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CO2 emissions from karst cascade hydropower reservoirs: mechanisms and reservoir effect
Carbon dioxide (CO2) emissions from aquatic surface to the atmosphere has been recognized as a significant factor contributing to the global carbon budget and environmental change. The influence of river damming on the CO2 emissions from reservoirs remains poorly constrained. This is hypothetically...
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Published in: | Environmental research letters 2021-04, Vol.16 (4), p.044013 |
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creator | Wang, Wanfa Si-Liang, Li Zhong, Jun Wang, Lichun Yang, Hong Xiao, Huayun Cong-Qiang Liu |
description | Carbon dioxide (CO2) emissions from aquatic surface to the atmosphere has been recognized as a significant factor contributing to the global carbon budget and environmental change. The influence of river damming on the CO2 emissions from reservoirs remains poorly constrained. This is hypothetically due to the change of hydraulic retention time (HRT) and thermal stratification intensity of reservoirs (related to the normal water level, NWL). To test this hypothesis, we quantified CO2 fluxes and related parameters in eight karst reservoirs on the Wujiang River, Southwest China. Our results showed that there was a significant difference in the values of pCO2 (mean = 3205.7 μatm, SD = 2183.4 μatm) and δ 13CCO2 (mean = −18.9‰, SD = 1.6‰) in the cascade reservoirs, suggesting that multiple processes regulate CO2 production. Moreover, the calculated CO2 fluxes showed obvious spatiotemporal variations, ranging from −9.0 to 2269.3 mmol m−2 d−1, with an average of 260.1 mmol m−2 d−1. Interestingly, the CO2 flux and δ 13CCO2 from reservoirs of this study and other reservoirs around the world had an exponential function with the reservoir effect index (Ri , HRT/NWL), suggesting the viability of our hypothesis on reservoir CO2 emission. This empirical function will help to estimate CO2 emissions from global reservoirs and provide theoretical support for reservoir regulation to mitigate carbon emission. |
doi_str_mv | 10.1088/1748-9326/abe962 |
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The influence of river damming on the CO2 emissions from reservoirs remains poorly constrained. This is hypothetically due to the change of hydraulic retention time (HRT) and thermal stratification intensity of reservoirs (related to the normal water level, NWL). To test this hypothesis, we quantified CO2 fluxes and related parameters in eight karst reservoirs on the Wujiang River, Southwest China. Our results showed that there was a significant difference in the values of pCO2 (mean = 3205.7 μatm, SD = 2183.4 μatm) and δ 13CCO2 (mean = −18.9‰, SD = 1.6‰) in the cascade reservoirs, suggesting that multiple processes regulate CO2 production. Moreover, the calculated CO2 fluxes showed obvious spatiotemporal variations, ranging from −9.0 to 2269.3 mmol m−2 d−1, with an average of 260.1 mmol m−2 d−1. Interestingly, the CO2 flux and δ 13CCO2 from reservoirs of this study and other reservoirs around the world had an exponential function with the reservoir effect index (Ri , HRT/NWL), suggesting the viability of our hypothesis on reservoir CO2 emission. This empirical function will help to estimate CO2 emissions from global reservoirs and provide theoretical support for reservoir regulation to mitigate carbon emission.</description><identifier>EISSN: 1748-9326</identifier><identifier>DOI: 10.1088/1748-9326/abe962</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Carbon dioxide ; Carbon dioxide emissions ; cascade reservoirs ; CO2 emissions ; Environmental changes ; Exponential functions ; Fluxes ; Hydraulic retention time ; Hydroelectric power ; Hypotheses ; Karst ; Mathematical analysis ; reservoir effect index ; Reservoirs ; Retention time ; Rivers ; Thermal stratification ; Water levels ; Water stratification ; δ 13CCO2</subject><ispartof>Environmental research letters, 2021-04, Vol.16 (4), p.044013</ispartof><rights>2021. This work is published under http://creativecommons.org/licenses/by/4.0 (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0001-8835-9808</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.proquest.com/docview/2512940613?