Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China
Exploitation and utilization for karst groundwater is an effective way of solving the imbalance between supply and demand of water resources in Guilin City, southwestern China. To better develop and utilize karst groundwater, the development characteristics of underground karst in Guilin City and th...
Gespeichert in:
| Veröffentlicht in: | Carbonates and evaporites 2024-06, Vol.39 (2), p.34, Article 34 |
|---|---|
| Hauptverfasser: | , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | |
|---|---|
| container_issue | 2 |
| container_start_page | 34 |
| container_title | Carbonates and evaporites |
| container_volume | 39 |
| creator | Pu, Zhenggong Huang, Qibo Liao, Hongwei Wu, Huaying Jiao, Youjun Luo, Fei Li, Tengfang Zhao, Guangshuai Zou, Changpei |
| description | Exploitation and utilization for karst groundwater is an effective way of solving the imbalance between supply and demand of water resources in Guilin City, southwestern China. To better develop and utilize karst groundwater, the development characteristics of underground karst in Guilin City and their influence on the development of karst groundwater were systematically investigated. The results show that the thick limestone formation of D
3
r
is the most ideal aquifer because it has the highest karst development and the most abundant karst groundwater. The main karst development zone is above 90 m a.s.l., and accounting for 88.5% of the karst caves, 11.5% karst caves are located in the weak karst development zone of 40–90 m a.s.l, and below 40 m a.s.l., the karst is not developed. Thus, the borehole depth for groundwater exploitation is suggested to be approximately 100–120 m owing to the ground-surface elevation of Guilin City being 140–160 m a.s.l. The zone above 120 m a.s.l. is not optimal for karst groundwater exploitation because of its high karst cave filling rate (82.89%) and low water-filling cavity ratio (16.95–30.08%), in which the karst groundwater is easily connected with surface water, therefore, an increase of possibility of collapse when abstracting groundwater. The zone between 120 and 90 m a.s.l. could be more optimal for groundwater extraction due to its medium scale of karst caves, relatively low karst cave filling rate (62.07%), and high water-filling cavity rate (30.43–62.10%) relatively. Meanwhile, a favorable groundwater exploitation and utilization region is located in the eastern study area, which has the highest underground karst development, with the highest percentage of boreholes encountering caverns (80.21%), linear karst rates (8.58%), and the medium karst cave filling rate (65.61%). This study provides a scientific basis for the exploitation of karst groundwater and construction of a backup emergency water sources for Guilin City. |
| doi_str_mv | 10.1007/s13146-024-00939-4 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2955977025</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2955977025</sourcerecordid><originalsourceid>FETCH-LOGICAL-c270t-61d3ce1128ac4972cc779197124d1ae97881d429f4037f0a8dd6d7e0ea8164573</originalsourceid><addsrcrecordid>eNp9kM9OxCAQxonRxHX1BTyReLUKlJZyNBv_JZt40TMhMHXRLqxAXX0E31q0m3jzNJmZ3_fN5EPolJILSoi4TLSmvK0I4xUhspYV30Mz2omuahhl-2hGOkkr1jTtITpK6YWQVnIpZ-jryVuIzzGM3uJXHVPGFt5hCJs1-IzNSkdtMkSXsjMJ60LlFbiIne-HEbwBHDyGj80QXNbZlSb0O6PJdauLvOD4dnRDKQuXP89xCmNebSGVXRmtnNfH6KDXQ4KTXZ2jp5vrx8VdtXy4vV9cLSvDBMlVS21tgFLWacOlYMYIIakUlHFLNUjRddRyJntOatET3VnbWgEEdEdb3oh6js4m300Mb2P5QL2EMfpyUjHZNFIIwppCsYkyMaQUoVeb6NY6fipK1E_kaopclcjVb-SKF1E9iVKB_TPEP-t_VN8dNob-</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2955977025</pqid></control><display><type>article</type><title>Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China</title><source>Springer Nature - Complete Springer Journals</source><creator>Pu, Zhenggong ; Huang, Qibo ; Liao, Hongwei ; Wu, Huaying ; Jiao, Youjun ; Luo, Fei ; Li, Tengfang ; Zhao, Guangshuai ; Zou, Changpei</creator><creatorcontrib>Pu, Zhenggong ; Huang, Qibo ; Liao, Hongwei ; Wu, Huaying ; Jiao, Youjun ; Luo, Fei ; Li, Tengfang ; Zhao, Guangshuai ; Zou, Changpei</creatorcontrib><description>Exploitation and utilization for karst groundwater is an effective way of solving the imbalance between supply and demand of water resources in Guilin City, southwestern China. To better develop and utilize karst groundwater, the development characteristics of underground karst in Guilin City and their influence on the development of karst groundwater were systematically investigated. The results show that the thick limestone formation of D
