the influence of root cohesion, iii) the influence of rooting depth, and iv) the change in tree species (Figure 4). While under historical conditions the mobilized volume is constant over time, the mobilized volume increases for the moderate (ihec4.5) and warm (ihec8.5) to the warm and wet (ispl8.5) climate scenarios (Figure 4). A considerable decrease of the mobilized volume was, however, found for the warm and dry climate scenario (mohc8.5). Beside these trends the mobilized volume is for all climate scenarios and time periods constantly less for forest stands influenced by canopy disturbances. These conclusions are also preserved if the duration is changed from 240 minutes to 60 or 720 minutes, with the only difference that for the 60-minute scenario less volume and for the 720-minute scenario more volume is mobilized compared to the 240-minute scenario.
The lower landslide disposition for the warm and dry climate scenario (mohc8.5) may initially be contra-intuitive but can be explained by a closer look at the structural change of the forest stands. Regardless of the climate scenario or the time period, the share of heart and taproot systems is higher for forest stands with natural disturbances. While for the climate scenarios ihec4.5, ihec8.5 and ispl8.5 the share of trees with sinker root system increases over time, the share of trees with sinker root system decreases in the mohc8.5 scenario. This leads to an increase in slope stability due to a higher rooting depth and increased root cohesion. The results suggest that on steep slopes, stability due to disturbances can occur through a more rapid change in natural succession – especially when a change in climate leads to a change in tree species with a higher root cohesion capacity.
5. Conclusion
Forest disturbances which have a possible influence on natural hazard processes are understood to refer primarily to large-scale disturbances, i.e. disturbances which cause large-scale deforestation. After such large-scale disturbances, technical protection structures are very often installed as immediate measures to compensate for the loss of forest’s protective effects. Frequently recurring disturbances are often much smaller in relation to “catastrophic” large-scale disturbances and thus less in the awareness of natural hazard experts, but very much in the attention of forest experts. The canopy disturbance intensities modeled in this study affected less than 20% of the forested area of the considered catchments – somehow a critical size of disturbances regarding change in runoff regimes [18, 19, 20]. Although the runoff simulations do not permit clear quantifiable statements, it must be noted that such critical size of the natural disturbance is more likely to be reached in steep and small torrent basins especially in causing a change in runoff behavior. However, future research questions will most certainly address quantifying the size of a critical disturbance area, i.e., determining the area above which a significant impact on the hydrologic regime in steep torrent catchments would be evident. The influence of critical disturbances on slope stability showed, in a first moment, contra intuitive results, especially for the smallest and most densely forested investigation area. Here we have noticed an increase in slope stability with an increase in the disturbed area, significantly for the climate scenario with high temperatures in combination with lower precipitation (mohc 8.5). As trees exert a kind of cohesion on the soil layer due to their roots, the formation of the root system plays an important role regarding slope stability. However, the shape of the root system depends mainly on the tree species and the age. Both are subject to significant changes due to the influence of climate and the occurrence of natural disturbances and thus influence stability on steep forested slopes. In the Alpine region, the treatment of protective forests faces more than ever the challenges of sustainable and proactive management. While it is still too early to define general management strategies to maintain or improve the protective effect of forests in relation to runoff formation in the context of disturbances, it can be stated that scenarios of future climate projections suggest the targeted promotion of tree species with deep-root or heart-root systems as necessary, especially on landslide-prone sites.
Acknowledgments
The study was funded by the Austrian Climate Research Program PROTECTED (KR16AC0K13167). R.S. and W.R. further acknowledge support through the Austrian Science Fund (FWF) through START grant Y895-B25. We thank K. Albrich for help with data preparation for the simulations with iLand.
Conflict of interest
The authors declare no conflict of interest.
