Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation
Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, fi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wei, Jiuchuan [verfasserIn] Li, Guanghui [verfasserIn] Xie, Daolei [verfasserIn] Yu, Gongyishan [verfasserIn] Man, Xiaoquan [verfasserIn] Wang, Jie [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 13(2020), 17 vom: 28. Aug. |
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| Übergeordnetes Werk: |
volume:13 ; year:2020 ; number:17 ; day:28 ; month:08 |
| Links: |
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| DOI / URN: |
10.1007/s12517-020-05894-7 |
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SPR04080481X |
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| 520 | |a Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. | ||
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| 650 | 4 | |a Source discrimination of water inflow |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Multivariate mixed model |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Fuzzy comprehensive evaluation |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Li, Guanghui |e verfasserin |4 aut | |
| 700 | 1 | |a Xie, Daolei |e verfasserin |4 aut | |
| 700 | 1 | |a Yu, Gongyishan |e verfasserin |4 aut | |
| 700 | 1 | |a Man, Xiaoquan |e verfasserin |4 aut | |
| 700 | 1 | |a Wang, Jie |e verfasserin |4 aut | |
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10.1007/s12517-020-05894-7 doi (DE-627)SPR04080481X (SPR)s12517-020-05894-7-e DE-627 ger DE-627 rakwb eng 550 ASE Wei, Jiuchuan verfasserin aut Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 Li, Guanghui verfasserin aut Xie, Daolei verfasserin aut Yu, Gongyishan verfasserin aut Man, Xiaoquan verfasserin aut Wang, Jie verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 13(2020), 17 vom: 28. Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:13 year:2020 number:17 day:28 month:08 https://dx.doi.org/10.1007/s12517-020-05894-7 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 13 2020 17 28 08 |
| spelling |
10.1007/s12517-020-05894-7 doi (DE-627)SPR04080481X (SPR)s12517-020-05894-7-e DE-627 ger DE-627 rakwb eng 550 ASE Wei, Jiuchuan verfasserin aut Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 Li, Guanghui verfasserin aut Xie, Daolei verfasserin aut Yu, Gongyishan verfasserin aut Man, Xiaoquan verfasserin aut Wang, Jie verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 13(2020), 17 vom: 28. Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:13 year:2020 number:17 day:28 month:08 https://dx.doi.org/10.1007/s12517-020-05894-7 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 13 2020 17 28 08 |
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10.1007/s12517-020-05894-7 doi (DE-627)SPR04080481X (SPR)s12517-020-05894-7-e DE-627 ger DE-627 rakwb eng 550 ASE Wei, Jiuchuan verfasserin aut Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 Li, Guanghui verfasserin aut Xie, Daolei verfasserin aut Yu, Gongyishan verfasserin aut Man, Xiaoquan verfasserin aut Wang, Jie verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 13(2020), 17 vom: 28. Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:13 year:2020 number:17 day:28 month:08 https://dx.doi.org/10.1007/s12517-020-05894-7 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 13 2020 17 28 08 |
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10.1007/s12517-020-05894-7 doi (DE-627)SPR04080481X (SPR)s12517-020-05894-7-e DE-627 ger DE-627 rakwb eng 550 ASE Wei, Jiuchuan verfasserin aut Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 Li, Guanghui verfasserin aut Xie, Daolei verfasserin aut Yu, Gongyishan verfasserin aut Man, Xiaoquan verfasserin aut Wang, Jie verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 13(2020), 17 vom: 28. Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:13 year:2020 number:17 day:28 month:08 https://dx.doi.org/10.1007/s12517-020-05894-7 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 13 2020 17 28 08 |
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10.1007/s12517-020-05894-7 doi (DE-627)SPR04080481X (SPR)s12517-020-05894-7-e DE-627 ger DE-627 rakwb eng 550 ASE Wei, Jiuchuan verfasserin aut Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 Li, Guanghui verfasserin aut Xie, Daolei verfasserin aut Yu, Gongyishan verfasserin aut Man, Xiaoquan verfasserin aut Wang, Jie verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 13(2020), 17 vom: 28. Aug. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:13 year:2020 number:17 day:28 month:08 https://dx.doi.org/10.1007/s12517-020-05894-7 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_381 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 13 2020 17 28 08 |
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Enthalten in Arabian journal of geosciences 13(2020), 17 vom: 28. Aug. volume:13 year:2020 number:17 day:28 month:08 |
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Wei, Jiuchuan @@aut@@ Li, Guanghui @@aut@@ Xie, Daolei @@aut@@ Yu, Gongyishan @@aut@@ Man, Xiaoquan @@aut@@ Wang, Jie @@aut@@ |
