Agronomic indices for N-use efficiency for forages.
There is a concern about the growing population and limitation in natural resources which are taking the population to direct its agricultural systems into a more productive and efficient activity, looking to avoid a negative impact on the surrounding environment. The industry energy expended to produce nitrogen (N)-fertilizer is considered an indirect consumption of energy in agriculture, which is higher with an increasing forage yield. Nitrogen is the key nutrient associated with high-yielding production in forage grass and grain crops. The aim of this chapter is to introduce the best management practices (BMPs) for N-fertilizer application in forage grasses to improve N-use efficiency, since the most economical way to feed livestock is forage plants where its potential biomass production is not well explored. The BMPs basically follow three management practices: (1) soil nutrient availability and forage requirement, (2) fertilizer application, and (3) decrease in nutrient losses from soil. In order to take a decision on applying N-fertilizer to accomplish forage grasses production with social, economic, and environmental benefits, the N-fertilizer use in forage grasses is going to follow the “Right rate, Right source, Right place, and Right time (4R) nutrient stewardship.” The application of the 4R’s nutrients stewardship is directly associated with economic, social, and environmental impact. The capacity of the 4R’s implementation worldwide turns into a best guide to improve the striving of better N-use efficiency in forage grass. The 4R’s are interrelated; thus, the recommendation of N-fertilizer rates cannot be prescribed without the combination of the 4R’s where a whole system to be followed should be considered to decide about N-fertilizer in pasture. Consequently, any decision in one of the 4R’s is going to affect the expected N-fertilizer results and dry matter production.
- soil fertility
- N-fertilizer recovery
- N-use efficiency
- Brachiaria spp.
- Panicum maximum
A remarkable increase in cattle herd in Brazil occurred from 1977 to 2012, with the Midwest region showing a high increase . However, extending to new frontiers for Brazilian cattle herd is constraint to limited areas and consequently the yield of forage grass needs to be increased. Thus, the intensification of livestock production tends to intensive management. Increasing livestock production due to the world demand for meat is quite associated with an improvement in forage production. To feed grazed animal in livestock, tropical forages are the cheapest source of food in Brazil. Brachiaria spp., Panicum maximum, and Stylosanthes spp. are the majorly cultivated forage in Brazil. Among the gender Brachiaria spp., B. brizantha cv. Marandu is majorly cultivated in Brazil with 45% of the whole area with cultivated pastures , which correspond to approximately 45 million hectares. However, in Brazil there are millions of hectares with degraded pastures, due to soil with low fertility and no replacement of nutrients removed from soil over the years.
The uses of synthetic fertilizers in agriculture are primordial to sustain the growing population worldwide, which tends to increase linearly with population growth at least until 2050 . Different from phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), and micronutrients [boron (B), zinc (Zn), iron (Fe), manganese (Mn), and copper (Cu)], N needs to be applied to every cropping season, because N does not remain longer in soil profile. Soil organic matter (SOM) is the main source of N, which can compile 95% of the total N and 5% remain as NO3-N and NH4-N. However, the amount of N in soil varies a lot due to many factors including soil clay content, moisture, aeration, temperature, tillage, rainfall, and so on, which implies a high N dynamic in soil and consequently the problem in measuring the inorganic soil N-content (NO3-N and NH4-N).
Nitrogen and phosphorus represent the most limited macronutrients in tropical forages. Forage grasses are quite responsive to N-fertilizer; its applications may result in increasing crude protein (CP), number of tillers and leaves, and consequently dry matter (DM) production, since other production factors are not limited . Nitrogen-fertilizer in forage grasses has shown low-use efficiency on tropical climate region. Nitrogen-fertilizer is usually applied in intensive management systems and results in high NH3-N losses, causing low N-use efficiency (NUE).
Using N-fertilizer in forage grass must be well thought because overrates of N-fertilizer can promote excess of forage biomass above the capacity of consumption of animal grazing; thus the stocking rate needs to be adjusted in accordance with forage availability. We must keep in mind that the response to N-fertilizer is closely related to the adequate content of P, K, and other nutrients available in soil. Just N application in forages cannot result in a satisfactory increase of biomass production, if there are constraints of other nutrients in soil, occasioning in low NUE .