\n',keywords:"canopy disturbance, runoff, hillslope stability, torrential catchment, protective forest",chapterPDFUrl:"https://cdn.intechopen.com/pdfs/78126.pdf",chapterXML:"https://mts.intechopen.com/source/xml/78126.xml",downloadPdfUrl:"/chapter/pdf-download/78126",previewPdfUrl:"/chapter/pdf-preview/78126",totalDownloads:140,totalViews:0,totalCrossrefCites:0,dateSubmitted:"July 16th 2021",dateReviewed:"July 22nd 2021",datePrePublished:"August 23rd 2021",datePublished:null,dateFinished:"August 17th 2021",readingETA:"0",abstract:"As protective forests have a major control function on runoff and erosion, they directly affect the risk from hydrogeomorphic processes such as sediment transport processes or debris flows. In this context, future scenarios of climate-related canopy disturbances and their influence on the protective effect remain, however, an unsolved problem. With the individual-based forest landscape and disturbance model iLand, an ensemble of forest landscape simulations was carried out and the effects of future changes in natural disturbance regimes were evaluated. To determine peak runoff, hydrological simulations have been conducted, using the conceptual hydrological model ZEMOKOST as well as the deterministic model GEOtop. Effects of forest disturbances on hillslope stability were investigated, based on a modified Coulomb landslide model. Our results suggest no influence of the disturbance regime on the runoff. The climate-related increase in the frequency of disturbances is not reflected in increased runoff during the period under consideration. Contrary, slope stability analyses indicate that the availability of shallow landslides in steep forested torrent catchments might be decreased by the occurrence of disturbances – especially for a warm and dry climate projection. Canopy disturbances seem to accelerate the adaptation of tree species to future climate conditions, which is likely to be accompanied by a change in root systems away from flat roots that currently predominate in torrential catchments. In terms of managing the protective effect of forests against shallow landslides, such natural disturbances can thus be considered as positive interventions in the existing forest ecosystem by promoting natural succession.",reviewType:"peer-reviewed",bibtexUrl:"/chapter/bibtex/78126",risUrl:"/chapter/ris/78126",signatures:"Christian Scheidl, Micha Heiser, Sebastian Kamper, Thomas Thaler, Werner Rammer, Rupert Seidl, Klaus Klebinder, Veronika Lechner, Fabian Nagl, Bernhard Kohl and Gerhard Markart",book:{id:"10812",type:"book",title:"Protective forests as Ecosystem-based solution for Disaster Risk Reduction (ECO-DRR)",subtitle:null,fullTitle:"Protective forests as Ecosystem-based solution for Disaster Risk Reduction (ECO-DRR)",slug:null,publishedDate:null,bookSignature:"Dr. Michaela Teich, Dr. Cristian Accastello, Dr. Frank Perzl and Dr. Karl Kleemayr",coverURL:"//cdnintech.com/web/frontend/www/assets/cover.jpg",licenceType:"CC BY-NC 4.0",editedByType:null,isbn:"978-1-83969-326-7",printIsbn:"978-1-83969-325-0",pdfIsbn:"978-1-83969-327-4",isAvailableForWebshopOrdering:!0,editors:[{id:"428790",title:"Dr.",name:"Michaela",middleName:null,surname:"Teich",slug:"michaela-teich",fullName:"Michaela Teich"}],productType:{id:"3",title:"Monograph",chapterContentType:"chapter",authoredCaption:"Authored by"}},authors:null,sections:[{id:"sec_1",title:"1. Introduction",level:"1"},{id:"sec_2",title:"2. Runoff and landslide simulations in forested headwater catchments affected by canopy disturbances",level:"1"},{id:"sec_2_2",title:"2.1 Climate and precipitation scenarios",level:"2"},{id:"sec_3_2",title:"2.2 Runoff simulations",level:"2"},{id:"sec_4_2",title:"2.3 Slope stability simulations",level:"2"},{id:"sec_6",title:"3. Future possible tendencies of canopy disturbances show no significant influence on runoff after heavy rainfall events",level:"1"},{id:"sec_7",title:"4. Climate change and climate-driven development of canopy disturbances are directly related to the disposition of landslides",level:"1"},{id:"sec_8",title:"5. Conclusion",level:"1"},{id:"sec_9",title:"Acknowledgments",level:"1"},{id:"sec_12",title:"Conflict of interest",level:"1"}],chapterReferences:[{id:"B1",body:'Fuchs S, Keiler M, Zischg A. A spatiotemporal multi-hazard exposure assessment based on property data. 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Das Niederschlags−/Abflussmodell ZEMOKOST: Entwicklung eines praktikablen Modells zur Ermittlung von Hochwasserabflüssen in Wildbacheinzugsgebieten unter Einbeziehung verbesserter Felddaten [PhD Thesis]. na; 2011'},{id:"B15",body:'Markart G, Kohl B, Sotier B, Klebinder K, Schauer T, Bunza G, et al. A Simple Code of Practice for the Assessment of Surface Runoff Coefficients for Alpine Soil-/Vegetation Units in Torrential Rain (Version 2.0). Natural Hazards and Landscaper (BFW), Innsbruck [Internet]. 