Thermal recovery process of a backfilled open-pit in permafrost area at the Gulian strip coal mine in Northeast China
Timely and proper backfilling of open-pits in strip coal-mines has been an effective measurement for the recovery of the hydrothermal regimes and ecological environment in permafrost regions. In this study, numerical simulations and statistical regressions were applied for analyzing the recovery pro...
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description | Timely and proper backfilling of open-pits in strip coal-mines has been an effective measurement for the recovery of the hydrothermal regimes and ecological environment in permafrost regions. In this study, numerical simulations and statistical regressions were applied for analyzing the recovery processes of the backfill and its major influencing factors for the thermal equilibrium in recently backfilled open pits at the Gulian strip coalmine in Mo'he, Northeast China. Results show that the thermal recovery time of backfilled areas is positively correlated to the backfill depth (BD) of the soils, the backfilled soil temperature (BST), and the mean annual ground surface temperature (MAGST); meanwhile, climate warming can impact on thermal regimes of the backfill area. The impact of climate warming on ground temperature of the backfill will show up significantly in about 50 years after backfilling (BD at 10.0 and 20.0 m, BST at 20.0°C) under the climate warming scenario (CWS) of 0.025°C·year−1. Grey-relation analyses show that the sensitivity of the backfill recovery time declines in the order of the BD, BST and MAGST. On the basis of the abovementioned studies, the layer-by-layer backfilling in cold seasons is advised for more effective and more rapid recovery of thermal regimes of the backfilled open-pits in cold regions. |
doi_str_mv | 10.1007/s11629-017-4439-3 |
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In this study, numerical simulations and statistical regressions were applied for analyzing the recovery processes of the backfill and its major influencing factors for the thermal equilibrium in recently backfilled open pits at the Gulian strip coalmine in Mo'he, Northeast China. Results show that the thermal recovery time of backfilled areas is positively correlated to the backfill depth (BD) of the soils, the backfilled soil temperature (BST), and the mean annual ground surface temperature (MAGST); meanwhile, climate warming can impact on thermal regimes of the backfill area. The impact of climate warming on ground temperature of the backfill will show up significantly in about 50 years after backfilling (BD at 10.0 and 20.0 m, BST at 20.0°C) under the climate warming scenario (CWS) of 0.025°C·year−1. Grey-relation analyses show that the sensitivity of the backfill recovery time declines in the order of the BD, BST and MAGST. On the basis of the abovementioned studies, the layer-by-layer backfilling in cold seasons is advised for more effective and more rapid recovery of thermal regimes of the backfilled open-pits in cold regions.</description><identifier>ISSN: 1672-6316</identifier><identifier>EISSN: 1993-0321</identifier><identifier>EISSN: 1008-2786</identifier><identifier>DOI: 10.1007/s11629-017-4439-3</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Backfill ; Climate ; Climate change ; Coal ; Coal mines ; Cold regions ; Cold season ; Computer simulation ; Earth and Environmental Science ; Earth Sciences ; Ecological effects ; Ecological monitoring ; Ecology ; Environment ; Geography ; Global warming ; Measurement ; Permafrost ; Pits ; Recovery ; Recovery time ; Regression analysis ; Sensitivity analysis ; Soil ; Soil temperature ; Strip ; Surface temperature ; Temperature effects ; Thermodynamic equilibrium</subject><ispartof>Journal of mountain science, 2017-11, Vol.14 (11), p.2212-2229</ispartof><rights>Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2017</rights><rights>Copyright Springer Science & Business Media Nov 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-28110c6d9bc60c0a2a67fe63ac77864ad6a442ae07467d3a633cd1fded6947573</citedby><cites>FETCH-LOGICAL-c316t-28110c6d9bc60c0a2a67fe63ac77864ad6a442ae07467d3a633cd1fded6947573</cites><orcidid>0000-0003-3133-5607 ; 0000-0002-6501-6121 ; 0000-0001-5844-3638 ; 0000-0003-3208-3480 ; 0000-0002-7855-9758 ; 