In order to increase N-fertilizer efficiency in forage grasses, one must keep in mind that the concepts of best management practices (BMPs) for fertilizer application must be followed, which combines the Right source, Right rate, Right place, and Right time’s (4R) nutrient stewardship . These concepts are universally applied, but the adjustment of the 4R’s recommendation depends on site-specific conditions, thus the use of a specific nutrient rate for one location is unpractical and even more unrealistic for other regions. Based on the earlier explanation, this chapter introduces the concept of the 4R’s to direct BMPs to improve NUE in forage grasses, in order to combine all practices forward the best economic, social, and environment conditions.
2. Nitrogen-use efficiency
The concept of best management practices (BMPs) for fertilizer use is quite important to improve N-use efficiency (NUE) in forage grasses. In forage breeding programs, the application of NUE could be a useful tool to select forage genotypes with higher capacity of biomass production under lower amount of N-fertilizer rate. The improvement of NUE can result in higher quantity and quality of dry matter production on grassland. Even with the majority of methodologies conducted using grain crops as shown in Table 1 , the adaptation of these procedures can be well applied in forage grasses.
|N-use efficiency index||Calculation||References|
|AEN = Agronomic|
efficiency of applied N (kg yield increased per kg N applied)
|AEN = (YN−Y0)/FN||[51, 52]|
|NER = N-efficiency ratio (kg of yield per kg of N in tissue)||NER = [(Units of yield)/(Units of N in tissue)]|||
|PEN = Physiological efficiency of applied N (kg yield increase per kg increase in N-uptake from fertilizer)||PEN = (YN−Y0)/(UN−U0)||[51, 52]|
|NFR = N-fertilizer recovery (%)||NFR (%) = [(UN−U0)/(FN)].100||[52, 54]|
|SNS = Soil N-recovery (%)||GNCu/GNCf multiplied by 100||[52, 54]|
In general, the concept of NUE is associated with higher yield and low N-fertilizer input; thus, it can be achieved if other N-management has already applied. The use of N-sources can change NUE and even the rate, place, and time of N-fertilizer. To improve NUE, it is a complex combination, where the concepts of BMPs must be followed step by step, which are associated with the Right rate, Right source, Right place, and Right time (4R’s) of N-fertilizer application on forage grass or grain crops . Thus, all the concepts reported in the following subheadings will achieve a higher dry matter production with low N-input in the forage production, combined with social, economic, and environment benefits.
Another manner to assess fertilizer application is through the bioeconomic efficiency that is compiled by the conversion efficiency of N-fertilizer into forage dry matter produced, by the efficiency that the produced forages are consumed by the grazing animal, and through the efficiency to convert forage into animal products .
3. The 4R’s for N-fertilizer in forage grass
The consequences of uncorrected N-management practice can have an impact on the increasing greenhouse gas (GHG) emission, NH3-N volatilization, N-runoff, and water eutrophication, which are directly associated with a negative impact on environment. The success of N-fertilizer in forage depends on the combination of rate, source, place, and time of application.
In general, BMPs are followed by three management practices that include the combination of soil nutrient availability and forage requirement, fertilizer application, and decreased N-losses from soil. The BMPs for fertilizer application are based on the 4R’s nutrient stewardship (Right source, Right rate, Right place and Right time) ( Figure 1 ). These concepts combined direct understanding on how one can advance under a sustainable agriculture. The 4R’s are considered universal; then the scientific practices that direct the 4R’s can be applied and adjusted in site-specific around the world. Therefore, for each region and even each farmer there will be a set of practices that are site-specific to implement the 4R’s nutrient stewardship. The idea to have just one common recommendation for N-fertilizer cannot be followed any longer.
