The rate of comments written with under 75 characters on the popular/unfair videos.
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More than half of the publishers listed alongside IntechOpen (18 out of 30) are Social Science and Humanities publishers. IntechOpen is an exception to this as a leader in not only Open Access content but Open Access content across all scientific disciplines, including Physical Sciences, Engineering and Technology, Health Sciences, Life Science, and Social Sciences and Humanities.
\\n\\nOur breakdown of titles published demonstrates this with 47% PET, 31% HS, 18% LS, and 4% SSH books published.
\\n\\n“Even though ItechOpen has shown the potential of sci-tech books using an OA approach,” other publishers “have shown little interest in OA books.”
\\n\\nAdditionally, each book published by IntechOpen contains original content and research findings.
\\n\\nWe are honored to be among such prestigious publishers and we hope to continue to spearhead that growth in our quest to promote Open Access as a true pioneer in OA book publishing.
\\n\\n\\n\\n
\\n"}]',published:!0,mainMedia:{caption:"IntechOpen Maintains",originalUrl:"/media/original/113"}},components:[{type:"htmlEditorComponent",content:'
Simba Information has released its Open Access Book Publishing 2020 - 2024 report and has again identified IntechOpen as the world’s largest Open Access book publisher by title count.
\n\nSimba Information is a leading provider for market intelligence and forecasts in the media and publishing industry. The report, published every year, provides an overview and financial outlook for the global professional e-book publishing market.
\n\nIntechOpen, De Gruyter, and Frontiers are the largest OA book publishers by title count, with IntechOpen coming in at first place with 5,101 OA books published, a good 1,782 titles ahead of the nearest competitor.
\n\nSince the first Open Access Book Publishing report published in 2016, IntechOpen has held the top stop each year.
\n\n\n\nMore than half of the publishers listed alongside IntechOpen (18 out of 30) are Social Science and Humanities publishers. IntechOpen is an exception to this as a leader in not only Open Access content but Open Access content across all scientific disciplines, including Physical Sciences, Engineering and Technology, Health Sciences, Life Science, and Social Sciences and Humanities.
\n\nOur breakdown of titles published demonstrates this with 47% PET, 31% HS, 18% LS, and 4% SSH books published.
\n\n“Even though ItechOpen has shown the potential of sci-tech books using an OA approach,” other publishers “have shown little interest in OA books.”
\n\nAdditionally, each book published by IntechOpen contains original content and research findings.
\n\nWe are honored to be among such prestigious publishers and we hope to continue to spearhead that growth in our quest to promote Open Access as a true pioneer in OA book publishing.
\n\n\n\n
\n'}],latestNews:[{slug:"intechopen-supports-asapbio-s-new-initiative-publish-your-reviews-20220729",title:"IntechOpen Supports ASAPbio’s New Initiative Publish Your Reviews"},{slug:"webinar-introduction-to-open-science-wednesday-18-may-1-pm-cest-20220518",title:"Webinar: Introduction to Open Science | Wednesday 18 May, 1 PM CEST"},{slug:"step-in-the-right-direction-intechopen-launches-a-portfolio-of-open-science-journals-20220414",title:"Step in the Right Direction: IntechOpen Launches a Portfolio of Open Science Journals"},{slug:"let-s-meet-at-london-book-fair-5-7-april-2022-olympia-london-20220321",title:"Let’s meet at London Book Fair, 5-7 April 2022, Olympia London"},{slug:"50-books-published-as-part-of-intechopen-and-knowledge-unlatched-ku-collaboration-20220316",title:"50 Books published as part of IntechOpen and Knowledge Unlatched (KU) Collaboration"},{slug:"intechopen-joins-the-united-nations-sustainable-development-goals-publishers-compact-20221702",title:"IntechOpen joins the United Nations Sustainable Development Goals Publishers Compact"},{slug:"intechopen-signs-exclusive-representation-agreement-with-lsr-libros-servicios-y-representaciones-s-a-de-c-v-20211123",title:"IntechOpen Signs Exclusive Representation Agreement with LSR Libros Servicios y Representaciones S.A. de C.V"},{slug:"intechopen-expands-partnership-with-research4life-20211110",title:"IntechOpen Expands Partnership with Research4Life"}]},book:{item:{type:"book",id:"432",leadTitle:null,fullTitle:"Pesticides in the Modern World - Pesticides Use and Management",title:"Pesticides in the Modern World",subtitle:"Pesticides Use and Management",reviewType:"peer-reviewed",abstract:"This book brings together issues on pesticides and biopesticides use with the related subjects of pesticides management and sustainable development. 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With the recent proliferation of mobile devices such as smartphones and tablets, a wide variety of videos has become easily accessible on the Internet. Video sharing sites have been utilized for various purposes to share private activities or the public relations activities of companies or to distribute the latest news. Nicovideos [1], one of the most popular video sharing sites in Japan, uses its original system to rank its videos according to the total number of plays, the total number of times the title has been added to the users’ favourites list (called ‘my list’) and the total number of comments annotated to the videos.
\nUnfortunately, evaluations under this system can be intentionally distorted by dishonest users who want to influence the evaluation of a specific video by using multiple accounts. Such manipulation can dishonestly seek to improve a video’s ranking in an effort to have it attract more attention. That is to say, it could be used to create a bandwagon effect that produces increased viewing. To combat such efforts, a new evaluation method, one that is more effective and goes beyond computing a simple numerical value, is necessary.
\nIn this study, we propose a method to detect ratings of cheating caused by dishonest multiple comment postings, focusing on a time-series analysis of the number of comments accumulated by the video. We define videos that receive a substantial number of comments as a result of unfair cheating as unfair videos; videos that appear to be relatively free of such manufactured comments are defined as popular videos. Our proposed detection method focuses on differences in the chronological distributions of comments for the two video classifications—popular videos versus unfair videos.
\nIn the Japanese Internet culture, there are terms or expressions specific to an Internet community that appears to be slowly sinking in with the broader community of Internet users. For example, on the anonymous message board
In our study, we pursued the idea that generalization of these expressions beyond their domain is required. As the services and communities involved are liquid, the expressions are constantly increasing and changing. Because of this, analysis of the content of user comments may be necessary, requiring the conversion of the comments into semantic primitive form in order to conduct an analysis of word distributed representation. However, because some domain-specific expressions are neologisms not defined in an existing dictionary, it is not always effective to treat these expressions as semantic primitives.
\nIn the case of distributed representation, it is necessary to train some quantity of corpus, which can be expensive since there is a cost to updating training data repeatedly for adaptation to new expressions. Our proposed unfair video detection method is independent of the culture specific to the video sharing site, as it analyses the quantitative variation of comments in viewer’s feedback to the video. In this method, it is effective that the statistical approach to language information be the same as the analytic approach used for Internet flaming or Internet trend. In the field of sociolinguistics, there are many studies focusing on a language feature by unit of community or attribute. However, on the Internet, the cultural barriers fall year by year, and there are language expressions that are imported from various cultures which messily exist. In such a situation, it is effective that the analysis model uses a domain-specific dictionary or corpus; however, it is difficult to decide the parameters to be applied for each domain. Therefore, we should discuss the effectiveness of simply treating a language that acts as a numerical value.
