Variation of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming
To investigate the variation of the biogeochemical cycle of riverine dissolved inorganic carbon (DIC) and silicon (DSi) with the cascade damming, the bicarbonate ( HCO 3 − ), dissolved silicon (DSi), and other environmental factors within the cascade reservoirs of the lower reaches of Yalongjiang Ri...
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| creator | Deng, Haojun Tao, Zhen Gao, Quanzhou Yao, Ling Feng, Yong Li, Yinhua Ding, Jian Wang, Zhengang Lyu, Xiaoxi Xu, Peng |
| description | To investigate the variation of the biogeochemical cycle of riverine dissolved inorganic carbon (DIC) and silicon (DSi) with the cascade damming, the bicarbonate (
HCO
3
−
), dissolved silicon (DSi), and other environmental factors within the cascade reservoirs of the lower reaches of Yalongjiang River, passing through the southeastern Qinghai-Tibet Plateau, were systematically analyzed by collecting water samples during the wet season and dry season from 2018 to 2019, respectively. The results showed that the lower ratio of DSi to
HCO
3
–
(0.044 ± 0.001) was mainly controlled by the domination of carbonate mineral in the sedimentary rock of the Yalongjiang River drainage basin. The DSi:
HCO
3
–
ratio was positively correlated with discharge (
P
|
| doi_str_mv | 10.1007/s11356-020-09174-5 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_2404381730</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2404381730</sourcerecordid><originalsourceid>FETCH-LOGICAL-c412t-4d0969686b652fdaf3d4be17d10a80ad804852facb44d7473478651db74c69123</originalsourceid><addsrcrecordid>eNp9kUtPxCAUhYnR6Pj4Ay5MEzduqjxuoSyN8ZWYuFG3hAKdwbSg0NH470XHR-LCFYTznXPJPQjtE3xMMBYnmRDW8BpTXGNJBNTNGpoRTqAWIOU6mmEJUBMGsIW2c37EhZRUbKItRoG0WMoZGh908nryMVSxrzof5y6ahRu90UNl3szgPt6Tf3HJB1dZn3McXpytfIhproM3ldGpK3YdbJX94E25v_ppUU0LV7RstC0-PY4-zHfRRq-H7Pa-zh10f3F-d3ZV39xeXp-d3tQGCJ1qsFhyyVve8Yb2VvfMQueIsATrFmvbYmiLoE0HYAUIBqLlDbGdAMMloWwHHa1yn1J8Xro8qdFn44ZBBxeXWVHAwFoiGC7o4R_0MS5TKL8rFG2kbLhkhaIryqSYc3K9ekp-1OlNEaw-ylCrMlRZsfosQzXFdPAVvexGZ38s39svAFsBuUhh7tLv7H9i3wFc6JS_</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2425995693</pqid></control><display><type>article</type><title>Variation of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming</title><source>SpringerLink Journals - AutoHoldings</source><creator>Deng, Haojun ; Tao, Zhen ; Gao, Quanzhou ; Yao, Ling ; Feng, Yong ; Li, Yinhua ; Ding, Jian ; Wang, Zhengang ; Lyu, Xiaoxi ; Xu, Peng</creator><creatorcontrib>Deng, Haojun ; Tao, Zhen ; Gao, Quanzhou ; Yao, Ling ; Feng, Yong ; Li, Yinhua ; Ding, Jian ; Wang, Zhengang ; Lyu, Xiaoxi ; Xu, Peng</creatorcontrib><description>To investigate the variation of the biogeochemical cycle of riverine dissolved inorganic carbon (DIC) and silicon (DSi) with the cascade damming, the bicarbonate (
HCO
3
−
), dissolved silicon (DSi), and other environmental factors within the cascade reservoirs of the lower reaches of Yalongjiang River, passing through the southeastern Qinghai-Tibet Plateau, were systematically analyzed by collecting water samples during the wet season and dry season from 2018 to 2019, respectively. The results showed that the lower ratio of DSi to
HCO
3
–
(0.044 ± 0.001) was mainly controlled by the domination of carbonate mineral in the sedimentary rock of the Yalongjiang River drainage basin. The DSi:
HCO
3
–
ratio was positively correlated with discharge (
P
< 0.05), and negatively correlated with the water retention time (
P
< 0.01) and chlorophyll a, implying that the variations of DSi:
HCO
3
–
ratio were mainly determined by the rock chemical weathering processes and the hydrologic process outside the reservoirs and the biological processes within the cascade reservoirs. The phytoplankton photosynthetic process stoichiometrically assimilated DSi and
HCO
3
–
, resulted in 3.46 × 10
4
t·Si a
−1
and 1.89 × 10
4
t·C a
−1
sequestering in the cascade reservoirs, respectively. Compared with the situation of dam-free in the lower reaches of Yalongjiang River, the export flux of
HCO
3
−
and DSi at the mouth of Yalongjiang River was reduced by 11.87% and 62.50%, respectively; the ratio of DSi:
HCO
3
–