All strives to implement the 4R’s nutrient stewardship in grassland must be incentivized to improve NUE. The concern about high production cost and surrounding environment impact is quite evident in agricultural system, and N-fertilizer has a great quota of increasing these problems due to its high mobility in soil through NO3-N leaching, ammonium volatilization (NH3-N), and nitrous oxide (N2O) emission .
In order to apply the 4R’s nutrients stewardship, it is important to keep in mind that the 4R’s concept is directly associated with economic, social, and environmental impact ( Figure 1 ). The concepts shown in Figure 1 are interlinked; therefore, any decision in one of the 4R’s can influence directly on the results of N-fertilizer management and consequently on NUE.
3.1. Right rate
Nitrogen requirement for tropical forage and soil N-supply must be balanced with N-fertilizer rates, which is the most important nutrient removed from the soil in perennial pasture. Quantification of soil N-availability is quite difficult; because N is very dynamic, changing from organic to inorganic forms depending on weather conditions, and soil feature, as aeration, bulk density, soil water content, moisture, etc. Thus, N-quantification through soil analysis becomes incorrect or not much realistic. On the other hand, for other nutrients like P, K, Ca, Mg, S, and micronutrients, soil nutrient quantification using chemical extractors can result in accurate diagnosis.
Preview researches related to total N in soil quantify that 95% of the whole N in soil are combined in organic compounds that is available for plant uptake after the mineralization process, resulting in inorganic forms of N (NO3-N and NH4-N) . The total N in soil with pasture can achieve on average 2 Mg ha−1 of organic N with 5 years of pasture implemented under rotation with soybean and maize . Consequently, the total N in soil and labile N are indicative of soil supply ( Figure 2 ). In comparison to other crops and intercropping, B. ruziziensis and B. brizantha cv. Marandu cultivated without intercropping showed higher labile N in soil . Thus, even with constraints in evaluating soil N-supply, the quantification of SOM, total N, and labile N can direct some information to guide the recommendation of N-fertilizer rates.
Nitrogen is required by tropical forage in high amounts, and the answer has varied among the forage species which range from 200 to 1.800 kg N ha−1 per year . In order to recommend N-fertilizer rates, besides the factors already mentioned, it is necessary to take into account the capacity of N-fertilizer use efficiency by forage plants and its impact on the stocking rate. Thus, the amount of cattle herd is capable to consume the forage and the management for feeding to avoid excess and absence of forage .
Even with high response to N-fertilizer rate by tropical forage, resulting in increasing crude protein (CP), and other bromatological features , the risk of higher downward residual NO3-N movement in soil and high concentration of NO3-N in biomass due to N-fertilizer above plant requirement must be considered to avoid environment contamination and animal health problems [11, 12].
In order to increase forage biomass production, the balance of nutrients in soil and plants must be considered, and the constraint of other nutrients cannot be replaced by an increasing rate of N-fertilizer, and thus the expected dry matter production associated with plant requirement is the guide to determine the appropriate N-fertilizer rate. The low S supply may increase NO3-N accumulation and soluble protein in plant tissue , due to possible restriction in NO3-N reductase enzyme .
In a condition without N-fertilizer, biological fixation of N2, and atmospheric deposition, the N available for forage plant uptakes is just the N mineralized from SOM . Thus, avoiding N-fertilizer in forage can deplete its biomass production over time, since soil N-mineralization is slow and not able to supply forage requirement for a long time. One must keep in mind that grazed animals must consume the biomass production in forage; therefore, the stocking rate management must be taken into consideration to decide the N-fertilizer rate.
Usually, the recommendation of N-fertilizer in forage follows the concept of yield response with an expected production and stocking rate associated to consume the excess production, both associated with N-fertilizer rate experiments in site-specific conditions.