\nTo improve a video’s quality of experience (QoE), Yoshimura and [2] proposed a method that uses a score based on the PageRank algorithm as a video evaluation parameter. The method uses link information such as author information and publicly opened favourites lists (
This method judges videos with higher relevance as more beneficial. However, both author information and publicly opened
Hirasawa et al. [3] defined a video that ‘is not yet known socially but would interest many people if it is recommended’ as a video with ‘social novelty’. To discover these videos, the researchers focused on three features:
\nVideo content: directly expresses the content of a video based on tags annotated to the video.
Comments: used to indicate viewer opinion based on comments posted on the video.
Viewing activity: represents users’ viewing actions based on the number of video plays, the number of comments and the number of
The study’s authors proposed a method to estimate social-novelty videos by machine learning, using these three features. They focused on the tag: ‘the video should be evaluated higher’, which is annotated when ‘although the video’s quality is good and interesting, the video has not been played many times and not been widely known’ and evaluated the videos using a feature analysis of the videos with the tag. They confirmed that videos annotated with the ‘should be evaluated higher’ tag were commented on with many positive words. However, because the tags on Nicovideo can be edited by the video’s author himself/herself, it is possible for the author to remove appropriate tags or annotate non-related tags. In addition, because the video author can set the configuration to prevent viewers from changing the tags, a video’s evaluation can become improperly inflated.
\nAn example of the Nicovideo interface is shown in Figure 1. In the video display area, comments posted for a scene in the video are indicated moving from right to left. Comments are reflected and indicated in real-time; older comments posted more than a certain period of time from their posted dates/times are not included.
\nReplay interface GUI of Nicovideo.
Eugene et al. [4] focused on analysing the quality of User Generated Content (UGC) on social media and proposed a method to automatically analyse the content’s quality by calculating a value defined as a ‘quality score’. In this study, the authors considered the interaction between the content creator and the users and estimated the quality of question and answer on the question/answer (QA) site. As in QA, the questions and their answers are described in natural language; both the questioner and the answerer can be the content generators.
\nIn contrast, our study deals with videos posted to a video sharing site and considers the comments posted by viewers. While creators post their videos to the site, users (viewers) are able to watch the videos, post comments and add their favourite videos to their
The unfair videos dealt with in our study are those which receive a remarkably high number of plays or comments, even though their contents are relatively poor (without any change in the picture displayed or the sound heard, as shown in Figure 2). Although it is not easy to evaluate the quality of a variety of video contents, having a tag on the video to identify whether the video is fair or unfair might allow us to use such a tag for the evaluation of content quality.
\nThe screen shot of unfair videos (in the 15th rank).
By being (undeservedly) highly ranked, unfair videos receive more attention from viewers than they otherwise would. This increased attention can sometimes result in many viewers submitting negative reports to the site manager, who will, in response, delete the offending video. Therefore, in devising our study, we believed that there would not be very many unfair videos among those in the higher ranks (based on comments and plays). In addition, we chose not to examine unfair videos whose contents violated copyright laws.
\nWe calculated the number of the comments posted on both popular videos and unfair videos. We used Nicovideo dataset [5]. Figure 3 shows the ratio of the comments on each day since the video was uploaded. The horizontal axis indicates the elapsed days and the vertical axis indicates the comment rate. The rate of comment (
Transition of the comment numbers on each day since the video was uploaded.
Here,
Viewers on the Nicovideo site are able to post their comments using a maximum of 75 characters at any one time. To find basis for judging whether a video has been unfairly evaluated, we analysed videos that received a large number of comments, calculating the length of the character string of the comments posted for both the popular and the unfair videos. The results are shown in Table 1.
\nLength | \nPopular | \nUnfair |
---|---|---|
0 < | \n83.6% | \n98.4% |
15 < | \n14.3% | \n0.7% |
30 < | \n1.6% | \n0.3% |
45 < | \n0.4% | \n0.4% |
60 < | \n0.1% | \n0.2% |
Total number of comments | \n3,920,203 | \n5,089,784 |
The rate of comments written with under 75 characters on the popular/unfair videos.
Overall, the comments tended to be written in under 15 characters. As indicated in the table, for the popular videos, over 83% of the comments were written in under 15 characters; for the unfair videos, over 98% of the comments were written in under 15 characters. Table 2 shows the breakdown of these under-15-character comments.
\nLength | \nPopular | \nUnfair |
---|---|---|
0 < | \n35.0% | \n99.3% |
5 < | \n42.2% | \n0.4% |
10 < | \n22.8% | \n0.3% |
Total number of comments | \n3,277,234 | \n5,010,393 |
The rate of the comments written with under 15 characters on the popular/unfair videos.
Indeed, many comments were written in under five characters. For the popular videos, approximately 70% of the comments were written in under 10 characters. From these results, it is clear that comments tend to be written in short sentences, making it difficult to judge whether a video is ‘fair’ or ‘unfair’ solely from the meanings of the comments posted for it.
\nAs mentioned in the previous section, we attempted to analyse the quality of the comments to demonstrate the difficulty of judging the ‘fairness’ of a video from the meanings of the comment sentences. We used information entropy as an index.
\nInformation entropy [6] has been defined in information theory. It is a measure applied to an event that rarely happens. If an event’s entropy value is high, it is a rare and important event. If the entropy value of a particular event is higher than that of some other event, it can be inferred that the higher valued event includes more information.
\nWe calculated the information entropy value of the characters, words, parts of speeches and primitive semantics of the words used in the comments and analysed the difference between these values for the popular videos and the unfair videos. The entropy equation of video
To divide the comments into word units, we used MeCab, a Japanese morphological analyser [7]. To judge the primitive semantics, we used four kinds of dictionaries: Goi-Taikei (a Japanese lexicon) [8], Word-Classification Lexicon [9], Japanese WordNet [10] and the EDR Concept Dictionary [11].
\nAs the analysis target, we manually prepared 100 popular and unfair videos, and calculated the entropy of character/word/part of speech/primitive semantics. The average/maximum/minimum entropy values are shown in Table 3.
\nCategory | \nAvg/Max/Min | \nNo. of comments | \nAvg. of comment length | \nWord entropy | \nChar. entropy | \nPos. entropy | \nSem. entropy |
---|---|---|---|---|---|---|---|
Unfair | \nAvg. | \n62344.70 | \n21.97 | \n3.97 | \n3.51 | \n2.18 | \n7.32 |
Max | \n4008986 | \n50.18 | \n9.41 | \n5.11 | \n3.79 | \n9.69 | |
Min | \n1001 | \n1.07 | \n0.72 | \n0.02 | \n0.80 | \n1.10 | |
Popular | \nAvg. | \n18800.64 | \n10.05 | \n5.93 | \n4.25 | \n3.54 | \n9.27 |
Max | \n29915 | \n17.28 | \n6.49 | \n5.38 | \n3.93 | \n9.70 | |
Min | \n10536 | \n6.94 | \n5.03 | \n2.57 | \n2.85 | \n8.76 |
Analysis result of each kind of entropy.
