Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China

Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of thes...
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Autor*in:	Liu, Jiutan [verfasserIn] Gao, Zongjun [verfasserIn] Wang, Min [verfasserIn] Li, Yingzhi [verfasserIn] Shi, Mengjie [verfasserIn] Zhang, Hongying [verfasserIn] Ma, Yuanyuan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	Groundwater Hydrochemical characteristics Hydrochemical processes Yarlung Zangbo River Valley

Übergeordnetes Werk:	Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 78(2019), 3 vom: 24. Jan.
Übergeordnetes Werk:	volume:78 ; year:2019 ; number:3 ; day:24 ; month:01

Links:	Volltext

DOI / URN:	10.1007/s12665-019-8101-y

Katalog-ID:	SPR026755866

Internformat


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245	1	0	\|a Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
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520			\|a Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−.
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650		4	\|a Yarlung Zangbo River Valley \|7 (dpeaa)DE-He213
700	1		\|a Gao, Zongjun \|e verfasserin \|4 aut
700	1		\|a Wang, Min \|e verfasserin \|4 aut
700	1		\|a Li, Yingzhi \|e verfasserin \|4 aut
700	1		\|a Shi, Mengjie \|e verfasserin \|4 aut
700	1		\|a Zhang, Hongying \|e verfasserin \|4 aut
700	1		\|a Ma, Yuanyuan \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Environmental earth sciences \|d Berlin : Springer, 2009 \|g 78(2019), 3 vom: 24. Jan. \|w (DE-627)599673451 \|w (DE-600)2493699-6 \|x 1866-6299 \|7 nnns
773	1	8	\|g volume:78 \|g year:2019 \|g number:3 \|g day:24 \|g month:01
856	4	0	\|u https://dx.doi.org/10.1007/s12665-019-8101-y \|z lizenzpflichtig \|3 Volltext
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author_variant	j l jl z g zg m w mw y l yl m s ms h z hz y m ym
matchkey_str	article:18666299:2019----::yrceiacaatrsisnpsilcnrliterudaeoteal
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publishDate	2019
allfields	10.1007/s12665-019-8101-y doi (DE-627)SPR026755866 (SPR)s12665-019-8101-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.95 bkl Liu, Jiutan verfasserin aut Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−. Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213 Gao, Zongjun verfasserin aut Wang, Min verfasserin aut Li, Yingzhi verfasserin aut Shi, Mengjie verfasserin aut Zhang, Hongying verfasserin aut Ma, Yuanyuan verfasserin aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 78(2019), 3 vom: 24. Jan. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:78 year:2019 number:3 day:24 month:01 https://dx.doi.org/10.1007/s12665-019-8101-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 ASE AR 78 2019 3 24 01
spelling	10.1007/s12665-019-8101-y doi (DE-627)SPR026755866 (SPR)s12665-019-8101-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.95 bkl Liu, Jiutan verfasserin aut Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−. Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213 Gao, Zongjun verfasserin aut Wang, Min verfasserin aut Li, Yingzhi verfasserin aut Shi, Mengjie verfasserin aut Zhang, Hongying verfasserin aut Ma, Yuanyuan verfasserin aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 78(2019), 3 vom: 24. Jan. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:78 year:2019 number:3 day:24 month:01 https://dx.doi.org/10.1007/s12665-019-8101-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 ASE AR 78 2019 3 24 01
allfields_unstemmed	10.1007/s12665-019-8101-y doi (DE-627)SPR026755866 (SPR)s12665-019-8101-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.95 bkl Liu, Jiutan verfasserin aut Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−. Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213 Gao, Zongjun verfasserin aut Wang, Min verfasserin aut Li, Yingzhi verfasserin aut Shi, Mengjie verfasserin aut Zhang, Hongying verfasserin aut Ma, Yuanyuan verfasserin aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 78(2019), 3 vom: 24. Jan. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:78 year:2019 number:3 day:24 month:01 https://dx.doi.org/10.1007/s12665-019-8101-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 ASE AR 78 2019 3 24 01
allfieldsGer	10.1007/s12665-019-8101-y doi (DE-627)SPR026755866 (SPR)s12665-019-8101-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.95 bkl Liu, Jiutan verfasserin aut Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−. Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213 Gao, Zongjun verfasserin aut Wang, Min verfasserin aut Li, Yingzhi verfasserin aut Shi, Mengjie verfasserin aut Zhang, Hongying verfasserin aut Ma, Yuanyuan verfasserin aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 78(2019), 3 vom: 24. Jan. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:78 year:2019 number:3 day:24 month:01 https://dx.doi.org/10.1007/s12665-019-8101-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 ASE AR 78 2019 3 24 01
