Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China
Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Li, Xiangquan [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2008 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag 2007 |
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| Übergeordnetes Werk: |
Enthalten in: Hydrogeology journal - Springer-Verlag, 1995, 16(2008), 2 vom: 05. Jan., Seite 335-348 |
|---|---|
| Übergeordnetes Werk: |
volume:16 ; year:2008 ; number:2 ; day:05 ; month:01 ; pages:335-348 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10040-007-0269-7 |
|---|
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OLC204001618X |
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| 520 | |a Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. | ||
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10.1007/s10040-007-0269-7 doi (DE-627)OLC204001618X (DE-He213)s10040-007-0269-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Li, Xiangquan verfasserin aut Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. Arid regions Groundwater flow Hydrochemistry Stable isotopes China Zhang, Li aut Hou, Xinwei aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 16(2008), 2 vom: 05. Jan., Seite 335-348 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:16 year:2008 number:2 day:05 month:01 pages:335-348 https://doi.org/10.1007/s10040-007-0269-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4277 AR 16 2008 2 05 01 335-348 |
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10.1007/s10040-007-0269-7 doi (DE-627)OLC204001618X (DE-He213)s10040-007-0269-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Li, Xiangquan verfasserin aut Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. Arid regions Groundwater flow Hydrochemistry Stable isotopes China Zhang, Li aut Hou, Xinwei aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 16(2008), 2 vom: 05. Jan., Seite 335-348 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:16 year:2008 number:2 day:05 month:01 pages:335-348 https://doi.org/10.1007/s10040-007-0269-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4277 AR 16 2008 2 05 01 335-348 |
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10.1007/s10040-007-0269-7 doi (DE-627)OLC204001618X (DE-He213)s10040-007-0269-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Li, Xiangquan verfasserin aut Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. Arid regions Groundwater flow Hydrochemistry Stable isotopes China Zhang, Li aut Hou, Xinwei aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 16(2008), 2 vom: 05. Jan., Seite 335-348 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:16 year:2008 number:2 day:05 month:01 pages:335-348 https://doi.org/10.1007/s10040-007-0269-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4277 AR 16 2008 2 05 01 335-348 |
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10.1007/s10040-007-0269-7 doi (DE-627)OLC204001618X (DE-He213)s10040-007-0269-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Li, Xiangquan verfasserin aut Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. Arid regions Groundwater flow Hydrochemistry Stable isotopes China Zhang, Li aut Hou, Xinwei aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 16(2008), 2 vom: 05. Jan., Seite 335-348 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:16 year:2008 number:2 day:05 month:01 pages:335-348 https://doi.org/10.1007/s10040-007-0269-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4277 AR 16 2008 2 05 01 335-348 |
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10.1007/s10040-007-0269-7 doi (DE-627)OLC204001618X (DE-He213)s10040-007-0269-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Li, Xiangquan verfasserin aut Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. Arid regions Groundwater flow Hydrochemistry Stable isotopes China Zhang, Li aut Hou, Xinwei aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 16(2008), 2 vom: 05. Jan., Seite 335-348 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:16 year:2008 number:2 day:05 month:01 pages:335-348 https://doi.org/10.1007/s10040-007-0269-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4277 AR 16 2008 2 05 01 335-348 |
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Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China |
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| title_full |
Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China |
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Li, Xiangquan |
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Hydrogeology journal |
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Hydrogeology journal |
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eng |
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2008 |
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Li, Xiangquan Zhang, Li Hou, Xinwei |
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Li, Xiangquan |
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10.1007/s10040-007-0269-7 |
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550 |
| title_sort |
use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in qingshuihe basin, northwestern china |
| title_auth |
Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China |
| abstract |
Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. © Springer-Verlag 2007 |
| abstractGer |
Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. © Springer-Verlag 2007 |
| abstract_unstemmed |
Abstract Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater: (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na–$ HCO_{3} $, which dominates type (1), and Na–$ SO_{4} $, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of $ CO_{2} $ gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70–100 years. © Springer-Verlag 2007 |
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| title_short |
Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China |
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https://doi.org/10.1007/s10040-007-0269-7 |
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