decreased by 36.01% for only building the Ertan dam and 53.15% for the cascade damming, respectively. The water renewal time prolonged from 45 to 126.6 days due to the regulation of the cascade reservoirs in the mainstream. Ultimately, a conceptual model on migration-transformation of DIC and DSi within the cascade reservoirs in the lower reaches of Yalongjiang River was established. These findings demonstrated that riverine cascade damming could extend the biogeochemical coupling cycle of DIC and DSi within the inland aquatic ecosystems and ensure the ecological environment security in the hot-dry valley.</description><identifier>ISSN: 0944-1344</identifier><identifier>EISSN: 1614-7499</identifier><identifier>DOI: 10.1007/s11356-020-09174-5</identifier><identifier>PMID: 32418099</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aquatic ecosystems ; Aquatic Pollution ; Atmospheric Protection/Air Quality Control/Air Pollution ; Bicarbonates ; Biogeochemical cycles ; Biogeochemistry ; Biological activity ; Carbon ; Chlorophyll ; Dam construction ; Dams ; Dissolved inorganic carbon ; Drainage basins ; Dry season ; Earth and Environmental Science ; Ecotoxicology ; Environment ; Environmental Chemistry ; Environmental factors ; Environmental Health ; Environmental science ; Hydrology ; Photosynthesis ; Phytoplankton ; Rainy season ; Research Article ; Reservoirs ; Retention time ; River basins ; Rivers ; Sedimentary rocks ; Sequestering ; Silicon ; Variation ; Waste Water Technology ; Water analysis ; Water Management ; Water Pollution Control ; Water sampling</subject><ispartof>Environmental science and pollution research international, 2020-08, Vol.27 (23), p.28840-28852</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-4d0969686b652fdaf3d4be17d10a80ad804852facb44d7473478651db74c69123</citedby><cites>FETCH-LOGICAL-c412t-4d0969686b652fdaf3d4be17d10a80ad804852facb44d7473478651db74c69123</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11356-020-09174-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11356-020-09174-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32418099$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Deng, Haojun</creatorcontrib><creatorcontrib>Tao, Zhen</creatorcontrib><creatorcontrib>Gao, Quanzhou</creatorcontrib><creatorcontrib>Yao, Ling</creatorcontrib><creatorcontrib>Feng, Yong</creatorcontrib><creatorcontrib>Li, Yinhua</creatorcontrib><creatorcontrib>Ding, Jian</creatorcontrib><creatorcontrib>Wang, Zhengang</creatorcontrib><creatorcontrib>Lyu, Xiaoxi</creatorcontrib><creatorcontrib>Xu, Peng</creatorcontrib><title>Variation of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming</title><title>Environmental science and pollution research international</title><addtitle>Environ Sci Pollut Res</addtitle><addtitle>Environ Sci Pollut Res Int</addtitle><description>To investigate the variation of the biogeochemical cycle of riverine dissolved inorganic carbon (DIC) and silicon (DSi) with the cascade damming, the bicarbonate (
HCO
3
−
), dissolved silicon (DSi), and other environmental factors within the cascade reservoirs of the lower reaches of Yalongjiang River, passing through the southeastern Qinghai-Tibet Plateau, were systematically analyzed by collecting water samples during the wet season and dry season from 2018 to 2019, respectively. The results showed that the lower ratio of DSi to
HCO
3
–
(0.044 ± 0.001) was mainly controlled by the domination of carbonate mineral in the sedimentary rock of the Yalongjiang River drainage basin. The DSi:
HCO
3
–
ratio was positively correlated with discharge (
P
< 0.05), and negatively correlated with the water retention time (
P
< 0.01) and chlorophyll a, implying that the variations of DSi:
HCO
3
–
ratio were mainly determined by the rock chemical weathering processes and the hydrologic process outside the reservoirs and the biological processes within the cascade reservoirs. The phytoplankton photosynthetic process stoichiometrically assimilated DSi and
HCO
3
–
, resulted in 3.46 × 10
4
t·Si a
−1
and 1.89 × 10
4
t·C a
−1
sequestering in the cascade reservoirs, respectively. Compared with the situation of dam-free in the lower reaches of Yalongjiang River, the export flux of
HCO
3
−
and DSi at the mouth of Yalongjiang River was reduced by 11.87% and 62.50%, respectively; the ratio of DSi:
HCO
3
–
