The cumulative effects of cascade reservoirs control nitrogen and phosphorus flux: Base on biogeochemical processes
The reservoir serves as a water source, a flood control structure, a navigational aid, and also impacts the downstream ecosystem as well as the reservoir zone. However, debate exists about effectiveness of cascade reservoirs in controlling the transportation of nutrients, particularly in the Yangtze...
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creator | Li, Leifang Chen, Lei Chen, Shibo Zhang, Yuhan Xu, Yanzhe Zhi, Xiaosha Meng, Xinyi Shen, Zhenyao Liu, Yong Yang, Dawen Tang, Lihua |
description | The reservoir serves as a water source, a flood control structure, a navigational aid, and also impacts the downstream ecosystem as well as the reservoir zone. However, debate exists about effectiveness of cascade reservoirs in controlling the transportation of nutrients, particularly in the Yangtze River basin, which has been significantly affected by reservoir development. This research develops a new model X-NPSEM (X with Nitrogen and Phosphorus Steady-state Reservoir Model) based on biogeochemical processes of nitrogen and phosphorus reaction for investigating the dynamic storage capacity of cascade reservoirs at both reservoir- and watershed scales. Then the cumulative effects of cascade reservoirs and the related mechanism were investigated in Fujiang watershed, China. Based on the results, cascade reservoirs retained 16.3 % of nitrogen fluxes and 37.6 % of phosphorus fluxes annually. Downstream reservoirs have higher retention rates of phosphorus (0.48/d) compared to upstream reservoirs (0.10/d), mainly due to inflow sediment. Nitrogen retention rates show seasonal variations: wet season (0.21/d) and dry season (0.17/d). These fluctuations in nitrogen retention are primarily influenced by changes in temperature rather than other factors such as operation period, nitrogen and phosphorus concentration, or the nitrogen/phosphorus ratio. In upstream, the concentration of sediment entering the reservoir plays a decisive role in the transformation of P retention from sink to source. The X-NPSRM coupler model could be used for global reservoir operation and watershed management.
•New model was developed and could be with other models for simulating reservoir processes.•Cumulative effects of cascade reservoirs were quantified with higher downstream retention rates.•It was found that nitrogen retention rate in reservoir is higher in wet season than dry season.•A transition of phosphorus from being a sink to becoming a source exists in reservoir region.
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doi_str_mv | 10.1016/j.watres.2024.121177 |
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•New model was developed and could be with other models for simulating reservoir processes.•Cumulative effects of cascade reservoirs were quantified with higher downstream retention rates.•It was found that nitrogen retention rate in reservoir is higher in wet season than dry season.•A transition of phosphorus from being a sink to becoming a source exists in reservoir region.
[Display omitted]</description><identifier>ISSN: 0043-1354</identifier><identifier>EISSN: 1879-2448</identifier><identifier>DOI: 10.1016/j.watres.2024.121177</identifier><identifier>PMID: 38290240</identifier><language>eng</language><publisher>England: Elsevier Ltd</publisher><subject>Biogeochemical reaction processes ; Cascade reservoirs ; China ; Cumulative effects ; dry season ; Ecosystem ; ecosystems ; Environmental Monitoring ; flood control ; Nitrogen ; Nitrogen - analysis ; nitrogen retention ; Phosphorus ; Phosphorus - analysis ; Retention rate ; sediments ; temperature ; transportation ; water ; Water Pollutants, Chemical - analysis ; watershed management ; watersheds ; wet season ; Yangtze River</subject><ispartof>Water research (Oxford), 2024-03, Vol.252, p.121177-121177, Article 121177</ispartof><rights>2024 Elsevier Ltd</rights><rights>Copyright © 2024 Elsevier Ltd. All rights reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c344t-9fe7a0df1014d36edfe1bfa78b85e730ea20135743935162c8c0499c4e53d65d3</cites><orcidid>0000-0002-6620-1943 ; 0000-0001-8415-3896</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0043135424000770$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/38290240$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Li, Leifang</creatorcontrib><creatorcontrib>Chen, Lei</creatorcontrib><creatorcontrib>Chen, Shibo</creatorcontrib><creatorcontrib>Zhang, Yuhan</creatorcontrib><creatorcontrib>Xu, Yanzhe</creatorcontrib><creatorcontrib>Zhi, Xiaosha</creatorcontrib><creatorcontrib>Meng, Xinyi</creatorcontrib><creatorcontrib>Shen, Zhenyao</creatorcontrib><creatorcontrib>Liu, Yong</creatorcontrib><creatorcontrib>Yang, Dawen</creatorcontrib><creatorcontrib>Tang, Lihua</creatorcontrib><title>The cumulative effects of cascade reservoirs control nitrogen and phosphorus flux: Base on biogeochemical processes</title><title>Water research (Oxford)</title><addtitle>Water Res</addtitle><description>The reservoir serves as a water source, a flood control structure, a navigational aid, and also impacts the downstream ecosystem as well as the reservoir zone. However, debate exists about effectiveness of cascade reservoirs in controlling the transportation of nutrients, particularly in the Yangtze River basin, which has been significantly affected by reservoir development. This research develops a new model X-NPSEM (X with Nitrogen and Phosphorus Steady-state Reservoir Model) based on biogeochemical processes of nitrogen and phosphorus reaction for investigating the dynamic storage capacity of cascade reservoirs at both reservoir- and watershed scales. Then the cumulative effects of cascade reservoirs and the related mechanism were investigated in Fujiang watershed, China. Based on the results, cascade reservoirs retained 16.3 % of nitrogen fluxes and 37.6 % of phosphorus fluxes annually. Downstream reservoirs have higher retention rates of phosphorus (0.48/d) compared to upstream reservoirs (0.10/d), mainly due to inflow sediment. Nitrogen retention rates show seasonal variations: wet season (0.21/d) and dry season (0.17/d). These fluctuations in nitrogen retention are primarily influenced by changes in temperature rather than other factors such as operation period, nitrogen and phosphorus concentration, or the nitrogen/phosphorus ratio. In upstream, the concentration of sediment entering the reservoir plays a decisive role in the transformation of P retention from sink to source. The X-NPSRM coupler model could be used for global reservoir operation and watershed management.