3.2. Right source
Soil organic matter (SOM) is the highest supplier of N for forage growth, which can reach 85% of the whole N required by forages ; thus, the absence of N-fertilizer rates to replace the plant uptakes can conduct to pasture degradation. Forage plants uptake N majority through nitrate (NO3-N) and ammonium (NH4-N) , which depend on their contents in soil solution ( Figure 3 ). The proportion of NO3-N and NH4-N is determined by soil conditions, NO3-N can be predominant in aerobic condition where nitrification can occur. On the other hand, NH4-N can be predominant in acid soil and anaerobic soil. However, the assimilation of NO3-N in plants tends to expend to be more energetic than NH4-N assimilation. Through the action of inducible enzyme (nitrate reductase), the NO3-N is reduced to NH4-N and finally incorporated to glutamine . When the uptake occurs through NH4-N, the expenditure of energy with the NO3-N reduction is solved.
Good result in forage production was shown when NO3-N and NH4-N had 70 and 30% in soil, respectively [17, 18]. On the other hand, the use of NO3-N:NH4-N mixture at the ratio of 55:45% instead of the NO3-N solely as N source in the nutrient solution enhanced the production of tillers (30%), leaves (20%), and the leaf area surface (30%) of P. maximum Jacq. cv. Aruana (Aruana guineagrass) .
Anyway, both forms of N (NO3 or NH4) are incorporated to amino acids through the glutamine synthetase-glutamate . However, the major problem is the accumulation of NO3-N in forage, because high NO3-N concentrations (above 4500 mg kg−1 of dry matter considered highly toxic) can cause animal mortalities .
There are many N-fertilizer sources for use in forage ( Table 2 ). Nitrogen-fertilizer sources with a higher content of N are preferable to apply in grassland due to lower transport cost and facility of application. Urea, ammonium sulfate, and nitrate are the three majority sources of N used in forage grass. However, each of them has peculiarity in relation to using in forage with its pros and cons.
|Fertilizer source||Minimum guarantee|
|Nutrient content and form||Nutrient solubility/granulometry|
|Urea||45% of N||Total content of N.|
|Ammonium sulfate||20% of N|
22% of S
|Total content of N and S.|
|Fosfato Diamônico (DAP)||17% of N|
45% of P2O5
|Total content of N and P2O5 content soluble in CNA plus water and minimum of 44% soluble in water.|
|Fosfato Monoamônico (MAP)||9% of N|
48% of P2O5
|Total content of N and P2O5 content soluble in CNA plus water and minimum of 44% soluble in water.|
|Ammonium nitrate||32% of N||Total content of N.|
On the one hand, urea [CO(NH2)2] shows the highest concentration of N ( Table 2 ), and lower price per N unit in its composition, and causes less soil acidification compared with ammonium sulfate , on the other hand, urea is the N-fertilizer source that causes higher NH3-N losses through volatilization , and consequently lower NUE.
In order to decrease losses of NH3-N from urea source, the application in season with higher rainfall would be indicated, and as other alternative, the use of urea with the inhibitor of urease can be a viable alternative in forage grass; nevertheless, the still high cost of urea with urease inhibitor can restraint its use in forage grass. In studying with six sources of N-fertilizer B. brizantha cv. Marandu, it was observed that N-sources do not change the performance of dry matter; however, urea with urease inhibitor and polymer-coated urea improved NUE . Urea mechanical incorporation or rain after N-fertilizer application can decrease the amount of NH3-N losses, due to higher speed of urea incorporated in soil .
Ammonium sulfate [(NH4)2SO4] has 22% of sulfur (S) and 20% of N in composition ( Table 2 ); this S content is quite interesting because of the improvement of N-use efficiency by forages. Nevertheless, ammonium sulfate acidifies the soil due to the nitrification process. Among urea, ammonium sulfate, and potassium nitrate fertilizers applied in forage grasses, ammonium sulfate has the highest capacity to increase soil acidity .
Nitrogen and S are closely related to plant metabolism, resulting in increasing protein content when both are in adequate balance for forage. The ratio of N/S for B. brizantha (Hochst. ex A. Rich.) Stapf. cv. Marandu was 10/1; the fertilization promoted high yield, adequate N- and S-concentrations for plant metabolism, and forage production, as well as maintained and/or raised the soil fertility in relation to these nutrients .