2011 [cited 2017 May 10]; Available from: https://www.researchgate.net/profile/Gerhard_Markart/publication/273761280_A_Simple_Code_of_Practice_for_the_Assessment_of_Surface_Runoff_Coefficients_for_Alpine_Soil-Vegetation_Units_in_Torrential_Rain_(Version_2.0)/links/550ae07c0cf265693cee3e89.pdf'},{id:"B16",body:'Saxton KE, Rawls WJ. Soil water characteristic estimates by texture and organic matter for hydrologic solutions. Soil Sci Soc Am J. 2006 Sep;70(5):1569–1578'},{id:"B17",body:'Carsel RF, Parrish RS. Developing joint probability distributions of soil water retention characteristics. Water Resources Research. 1988;24(5):755–769'},{id:"B18",body:'Hibbert AR. Forest Treatment Effects on Water Yield. Coweeta Hydrologic Laboratory, Southeastern Forest Experiment Station; 1965. 86 p'},{id:"B19",body:'Johnson R. The forest cycle and low river flows: A review of UK and international studies. Forest Ecology and Management. 1998 Sep 16;109(1):1–7'},{id:"B20",body:'Brown AE, Zhang L, McMahon TA, Western AW, Vertessy RA. A review of paired catchment studies for determining changes in water yield resulting from alterations in vegetation. Journal of Hydrology. 2005 Aug 1;310(1):28–61'}],footnotes:[],contributors:[{corresp:"yes",contributorFullName:"Christian Scheidl",address:"christian.scheidl@boku.ac.at",affiliation:'
Institute of Mountain Risk Engineering, University of Natural Resources and Life Sciences, Austria
Department of Natural Hazards, Federal Research and Training Centre for Forests, Natural Hazards and Landscape, Austria
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Her research interests include archaea metabolism, enzymes purification and characterization, gene regulation, carotenoids and bioplastics production, antioxidant\ncompounds, waste water treatments, and brines bioremediation.\nRosa María’s other roles include editorial board member for several journals related\nto biochemistry, reviewer for more than 60 journals (biochemistry, molecular biology, biotechnology, chemistry and microbiology) and president of several organizing committees in international meetings related to the N-cycle or respiratory processes.",institutionString:null,institution:{name:"University of Alicante",institutionURL:null,country:{name:"Spain"}}},editorTwo:null,editorThree:null,series:{id:"11",title:"Biochemistry",doi:"10.5772/intechopen.72877",issn:"2632-0983"},editorialBoard:[{id:"79367",title:"Dr.",name:"Ana Isabel",middleName:null,surname:"Flores",slug:"ana-isabel-flores",fullName:"Ana Isabel Flores",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRpIOQA0/Profile_Picture_1632418099564",institutionString:null,institution:{name:"Hospital Universitario 12 De Octubre",institutionURL:null,country:{name:"Spain"}}},{id:"328234",title:"Ph.D.",name:"Christian",middleName:null,surname:"Palavecino",slug:"christian-palavecino",fullName:"Christian Palavecino",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y000030DhEhQAK/Profile_Picture_1628835318625",institutionString:null,institution:{name:"Central University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"186585",title:"Dr.",name:"Francisco Javier",middleName:null,surname:"Martin-Romero",slug:"francisco-javier-martin-romero",fullName:"Francisco Javier Martin-Romero",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSB3HQAW/Profile_Picture_1631258137641",institutionString:null,institution:{name:"University of Extremadura",institutionURL:null,country:{name:"Spain"}}}]},onlineFirstChapters:{paginationCount:34,paginationItems:[{id:"81595",title:"Prosthetic Concepts in Dental Implantology",doi:"10.5772/intechopen.104725",signatures:"Ivica Pelivan",slug:"prosthetic-concepts-in-dental-implantology",totalDownloads:22,totalCrossrefCites:0,totalDimensionsCites:0,authors:null,book:{title:"Current Concepts in Dental Implantology - 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\r\n\tIn general, the harsher the environmental conditions in an ecosystem, the lower the biodiversity. Changes in the environment caused by human activity accelerate the impoverishment of biodiversity.
\r\n
\r\n\tBiodiversity refers to “the variability of living organisms from any source, including terrestrial, marine and other aquatic ecosystems and the ecological complexes of which they are part; it includes diversity within each species, between species, and that of ecosystems”.
\r\n
\r\n\tBiodiversity provides food security and constitutes a gene pool for biotechnology, especially in the field of agriculture and medicine, and promotes the development of ecotourism.