As can be seen in the table, the entropy values were uneven, depending on the video. However, the entropy values of the unfair videos were lower, on average, than the popular video entropy values. Because the entropy of primitive semantics was calculated using an existing thesaurus, which means that it was unable to handle the latest buzz terms, it is possible that important or meaningful words were ignored. Given these results, we concluded that we can classify unfair/popular videos by using entropy values as a feature.
\nFigure 4 shows the distribution of comments for the popular videos. Figure 5 shows the comment distribution for the unfair videos. In each case, the vertical axis indicates the date of the comment’s posting, while the horizontal axis indicates the position of the posted comment.
\nComment distribution of a popular video.
Comment distribution of an unfair video.
There are clear differences between the two graphs
\nFor the popular videos, the number of comments decreased gradually, day-by-day. On the other hand, for the unfair videos, the number of comments decreased at a certain time of the day. Furthermore, the days with many comments and the days with few comments were distinctively distributed.
For the popular videos, the scenes at which the comments were posted showed little variation; on the other hand, for the unfair videos, the scenes at which the comments were posted varied widely. Given these two tendencies, we based our method for detecting unfair videos on the chronological fluctuation feature of the comments.
As already mentioned, we concluded that popular videos and unfair videos had distinctive differences in comment posting dates and the degree of variation in the scenes at which the comments were posted.
\nBased on the information obtained from the videos that we examined, we attempted to determine a method to extract unfair videos from a video database. Below are the steps we followed to determine a basis for identifying the unfair videos (Figure 6)
\nWe prepared training data for unfair/popular videos that received a large number of comments.
We prepared comment data from the training data and extracted the dates when the comments were posted and the scenes where the comments were posted.
We sought to find a basis to judge unfair/popular videos based on the posting dates and posting position.
Flow of the training phase and test phase to judge unfairness.
We attempted to find useful information with which to judge whether a video is popular or unfair by examining the fluctuations in the number of comments on a day-to-day basis. Firstly, we split the video into various segments chronologically. We then counted the number of comments posted in each segment for each day and calculated the correlation coefficient between neighbouring dates.
\nUsing the comment data, we calculated the correlation coefficient
The comment data obtained
The number of comments,
The average of
A threshold value to judge whether the video is popular or unfair was determined for the correlation coefficient for each neighbouring date, up to 7 days from the date the video was uploaded. A threshold is the value of the boundary line between two categories. In this study, we classify videos as either over-threshold or under-threshold by establishing the threshold of the coefficient of correlation.
Calculation of correlation coefficient by analysing chronological data of the comment numbers.
A method to extract comment distribution data chronologically.
Based on the comment data posted for the popular/unfair videos, we plotted the number of comments posted on the
Similarity of the comment numbers posted on the videos.
We proposed the following two types of judgment methods using features of the maximum/minimum/average of the correlation coefficient
Calculate the correlation coefficients as described above. From the minimum values of the correlation coefficients, use the maximum value to determine the judgement threshold
Convert the maximum/minimum/average values of the comment correlation coefficient of video
The number of videos included in the experiment is shown in Table 4. The average number of comments posted to the videos is shown in Table 5.
\n\n | Training data | \nTest data |
---|---|---|
Popular video | \n100 | \n65 |
Unfair video | \n100 | \n65 |
The number of experimental data.
\n | Average number of comments |
---|---|
Popular video | \n18801 |
Unfair video | \n40573 |
The average number of comments.
The following conditions were used to select unfair videos for the experiment
\nCondition 1. The number of comments is larger than the number of plays, and the number of comments is over 10,000.
\nCondition 2. Satisfying Condition 1, the number of the viewers who registered the video in
Condition 3. Despite the fact that the video does not contain a motion picture or any sound, a large number of comments are posted.
\nCondition 4. Although the video shows only one still picture and the same sound is repeated, a large number of comments are posted.
\nWhen the number of comments is larger than the number of plays, the implication is that each viewer posted a comment at least once. If the video satisfies this condition, it is highly likely that viewers posted multiple comments for one play; therefore, we set Condition 1. Since it is difficult to increase the number of
Popular videos were defined as videos previously ranked in the top 50 on Nicovideo’s official site [1].
\nAs our baseline method, we chose a method to binary-classify a video as either popular or unfair from the contents of the comments. Existing studies on the document classification task often use a method that calculates word weights as a score based on term frequency or global document frequency, using them as a bag-of-words feature value in machine learning.
\nEbata et al. [13] calculated the importance value of a video using term frequency-inverse document frequency (tf-idf). Our study also uses morpheme as a minimum unit to express a comment’s content and uses tf-idf [14] as the feature value. Tf-idf is an abbreviation of term frequency-inverse document frequency. This is a measure that considers two word characteristics: high-frequency in the document (high TF word), which means it is important; and strongly related to the document’s topic. It is often difficult to distinguish a document’s topic by words which appear in multiple documents.
\nFor our baseline method, we applied a machine learning method that binary-classified popular/unfair videos by training feature using a support vector machine (SVM). Because general document classification tasks often use the number of words of a particular kind as a dimension and importance value, we used the tf-idf-based machine learning method as our baseline method. The calculation of tf-idf follows Eq. (6) through Eq. (9).
\nHere,
To produce another baseline method using comment contents, we applied a method in which the feature quantity is obtained by using comment entropy analysis. Because the scales of the comment entropy values differ depending on the basis units (character/word/part of speech/primitive semantics), we used the feature quantity scaled in advance.
\nWe conducted a preliminary experiment to examine the judgment method using a correlation coefficient threshold. We calculated correlation coefficients from the training data shown in Table 4, then calculated the average value, the maximum average value and the minimum average value based on the correlation coefficients, as shown in Table 6.
\nVideo type | \nAverage | \nAveraged maximum value | \nAveraged minimum Value |
---|---|---|---|
Popular video | \n0.979 | \n0.993 | \n0.848 |
Unfair video | \n0.778 | \n0.972 | \n0.496 |
Average correlation coefficient.
As the table indicates, there were substantial differences between the minimum values of the popular videos and those of the unfair videos. Table 7 shows the judgement result of the test data using the minimum value as the feature.
\n\n | Threshold | \nDetection rate | \nFalse detection rate |
---|---|---|---|
Proposed method | \n0.5 | \n84.8% | \n0% |
0.6 | \n93.8% | \n0% | |
0.7 | \n98.5% | \n1.5% | |
0.8 | \n100% | \n10.7% | |
tf-idf + SVM | \n— | \n75.8% | \n1.0% |
Unfair detection rate and false detection rate.