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,25751,27922,27923,37010,44588</link.rule.ids></links><search><creatorcontrib>Wang, Wanfa</creatorcontrib><creatorcontrib>Si-Liang, Li</creatorcontrib><creatorcontrib>Zhong, Jun</creatorcontrib><creatorcontrib>Wang, Lichun</creatorcontrib><creatorcontrib>Yang, Hong</creatorcontrib><creatorcontrib>Xiao, Huayun</creatorcontrib><creatorcontrib>Cong-Qiang Liu</creatorcontrib><title>CO2 emissions from karst cascade hydropower reservoirs: mechanisms and reservoir effect</title><title>Environmental research letters</title><description>Carbon dioxide (CO2) emissions from aquatic surface to the atmosphere has been recognized as a significant factor contributing to the global carbon budget and environmental change. The influence of river damming on the CO2 emissions from reservoirs remains poorly constrained. This is hypothetically due to the change of hydraulic retention time (HRT) and thermal stratification intensity of reservoirs (related to the normal water level, NWL). To test this hypothesis, we quantified CO2 fluxes and related parameters in eight karst reservoirs on the Wujiang River, Southwest China. Our results showed that there was a significant difference in the values of pCO2 (mean = 3205.7 μatm, SD = 2183.4 μatm) and δ 13CCO2 (mean = −18.9‰, SD = 1.6‰) in the cascade reservoirs, suggesting that multiple processes regulate CO2 production. Moreover, the calculated CO2 fluxes showed obvious spatiotemporal variations, ranging from −9.0 to 2269.3 mmol m−2 d−1, with an average of 260.1 mmol m−2 d−1. Interestingly, the CO2 flux and δ 13CCO2 from reservoirs of this study and other reservoirs around the world had an exponential function with the reservoir effect index (Ri , HRT/NWL), suggesting the viability of our hypothesis on reservoir CO2 emission. This empirical function will help to estimate CO2 emissions from global reservoirs and provide theoretical support for reservoir regulation to mitigate carbon emission.</description><subject>Carbon dioxide</subject><subject>Carbon dioxide emissions</subject><subject>cascade reservoirs</subject><subject>CO2 emissions</subject><subject>Environmental changes</subject><subject>Exponential functions</subject><subject>Fluxes</subject><subject>Hydraulic retention time</subject><subject>Hydroelectric power</subject><subject>Hypotheses</subject><subject>Karst</subject><subject>Mathematical analysis</subject><subject>reservoir effect index</subject><subject>Reservoirs</subject><subject>Retention time</subject><subject>Rivers</subject><subject>Thermal stratification</subject><subject>Water levels</subject><subject>Water stratification</subject><subject>δ 13CCO2</subject><issn>1748-9326</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpFjktLAzEURoMgWKt7lwHXY_OaTMadFB-FQjcFl-FOcmOndiY1mSr99w5WdPXB-eBwCLnh7I4zY2a8UqaopdAzaLDW4oxM_tAFucx5y1ipyspMyOt8JSh2bc5t7DMNKXb0HVIeqIPswCPdHH2K-_iFiSbMmD5jm_I97dBtoG9zlyn0_v-iGAK64YqcB9hlvP7dKVk_Pa7nL8Vy9byYPywLL7geiop7oVUoa2-0FyX3lfJMqgZq6dDzoJkLLATnOJTCqIZVspKsaaR2Kigmp2Rx0voIW7tPbQfpaCO09gfE9GYhDa3bofVO1g6VQ6MrhcHAaIPGiUaWTDPhR9ftybVP8eOAebDbeEj9WG_HMlErprmU327Ea94</recordid><startdate>20210401</startdate><enddate>20210401</enddate><creator>Wang, Wanfa</creator><creator>Si-Liang, Li</creator><creator>Zhong, Jun</creator><creator>Wang, Lichun</creator><creator>Yang, Hong</creator><creator>Xiao, Huayun</creator><creator>Cong-Qiang Liu</creator><general>IOP Publishing</general><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M7S</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0001-8835-9808</orcidid></search><sort><creationdate>20210401</creationdate><title>CO2 emissions from karst cascade hydropower reservoirs: mechanisms and reservoir effect</title><author>Wang, Wanfa ; Si-Liang, Li ; Zhong, Jun ; Wang, Lichun ; Yang, Hong ; Xiao, Huayun ; Cong-Qiang Liu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-d216t-71d264f59d86d251d74d034ba93ced1f60cf0ffcc1a5284b073730bb36c4f403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Carbon dioxide</topic><topic>Carbon dioxide emissions</topic><topic>cascade reservoirs</topic><topic>CO2 emissions</topic><topic>Environmental changes</topic><topic>Exponential functions</topic><topic>Fluxes</topic><topic>Hydraulic retention time</topic><topic>Hydroelectric power</topic><topic>Hypotheses</topic><topic>Karst</topic><topic>Mathematical analysis</topic><topic>reservoir effect index</topic><topic>Reservoirs</topic><topic>Retention time</topic><topic>Rivers</topic><topic>Thermal stratification</topic><topic>Water levels</topic><topic>Water stratification</topic><topic>δ 13CCO2</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Wanfa</creatorcontrib><creatorcontrib>Si-Liang, Li</creatorcontrib><creatorcontrib>Zhong, Jun</creatorcontrib><creatorcontrib>Wang, Lichun</creatorcontrib><creatorcontrib>Yang, Hong</creatorcontrib><creatorcontrib>Xiao, Huayun</creatorcontrib><creatorcontrib>Cong-Qiang Liu</creatorcontrib><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Engineering Collection</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content (ProQuest)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Environmental research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Wanfa</au><au>Si-Liang, Li</au><au>Zhong, Jun</au><au>Wang, Lichun</au><au>Yang, Hong</au><au>Xiao, Huayun</au><au>Cong-Qiang Liu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>CO2 emissions from karst cascade hydropower reservoirs: mechanisms and reservoir effect</atitle><jtitle>Environmental research letters</jtitle><date>2021-04-01</date><risdate>2021</risdate><volume>16</volume><issue>4</issue><spage>044013</spage><pages>044013-</pages><eissn>1748-9326</eissn><abstract>Carbon dioxide (CO2) emissions from aquatic surface to the atmosphere has been recognized as a significant factor contributing to the global carbon budget and environmental change. The influence of river damming on the CO2 emissions from reservoirs remains poorly constrained. This is hypothetically due to the change of hydraulic retention time (HRT) and thermal stratification intensity of reservoirs (related to the normal water level, NWL). To test this hypothesis, we quantified CO2 fluxes and related parameters in eight karst reservoirs on the Wujiang River, Southwest China. Our results showed that there was a significant difference in the values of pCO2 (mean = 3205.7 μatm, SD = 2183.4 μatm) and δ 13CCO2 (mean = −18.9‰, SD = 1.6‰) in the cascade reservoirs, suggesting that multiple processes regulate CO2 production. Moreover, the calculated CO2 fluxes showed obvious spatiotemporal variations, ranging from −9.0 to 2269.3 mmol m−2 d−1, with an average of 260.1 mmol m−2 d−1. Interestingly, the CO2 flux and δ 13CCO2 from reservoirs of this study and other reservoirs around the world had an exponential function with the reservoir effect index (Ri , HRT/NWL), suggesting the viability of our hypothesis on reservoir CO2 emission. This empirical function will help to estimate CO2 emissions from global reservoirs and provide theoretical support for reservoir regulation to mitigate carbon emission.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1748-9326/abe962</doi><orcidid>https://orcid.org/0000-0001-8835-9808</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Carbon dioxide Carbon dioxide emissions cascade reservoirs CO2 emissions Environmental changes Exponential functions Fluxes Hydraulic retention time Hydroelectric power Hypotheses Karst Mathematical analysis reservoir effect index Reservoirs Retention time Rivers Thermal stratification Water levels Water stratification δ 13CCO2 |
title | CO2 emissions from karst cascade hydropower reservoirs: mechanisms and reservoir effect |
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