decreased by 36.01% for only building the Ertan dam and 53.15% for the cascade damming, respectively. The water renewal time prolonged from 45 to 126.6 days due to the regulation of the cascade reservoirs in the mainstream. Ultimately, a conceptual model on migration-transformation of DIC and DSi within the cascade reservoirs in the lower reaches of Yalongjiang River was established. These findings demonstrated that riverine cascade damming could extend the biogeochemical coupling cycle of DIC and DSi within the inland aquatic ecosystems and ensure the ecological environment security in the hot-dry valley.</description><subject>Aquatic ecosystems</subject><subject>Aquatic Pollution</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Bicarbonates</subject><subject>Biogeochemical cycles</subject><subject>Biogeochemistry</subject><subject>Biological activity</subject><subject>Carbon</subject><subject>Chlorophyll</subject><subject>Dam construction</subject><subject>Dams</subject><subject>Dissolved inorganic carbon</subject><subject>Drainage basins</subject><subject>Dry season</subject><subject>Earth and Environmental Science</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental factors</subject><subject>Environmental Health</subject><subject>Environmental science</subject><subject>Hydrology</subject><subject>Photosynthesis</subject><subject>Phytoplankton</subject><subject>Rainy season</subject><subject>Research Article</subject><subject>Reservoirs</subject><subject>Retention time</subject><subject>River basins</subject><subject>Rivers</subject><subject>Sedimentary rocks</subject><subject>Sequestering</subject><subject>Silicon</subject><subject>Variation</subject><subject>Waste Water Technology</subject><subject>Water analysis</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>Water sampling</subject><issn>0944-1344</issn><issn>1614-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kUtPxCAUhYnR6Pj4Ay5MEzduqjxuoSyN8ZWYuFG3hAKdwbSg0NH470XHR-LCFYTznXPJPQjtE3xMMBYnmRDW8BpTXGNJBNTNGpoRTqAWIOU6mmEJUBMGsIW2c37EhZRUbKItRoG0WMoZGh908nryMVSxrzof5y6ahRu90UNl3szgPt6Tf3HJB1dZn3McXpytfIhproM3ldGpK3YdbJX94E25v_ppUU0LV7RstC0-PY4-zHfRRq-H7Pa-zh10f3F-d3ZV39xeXp-d3tQGCJ1qsFhyyVve8Yb2VvfMQueIsATrFmvbYmiLoE0HYAUIBqLlDbGdAMMloWwHHa1yn1J8Xro8qdFn44ZBBxeXWVHAwFoiGC7o4R_0MS5TKL8rFG2kbLhkhaIryqSYc3K9ekp-1OlNEaw-ylCrMlRZsfosQzXFdPAVvexGZ38s39svAFsBuUhh7tLv7H9i3wFc6JS_</recordid><startdate>20200801</startdate><enddate>20200801</enddate><creator>Deng, Haojun</creator><creator>Tao, Zhen</creator><creator>Gao, 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of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming</title><author>Deng, Haojun ; Tao, Zhen ; Gao, Quanzhou ; Yao, Ling ; Feng, Yong ; Li, Yinhua ; Ding, Jian ; Wang, Zhengang ; Lyu, Xiaoxi ; Xu, Peng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c412t-4d0969686b652fdaf3d4be17d10a80ad804852facb44d7473478651db74c69123</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Aquatic ecosystems</topic><topic>Aquatic Pollution</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Bicarbonates</topic><topic>Biogeochemical cycles</topic><topic>Biogeochemistry</topic><topic>Biological activity</topic><topic>Carbon</topic><topic>Chlorophyll</topic><topic>Dam construction</topic><topic>Dams</topic><topic>Dissolved inorganic carbon</topic><topic>Drainage basins</topic><topic>Dry season</topic><topic>Earth and Environmental Science</topic><topic>Ecotoxicology</topic><topic>Environment</topic><topic>Environmental Chemistry</topic><topic>Environmental factors</topic><topic>Environmental Health</topic><topic>Environmental science</topic><topic>Hydrology</topic><topic>Photosynthesis</topic><topic>Phytoplankton</topic><topic>Rainy season</topic><topic>Research Article</topic><topic>Reservoirs</topic><topic>Retention time</topic><topic>River basins</topic><topic>Rivers</topic><topic>Sedimentary rocks</topic><topic>Sequestering</topic><topic>Silicon</topic><topic>Variation</topic><topic>Waste Water Technology</topic><topic>Water analysis</topic><topic>Water Management</topic><topic>Water Pollution Control</topic><topic>Water sampling</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Deng, Haojun</creatorcontrib><creatorcontrib>Tao, Zhen</creatorcontrib><creatorcontrib>Gao, Quanzhou</creatorcontrib><creatorcontrib>Yao, 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Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>ProQuest