From this result, it was found that in the range of threshold values of 0.6–0.7, the unfair videos were detected in less than 10% of the cases. On the other hand, the popular videos were detected in over 90% of the cases. We also found that the proposed method using the correlation coefficients achieved a higher unfair detection rate than the comment content–based judgment method.
\nWe used the 100 popular/unfair videos from the preliminary experiment and evaluated the following four methods
\nBaseline method
tf-idf + SVM
Entropy feature + SVM
Proposed method
Method based on the threshold of the time-series correlation coefficient
Machine learning method using the maximum/minimum/average value of correlation coefficient as feature
The results of the leave-one-out cross-validation test are shown in Table 8. We used the Radial Basis Function (RBF) kernel for the SVM kernel parameter. In the proposed method, the number of image segmentations used to calculate the correlation coefficient was set at 10.
\nMethod | \nUnfair video detection rate | \nFalse detection rate | |
---|---|---|---|
Baseline method | \nTf-idf + SVM | \n0.726 | \n0.025 |
\n | Entropy + SVM | \n0.970 | \n0.030 |
Proposed method | \nCoefficient + threshold | \n0.991 | \n0.015 |
\n | Coefficient + SVM | \n0.890 | \n0.070 |
The result of cross validation test of unfair video detection.
We found that the unfair video detection rate for the baseline method was 72.3%, while the rate for the proposed method based on the correlation coefficient was approximately 99%. However, in the case of the baseline method, the false detection rate of popular videos was only 0.5%, while the false detection rate for the proposed method was 1.5%. This result confirmed that our proposed method was effective for unfair video detection.
\nIn the evaluation experiment using the cross-validation test, the baseline method (tf-idf + SVM) had an average detection rate of 72.3%, which was not particularly high. This might be caused by the fact that there were many comments in which the character strings were short and their meanings were nonsense. To improve the comment contents–based method, we would need a way to extract for analysis only those comments that make sense according to a certain standard.
\nOn the other hand, the performance of the judgment method using the entropy feature was equivalent to the performance of the method using the correlation coefficient vector. This result indicated that the entropy feature was able to express the features of the comments on the unfair/popular videos without using time-series information.
\nIn the preliminary experiment, which examined the judgment method based on the correlation coefficients, when the threshold of the correlation coefficient was set at 0.60, only 4.2% of the unfair videos were detected. To illustrate the problem, in cases where not-so-high and not-so-low correlation coefficient values were continuously calculated, when all the values were larger than 0.60 but smaller than 0.65, the video was suspected of being unfair, but the proposed method was unable to identify them as such.
\nFigure 10 shows additional experimental results for the SVM-based judgment method that used the maximum/minimum/average correlation coefficient as the feature. The value of
Accuracy of detection and false detection rate.
In all, 1332 unclassified videos were classified into unfair/not unfair by the proposed method using the split number 30. Figure 11 shows the classification results for each category annotated to the video. The results show that there were categories that were subjected to being judged as unfair.
\nUnfair/not unfair rate for each video category.
We proposed a method to detect unfair videos—videos whose rankings were falsely influenced—among the videos uploaded to a video sharing site. We focused on differences in the comment distribution tendencies between the unfair videos and what we termed popular videos (videos whose rankings were not falsely influenced). The play time of the video was divided into
Our proposed method did not focus on the quality of a comment’s content; rather it focused on the specificity of comment postings by unfair (fraudulent) users. In our evaluation experiment, we found that the proposed method was able to detect unfair videos with 90% accuracy by extracting the video feature based on a time-series analysis of comment data, irrespective of the number of comments.
\nIt should be noted that in this study, we targeted unfair videos that were obviously unfair. Therefore, it is not clear that the threshold of the proposed method can work for less obvious unfair videos or in-between videos that are not popular but not unfair, because their patterns of comment posting are likely to be different. In our experiment, we calculated the correlation coefficients from the time-series distribution of comments and determined threshold values to classify the videos. However, the proposed method lacks versatility because the method is specific to the comment distribution of Nicovideo.
\nIt is likely that a more versatile method could be developed by using other features such as the quality of contents or comment content similarities. In future studies, we plan to develop an automatic video evaluation basis that focuses on the degree of the match between the sense of the video and the content of the comments.
\nThis research was partially supported by JSPS KAKENHI Grant Numbers 15K00425, 15K00309, 15K16077.
\nThe problem of fresh water and the assessment of the ecological state of rivers, lakes, and reservoirs are acute for humanity in the era of anthropogenic stress and global climate change. At the beginning of the twenty-first century, global climate changes continue [1]. There is an increase in surface air temperature, as well as the temperature of water bodies, which have a significant impact on the structure and dynamics of biological communities in aquatic ecosystems [2, 3, 4]. Climate is an important driver of the distributional patterns of individual hydrobionts that may cause changes in community composition [5]. An increase in temperature is considered as eutrophication factor that changes the availability of nutrients, promotes an increase in the internal phosphorus load, and also stimulates abundant and prolonged vegetation of cyanoprokaryotes (blue-green algae) that are the causative agents of water bloom [6, 7, 8].
Algae are the basis of the trophic pyramid in the freshwater ecosystem. The main ecological role of algae is oxygen generation and photosynthetic production of autochthonous organic matter, which forms the energy basis for organisms of higher trophic levels and for all subsequent stages of the production process in large lakes and reservoirs [9, 10]. Cells of algae contain photosynthetic pigments that are among the most common indicators used in the study of algocenoses. The main pigment of green plants, chlorophyll-a (Chl), is considered to be a universal ecological and physiological marker of algae. Chlorophyll is an optically active component of the aquatic environment due to its ability to absorb light in a narrow wavelength range. In particular, this unique property of Chl has found application in remote sensing of large water areas [11, 12].
The amount of chlorophyll is closely related to the biomass of algae which makes it possible to express biomass in units of this important component of the plant cell and use Chl as an indicator of the temporal and spatial dynamics of phytoplankton [13, 14, 15, 16, 17]. A detailed review of studies of the relationship between Chl and algae biomass is given in [18, 19].
The chlorophyll molecule absorbs light quanta and triggers a complex mechanism of photophysical and photochemical reactions, and therefore, it is not surprising that a close relationship is found between Chl concentration and algae photosynthesis [20, 21]. The rate of photosynthesis calculated per unit of Chl, the assimilation number, is used in studies on primary production [22, 23, 24]. The changes in assimilation number under various conditions are considered depending on environmental factors, development and composition of algae [25, 26, 27, 28, 29, 30]. From the assimilation number and chlorophyll concentration, primary production can be calculated [31].
