Major element chemistry of the Changjiang (Yangtze River)
The chemistry of major elements (Ca, Mg, Na, K, HCO3, SO4, Cl, and Si) in the river water of the Changjiang (Yangtze River) was studied, based on continuously monitored data at 191 stations in the drainage basin for the period 1958-1990. The results show that the total dissolved solid (TDS) concentr...
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化工地质
2002
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Online Access: | https://hdl.handle.net/20.500.11897/208746 https://doi.org/10.1016/S0009-2541(02)00032-3 |
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ftpekinguniv:oai:localhost:20.500.11897/208746 2023-05-15T17:07:40+02:00 Major element chemistry of the Changjiang (Yangtze River) Chen, JS Wang, FY Xia, XH Zhang, LT Wang, FY (reprint author), Univ Manitoba, Environm Sci Program, Winnipeg, MB R3T 2N2, Canada. Univ Manitoba, Environm Sci Program, Winnipeg, MB R3T 2N2, Canada. Univ Manitoba, Dept Chem, Winnipeg, MB R3T 2N2, Canada. Peking Univ, Dept Geog, Beijing 100871, Peoples R China. 2002 https://hdl.handle.net/20.500.11897/208746 https://doi.org/10.1016/S0009-2541(02)00032-3 en eng 化工地质 CHEMICAL GEOLOGY.2002,187,(3-4),231-255. 762527 0009-2541 http://hdl.handle.net/20.500.11897/208746 doi:10.1016/S0009-2541(02)00032-3 WOS:000177462500004 SCI Changjiang Yangtze River geochemistry major ion chemistry weathering acid deposition FLUVIAL GEOCHEMISTRY WEATHERING PROCESSES WATER CHEMISTRY EASTERN SIBERIA DISSOLVED-LOAD ION CHEMISTRY LENA RIVER AMAZON CHINA TRIBUTARIES Journal 2002 ftpekinguniv https://doi.org/20.500.11897/208746 https://doi.org/10.1016/S0009-2541(02)00032-3 2021-08-01T08:31:36Z The chemistry of major elements (Ca, Mg, Na, K, HCO3, SO4, Cl, and Si) in the river water of the Changjiang (Yangtze River) was studied, based on continuously monitored data at 191 stations in the drainage basin for the period 1958-1990. The results show that the total dissolved solid (TDS) concentration of the Changjiang varies over an order of magnitude throughout the basin (49.7-518.1 mg/l), with a medium TDS concentration of 205.9 mg/l, about three times the global average. In contrast, the TDS at a given main-channel station varies only slightly in different seasons with a variation factor less than 2.0, despite a substantial water dilution in the summer flood season. The major element chemistry of the Changjiang is mainly controlled by rock weathering, with the anion HCO3 and the cation Ca dominating the major ion composition, due to the abundance of carbonate rocks in the basin. A persistently increasing trend has been observed in the concentrations Of SO4 and, to a lesser extent, Cl in the Changjiang, a signature of considerable anthropogenic impacts (e.g., acid deposition). Flux calculations at Datong (the most downstream main-channel station without tidal influence) indicate that the Changjiang transports ca. 154 x 10(6) tons/year of TDS to the sea, second only to the Amazon in the world. (C) 2002 Elsevier Science B.V. All rights reserved. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000177462500004&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geochemistry & Geophysics SCI(E) 132 ARTICLE 3-4 231-255 187 Journal/Newspaper lena river Siberia Peking University Institutional Repository (PKU IR) Chemical Geology 187 3-4 231 255 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
Changjiang Yangtze River geochemistry major ion chemistry weathering acid deposition FLUVIAL GEOCHEMISTRY WEATHERING PROCESSES WATER CHEMISTRY EASTERN SIBERIA DISSOLVED-LOAD ION CHEMISTRY LENA RIVER AMAZON CHINA TRIBUTARIES |
spellingShingle |