allfieldsSound	10.1007/s12665-019-8101-y doi (DE-627)SPR026755866 (SPR)s12665-019-8101-y-e DE-627 ger DE-627 rakwb eng 550 ASE 38.95 bkl Liu, Jiutan verfasserin aut Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−. Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213 Gao, Zongjun verfasserin aut Wang, Min verfasserin aut Li, Yingzhi verfasserin aut Shi, Mengjie verfasserin aut Zhang, Hongying verfasserin aut Ma, Yuanyuan verfasserin aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 78(2019), 3 vom: 24. Jan. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:78 year:2019 number:3 day:24 month:01 https://dx.doi.org/10.1007/s12665-019-8101-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 ASE AR 78 2019 3 24 01
language	English
source	Enthalten in Environmental earth sciences 78(2019), 3 vom: 24. Jan. volume:78 year:2019 number:3 day:24 month:01
sourceStr	Enthalten in Environmental earth sciences 78(2019), 3 vom: 24. Jan. volume:78 year:2019 number:3 day:24 month:01
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Groundwater Hydrochemical characteristics Hydrochemical processes Yarlung Zangbo River Valley
dewey-raw	550
isfreeaccess_bool	false
container_title	Environmental earth sciences
authorswithroles_txt_mv	Liu, Jiutan @@aut@@ Gao, Zongjun @@aut@@ Wang, Min @@aut@@ Li, Yingzhi @@aut@@ Shi, Mengjie @@aut@@ Zhang, Hongying @@aut@@ Ma, Yuanyuan @@aut@@
publishDateDaySort_date	2019-01-24T00:00:00Z
hierarchy_top_id	599673451
dewey-sort	3550
id	SPR026755866
language_de	englisch
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author	Liu, Jiutan
spellingShingle	Liu, Jiutan ddc 550 bkl 38.95 misc Groundwater misc Hydrochemical characteristics misc Hydrochemical processes misc Yarlung Zangbo River Valley Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
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topic_title	550 ASE 38.95 bkl Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China Groundwater (dpeaa)DE-He213 Hydrochemical characteristics (dpeaa)DE-He213 Hydrochemical processes (dpeaa)DE-He213 Yarlung Zangbo River Valley (dpeaa)DE-He213
topic	ddc 550 bkl 38.95 misc Groundwater misc Hydrochemical characteristics misc Hydrochemical processes misc Yarlung Zangbo River Valley
topic_unstemmed	ddc 550 bkl 38.95 misc Groundwater misc Hydrochemical characteristics misc Hydrochemical processes misc Yarlung Zangbo River Valley
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title	Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
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title_full	Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
author_sort	Liu, Jiutan
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author_browse	Liu, Jiutan Gao, Zongjun Wang, Min Li, Yingzhi Shi, Mengjie Zhang, Hongying Ma, Yuanyuan
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title_sort	hydrochemical characteristics and possible controls in the groundwater of the yarlung zangbo river valley, china
title_auth	Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
abstract	Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−.
abstractGer	Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−.
abstract_unstemmed	Abstract The Yarlung Zangbo River Valley is situated in the Qinghai Tibet Plateau with high elevation, abundant water resources and less influence from human activities. In this study, 47 groundwater samples were collected to investigate the hydrochemical characteristics and possible control of these characteristics in the groundwater of the Yarlung Zangbo River Valley; the samples were statistically analyzed using a Durov diagram, Gibbs plot, ratio graphs of ions, and factor analysis. The study results showed that the mean concentrations of the major ions in groundwater were relatively low, and the predominance of cations and anions in the groundwater was $ Ca^{2+} $ > $ Mg^{2+} $ > $ Na^{+} $ > $ K^{+} $ and $ HCO_{3} $− > $ SO_{4} $2− > $ Cl^{−} $, respectively. Most groundwater samples fall in the category of $ HCO_{3} $–Ca and mixed $ HCO_{3} $·$ SO_{4} $–Ca·Mg. Upstream to downstream, the total dissolved solids and major cations and anions in the groundwater show a gradual decreasing trend due to the dilution effect of precipitation and lateral runoff recharge, except for the $ K^{+} $. The water–rock interaction was the primary mechanism controlling the groundwater chemistry in the study area. The dissolution of carbonates was the major contributor to the formation of the groundwater chemistry, and the dissolution of silicate and sulfate also contributed to the chemical composition of the groundwater in the study area, whereas the cation exchange was weak. In addition, $ H_{2} %$ SO_{4} $ participation in the dissolution and weathering of carbonate was an important source of $ SO_{4} $2−.
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container_issue	3
title_short	Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China
url	https://dx.doi.org/10.1007/s12665-019-8101-y
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author2	Gao, Zongjun Wang, Min Li, Yingzhi Shi, Mengjie Zhang, Hongying Ma, Yuanyuan
author2Str	Gao, Zongjun Wang, Min Li, Yingzhi Shi, Mengjie Zhang, Hongying Ma, Yuanyuan
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doi_str	10.1007/s12665-019-8101-y
up_date	2024-07-03T22:36:14.687Z
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Hydrochemical characteristics and possible controls in the groundwater of the Yarlung Zangbo River Valley, China

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