\r\n
\r\n\tCurrently, biologists admit that we are witnessing the first phases of the seventh mass extinction caused by human intervention. It is estimated that the current rate of extinction is between a hundred and a thousand times faster than it was when man first appeared. The disappearance of species is caused not only by an accelerated rate of extinction, but also by a decrease in the rate of emergence of new species as human activities degrade the natural environment. The conservation of biological diversity is "a common concern of humanity" and an integral part of the development process. Its objectives are “the conservation of biological diversity, the sustainable use of its components, and the fair and equitable sharing of the benefits resulting from the use of genetic resources”.
\r\n
\r\n\tThe following are the main causes of biodiversity loss:
\r\n
\r\n\t• The destruction of natural habitats to expand urban and agricultural areas and to obtain timber, minerals and other natural resources.
\r\n
\r\n\t• The introduction of alien species into a habitat, whether intentionally or unintentionally which has an impact on the fauna and flora of the area, and as a result, they are reduced or become extinct.
\r\n
\r\n\t• Pollution from industrial and agricultural products, which devastate the fauna and flora, especially those in fresh water.
\r\n
\r\n\t• Global warming, which is seen as a threat to biological diversity, and will become increasingly important in the future.
",coverUrl:"https://cdn.intechopen.com/series_topics/covers/40.jpg",keywords:"Ecosystems, Biodiversity, Fauna, Taxonomy, Invasive species, Destruction of habitats, Overexploitation of natural resources, Pollution, Global warming, Conservation of natural spaces, Bioremediation"},{id:"39",title:"Environmental Resilience and Management",scope:"
\r\n\tThe environment is subject to severe anthropic effects. Among them are those associated with pollution, resource extraction and overexploitation, loss of biodiversity, soil degradation, disorderly land occupation and planning, and many others. These anthropic effects could potentially be caused by any inadequate management of the environment. However, ecosystems have a resilience that makes them react to disturbances which mitigate the negative effects. It is critical to understand how ecosystems, natural and anthropized, including urban environments, respond to actions that have a negative influence and how they are managed. It is also important to establish when the limits marked by the resilience and the breaking point are achieved and when no return is possible. The main focus for the chapters is to cover the subjects such as understanding how the environment resilience works, the mechanisms involved, and how to manage them in order to improve our interactions with the environment and promote the use of adequate management practices such as those outlined in the United Nations’ Sustainable Development Goals.
\r\n\tPollution is caused by a wide variety of human activities and occurs in diverse forms, for example biological, chemical, et cetera. In recent years, significant efforts have been made to ensure that the environment is clean, that rigorous rules are implemented, and old laws are updated to reduce the risks towards humans and ecosystems. However, rapid industrialization and the need for more cultivable sources or habitable lands, for an increasing population, as well as fewer alternatives for waste disposal, make the pollution control tasks more challenging. Therefore, this topic will focus on assessing and managing environmental pollution. It will cover various subjects, including risk assessment due to the pollution of ecosystems, transport and fate of pollutants, restoration or remediation of polluted matrices, and efforts towards sustainable solutions to minimize environmental pollution.
\r\n\tWater is not only a crucial substance needed for biological life on Earth, but it is also a basic requirement for the existence and development of the human society. Owing to the importance of water to life on Earth, early researchers conducted numerous studies and analyses on the liquid form of water from the perspectives of chemistry, physics, earth science, and biology, and concluded that Earth is a "water polo". Water covers approximately 71% of Earth's surface. However, 97.2% of this water is seawater, 21.5% is icebergs and glaciers, and only 0.65% is freshwater that can be used directly by humans. As a result, the amount of water reserves available for human consumption is limited. The development, utilization, and protection of freshwater resources has become the focus of water science research for the continued improvement of human livelihoods and society.
\r\n
\r\n\tWater exists as solid, liquid, and gas within Earth’s atmosphere, lithosphere, and biosphere. Liquid water is used for a variety of purposes besides drinking, including power generation, ecology, landscaping, and shipping. Because water is involved in various environmental hydrological processes as well as numerous aspects of the economy and human society, the study of various phenomena in the hydrosphere, the laws governing their occurrence and development, the relationship between the hydrosphere and other spheres of Earth, and the relationship between water and social development, are all part of water science. Knowledge systems for water science are improving continuously. Water science has become a specialized field concerned with the identification of its physical, chemical, and biological properties. In addition, it reveals the laws of water distribution, movement, and circulation, and proposes methods and tools for water development, utilization, planning, management, and protection. Currently, the field of water science covers research related to topics such as hydrology, water resources and water environment. It also includes research on water related issues such as safety, engineering, economy, law, culture, information, and education.