0000-0002-8402-7897</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11629-017-4439-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11629-017-4439-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Gao, Shu-hui</creatorcontrib><creatorcontrib>He, Rui-xia</creatorcontrib><creatorcontrib>Jin, Hui-jun</creatorcontrib><creatorcontrib>Huang, Ya-dong</creatorcontrib><creatorcontrib>Zhang, Jian-ming</creatorcontrib><creatorcontrib>Luo, Dong-liang</creatorcontrib><title>Thermal recovery process of a backfilled open-pit in permafrost area at the Gulian strip coal mine in Northeast China</title><title>Journal of mountain science</title><addtitle>J. Mt. Sci</addtitle><description>Timely and proper backfilling of open-pits in strip coal-mines has been an effective measurement for the recovery of the hydrothermal regimes and ecological environment in permafrost regions. In this study, numerical simulations and statistical regressions were applied for analyzing the recovery processes of the backfill and its major influencing factors for the thermal equilibrium in recently backfilled open pits at the Gulian strip coalmine in Mo'he, Northeast China. Results show that the thermal recovery time of backfilled areas is positively correlated to the backfill depth (BD) of the soils, the backfilled soil temperature (BST), and the mean annual ground surface temperature (MAGST); meanwhile, climate warming can impact on thermal regimes of the backfill area. The impact of climate warming on ground temperature of the backfill will show up significantly in about 50 years after backfilling (BD at 10.0 and 20.0 m, BST at 20.0°C) under the climate warming scenario (CWS) of 0.025°C·year−1. Grey-relation analyses show that the sensitivity of the backfill recovery time declines in the order of the BD, BST and MAGST. On the basis of the abovementioned studies, the layer-by-layer backfilling in cold seasons is advised for more effective and more rapid recovery of thermal regimes of the backfilled open-pits in cold regions.</description><subject>Backfill</subject><subject>Climate</subject><subject>Climate change</subject><subject>Coal</subject><subject>Coal mines</subject><subject>Cold regions</subject><subject>Cold season</subject><subject>Computer simulation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecological effects</subject><subject>Ecological monitoring</subject><subject>Ecology</subject><subject>Environment</subject><subject>Geography</subject><subject>Global warming</subject><subject>Measurement</subject><subject>Permafrost</subject><subject>Pits</subject><subject>Recovery</subject><subject>Recovery time</subject><subject>Regression analysis</subject><subject>Sensitivity analysis</subject><subject>Soil</subject><subject>Soil temperature</subject><subject>Strip</subject><subject>Surface temperature</subject><subject>Temperature effects</subject><subject>Thermodynamic equilibrium</subject><issn>1672-6316</issn><issn>1993-0321</issn><issn>1008-2786</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kD1PwzAQhi0EEuXjB7BZYjb4I7XjEVVQkCpYymxdnQt1SZNgJ0j99zgqAwuTb3if93wPITeC3wnOzX0SQkvLuDCsKJRl6oTMhLWKcSXFaZ61kUwroc_JRUo7zrWxpZiRcb3FuIeGRvTdN8YD7WPnMSXa1RToBvxnHZoGK9r12LI-DDS0tJ-YOnZpoBARKAx02CJdjk2AlqYhhp76LrfuQ4sT8NrFHICcX2xDC1fkrIYm4fXve0nenx7Xi2e2elu-LB5WzOefDkyWQnCvK7vxmnsOErSpUSvwxpS6gEpDUUhAbgptKgVaKV-JusJK28LMjbokt8fefNTXiGlwu26MbV7phM02TDkvZU6JY8rni1LE2vUx7CEenOBusuuOdl226ya7TmVGHpmUs-0Hxj_N_0I_rYh9jg</recordid><startdate>20171101</startdate><enddate>20171101</enddate><creator>Gao, Shu-hui</creator><creator>He, Rui-xia</creator><creator>Jin, Hui-jun</creator><creator>Huang, Ya-dong</creator><creator>Zhang, Jian-ming</creator><creator>Luo, Dong-liang</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0003-3133-5607</orcidid><orcidid>https://orcid.org/0000-0002-6501-6121</orcidid><orcidid>https://orcid.org/0000-0001-5844-3638</orcidid><orcidid>https://orcid.org/0000-0003-3208-3480</orcidid><orcidid>https://orcid.org/0000-0002-7855-9758</orcidid><orcidid>https://orcid.org/0000-0002-8402-7897</orcidid></search><sort><creationdate>20171101</creationdate><title>Thermal recovery process of a backfilled open-pit in permafrost area at the Gulian strip coal mine in Northeast China</title><author>Gao, Shu-hui ; He, Rui-xia ; Jin, Hui-jun ; Huang, Ya-dong ; Zhang, Jian-ming ; Luo, Dong-liang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-28110c6d9bc60c0a2a67fe63ac77864ad6a442ae07467d3a633cd1fded6947573</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Backfill</topic><topic>Climate</topic><topic>Climate change</topic><topic>Coal</topic><topic>Coal mines</topic><topic>Cold regions</topic><topic>Cold season</topic><topic>Computer simulation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecological effects</topic><topic>Ecological monitoring</topic><topic>Ecology</topic><topic>Environment</topic><topic>Geography</topic><topic>Global warming</topic><topic>Measurement</topic><topic>Permafrost</topic><topic>Pits</topic><topic>Recovery</topic><topic>Recovery time</topic><topic>Regression analysis</topic><topic>Sensitivity analysis</topic><topic>Soil</topic><topic>Soil temperature</topic><topic>Strip</topic><topic>Surface temperature</topic><topic>Temperature effects</topic><topic>Thermodynamic equilibrium</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gao, Shu-hui</creatorcontrib><creatorcontrib>He, Rui-xia</creatorcontrib><creatorcontrib>Jin, Hui-jun</creatorcontrib><creatorcontrib>Huang, Ya-dong</creatorcontrib><creatorcontrib>Zhang, Jian-ming</creatorcontrib><creatorcontrib>Luo, Dong-liang</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of mountain science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gao, Shu-hui</au><au>He, Rui-xia</au><au>Jin, Hui-jun</au><au>Huang, Ya-dong</au><au>Zhang, Jian-ming</au><au>Luo, Dong-liang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Thermal recovery process of a backfilled open-pit in permafrost area at the Gulian strip coal mine in Northeast China</atitle><jtitle>Journal of mountain science</jtitle><stitle>J. Mt. Sci</stitle><date>2017-11-01</date><risdate>2017</risdate><volume>14</volume><issue>11</issue><spage>2212</spage><epage>2229</epage><pages>2212-2229</pages><issn>1672-6316</issn><eissn>1993-0321</eissn><eissn>1008-2786</eissn><abstract>Timely and proper backfilling of open-pits in strip coal-mines has been an effective measurement for the recovery of the hydrothermal regimes and ecological environment in permafrost regions. In this study, numerical simulations and statistical regressions were applied for analyzing the recovery processes of the backfill and its major influencing factors for the thermal equilibrium in recently backfilled open pits at the Gulian strip coalmine in Mo'he, Northeast China. Results show that the thermal recovery time of backfilled areas is positively correlated to the backfill depth (BD) of the soils, the backfilled soil temperature (BST), and the mean annual ground surface temperature (MAGST); meanwhile, climate warming can impact on thermal regimes of the backfill area. The impact of climate warming on ground temperature of the backfill will show up significantly in about 50 years after backfilling (BD at 10.0 and 20.0 m, BST at 20.0°C) under the climate warming scenario (CWS) of 0.025°C·year−1. Grey-relation analyses show that the sensitivity of the backfill recovery time declines in the order of the BD, BST and MAGST. On the basis of the abovementioned studies, the layer-by-layer backfilling in cold seasons is advised for more effective and more rapid recovery of thermal regimes of the backfilled open-pits in cold regions.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11629-017-4439-3</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0003-3133-5607</orcidid><orcidid>https://orcid.org/0000-0002-6501-6121</orcidid><orcidid>https://orcid.org/0000-0001-5844-3638</orcidid><orcidid>https://orcid.org/0000-0003-3208-3480</orcidid><orcidid>https://orcid.org/0000-0002-7855-9758</orcidid><orcidid>https://orcid.org/0000-0002-8402-7897</orcidid></addata></record> |
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subjects | Backfill Climate Climate change Coal Coal mines Cold regions Cold season Computer simulation Earth and Environmental Science Earth Sciences Ecological effects Ecological monitoring Ecology Environment Geography Global warming Measurement Permafrost Pits Recovery Recovery time Regression analysis Sensitivity analysis Soil Soil temperature Strip Surface temperature Temperature effects Thermodynamic equilibrium |
title | Thermal recovery process of a backfilled open-pit in permafrost area at the Gulian strip coal mine in Northeast China |
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