Planktonic algae serve as indicator organisms of the ecological state in water bodies. In this aspect, Chl plays not only a functional, but also an indicator role in aquatic ecosystems. The content of Chl is the basis for the scales developed to assess the trophic status and water quality of marine and fresh waters [9, 10, 32, 33]. An analysis of these scales made it possible to identify the boundary concentrations of Chl for oligotrophic, mesotrophic, moderately eutrophic, eutrophic, hypertrophic, and polytrophic waters that are <1–3, 3–10, 10–15, 15–30, 30–60, and > 60 μg/L, respectively [34].
The present chapter has the aim to considerate the most significant aspects of chlorophyll applications in the ecological study of fresh waters on the example of the Volga River reservoirs.
Our data includes two large blocks that are (1) the route surveys carried out at 70–80 stations of seven run-of-river reservoirs in the summer of 2015–2020, and (2) seasonal observations during 2009–2019 carried out once or twice a month from May to October at six standard stations in the lake-like Rybinsk reservoir. Throughout the period, we used integral samples obtained by mixing equal volumes of water taken from each meter of the water column with a 1 m Elgmork bathometer. Chl was determined by the standard spectrophotometric method in seven reservoirs of the Volga River and by the fluorescent method in the Rybinsk reservoir. We have shown good convergence of the results obtained by these methods with coefficient of determination R2 = 0.94 [35].
The spectrophotometric method [36, 37] due to its simplicity and accessibility, is widely used in the study of algae. Phytoplankton was concentrated on membrane filters with a pore diameter of 3–5 μm. The filters were dried in the dark at room temperature and stored in a refrigerator until analysis. Pigments were determined in 90% acetone extract on a Lambda25 PerkinElmer spectrophotometer; Chl concentrations were calculated using the Jeffrey & Humphrey equation [38].
Currently, the attention of researchers is attracted by the determination of Chl using fluorimeters of various designs. Measurements of chlorophyll fluorescence are taken directly in natural water that makes it possible to evaluate a number of parameters without affecting the integrity of phytoplankton and promptly measure a large number of samples. We used a modification of the method based on the specificity of light-harvesting pigment-protein complexes of the main taxonomic groups of freshwater phytoplankton that are diatoms, blue-green (cyanoprokaryotes), and green algae [39]. The fluorescence intensity was measured in the red region of the spectrum (λ ~ 680 nm) upon excitation with wavelengths of 410, 490, 540 nm before and after the inhibitor of electron transport chain (ETC) was added to the cuvette and the fluorescence yield increases to the maximum level. Chl concentrations were calculated using equations from [40].
We used the available published data including our own papers [20, 41, 42, 43, 44, 45, 46, 47] to discuss the results. Standard software packages for a personal computer Statistic10 and MS Excel 2010 were applied for statistical data processing. Spearman’s rank correlation coefficient (rS) was calculated for small number of observations with n < 30.
The Volga River, at 3690 km, is the longest river in Europe and 16th in the world historically has attracted the attention of many scientists from different fields. Much of the principal information has been summarized in the monographs [48, 49]. The river network of the Volga looks like a branching tree in the north that evolves into a single trunk rooting as a delta in the Caspian Sea in the south. The Volga catchment area is located on the Russian Plain, covering various latitudinal and climatic zones from the southern taiga to semi-desert. The most of the Volga River from the town of Tver’ to Volgograd that is over 2500 km long, is affected by an uninterrupted cascade of eight large shallow reservoirs, considerably slowing the flow velocity of the river. The reservoirs differ in terms of morphometry, optical regime, chemistry, lateral inflow, water exchange, and trophic status [49]. A schematic map of the reservoirs is shown in Figure 1 and their basic characteristics are given in Table 1.
Schematic map of the Volga River reservoirs and the location of observation stations at the Rybinsk reservoir. 1 – boundary of reservoirs; 2 – sample stations. (Author’s compilation based on figures from [
Parameters | Upper Volga | Middle Volga | Lower Volga | ||||
---|---|---|---|---|---|---|---|
Ivankovo | Uglich | Gorky | Cheboksary | Kuibyshev | Saratov | Volgograd | |
Total water input, km3 per year | 10.07 | 11.46 | 49.53 | 118.89 | 244.3 | 248.3 | 259.2 |
Surface area, km2 | 327 | 249 | 1591 | 1080 | 6150 | 1831 | 3117 |
Length, km | 120 | 143 | 430 | 321 | 484 | 348 | 546 |
Mean depth, m | 3.4 | 5.0 | 6.1 | 4.2 | 8.9 | 7.3 | 10.1 |
Total storage, km3 | 1.12 | 1.25 | 8.82 | 4.60 | 57.30 | 12.87 | 31.45 |
Water exchange, year−1 | 10.6 | 10.1 | 6.1 | 20.9 | 4.2 | 19.1 | 8.0 |
Transparency, m | 0.8 | 0.8 | 1.2 | 1.2 | 1.5 | 2.2 | 2.0 |
Water color, Cr-Co degree | 53 | 51 | 53 | 42 | 38 | 36 | 34 |
Conductivity, μSim/cm | 240 | 250 | 206 | 355 | 315 | 345 | 424 |
Total nitrogen, mg/L | 1.34 | 1.27 | 1.09 | 1.14 | 1.08 | 0.99 | 0.98 |
Total phosphorus, μg/L | 90 | 93 | 68 | 124 | 145 | 127 | 134 |
In accordance with the geographical zonality, three sections are distinguished in the cascade that are Upper Volga (56°51′N, 35°55′ E–57°29′ N, 38°17′ E), Middle Volga (58°03′ N, 38°50′ E–53°31′ N, 49°25′ E), and Lower Volga (53°28′ N, 49°42′ E–46°23′ N, 48°02′ E). With a change of conditions in the drainage basin, the total amount of ions (conductivity) increases and the color of the water decreases from the Upper Volga to the Lower Volga. Water transparency increases with the depth in lower reservoirs. The content of nitrogen and phosphorus compounds in the entire cascade is high enough and do not limit the development of algae [49].
Studies of phytoplankton pigments in the Volga River were started in the middle of the twentyth century, but most of them were carried out at separate reservoirs [41, 50, 51, 52]. Our data [43, 44, 45, 46] cover the entire cascade and are of interest for a comparative assessment of the development and state of planktonic algae in reservoirs located in different geographical zones. These are the data needed for environmental monitoring, as well as analysis and forecasting of changes that occur in the aquatic ecosystem under various external impact.