",coverUrl:"https://cdn.intechopen.com/series_topics/covers/41.jpg",keywords:"Water, Water resources, Freshwater, Hydrological processes, Utilization, Protection"}],annualVolumeBook:{},thematicCollection:[],selectedSeries:{title:"Environmental Sciences",id:"25"},selectedSubseries:null},seriesLanding:{item:{id:"11",title:"Biochemistry",doi:"10.5772/intechopen.72877",issn:"2632-0983",scope:"Biochemistry, the study of chemical transformations occurring within living organisms, impacts all areas of life sciences, from molecular crystallography and genetics to ecology, medicine, and population biology. Biochemistry examines macromolecules - proteins, nucleic acids, carbohydrates, and lipids – and their building blocks, structures, functions, and interactions. Much of biochemistry is devoted to enzymes, proteins that catalyze chemical reactions, enzyme structures, mechanisms of action and their roles within cells. Biochemistry also studies small signaling molecules, coenzymes, inhibitors, vitamins, and hormones, which play roles in life processes. Biochemical experimentation, besides coopting classical chemistry methods, e.g., chromatography, adopted new techniques, e.g., X-ray diffraction, electron microscopy, NMR, radioisotopes, and developed sophisticated microbial genetic tools, e.g., auxotroph mutants and their revertants, fermentation, etc. More recently, biochemistry embraced the ‘big data’ omics systems. Initial biochemical studies have been exclusively analytic: dissecting, purifying, and examining individual components of a biological system; in the apt words of Efraim Racker (1913 –1991), “Don’t waste clean thinking on dirty enzymes.” Today, however, biochemistry is becoming more agglomerative and comprehensive, setting out to integrate and describe entirely particular biological systems. 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He has published more than 100 peer-reviewed research articles and graduated numerous Ph.D. and postdoctoral students.",institutionString:null,institution:{name:"New York University Langone Medical Center",institutionURL:null,country:{name:"United States of America"}}},subseries:[{id:"14",title:"Cell and Molecular Biology",keywords:"Omics (Transcriptomics; Proteomics; Metabolomics), Molecular Biology, Cell Biology, Signal Transduction and Regulation, Cell Growth and Differentiation, Apoptosis, Necroptosis, Ferroptosis, Autophagy, Cell Cycle, Macromolecules and Complexes, Gene Expression",scope:"The Cell and Molecular Biology topic within the IntechOpen Biochemistry Series aims to rapidly publish contributions on all aspects of cell and molecular biology, including aspects related to biochemical and genetic research (not only in humans but all living beings). We encourage the submission of manuscripts that provide novel and mechanistic insights that report significant advances in the fields. Topics include, but are not limited to: Advanced techniques of cellular and molecular biology (Molecular methodologies, imaging techniques, and bioinformatics); Biological activities at the molecular level; Biological processes of cell functions, cell division, senescence, maintenance, and cell death; Biomolecules interactions; Cancer; Cell biology; Chemical biology; Computational biology; Cytochemistry; Developmental biology; Disease mechanisms and therapeutics; DNA, and RNA metabolism; Gene functions, genetics, and genomics; Genetics; Immunology; Medical microbiology; Molecular biology; Molecular genetics; Molecular processes of cell and organelle dynamics; Neuroscience; Protein biosynthesis, degradation, and functions; Regulation of molecular interactions in a cell; Signalling networks and system biology; Structural biology; Virology and microbiology.",annualVolume:11410,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/14.jpg",editor:{id:"165627",title:"Dr.",name:"Rosa María",middleName:null,surname:"Martínez-Espinosa",fullName:"Rosa María Martínez-Espinosa",profilePictureURL:"https://mts.intechopen.com/storage/users/165627/images/system/165627.jpeg",institutionString:null,institution:{name:"University of Alicante",institutionURL:null,country:{name:"Spain"}}},editorTwo:null,editorThree:null,editorialBoard:[{id:"79367",title:"Dr.",name:"Ana Isabel",middleName:null,surname:"Flores",fullName:"Ana Isabel Flores",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRpIOQA0/Profile_Picture_1632418099564",institutionString:null,institution:{name:"Hospital Universitario 12 De Octubre",institutionURL:null,country:{name:"Spain"}}},{id:"328234",title:"Ph.D.",name:"Christian",middleName:null,surname:"Palavecino",fullName:"Christian Palavecino",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y000030DhEhQAK/Profile_Picture_1628835318625",institutionString:null,institution:{name:"Central University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"186585",title:"Dr.",name:"Francisco