•New model was developed and could be with other models for simulating reservoir processes.•Cumulative effects of cascade reservoirs were quantified with higher downstream retention rates.•It was found that nitrogen retention rate in reservoir is higher in wet season than dry season.•A transition of phosphorus from being a sink to becoming a source exists in reservoir region.
[Display omitted]</description><subject>Biogeochemical reaction processes</subject><subject>Cascade reservoirs</subject><subject>China</subject><subject>Cumulative effects</subject><subject>dry season</subject><subject>Ecosystem</subject><subject>ecosystems</subject><subject>Environmental Monitoring</subject><subject>flood control</subject><subject>Nitrogen</subject><subject>Nitrogen - analysis</subject><subject>nitrogen retention</subject><subject>Phosphorus</subject><subject>Phosphorus - analysis</subject><subject>Retention rate</subject><subject>sediments</subject><subject>temperature</subject><subject>transportation</subject><subject>water</subject><subject>Water Pollutants, Chemical - analysis</subject><subject>watershed management</subject><subject>watersheds</subject><subject>wet season</subject><subject>Yangtze River</subject><issn>0043-1354</issn><issn>1879-2448</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqFkc1O3DAURi1UBFPgDarKy24y9V_ipItKLaKAhMQG1pbHvu54lMRT32Ra3h6j0C7Lwrqb8_nz9SHkA2drznjzebf-bacMuBZMqDUXnGt9RFa81V0llGrfkRVjSlZc1uqUvEfcMcaEkN0JOZWt6EqKrQg-bIG6eZh7O8UDUAgB3IQ0BeosOuuBlg7IhxQzUpfGKaeejrGMnzBSO3q63yYsJ89IQz__-UK_WwSaRrqJhUluC0N0tqf7nBwgAp6T42B7hIvXeUYef1w9XN5Ud_fXt5ff7ionlZqqLoC2zIeyrfKyAR-Ab4LV7aatQUsGVrCynFaykzVvhGsdU13nFNTSN7WXZ-TTcm9p_jUDTmaI6KDv7QhpRiN5LRvOtBZvoqITrNblJXVB1YK6nBAzBLPPcbD5yXBmXsyYnVnMmBczZjFTYh9fG-bNAP5f6K-KAnxdAChfcoiQDboIowMfc1FifIr_b3gGJK6ifg</recordid><startdate>20240315</startdate><enddate>20240315</enddate><creator>Li, Leifang</creator><creator>Chen, Lei</creator><creator>Chen, Shibo</creator><creator>Zhang, Yuhan</creator><creator>Xu, Yanzhe</creator><creator>Zhi, Xiaosha</creator><creator>Meng, Xinyi</creator><creator>Shen, Zhenyao</creator><creator>Liu, Yong</creator><creator>Yang, Dawen</creator><creator>Tang, Lihua</creator><general>Elsevier Ltd</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>7S9</scope><scope>L.6</scope><orcidid>https://orcid.org/0000-0002-6620-1943</orcidid><orcidid>https://orcid.org/0000-0001-8415-3896</orcidid></search><sort><creationdate>20240315</creationdate><title>The cumulative effects of cascade reservoirs control nitrogen and phosphorus flux: Base on biogeochemical processes</title><author>Li, Leifang ; Chen, Lei ; Chen, Shibo ; Zhang, Yuhan ; Xu, Yanzhe ; Zhi, Xiaosha ; Meng, Xinyi ; Shen, Zhenyao ; Liu, Yong ; Yang, Dawen ; Tang, Lihua</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c344t-9fe7a0df1014d36edfe1bfa78b85e730ea20135743935162c8c0499c4e53d65d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Biogeochemical reaction processes</topic><topic>Cascade reservoirs</topic><topic>China</topic><topic>Cumulative effects</topic><topic>dry season</topic><topic>Ecosystem</topic><topic>ecosystems</topic><topic>Environmental Monitoring</topic><topic>flood control</topic><topic>Nitrogen</topic><topic>Nitrogen - analysis</topic><topic>nitrogen retention</topic><topic>Phosphorus</topic><topic>Phosphorus - analysis</topic><topic>Retention rate</topic><topic>sediments</topic><topic>temperature</topic><topic>transportation</topic><topic>water</topic><topic>Water Pollutants, Chemical - analysis</topic><topic>watershed management</topic><topic>watersheds</topic><topic>wet season</topic><topic>Yangtze