One Business</collection><collection>ProQuest One Business (Alumni)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>MEDLINE - Academic</collection><jtitle>Environmental science and pollution research international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Deng, Haojun</au><au>Tao, Zhen</au><au>Gao, Quanzhou</au><au>Yao, Ling</au><au>Feng, Yong</au><au>Li, Yinhua</au><au>Ding, Jian</au><au>Wang, Zhengang</au><au>Lyu, Xiaoxi</au><au>Xu, Peng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Variation of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming</atitle><jtitle>Environmental science and pollution research international</jtitle><stitle>Environ Sci Pollut Res</stitle><addtitle>Environ Sci Pollut Res Int</addtitle><date>2020-08-01</date><risdate>2020</risdate><volume>27</volume><issue>23</issue><spage>28840</spage><epage>28852</epage><pages>28840-28852</pages><issn>0944-1344</issn><eissn>1614-7499</eissn><abstract>To investigate the variation of the biogeochemical cycle of riverine dissolved inorganic carbon (DIC) and silicon (DSi) with the cascade damming, the bicarbonate (
HCO
3
−
), dissolved silicon (DSi), and other environmental factors within the cascade reservoirs of the lower reaches of Yalongjiang River, passing through the southeastern Qinghai-Tibet Plateau, were systematically analyzed by collecting water samples during the wet season and dry season from 2018 to 2019, respectively. The results showed that the lower ratio of DSi to
HCO
3
–
(0.044 ± 0.001) was mainly controlled by the domination of carbonate mineral in the sedimentary rock of the Yalongjiang River drainage basin. The DSi:
HCO
3
–
ratio was positively correlated with discharge (
P
< 0.05), and negatively correlated with the water retention time (
P
< 0.01) and chlorophyll a, implying that the variations of DSi:
HCO
3
–
ratio were mainly determined by the rock chemical weathering processes and the hydrologic process outside the reservoirs and the biological processes within the cascade reservoirs. The phytoplankton photosynthetic process stoichiometrically assimilated DSi and
HCO
3
–
, resulted in 3.46 × 10
4
t·Si a
−1
and 1.89 × 10
4
t·C a
−1
sequestering in the cascade reservoirs, respectively. Compared with the situation of dam-free in the lower reaches of Yalongjiang River, the export flux of
HCO
3
−
and DSi at the mouth of Yalongjiang River was reduced by 11.87% and 62.50%, respectively; the ratio of DSi:
HCO
3
–
decreased by 36.01% for only building the Ertan dam and 53.15% for the cascade damming, respectively. The water renewal time prolonged from 45 to 126.6 days due to the regulation of the cascade reservoirs in the mainstream. Ultimately, a conceptual model on migration-transformation of DIC and DSi within the cascade reservoirs in the lower reaches of Yalongjiang River was established. These findings demonstrated that riverine cascade damming could extend the biogeochemical coupling cycle of DIC and DSi within the inland aquatic ecosystems and ensure the ecological environment security in the hot-dry valley.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><pmid>32418099</pmid><doi>10.1007/s11356-020-09174-5</doi><tpages>13</tpages></addata></record> |
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| ispartof | Environmental science and pollution research international, 2020-08, Vol.27 (23), p.28840-28852 |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | Aquatic ecosystems Aquatic Pollution Atmospheric Protection/Air Quality Control/Air Pollution Bicarbonates Biogeochemical cycles Biogeochemistry Biological activity Carbon Chlorophyll Dam construction Dams Dissolved inorganic carbon Drainage basins Dry season Earth and Environmental Science Ecotoxicology Environment Environmental Chemistry Environmental factors Environmental Health Environmental science Hydrology Photosynthesis Phytoplankton Rainy season Research Article Reservoirs Retention time River basins Rivers Sedimentary rocks Sequestering Silicon Variation Waste Water Technology Water analysis Water Management Water Pollution Control Water sampling |
| title | Variation of biogeochemical cycle of riverine dissolved inorganic carbon and silicon with the cascade damming |
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