The study of summer plankton is of considerable interest, since at this time the negative trends caused by eutrophication or climate change appear in the water ecosystem. Given the great length of the Volga reservoirs, their complex morphometry, and their differences in a number of parameters, the Chl concentrations vary widely in each of them (Figure 2). Chl concentrations were typical of summer phytoplankton and generally fell within the same limits as 30 years ago (1989–1991) [43]. The minimum Chl values in all reservoirs were close and amounted to 2.5–9 μg/L, while the maximum values differed to a greater extent. Three groups of reservoirs can be distinguished according to the upper limit of Chl. These are Gorky, Saratov, and Volgograd reservoir with the lowest upper limit of 25–36 μg/L; Uglich and Kuibyshev reservoir with intermediate values of 52–59 μg/L; Ivankovo and Cheboksary reservoir with maximum concentrations over 100 μg/L. In all reservoirs of the Volga, interannual differences in Chl were revealed. Over 6 years of research, Chl concentrations at observation sites differed by 3 and 8 times in the Uglich and Gorky reservoirs, by 50 times in the Cheboksary reservoir, and by 13–16 times in others. The interannual differences in the mean values were much smaller, from 1.6 to 2.6 times only (Table 2). The results of ANOVA analysis (Table 3) show that the interannual difference in Chl is significant in the Uglich and Gorky reservoirs (p < 0.01), is on the verge of significance in the Ivankovo reservoir, and is insignificant in the other four reservoirs.
Box plots of chlorophyll concentrations in the Volga River reservoirs in 2015–2020. Unpublished data.
Reservoir | 2015 | 2016 | 2017 | 2018 | 2019 | 2020 |
---|---|---|---|---|---|---|
Ivankovo | 24.0 ± 4.0 (54) | 20.7 ± 3.7 (56) | 22.5 ± 3.6 (47) | 41.2 ± 7.3 (58) | 38.3 ± 5.9 (55) | 23.8 ± 2.0 (60) |
Uglich | 25.5 ± 2.8 (32) | 17.7 ± 3.0 (47) | 16.5 ± 1.9 (29) | 26.1 ± 4.6 (45) | 20.4 ± 2.8 (49) | 17.4 ± 4.1 (57) |
Gorky | 18.4 ± 1.1 (21) | 7.5 ± 1.3 (56) | 6.7 ± 0.8 (40) | 13.1 ± 1.4 (41) | 10.1 ± 1.5 (51) | 12.1 ± 1.8 (63) |
Cheboksary | 29.6 ± 8.1 (81) | 16.9 ± 6.7 (102) | 17.8 ± 6.1 (90) | 25.0 ± 0.8 (107) | 44.0 ± 15.8 (117) | 25.3 ± 10.1 (143) |
Kuibyshev | 6.1 ± 0.8 (42) | 14.8 ± 2.8 (57) | 8.3 ± 2.0 (48) | 9.8 ± 2.6 (117) | 6.1 ± 0.9 (61) | 11.9 ± 2.5 (64) |
Saratov | 5.7 ± 1.0 (41) | — | 4.9 ± 1.5 (72) | 10.6 ± 2.8 (78) | 3.6 ± 0.6 (51) | 8.5 ± 2.4 (48) |
Volgograd | — | — | 6.7 ± 1.0 (44) | 9.6 ± 2.2 (86) | 4.3 ± 0.7 (56) | 10.1 ± 2.7 (25) |
Chlorophyll content in the Volga River reservoirs in the years of study according to [46] with additions (mean values with standard error, μg/L; in brackets coefficient of variation, %; dash is missing data).
Reservoir | SS | df | MS | F | p |
---|---|---|---|---|---|
Ivankovo | 11,002 | 5 | 2200 | 2.25 | 0.06 |
Uglich | 4517 | 5 | 903 | 3.40 | 0.01 |
Gorky | 1235 | 5 | 247 | 13.5 | 0.00 |
Cheboksary | 2777 | 5 | 555 | 0.59 | 0.71 |
Kuibyshev | 594 | 5 | 119 | 1.41 | 0.23 |
Saratov | 60 | 4 | 15 | 0.83 | 0.52 |
Volgograd | 208 | 3 | 69 | 2.12 | 0.11 |
Comparison of the mean chlorophyll concentrations in the Volga River reservoirs in the years of study using one-way analysis of variance (ANOVA) (SS – sum of squared deviations, df – number of degrees of freedom, MS – mean square, F – Fisher’s test, p – significance level). Ftabl > 2.30. Unpublished data.
The distribution of phytoplankton over the water area of the reservoirs was non-uniform. The coefficients of variation of mean Chl concentrations in most cases were 50–70% and exceeded 100% in Cheboksary reservoir (Table 2). The heterogeneity of Chl distribution is due to the large extent and complex morphometry of reservoirs, the presence of water masses of different genesis, the inflow of tributary waters, changes in the flow regime in different areas, and surge phenomena. The features of Chl distribution over the water area of the reservoirs are generally preserved and repeated over a long period [43, 44, 45, 46]. Higher Chl concentrations are usually noted in areas isolated from the Volga channel; in estuarine sections of tributaries; in coastal shallow waters and bays; in the waters of the tributaries themselves. The amount of Chl in these areas is 1.5–3 times higher than at deep channel section. In all years, the largest tributary of the Volga, the Oka River, stands out with a very high Chl concentration [43, 44, 45, 46]. When it flows into the Cheboksary reservoir, Chl increases by an order of magnitude up to 100 μg/L and more. The waters of the Oka River, which differ from the Volga in high mineralization, can be traced in the reservoir for a long distance, creating significant chlorophyll gradients [51].
Throughout the Volga cascade, there is a steady decrease in Chl from the reservoirs of the Upper Volga to the reservoirs of the Lower Volga (Figure 3). The same trend was noted in 1989–1991 [43] and has not changed over a quarter of a century. A similar distribution is also observed for the phytoplankton biomass [8]. The explanation is the increase in flow velocity and volume of runoff downstream the Volga, as well as a decrease in the volume of lateral tributaries. It is the water conditions that limit the development of phytoplankton in the Volga to the greatest extent. This is evidenced by the negative relationship between average Chl concentrations in the reservoirs and the total volume of inflow for May–October (Figure 4). Similarly, in unregulated conditions in the river Thames, algae abundance decreased in years of high water flow [53], and high chlorophyll concentrations in the Lower Mississippi were noted during periods of low flow [54].
The course of chlorophyll in cascade of the Volga River reservoirs. Average values for 2015–2020 with standard error. Dotted line is a trend line. Unpublished data. Iv – Inankovo reservoir, Ugl – Uglich reservoir, Gork – Gorky reservoir, Cheb – Cheboksary reservoir, Kuib – Kuibyshev reservoir; Sar – Saratov reservoir, Volg – Volgograd reservoir.
Correlation between chlorophyll content in the Volga River reservoirs and the total volume of inflow for May–October in 2015–2020 according to [
In all reservoirs, interannual changes in Chl are observed, which are determined by the weather conditions of the years and the conditions of water content. However, the average concentrations of Chl over the past 6 years characterize the Ivankovo, Uglich, and Cheboksary reservoirs as eutrophic (Chl is over 15 mg/L), while the Saratov and Volgograd reservoirs are mesotrophic with Chl up to 10 mg/L. The trophic status of the Gorky and Kuibyshev reservoirs varies from mesotrophic to moderately eutrophic and eutrophic (Table 2).