In a study published by , the optimum N/S ratio was 14.02 in a high-yielding population defined through method DRIS (diagnosis and recommendation-integrated system). In order to use ammonium sulfate source, it is recommended to apply liming to correct the acidity promoted by this N-source.
Another way to improve N-availability to forage grass is the mixture of legumes and pasture. In Brazil, the native Stylosanthes spp. are used in mixture with Brachiaria spp. The use of a mixture of legume with gramineas is quite interesting to reduce N-fertilizer rate due to legume capacity to fix molecular N2 from atmosphere, but it is still a challenge to maintain the right proportion of these two species without competition, because the legume tends to disappear due to competition [26, 27].
Besides legumes, which has symbiotic association with microorganism in root system, Brachiaria spp. may be partially N supplied by inoculation with Azospirillum amazonense. The association of B. brizantha, B. decumbens, and B. humidicola with A. amazonense was observed by , which reported the capacity of A. amazonense in producing hormones as indole-3-acetic acid (IAA, 3-IAA). Accordingly, the inoculation of A. amazonenses with Brachiaria spp. may result in positive interaction, resulting in such improvement in promoting the growth of forages. The association of Brachiaria spp. and Ancylostoma brazilienses may promote increasing N-accumulation respective to 40 kg ha−1 of N-fertilizer rate. Besides previous information about Brachiaria spp. inoculation with Azospirillum spp., much more researches must be taken for better understanding about the efficiency of Brachiaria spp. inoculation.
Microorganisms in soil provide great contribution in N-availability through mineralization of SOM, basically due to enzyme activity in mineralization process. There are important correlations between microbial biomass carbon (C-MBC) and microbial biomass nitrogen (N-MBN) . In general, in crop rotation system the rate of C-MBC:C-organic and N-MBM:N-total is 1.1 and 2.6%, respectively, while in single crop the rate is 0.8 and 2.1% . As reported by , in pasture system values of 2.4 and 3.2% (N-MBM:C-MBC) were observed.
Under pasture system, the species of forages and soil cover promoted significant effect on C-MBC and enzymatic activity; therefore, these enzymes can be used as indicator of soil quality . Even with equal C-MBC and N-MBN, the activity of urease, protease, and dehydrogenase in pasture was different . The intensity and forms of different plant species influenced in N-cycle require further studying. As reported by , in order to increase the availability of inorganic N through the action of root exudates, the N-microbial mineralization depends on C availability and labile N. Depending on the type of exudation, the losses of N2 to atmosphere can be increased due to reduction of N2O to N2 . The importance of microorganism in improving N through mineralization is crucial in soil, which needs more researches in forage grass to improve our knowledge in N dynamic into this production system.
3.3. Right place
Broadcasting without incorporation is a common manner to apply N-fertilizer in forage grasses in tropical forage. Even with less effective for improvement of NUE, N-fertilizer broadcasting is considered the most practical procedure to apply in larger areas of livestock in tropical climate as the case of Brazil. Besides, this widely used procedure, there are other placement methods that can be used in forage and have already been applied successfully, as the case of banding N-fertilizer incorporated in soil . The N-fertilizer incorporation is the most effective way to decrease NH3-N and increase NUE when N-fertilizer source is the common urea. Conversely, the mechanical incorporation of N-fertilizer in pasture sometimes is not possible due to the absence of adequate implement faced by most farmers. Broadcasting ammonium nitrate and ammonium sulfate on soil surface is effective due to low NH3-N gas volatilization from both N-fertilizer sources.
Applications of urea broadcasting usually show a lower capacity of N-fertilizer recovery, resulting in biomass production of forages below the expected. Urea applied in soil depth markedly reduces the NH3-N gas volatilization without causing serious damage to forages; however, it is not common among Brazilian farmers. The placement of urea on soil surface can decrease above 40% of the whole N-fertilizer applied in forage grass . Ammonia volatilization resulted from urea application may cause environmental impact, with increasing the NH3-N in site-specific surrounding of 85% of the total NH3-N volatilized, and the remaining NH3-N is conducted to another region through winds .