River</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Leifang</creatorcontrib><creatorcontrib>Chen, Lei</creatorcontrib><creatorcontrib>Chen, Shibo</creatorcontrib><creatorcontrib>Zhang, Yuhan</creatorcontrib><creatorcontrib>Xu, Yanzhe</creatorcontrib><creatorcontrib>Zhi, Xiaosha</creatorcontrib><creatorcontrib>Meng, Xinyi</creatorcontrib><creatorcontrib>Shen, Zhenyao</creatorcontrib><creatorcontrib>Liu, Yong</creatorcontrib><creatorcontrib>Yang, Dawen</creatorcontrib><creatorcontrib>Tang, Lihua</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Water research (Oxford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Leifang</au><au>Chen, Lei</au><au>Chen, Shibo</au><au>Zhang, Yuhan</au><au>Xu, Yanzhe</au><au>Zhi, Xiaosha</au><au>Meng, Xinyi</au><au>Shen, Zhenyao</au><au>Liu, Yong</au><au>Yang, Dawen</au><au>Tang, Lihua</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The cumulative effects of cascade reservoirs control nitrogen and phosphorus flux: Base on biogeochemical processes</atitle><jtitle>Water research (Oxford)</jtitle><addtitle>Water Res</addtitle><date>2024-03-15</date><risdate>2024</risdate><volume>252</volume><spage>121177</spage><epage>121177</epage><pages>121177-121177</pages><artnum>121177</artnum><issn>0043-1354</issn><eissn>1879-2448</eissn><abstract>The reservoir serves as a water source, a flood control structure, a navigational aid, and also impacts the downstream ecosystem as well as the reservoir zone. However, debate exists about effectiveness of cascade reservoirs in controlling the transportation of nutrients, particularly in the Yangtze River basin, which has been significantly affected by reservoir development. This research develops a new model X-NPSEM (X with Nitrogen and Phosphorus Steady-state Reservoir Model) based on biogeochemical processes of nitrogen and phosphorus reaction for investigating the dynamic storage capacity of cascade reservoirs at both reservoir- and watershed scales. Then the cumulative effects of cascade reservoirs and the related mechanism were investigated in Fujiang watershed, China. Based on the results, cascade reservoirs retained 16.3 % of nitrogen fluxes and 37.6 % of phosphorus fluxes annually. Downstream reservoirs have higher retention rates of phosphorus (0.48/d) compared to upstream reservoirs (0.10/d), mainly due to inflow sediment. Nitrogen retention rates show seasonal variations: wet season (0.21/d) and dry season (0.17/d). These fluctuations in nitrogen retention are primarily influenced by changes in temperature rather than other factors such as operation period, nitrogen and phosphorus concentration, or the nitrogen/phosphorus ratio. In upstream, the concentration of sediment entering the reservoir plays a decisive role in the transformation of P retention from sink to source. The X-NPSRM coupler model could be used for global reservoir operation and watershed management.
•New model was developed and could be with other models for simulating reservoir processes.•Cumulative effects of cascade reservoirs were quantified with higher downstream retention rates.•It was found that nitrogen retention rate in reservoir is higher in wet season than dry season.•A transition of phosphorus from being a sink to becoming a source exists in reservoir region.
[Display omitted]</abstract><cop>England</cop><pub>Elsevier Ltd</pub><pmid>38290240</pmid><doi>10.1016/j.watres.2024.121177</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-6620-1943</orcidid><orcidid>https://orcid.org/0000-0001-8415-3896</orcidid></addata></record> |
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subjects | Biogeochemical reaction processes Cascade reservoirs China Cumulative effects dry season Ecosystem ecosystems Environmental Monitoring flood control Nitrogen Nitrogen - analysis nitrogen retention Phosphorus Phosphorus - analysis Retention rate sediments temperature transportation water Water Pollutants, Chemical - analysis watershed management watersheds wet season Yangtze River |
title | The cumulative effects of cascade reservoirs control nitrogen and phosphorus flux: Base on biogeochemical processes |
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