The assessment of the current trophic status of reservoirs in some cases differs from the assessment in 1989–1991 [43]. At the end of the twentieth century, the Uglich, Saratov, and Volgograd reservoirs were mesotrophic, the Kuibyshev reservoir was moderately eutrophic, and the Ivankovo, Gorky, and Cheboksary reservoirs were eutrophic. Chl concentrations now correspond to the eutrophic type (i.e., higher trophy category) for the Uglich reservoir and moderately eutrophic (lower trophy) for the Gorky reservoir. The values obtained for the Ivankovo, Uglich, and Cheboksary reservoirs during 2015–2020, related to the same trophic gradation, while for the Gorky and Kuibyshev reservoirs, they were different. These variations testify to the high dynamism of the development of the ecosystems of the Volga reservoirs.
Rybinsk reservoir, the third stage of the Volga River cascade, located in the southern taiga subzone (58°00′–59°05′ N, 37°28′–39°00′ E) (Figure 1). It is a large relatively shallow lake-like water body of slow water exchange of 1.4 year−1 [42]. The ratio of the surface area (4500 km2) and the average depth (5.6 m) is very high and equal to ~800. It indicates a high degree of openness of the reservoir [55] that is subject to frequent wind mixing. As a result, there is a decrease in water transparency and also resuspension of nutrients from bottom sediments.
The Rybinsk reservoir is one of the few large reservoirs in the world where systematic regular observations of the chlorophyll content have been carried out. The research began in 1969 continued for more than 50 years under the guidance of my colleague, teacher, and mentor Dr. Inna Pyrina. The results of long-term study of the seasonal and interannual Chl dynamics and its relationship with regional and global environmental factors were published in a series of original papers and summarized in monographs [20, 41, 42].
The seasonal development of plankton is an annual recurring process influenced by external factors and internal biotic interactions [56]. The development of phytoplankton in the Rybinsk reservoir during the open water period corresponds to the classical PEG model [57]. A short spring maximum with Chl concentration in different years from 15 to 50 μg/L is constantly formed in May–early June at water temperatures from 6–9°C to 11–15°C. In late May–early June, the Chl content becomes below 10 μg/L and remains low for 2–4 weeks. During this period there is a seasonal change of phytoplankton communities [8]. The summer maximum, at which Chl can exceed 100 μg/L in some parts of the water area, covers a long period in July–September. Warming up of the water mass to the maximum and its subsequent cooling occurs during this period. In autumn, the Chl content is usually below 10 μg/L, but in some years, it increased to 20–30 μg/L. The timing of the onset of Chl maxima, their duration, quantity, and the ratio of values vary in different years (Figure 5). This is explained by features of development conditions for the algae in a large shallow reservoir, which is an active dynamic environment. The course of seasonal succession of phytoplankton in such an environment is subject to frequent disturbing external influences [57, 58, 59], which include wind mixing [60, 61], and in the reservoirs also the operation of hydraulic structures. Diatom algae dominate the phytoplankton of the reservoir in spring and autumn [8]. The diatom maximum during these periods is usually observed in water bodies of the temperate zone [56, 57]. Active wind mixing of the water column promotes water circulation and maintenance of cells in suspension, and also provides an influx of nutrients [59]. The summer phytoplankton community is formed by blue-green algae (cyanoprokaryotes) and diatoms [8]. Cyanoprokaryotes develop abundantly at stable anticyclonic weather with a predominance of calm conditions; active hydrodynamics which is provided by wind mixing of the water column is favorable for diatoms.
Seasonal dynamics of chlorophyll in the Rybinsk reservoir during 2009–2019 according to [
In a generalized form, according to the data of long-term observations, five periods are distinguished in the seasonal cycle of phytoplankton in the Rybinsk reservoir [47]. The main parameters of these periods are given in Table 4. Each period is characterized by uniform temperature and transparency, which is an indicator of underwater light conditions. Variation coefficient of Chl is minimal at early summer during the seasonal change of communities and is significantly higher during the period of spring and summer phytoplankton maxima, indicating a change in the stability of algocenoses during the growing season.
Parameter | Spring | Early summer | Mid summer | Late summer | Autumn |
---|---|---|---|---|---|
n | 54 | 92 | 218 | 86 | 89 |
Chl, μg/L | 15.9 ± 1.9 (90) | 8.9 ± 0.6 (58) | 20.4 ± 1.0 (73) | 21.2 ± 1.6 (72) | 6.3 ± 0.5 (73) |
Temperature, °С | 9.9 ± 0.5 (38) | 15.7 ± 0.3 (19) | 20.4 ± 0.2 (11) | 15.0 ± 0.2 (12) | 7.2 ± 0.3 (36) |
Transparency, m | 1.20 ± 0.03 (24) | 1.11 ± 0.03 (25) | 1.13 ± 0.02 (23) | 1.06 ± 0.04 (32) | 1.12 ± 0.04 (37) |
Nmin, mg/L* | 0.45 | 0.31 | 0.19 | 0.14 | 0.14 |
Pmin, μg/L* | 21 | 18 | 21 | 26 | 65 |
TN, mg/L* | 0.99 | 1.02 | 0.91 | 1.02 | 0.93 |
TP, μg/L* | 48 | 48 | 64 | 67 | 140 |
Characteristics of the environmental conditions during five periods of phytoplankton seasonal succession in the Rybinsk reservoir in 2009–2019 according to [47] (mean values with standard error, in brackets coefficient of variation, %; n – observation number).
Note. * – data obtained in 2001–2012 according to [42]; Nmin – nitrates, Pmin – phosphates, TN – total nitrogen, TP – total phosphorus.
To analyze and predict the changes that occur in biological communities under anthropogenic pressure and climate change, long-term observations are required. Such observations are carried out in water bodies of the world [62, 63, 64, 65, 66, 67, 68]. According to published data including our own [20, 35, 42, 43], over the entire period of observations since 1969, the Chl content in the Rybinsk reservoir varied by two orders of magnitude, from 1 to 3 to more than 100 μg/L. This range is observed even during one growing season and causes outliers in the scatterplots (Figure 6).
Box plots of chlorophyll concentrations in the Rybinsk reservoir in 2009–2019 according to [
Seasonal average values vary within smaller limits from 5 to 22 μg/L. The long-term dynamics of Chl looks like a broken line with ups and downs (Figure 7). This shows the reaction of the community to changing external conditions, which have a multicomponent and complex effect on the development of phytoplankton. An analysis of long-term data reveals two key effects on interannual Chl variations in the Rybinsk reservoir. Temperature that belongs to the universal and irremovable factors of the environment is the first of them. Temperature is the main factor in the development, seasonal dynamics and spatial distribution of algae, as well as the factor of their geographical distribution and formation of the primary production of water bodies [69, 70, 71].