Urea with the inhibitor of urease is an alternative to reduce NH3-N volatilization and N2O when urea is broadcasting without incorporation , occasioning a lower content of NO3-N and NH4-N in soil, but increasing the plant uptake due to higher availability though time .
3.4. Right time
In order to optimize N-fertilizer use efficiency for pastures, the right time is decisive to achieve better results in terms of nutrient uptake and biomass production. The time of N-fertilizer application in forage grass varies through the growing season and higher demand of nutrients by plants. In tropical region, N-uptake is highly demanded in summer season, because of the highest biomass accumulation due to higher rainfall, adequate temperature, and sunlight for optimum forage growth ( Figure 4 ). The highest plant N-requirement is the right time for N-fertilizer in forage grasses , because it tends to improve N-uptake by plants and consequently NUE. For implementation of pasture, the application of N-fertilizer used to show low efficiency due to low plant requirement in the beginning of growth, and SOM mineralization tends to be enough for initial growth.
Even with the suggestion for N-fertilizer time shown in Figure 4 , time is dependent of intensive or extensive livestock system. In rotated grazing, it is used to apply N-fertilizer right after rotated animal. On the other hand, in extensive system N-fertilizer can follow the application time as suggested in Figure 4 . The rainfall information needs to be obtained in site-specific region to manage and develop the right time to maximize the NUE by forage grass. N-fertilizer application in dry season tends to show lower NUE due to water limitation for plant nutrient uptake, which is not recommended because of cost-effective being low.
Summer season is considered the best moment to apply N-fertilizer in forage grasses, resulting in higher NUE due to rainfall enough for better growth. In order to avoid the seasonality of forage growth, even with low NUE in comparison to summer season, the application of N-fertilizer at the end of summer season (March) can help to decrease the growth seasonality ( Figure 4 ). In a study with rates of N and irrigation for B. brizantha cv. Marandu in two periods of the year (dry and wet season) in the IIha Solteira City, Sao Paulo State, Brazil, it was observed that in the wet season, the average DM yield of Marandu grass was 1.9 t ha−1 in the irrigated experiment and 1.8 t ha−1 in the non-irrigated experiment, that is, with no statistically significant difference . In the dry season, the average DM yields were 8.1 t ha−1 in the irrigated treatment and 4.4 t ha−1 under non-irrigated treatment. The irrigated experiment produced 55% more than the non-irrigated one.
4. N-concentration and crude protein (CP) content in forage dry matter
The contents of CP are affected by N-fertilizer rates applied in each forage cut or rotated grazing, and by physiologic age of forage . The measurement of CP in dry matter (DM) of forage is directly related to N-concentration in DM, where the amount of CP is the multiplication of N-concentration by 6.25 . The coefficient is related to N-proportion in vegetal protein. However, this content of CP does not reflect just the real amount of crude protein because it is related to all N forms in tissue, even the NO3-N accounts to result in this amount of CP .
Nitrogen balanced in forage can result in higher leaf/stem ratio, palatability, and succulence in forages . According to Cornell or CNCPS model , the CP of forage plants and foods is divided into five fractions. The soluble part of protein is divided by A and B1 fractions. The fraction A is the N no-protein (NnP), since this fraction is highly soluble in rumen. The remaining B1 fraction is part of true protein, which also shows fast degradation in rumen. The fraction C corresponds to the unavailable protein and it is the part of protein content in acid detergent fiber (ADF), non-soluble N in acid detergent (nADF). These associations of lignin result in tannin complex and products from Maillard reactions that are resistant to microbial enzymatic degradation. The fraction of N in neutral detergent fiber (NDF) is denominated by N non-soluble in neutral detergent (nNDF). Another form of available protein in plant is the subtraction of nADF and nNDF, which are designated as the fraction B3; however, the rate of degradation is quite slow. The B2 fraction is the last, which shows medium degradation and is considered the non-soluble protein fraction; thus, the B2 fraction does not make a part of the cell wall and non-protein N.
