Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation
Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Tesmer, M. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2007 |
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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, 15(2007), 7 vom: 22. März, Seite 1291-1306 |
|---|---|
| Übergeordnetes Werk: |
volume:15 ; year:2007 ; number:7 ; day:22 ; month:03 ; pages:1291-1306 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10040-007-0176-y |
|---|
| Katalog-ID: |
OLC2040015906 |
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| 520 | |a Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. | ||
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10.1007/s10040-007-0176-y doi (DE-627)OLC2040015906 (DE-He213)s10040-007-0176-y-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Tesmer, M. verfasserin aut Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. Hydrochemistry Rare-earth elements Stable isotopes Hydrostratigraphy Brines Möller, P. aut Wieland, S. aut Jahnke, C. aut Voigt, H. aut Pekdeger, A. aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 15(2007), 7 vom: 22. März, Seite 1291-1306 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:15 year:2007 number:7 day:22 month:03 pages:1291-1306 https://doi.org/10.1007/s10040-007-0176-y 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 15 2007 7 22 03 1291-1306 |
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10.1007/s10040-007-0176-y doi (DE-627)OLC2040015906 (DE-He213)s10040-007-0176-y-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Tesmer, M. verfasserin aut Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. Hydrochemistry Rare-earth elements Stable isotopes Hydrostratigraphy Brines Möller, P. aut Wieland, S. aut Jahnke, C. aut Voigt, H. aut Pekdeger, A. aut Enthalten in Hydrogeology journal Springer-Verlag, 1995 15(2007), 7 vom: 22. März, Seite 1291-1306 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:15 year:2007 number:7 day:22 month:03 pages:1291-1306 https://doi.org/10.1007/s10040-007-0176-y 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 15 2007 7 22 03 1291-1306 |
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Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation |
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Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation |
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Tesmer, M. |
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Tesmer, M. Möller, P. Wieland, S. Jahnke, C. Voigt, H. Pekdeger, A. |
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deep reaching fluid flow in the north east german basin: origin and processes of groundwater salinisation |
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Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation |
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Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. © Springer-Verlag 2007 |
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Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. © Springer-Verlag 2007 |
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Abstract Major element chemistry, rare-earth element distribution, and H and O isotopes are conjointly used to study the sources of salinisation and interaquifer flow of saline groundwater in the North East German Basin. Chemical analyses from hydrocarbon exploration campaigns showed evidence of the existence of two different groups of brines: halite and halite Ca–Cl brines. Residual brines and leachates are identified by $ Br^{−} $/$ Cl^{−} $ ratios. Most of the brines are dissolution brines of Permian evaporites. New analyses show that the pattern of rare-earth elements and yttrium (REY) are closely linked to H and O isotope distribution. Thermal brines from deep wells and artesian wells indicate isotopically evaporated brines, which chemically interacted with their aquifer environment. Isotopes and rare-earth element patterns prove that cross flow exists, especially in the post-Rupelian aquifer. However, even at depths exceeding 2,000 m, interaquifer flow takes place. The rare-earth element pattern and H and O isotopes identify locally ascending brines. A large-scale lateral groundwater flow has to be assumed because all pre-Rupelian aquifer systems to a depth of at least 500 m are isotopically characterised by Recent or Pleistocene recharge conditions. © Springer-Verlag 2007 |
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Deep reaching fluid flow in the North East German Basin: origin and processes of groundwater salinisation |
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