3
r
is the most ideal aquifer because it has the highest karst development and the most abundant karst groundwater. The main karst development zone is above 90 m a.s.l., and accounting for 88.5% of the karst caves, 11.5% karst caves are located in the weak karst development zone of 40–90 m a.s.l, and below 40 m a.s.l., the karst is not developed. Thus, the borehole depth for groundwater exploitation is suggested to be approximately 100–120 m owing to the ground-surface elevation of Guilin City being 140–160 m a.s.l. The zone above 120 m a.s.l. is not optimal for karst groundwater exploitation because of its high karst cave filling rate (82.89%) and low water-filling cavity ratio (16.95–30.08%), in which the karst groundwater is easily connected with surface water, therefore, an increase of possibility of collapse when abstracting groundwater. The zone between 120 and 90 m a.s.l. could be more optimal for groundwater extraction due to its medium scale of karst caves, relatively low karst cave filling rate (62.07%), and high water-filling cavity rate (30.43–62.10%) relatively. Meanwhile, a favorable groundwater exploitation and utilization region is located in the eastern study area, which has the highest underground karst development, with the highest percentage of boreholes encountering caverns (80.21%), linear karst rates (8.58%), and the medium karst cave filling rate (65.61%). This study provides a scientific basis for the exploitation of karst groundwater and construction of a backup emergency water sources for Guilin City.</description><identifier>ISSN: 0891-2556</identifier><identifier>EISSN: 1878-5212</identifier><identifier>DOI: 10.1007/s13146-024-00939-4</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aquifers ; Boreholes ; Caves ; Earth and Environmental Science ; Earth Sciences ; Exploitation ; Geology ; Groundwater ; Karst ; Limestone ; Mineral Resources ; Mineralogy ; Original Article ; Surface water ; Underground caverns ; Water resources</subject><ispartof>Carbonates and evaporites, 2024-06, Vol.39 (2), p.34, Article 34</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c270t-61d3ce1128ac4972cc779197124d1ae97881d429f4037f0a8dd6d7e0ea8164573</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13146-024-00939-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s13146-024-00939-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Pu, Zhenggong</creatorcontrib><creatorcontrib>Huang, Qibo</creatorcontrib><creatorcontrib>Liao, Hongwei</creatorcontrib><creatorcontrib>Wu, Huaying</creatorcontrib><creatorcontrib>Jiao, Youjun</creatorcontrib><creatorcontrib>Luo, Fei</creatorcontrib><creatorcontrib>Li, Tengfang</creatorcontrib><creatorcontrib>Zhao, Guangshuai</creatorcontrib><creatorcontrib>Zou, Changpei</creatorcontrib><title>Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China</title><title>Carbonates and evaporites</title><addtitle>Carbonates Evaporites</addtitle><description>Exploitation and utilization for karst groundwater is an effective way of solving the imbalance between supply and demand of water resources in Guilin City, southwestern China. To better develop and utilize karst groundwater, the development characteristics of underground karst in Guilin City and their influence on the development of karst groundwater were systematically investigated. The results show that the thick limestone formation of D
3
r
is the most ideal aquifer because it has the highest karst development and the most abundant karst groundwater. The main karst development zone is above 90 m a.s.l., and accounting for 88.5% of the karst caves, 11.5% karst caves are located in the weak karst development zone of 40–90 m a.s.l, and below 40 m a.s.l., the karst is not developed. Thus, the borehole depth for groundwater exploitation is suggested to be approximately 100–120 m owing to the ground-surface elevation of Guilin City being 140–160 m a.s.l. The zone above 120 m a.s.l. is not optimal for karst groundwater exploitation because of its high karst cave filling rate (82.89%) and low water-filling cavity ratio (16.95–30.08%), in which the karst groundwater is easily connected with surface water, therefore, an increase of possibility of collapse when abstracting groundwater. The zone between 120 and 90 m a.s.l. could be more optimal for groundwater extraction due to its medium scale of karst caves, relatively low karst cave filling rate (62.07%), and high water-filling cavity rate (30.43–62.10%) relatively. Meanwhile, a favorable groundwater exploitation and utilization region is located in the eastern study area, which has the highest underground karst development, with the highest percentage of boreholes encountering caverns (80.21%), linear karst rates (8.58%), and the medium karst cave filling rate (65.61%). This study provides a scientific basis for the exploitation of karst groundwater and construction of a backup emergency water sources for Guilin City.