Hydrogeochemical Evolution Along Groundwater Flow Paths in the Manas River Basin, Northwest China

© 2018, National Ground Water Association.

Bibliographische Detailangaben
Veröffentlicht in:Ground water. - 1979. - 57(2019), 4 vom: 01. Juli, Seite 575-589
1. Verfasser: Wang, Jianjun (VerfasserIn)
Weitere Verfasser: Liang, Xing, Liu, Yanfeng, Jin, Menggui, Knappett, Peter S K, Liu, Yalei
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2019
Zugriff auf das übergeordnete Werk:Ground water
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Water Pollutants, Chemical
LEADER 01000naa a22002652 4500
001 NLM288827643
003 DE-627
005 20231225061211.0
007 cr uuu---uuuuu
008 231225s2019 xx |||||o 00| ||eng c
024 7 |a 10.1111/gwat.12829  |2 doi 
028 5 2 |a pubmed24n0962.xml 
035 |a (DE-627)NLM288827643 
035 |a (NLM)30246345 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Wang, Jianjun  |e verfasserin  |4 aut 
245 1 0 |a Hydrogeochemical Evolution Along Groundwater Flow Paths in the Manas River Basin, Northwest China 
264 1 |c 2019 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 09.09.2019 
500 |a Date Revised 09.09.2019 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a © 2018, National Ground Water Association. 
520 |a The impacts of long-term pumping on groundwater chemistry remain unclear in the Manas River Basin, Northwest China. In this study, major ions within five surface water and 105 groundwater samples were analyzed to identify hydrogeochemical processes affecting groundwater composition and evolution along the regional-scale groundwater flow paths using the multivariate techniques of hierarchical cluster analysis (HCA) and principal components analysis (PCA) and traditional graphical methods for analyzing groundwater geochemistry. HCA classified the groundwater samples into four clusters (C1 to C4). PCA reduced the dimensionality of geochemical data into three PCs, which explained 86% of the total variance. The results of HCA and PCA were used to identify three zones: "recharge," "transition," and "discharge." In the recharge zone the groundwater type is Ca-HCO3 -SO4 and is primarily impacted by the dissolution of calcite and silicate weathering. In the transition zone the groundwater type is Ca-HCO3 -SO4 -Cl and is impacted by rock dissolution and reverse ion exchange. In the discharge zone the groundwater type is Na-Cl and is impacted by evaporation and reverse ion exchange. In addition, anthropogenic activities impact the groundwater chemistry in the study area. The groundwater type generally changes from Ca-HCO3 -SO4 in the recharge area to Na-Cl in the discharge area along the regional-scale groundwater flow paths. This study provides a process-based knowledge for understanding the interaction of groundwater flow patterns and geochemical evolution within the Manas River Basin 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 7 |a Water Pollutants, Chemical  |2 NLM 
700 1 |a Liang, Xing  |e verfasserin  |4 aut 
700 1 |a Liu, Yanfeng  |e verfasserin  |4 aut 
700 1 |a Jin, Menggui  |e verfasserin  |4 aut 
700 1 |a Knappett, Peter S K  |e verfasserin  |4 aut 
700 1 |a Liu, Yalei  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Ground water  |d 1979  |g 57(2019), 4 vom: 01. Juli, Seite 575-589  |w (DE-627)NLM098182528  |x 1745-6584  |7 nnns 
773 1 8 |g volume:57  |g year:2019  |g number:4  |g day:01  |g month:07  |g pages:575-589 
856 4 0 |u http://dx.doi.org/10.1111/gwat.12829  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 57  |j 2019  |e 4  |b 01  |c 07  |h 575-589