Long-term dynamics of average annual chlorophyll concentrations in the Rybinsk reservoir according to [
Under global warming, a steady increase in the average water temperature for May–October at a rate of 0.8°С per 10 years has been revealed in the Rybinsk reservoir since 1976 [42]. Against this background, there is a reliable trend towards an increase in average annual Chl value over a 50-year observation period at a rate of 0.4 ± 0.03 μg/L per year (R2 = 0.75, p < 0.05) (Figure 7). The Spearman correlation coefficient between seasonal average Chl and temperature is not high (rS = 0.53, p < 0.05) but it confirms this effect.
The recurrence in Chl dynamics is associated with the second key factor which is the water regime of the reservoir in the years of observation. Negative Spearmen correlation coefficients were obtained between Chl and parameters of water regime: rS = −0.65 for inflow volume and rS = −0.85 for water level. The water regime, in turn, is associated with the cycles of general moisture. High-water periods with cyclonic weather are characterized by increased surface inflow, high water level, high wind activity, and lower temperatures. In low-water years, the anticyclonic type of weather prevails with little precipitation, low reservoir level, increased heating, and a predominance of calm. It is dry years that conditions are favorable for the intensive development of algae and especially the summer species [8, 43, 72, 73]. For the reservoir region, this situation was repeated once every few years over a 50-year period, namely in 1972–1973, 1981, 1984, 1994–1995, 1999–2001, 2010–2013. The conditions of these years served as a trigger for the subsequent increase in Chl, which gradually decreased after the rise, but generally remained at a higher level than in the previous years (Figure 7).
The annual increase in Chl over the entire period of research varied and amounted to 1.2 ± 0.1 μg/L in 1969–1984, 2.2 ± 0.3 μg/L in 1987–1996, and 2.4 ± 0.4 μg/L in 2008–2019. In recent years, under the global warming, this increase has become higher, indicating intensification of the eutrophication process. A particularly strong rise in Chl values was noted after 2010, when sunny weather at an anomalously high air temperature persisted for 40 days on the territory of European Russia [74]. Periodicity in rises and falls of Chl is close to the 11-year cycle of solar activity estimated by Wolf numbers (rS = 0.83). The same was noted earlier for a shorter observation period at the Rybinsk reservoir, as well as for the long-term dynamics of phytoplankton productivity in other water bodies [72, 73, 75, 76].
Seasonally average Chl concentrations serve as the basis for the trophic classification of water bodies [9, 32, 33]. The data in Figure 7 show that during the 51 years of observation, the reservoir was characterized as mesotrophic 18 times (mean Chl less than 10 μg/L), as moderately eutrophic 15 times (10–15 μg/L), and as eutrophic 18 times (15–22 μg/L).
General level of phytoplankton development and the trends in its long-term variations are well illustrated by the occurrence rate of Chl concentrations (Figure 8). In the first 10 years of observations (1969–1979), mesotrophic waters with a pigment concentrations of less than 10 μg/L prevailed in the reservoir. In the 80s and 90s twentieth century the share of eutrophic waters with Chl content equal to 10–30 μg/L, increased significantly. At the same time, the upper limit of Chl values increased, reaching 100 μg/L and above. In the early 2000s there has been a trend towards a decrease in the level of trophy, and the histogram of Chl frequency distribution repeated that of the late 1970s. Data of 2010–2014 showed a sharp rise in values with an absolute (about 70% of the total number of observations) predominance of eutrophic and highly eutrophic waters. In recent years, with high water content and a decrease in temperature, mesotrophic type waters began to predominate again, and the amount of high Chl concentrations decreased to 40%.
Occurrence rate of chlorophyll in the Rybinsk reservoir in different periods of 1969–2019 according to [
Chlorophyll-a, the main pigment of the green plants, serves as a universal ecological and physiological marker of biomass, photosynthetic activity, and production capabilities of algae. The study of the most significant aspects of chlorophyll applications in freshwater ecology on the example of the Volga River reservoirs made it possible to consider the spatial and temporal dynamics of phytoplankton.
Route surveys carried out on seven run-of-river reservoirs of the Volga, revealed a wide range of Chl in each of them with minimum values of 2.5–9 μg/L to maximum values from 25 to 36 to over 100 μg/L. The average Chl values obtained in different years differed to a lesser extent with a significant distinction in case of the Uglich and Gorky reservoirs only. Chl concentrations obtained in 2015–2020 were typical of summer phytoplankton and generally fell within the same limits as 30 years ago (1989–1991). The distribution of phytoplankton over the water area of the reservoirs was non-uniform due to the large extent and complex morphometry of reservoirs, the presence of water masses of different genesis, the inflow of tributary waters, changes in the flow regime in different areas, and surge phenomena. The steady decrease in Chl content from the reservoirs of the Upper Volga to the reservoirs of the Lower Volga is due to an increase in flow velocity and volume of runoff downstream the Volga, as well as a decrease in the volume of lateral tributaries. According to the average concentrations of Chl over the past 6 years, currently the Ivankovo, Uglich, and Cheboksary reservoirs are eutrophic, the Saratov and Volgograd reservoirs are mesotrophic, while the trophic status of the Gorky and Kuibyshev reservoirs varies from mesotrophic to moderately eutrophic and eutrophic.
Regular seasonal observations during 2009–2019 carried out at lake-like Rybinsk reservoir showed that phytoplankton development during the open water period corresponds to the classical PEG model with a short spring Chl maximum, long period summer maximum, and, in some years, a short autumn rise. The timing of the onset of Chl maxima, their duration, quantity, and the ratio of values change depending on the conditions of the year. The long-term dynamics of Chl over a 50-year period since 1969 looks like a broken line with ups and downs, reflecting the community’s response to changing external conditions. Two main factors that are temperature and water regime have a significant impact on the long-term development of planktonic algae. Seasonally average Chl concentrations that serve as the basis for the trophic classification of water bodies show that, depending on environmental conditions, the trophic status of the Rybinsk reservoir varies from mesotrophic to eutrophic. In recent years, under the global warming, the rate of eutrophication has been increasing.
The study was carried as part of State Task АААА-А18-118012690096-1. The author is sincerely grateful to Tatiana Zaykina for sampling in the field.
The author declares no conflict of interest.
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\\n\\nThe Claremont Colleges are pledging funds via the Knowledge Unlatched program to ensure academics can publish Open Access content more easily.
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\\n\\nThe University of Massachusetts, Amherst is pledging funds via the Knowledge Unlatched program to ensure academics can publish Open Access content more easily.
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\\n\\nThe University of Surrey is pledging funds via the Knowledge Unlatched program to ensure academics can publish Open Access content more easily.
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\n\nThe University of Massachusetts, Amherst is pledging funds via the Knowledge Unlatched program to ensure academics can publish Open Access content more easily.
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\n\nThe University of Surrey is pledging funds via the Knowledge Unlatched program to ensure academics can publish Open Access content more easily.
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Using Salsa20/12 stream cipher, the texture images can be encrypted using bit masking and permutation procedures and as part of a new scheme for encrypting 3D objects, which complements the existing methods for 3D object encryption. 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