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To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Juye coalfield</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Source discrimination of water inflow</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Multivariate mixed model</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fuzzy comprehensive evaluation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Guanghui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xie, Daolei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yu, Gongyishan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Man, Xiaoquan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Jie</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Arabian journal of geosciences</subfield><subfield code="d">Berlin : Springer, 2008</subfield><subfield code="g">13(2020), 17 vom: 28. 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| author |
Wei, Jiuchuan |
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Wei, Jiuchuan ddc 550 misc Juye coalfield misc Source discrimination of water inflow misc Multivariate mixed model misc Fuzzy comprehensive evaluation Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
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550 ASE Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation Juye coalfield (dpeaa)DE-He213 Source discrimination of water inflow (dpeaa)DE-He213 Multivariate mixed model (dpeaa)DE-He213 Fuzzy comprehensive evaluation (dpeaa)DE-He213 |
| topic |
ddc 550 misc Juye coalfield misc Source discrimination of water inflow misc Multivariate mixed model misc Fuzzy comprehensive evaluation |
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ddc 550 misc Juye coalfield misc Source discrimination of water inflow misc Multivariate mixed model misc Fuzzy comprehensive evaluation |
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ddc 550 misc Juye coalfield misc Source discrimination of water inflow misc Multivariate mixed model misc Fuzzy comprehensive evaluation |
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Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
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| title_full |
Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
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Wei, Jiuchuan |
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Arabian journal of geosciences |
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Arabian journal of geosciences |
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Wei, Jiuchuan Li, Guanghui Xie, Daolei Yu, Gongyishan Man, Xiaoquan Wang, Jie |
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10.1007/s12517-020-05894-7 |
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550 |
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| title_sort |
discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
| title_auth |
Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
| abstract |
Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. |
| abstractGer |
Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. |
| abstract_unstemmed |
Abstract The accurate discrimination of the mine water-inflow sources is one of the main focuses of mine hydrogeological work and represents the basis of coal mine water hazard prevention. To accurately discriminate the water-inflow source in the – 700-m air return tunnel of the Longgu Coal Mine, firstly, according to the water-inflow conditions of the coal mine, three water sources were preliminarily estimated: the Ordovician limestone aquifer, the No. 3 limestone aquifer, and the sandstone aquifer in the roof and floor of No. 3 coal seam. A number of water samples were then selected from each of the three aquifers as the standard comparison water samples. A sample of water inflow from the tunnel of the coal mine and nearby locations was selected as the water sample to be tested. Six conventional hydrochemical indexes ($ Na^{+} $ + $ K^{+} $, $ Ca^{2+} $, $ Mg^{2+} $, $ Cl^{−} $, $ SO_{4} $2−, and $ HCO_{3} $−) in the water sample to be tested and standard water sample were tested and discriminated by the multivariate mixed model and fuzzy comprehensive evaluation. The results show that the water-inflow source in the –n700-m air return tunnel is the Ordovician limestone aquifer, and a hydraulic connection was observed between the No. 3 limestone aquifer and the Ordovician limestone aquifer. The findings provide data support for the management of the water-inflow process in the Longgu Coal Mine, and have practical guiding significance for the discriminating water sources in other coal mines affected by water hazards. |
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Discrimination of mine water-inflow sources based on the multivariate mixed model and fuzzy comprehensive evaluation |
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https://dx.doi.org/10.1007/s12517-020-05894-7 |
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Li, Guanghui Xie, Daolei Yu, Gongyishan Man, Xiaoquan Wang, Jie |
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Li, Guanghui Xie, Daolei Yu, Gongyishan Man, Xiaoquan Wang, Jie |
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| doi_str |
10.1007/s12517-020-05894-7 |
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2024-07-03T18:22:13.546Z |
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| score |
7.4002237 |