Changjiang Yangtze River geochemistry major ion chemistry weathering acid deposition FLUVIAL GEOCHEMISTRY WEATHERING PROCESSES WATER CHEMISTRY EASTERN SIBERIA DISSOLVED-LOAD ION CHEMISTRY LENA RIVER AMAZON CHINA TRIBUTARIES Chen, JS Wang, FY Xia, XH Zhang, LT Major element chemistry of the Changjiang (Yangtze River) |
topic_facet |
Changjiang Yangtze River geochemistry major ion chemistry weathering acid deposition FLUVIAL GEOCHEMISTRY WEATHERING PROCESSES WATER CHEMISTRY EASTERN SIBERIA DISSOLVED-LOAD ION CHEMISTRY LENA RIVER AMAZON CHINA TRIBUTARIES |
description |
The chemistry of major elements (Ca, Mg, Na, K, HCO3, SO4, Cl, and Si) in the river water of the Changjiang (Yangtze River) was studied, based on continuously monitored data at 191 stations in the drainage basin for the period 1958-1990. The results show that the total dissolved solid (TDS) concentration of the Changjiang varies over an order of magnitude throughout the basin (49.7-518.1 mg/l), with a medium TDS concentration of 205.9 mg/l, about three times the global average. In contrast, the TDS at a given main-channel station varies only slightly in different seasons with a variation factor less than 2.0, despite a substantial water dilution in the summer flood season. The major element chemistry of the Changjiang is mainly controlled by rock weathering, with the anion HCO3 and the cation Ca dominating the major ion composition, due to the abundance of carbonate rocks in the basin. A persistently increasing trend has been observed in the concentrations Of SO4 and, to a lesser extent, Cl in the Changjiang, a signature of considerable anthropogenic impacts (e.g., acid deposition). Flux calculations at Datong (the most downstream main-channel station without tidal influence) indicate that the Changjiang transports ca. 154 x 10(6) tons/year of TDS to the sea, second only to the Amazon in the world. (C) 2002 Elsevier Science B.V. All rights reserved. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000177462500004&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geochemistry & Geophysics SCI(E) 132 ARTICLE 3-4 231-255 187 |
author2 |
Wang, FY (reprint author), Univ Manitoba, Environm Sci Program, Winnipeg, MB R3T 2N2, Canada. Univ Manitoba, Environm Sci Program, Winnipeg, MB R3T 2N2, Canada. Univ Manitoba, Dept Chem, Winnipeg, MB R3T 2N2, Canada. Peking Univ, Dept Geog, Beijing 100871, Peoples R China. |
format |
Journal/Newspaper |
author |
Chen, JS Wang, FY Xia, XH Zhang, LT |
author_facet |
Chen, JS Wang, FY Xia, XH Zhang, LT |
author_sort |
Chen, JS |
title |
Major element chemistry of the Changjiang (Yangtze River) |
title_short |
Major element chemistry of the Changjiang (Yangtze River) |
title_full |
Major element chemistry of the Changjiang (Yangtze River) |
title_fullStr |
Major element chemistry of the Changjiang (Yangtze River) |
title_full_unstemmed |
Major element chemistry of the Changjiang (Yangtze River) |
title_sort |
major element chemistry of the changjiang (yangtze river) |
publisher |
化工地质 |
publishDate |
2002 |
url |
https://hdl.handle.net/20.500.11897/208746 https://doi.org/10.1016/S0009-2541(02)00032-3 |
genre |
lena river Siberia |
genre_facet |
lena river Siberia |
op_source |
SCI |
op_relation |
CHEMICAL GEOLOGY.2002,187,(3-4),231-255. 762527 0009-2541 http://hdl.handle.net/20.500.11897/208746 doi:10.1016/S0009-2541(02)00032-3 WOS:000177462500004 |
op_doi |
https://doi.org/20.500.11897/208746 https://doi.org/10.1016/S0009-2541(02)00032-3 |
container_title |
Chemical Geology |
container_volume |
187 |
container_issue |
3-4 |
container_start_page |
231 |
op_container_end_page |
255 |
_version_ |
1766063154542936064 |