Crude protein fractionation is not commonly done in researches related to tropical forages; however, in some scientific results related to N-fertilizer an increase in CP and a decrease in nADF (fraction C) occur. The decrease in fraction C is desirable, because this fraction compiles the non-soluble protein, which is not degraded in the rumen [39–41].
5. Greenhouse gas (GHG) emissions in grazed pasture under N-fertilizer
The three most important greenhouse gases (GHG) in the atmosphere are carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O). Both of them are strongly affected by N-fertilizer in agricultural system , with a major responsibility of agriculture for methane (CH4) and nitrous oxide (N2O) emissions [43, 44].
Nitrous oxide is 310 times more dangerous for stratospheric ozone (O3) than CO2 and shows a lifetime of 112 years in the stratosphere . Nitrous oxide emission in grazed pasture is associated with animal stocking rate, animal excreta (urine and dungs), content of soil NO3-N, N-fertilizer rates, tillage, soil moisture, soil compaction, and other process that affect soil aeration [7, 42].
Nitrous oxide is a way of N-losses in grazed pasture, as well as NO3-N leaching and NH3-N volatilization; both forms of N-losses are related to environment depletion . Nitrogen-fertilizer efficiency is directly related to N2O emission, which is termed denitrification process [16, 46, 47]. In Brazilian Cerrado, the NH3-N and N2O through denitrification were observed to be the most important process of N-losses from cattle excreta for 7 months of rainy season in extensive pasture . As reported by , the emission of N2O in grazed pastures is partially associated with C and N deposited from the animal excreta on soil (urine and dungs) under anaerobic conditions, as the case of soil compaction caused by animal trampling.
The anaerobic circumstance can be observed in wet soil after animal trampling ; thus, the N-fertilizer applied under wet condition can increase the N2O emission through NO3-N content in soil that can be denitrified in pasture. The use of N-fertilizer sources with the inhibitor of urease and nitrification can reduce the N2O emission , due to slow process of urea hydrolase and permanence of NH4-N form instead of NO3-N.
Urine and dungs excreta by grazed animals are responsible for a great source of N2O emission in grazed pastures. Integrated crop-livestock-forestry (ICLFS) or livestock-forestry system (ILFS) can show a positive budget in mitigation GHG. The use of trees in ICLFS or ILFS has achieved positive budged in sequestrated CO2 equivalent in integrated system ( Figure 5A ). Brazilian Agricultural Research Corporation (Embrapa beef cattle) launched the concept of neutral carbon meat (NCM) ( Figure 5B ) , which are possible to affirm that the trees in ICLFS and ILFS have the capacity to neutralize the entire emission of GHG into this production system.
6. Concluding remarks
The 4R’s nutrient stewardship is universal, requiring adjustment in site-specific to improve the N-use efficiency. Based on the 4R’s, it is possible to direct the best management practices (BMPs) to achieve sustainable agricultural. The 4R’s must be well defined in order to obtain higher N-fertilizer use, consequently decreasing in social, economic, and environmental negative impact, resulting in increased nutrient use efficiency associated with high yielding.
A mixture of Brachiaria spp. with legumes must be incentivized to decrease the use of N-sources in forage grasses; however, the competition between species requires more understanding in order to avoid legume degradation in mixture with Brachiaria spp.
In order to improve NUE in forage grass, the N-fertilizer must be applied in the right rate, with the right source, followed by the right time and place; this is the sequence that one needs to keep in mind to adjust the 4R’s in site-specific to achieve social benefits with the absence of negative environmental impact and improvement of economic returns.
The 4R’s are interrelated and N-fertilizer rates cannot be recommended without the combination of the 4R’s where a whole system to be followed should be considered to decide about N-fertilizer in pasture. One must keep in mind that the modification of one principal is going to affect the result of the other.
The possibility to sequestrated greenhouse gas in integrated livestock-forestry system (ILFS) is quite important for the environment. As was reported in this chapter, the implementation of trees in integrated systems can neutralize the whole emission of GHG by cattle.