Javier",middleName:null,surname:"Martin-Romero",fullName:"Francisco Javier Martin-Romero",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSB3HQAW/Profile_Picture_1631258137641",institutionString:null,institution:{name:"University of Extremadura",institutionURL:null,country:{name:"Spain"}}}]},{id:"15",title:"Chemical Biology",keywords:"Phenolic Compounds, Essential Oils, Modification of Biomolecules, Glycobiology, Combinatorial Chemistry, Therapeutic peptides, Enzyme Inhibitors",scope:"Chemical biology spans the fields of chemistry and biology involving the application of biological and chemical molecules and techniques. In recent years, the application of chemistry to biological molecules has gained significant interest in medicinal and pharmacological studies. This topic will be devoted to understanding the interplay between biomolecules and chemical compounds, their structure and function, and their potential applications in related fields. Being a part of the biochemistry discipline, the ideas and concepts that have emerged from Chemical Biology have affected other related areas. 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Behind these definitions are hidden all the aspects of normal and pathological functioning of all processes that the topic ‘Metabolism’ will cover within the Biochemistry Series. 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Thus proteomics, an area of research that detects all protein forms expressed in an organism, including splice isoforms and post-translational modifications, is more suitable than genomics for a comprehensive understanding of the biochemical processes that govern life. The most common proteomics applications are currently in the clinical field for the identification, in a variety of biological matrices, of biomarkers for diagnosis and therapeutic intervention of disorders. From the comparison of proteomic profiles of control and disease or different physiological states, which may emerge, changes in protein expression can provide new insights into the roles played by some proteins in human pathologies. Understanding how proteins function and interact with each other is another goal of proteomics that makes this approach even more intriguing. Specialized technology and expertise are required to assess the proteome of any biological sample. Currently, proteomics relies mainly on mass spectrometry (MS) combined with electrophoretic (1 or 2-DE-MS) and/or chromatographic techniques (LC-MS/MS). MS is an excellent tool that has gained popularity in proteomics because of its ability to gather a complex body of information such as cataloging protein expression, identifying protein modification sites, and defining protein interactions. The Proteomics topic aims to attract contributions on all aspects of MS-based proteomics that, by pushing the boundaries of MS capabilities, may address biological problems that have not been resolved yet.",annualVolume:11414,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/18.jpg",editor:{id:"200689",title:"Prof.",name:"Paolo",middleName:null,surname:"Iadarola",fullName:"Paolo Iadarola",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSCl8QAG/Profile_Picture_1623568118342",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorTwo:{id:"201414",title:"Dr.",name:"Simona",middleName:null,surname:"Viglio",fullName:"Simona Viglio",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRKDHQA4/Profile_Picture_1630402531487",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorThree:null,editorialBoard:[{id:"72288",title:"Dr.",name:"Arli Aditya",middleName:null,surname:"Parikesit",fullName:"Arli Aditya Parikesit",profilePictureURL:"https://mts.intechopen.com/storage/users/72288/images/system/72288.jpg",institutionString:null,institution:{name:"Indonesia International Institute for Life Sciences",institutionURL:null,country:{name:"Indonesia"}}},{id:"40928",title:"Dr.",name:"Cesar",middleName:null,surname:"Lopez-Camarillo",fullName:"Cesar Lopez-Camarillo",profilePictureURL:"https://mts.intechopen.com/storage/users/40928/images/3884_n.png",institutionString:null,institution:{name:"Universidad Autónoma de la Ciudad de México",institutionURL:null,country:{name:"Mexico"}}},{id:"81926",title:"Dr.",name:"Shymaa",middleName:null,surname:"Enany",fullName:"Shymaa Enany",profilePictureURL:"https://mts.intechopen.com/storage/users/81926/images/system/81926.png",institutionString:"Suez Canal University",institution:{name:"Suez Canal University",institutionURL:null,country:{name:"Egypt"}}}]}]}},libraryRecommendation:{success:null,errors:{},institutions:[]},route:{name:"chapter.detail",path:"/chapters/47334",hash:"",query:{},params:{id:"47334"},fullPath:"/chapters/47334",meta:{},from:{name:null,path:"/",hash:"",query:{},params:{},fullPath:"/",meta:{}}}},function(){var e;(e=document.currentScript||document.scripts[document.scripts.length-1]).parentNode.removeChild(e)}()