Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin
Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhou, Xun [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 73(2015), 12 vom: 09. Jan., Seite 8565-8574 |
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| Übergeordnetes Werk: |
volume:73 ; year:2015 ; number:12 ; day:09 ; month:01 ; pages:8565-8574 |
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| DOI / URN: |
10.1007/s12665-015-4015-5 |
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SPR026703300 |
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| 100 | 1 | |a Zhou, Xun |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
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| 520 | |a Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. | ||
| 650 | 4 | |a Brine |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sedimentary basin |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Numerical simulation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Potassium |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sichuan Basin |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Jiang, Changlong |4 aut | |
| 700 | 1 | |a Zhao, Jingbo |4 aut | |
| 700 | 1 | |a Cao, Qin |4 aut | |
| 700 | 1 | |a Han, Jiajun |4 aut | |
| 700 | 1 | |a Wang, Xiaocui |4 aut | |
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10.1007/s12665-015-4015-5 doi (DE-627)SPR026703300 (SPR)s12665-015-4015-5-e DE-627 ger DE-627 rakwb eng Zhou, Xun verfasserin aut Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 Jiang, Changlong aut Zhao, Jingbo aut Cao, Qin aut Han, Jiajun aut Wang, Xiaocui aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2015), 12 vom: 09. Jan., Seite 8565-8574 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 https://dx.doi.org/10.1007/s12665-015-4015-5 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 AR 73 2015 12 09 01 8565-8574 |
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10.1007/s12665-015-4015-5 doi (DE-627)SPR026703300 (SPR)s12665-015-4015-5-e DE-627 ger DE-627 rakwb eng Zhou, Xun verfasserin aut Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 Jiang, Changlong aut Zhao, Jingbo aut Cao, Qin aut Han, Jiajun aut Wang, Xiaocui aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2015), 12 vom: 09. Jan., Seite 8565-8574 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 https://dx.doi.org/10.1007/s12665-015-4015-5 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 AR 73 2015 12 09 01 8565-8574 |
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10.1007/s12665-015-4015-5 doi (DE-627)SPR026703300 (SPR)s12665-015-4015-5-e DE-627 ger DE-627 rakwb eng Zhou, Xun verfasserin aut Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 Jiang, Changlong aut Zhao, Jingbo aut Cao, Qin aut Han, Jiajun aut Wang, Xiaocui aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2015), 12 vom: 09. Jan., Seite 8565-8574 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 https://dx.doi.org/10.1007/s12665-015-4015-5 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 AR 73 2015 12 09 01 8565-8574 |
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10.1007/s12665-015-4015-5 doi (DE-627)SPR026703300 (SPR)s12665-015-4015-5-e DE-627 ger DE-627 rakwb eng Zhou, Xun verfasserin aut Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 Jiang, Changlong aut Zhao, Jingbo aut Cao, Qin aut Han, Jiajun aut Wang, Xiaocui aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2015), 12 vom: 09. Jan., Seite 8565-8574 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 https://dx.doi.org/10.1007/s12665-015-4015-5 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 AR 73 2015 12 09 01 8565-8574 |
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10.1007/s12665-015-4015-5 doi (DE-627)SPR026703300 (SPR)s12665-015-4015-5-e DE-627 ger DE-627 rakwb eng Zhou, Xun verfasserin aut Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 Jiang, Changlong aut Zhao, Jingbo aut Cao, Qin aut Han, Jiajun aut Wang, Xiaocui aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 73(2015), 12 vom: 09. Jan., Seite 8565-8574 (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 https://dx.doi.org/10.1007/s12665-015-4015-5 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 AR 73 2015 12 09 01 8565-8574 |
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Enthalten in Environmental earth sciences 73(2015), 12 vom: 09. Jan., Seite 8565-8574 volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 |
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Enthalten in Environmental earth sciences 73(2015), 12 vom: 09. Jan., Seite 8565-8574 volume:73 year:2015 number:12 day:09 month:01 pages:8565-8574 |
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Brine Sedimentary basin Numerical simulation Potassium Sichuan Basin |
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Zhou, Xun @@aut@@ Jiang, Changlong @@aut@@ Zhao, Jingbo @@aut@@ Cao, Qin @@aut@@ Han, Jiajun @@aut@@ Wang, Xiaocui @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR026703300</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401015916.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s12665-015-4015-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR026703300</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s12665-015-4015-5-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhou, Xun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Brine</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sedimentary basin</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Numerical simulation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Potassium</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sichuan Basin</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jiang, Changlong</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhao, Jingbo</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cao, Qin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Han, Jiajun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Xiaocui</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Environmental earth sciences</subfield><subfield code="d">Berlin : Springer, 2009</subfield><subfield code="g">73(2015), 12 vom: 09. 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Zhou, Xun |
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Zhou, Xun misc Brine misc Sedimentary basin misc Numerical simulation misc Potassium misc Sichuan Basin Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
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Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin Brine (dpeaa)DE-He213 Sedimentary basin (dpeaa)DE-He213 Numerical simulation (dpeaa)DE-He213 Potassium (dpeaa)DE-He213 Sichuan Basin (dpeaa)DE-He213 |
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Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
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Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
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occurrence and resource evaluation of the subsurface high-k brines in the pingluoba brine-bearing structure in western sichuan basin |
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Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
| abstract |
Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. © Springer-Verlag Berlin Heidelberg 2015 |
| abstractGer |
Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. © Springer-Verlag Berlin Heidelberg 2015 |
| abstract_unstemmed |
Abstract In the western Sichuan Basin of China occurs an anticline in which high-K brines are found in the carbonate rocks of the Middle Triassic Leikoupo Group. The brine-bearing formation is at depth ranging from 4,465 to 4,565 m and the brines are enriched in a fault zone in the anticline. The PL4 well tapping the brine-bearing formation flows brines having TDS of 348.392–377.27 g/L, K contents of 48.95–53.267 g/L and B contents of 4.994 g/L. The TDS of the brines are close to those of the Yellow Sea water and the South China Sea water when evaporated to the stage of epsomite precipitation. The hydraulic head of the high-K brines in the PL4 well tapping the brine-bearing formation is calculated as high as 7,564 m and is 3,049 m above the land surface. A 3D numerical model is used to simulate the flow of the brines under the condition of exploitation and prediction calculation of the exploitation of the PL4 well is also performed. When the hydraulic head of the brines in the PL4 well is dropped to the land surface and to a depth of about 1,000 m below the land surface, the exploitable brine resources of the well are estimated as approximately 1.1 × $ 10^{6} $ and 3.8 × $ 10^{6} $ $ m^{3} $, respectively. © Springer-Verlag Berlin Heidelberg 2015 |
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| title_short |
Occurrence and resource evaluation of the subsurface high-K brines in the Pingluoba brine-bearing structure in western Sichuan Basin |
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https://dx.doi.org/10.1007/s12665-015-4015-5 |
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Jiang, Changlong Zhao, Jingbo Cao, Qin Han, Jiajun Wang, Xiaocui |
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2024-07-03T22:15:48.386Z |
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| score |
7.399727 |