</description><subject>Aquifers</subject><subject>Boreholes</subject><subject>Caves</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Exploitation</subject><subject>Geology</subject><subject>Groundwater</subject><subject>Karst</subject><subject>Limestone</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Original Article</subject><subject>Surface water</subject><subject>Underground caverns</subject><subject>Water resources</subject><issn>0891-2556</issn><issn>1878-5212</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kM9OxCAQxonRxHX1BTyReLUKlJZyNBv_JZt40TMhMHXRLqxAXX0E31q0m3jzNJmZ3_fN5EPolJILSoi4TLSmvK0I4xUhspYV30Mz2omuahhl-2hGOkkr1jTtITpK6YWQVnIpZ-jryVuIzzGM3uJXHVPGFt5hCJs1-IzNSkdtMkSXsjMJ60LlFbiIne-HEbwBHDyGj80QXNbZlSb0O6PJdauLvOD4dnRDKQuXP89xCmNebSGVXRmtnNfH6KDXQ4KTXZ2jp5vrx8VdtXy4vV9cLSvDBMlVS21tgFLWacOlYMYIIakUlHFLNUjRddRyJntOatET3VnbWgEEdEdb3oh6js4m300Mb2P5QL2EMfpyUjHZNFIIwppCsYkyMaQUoVeb6NY6fipK1E_kaopclcjVb-SKF1E9iVKB_TPEP-t_VN8dNob-</recordid><startdate>20240601</startdate><enddate>20240601</enddate><creator>Pu, Zhenggong</creator><creator>Huang, Qibo</creator><creator>Liao, Hongwei</creator><creator>Wu, Huaying</creator><creator>Jiao, Youjun</creator><creator>Luo, Fei</creator><creator>Li, Tengfang</creator><creator>Zhao, Guangshuai</creator><creator>Zou, Changpei</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20240601</creationdate><title>Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China</title><author>Pu, Zhenggong ; Huang, Qibo ; Liao, Hongwei ; Wu, Huaying ; Jiao, Youjun ; Luo, Fei ; Li, Tengfang ; Zhao, Guangshuai ; Zou, Changpei</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c270t-61d3ce1128ac4972cc779197124d1ae97881d429f4037f0a8dd6d7e0ea8164573</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Aquifers</topic><topic>Boreholes</topic><topic>Caves</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Exploitation</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Karst</topic><topic>Limestone</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Original Article</topic><topic>Surface water</topic><topic>Underground caverns</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pu, Zhenggong</creatorcontrib><creatorcontrib>Huang, Qibo</creatorcontrib><creatorcontrib>Liao, Hongwei</creatorcontrib><creatorcontrib>Wu, Huaying</creatorcontrib><creatorcontrib>Jiao, Youjun</creatorcontrib><creatorcontrib>Luo, Fei</creatorcontrib><creatorcontrib>Li, Tengfang</creatorcontrib><creatorcontrib>Zhao, Guangshuai</creatorcontrib><creatorcontrib>Zou, Changpei</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Carbonates and evaporites</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pu, Zhenggong</au><au>Huang, Qibo</au><au>Liao, Hongwei</au><au>Wu, Huaying</au><au>Jiao, Youjun</au><au>Luo, Fei</au><au>Li, Tengfang</au><au>Zhao, Guangshuai</au><au>Zou, Changpei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China</atitle><jtitle>Carbonates and evaporites</jtitle><stitle>Carbonates Evaporites</stitle><date>2024-06-01</date><risdate>2024</risdate><volume>39</volume><issue>2</issue><spage>34</spage><pages>34-</pages><artnum>34</artnum><issn>0891-2556</issn><eissn>1878-5212</eissn><abstract>Exploitation and utilization for karst groundwater is an effective way of solving the imbalance between supply and demand of water resources in Guilin City, southwestern China. To better develop and utilize karst groundwater, the development characteristics of underground karst in Guilin City and their influence on the development of karst groundwater were systematically investigated. The results show that the thick limestone formation of D
3
r
is the most ideal aquifer because it has the highest karst development and the most abundant karst groundwater. The main karst development zone is above 90 m a.s.l., and accounting for 88.5% of the karst caves, 11.5% karst caves are located in the weak karst development zone of 40–90 m a.s.l, and below 40 m a.s.l., the karst is not developed. Thus, the borehole depth for groundwater exploitation is suggested to be approximately 100–120 m owing to the ground-surface elevation of Guilin City being 140–160 m a.s.l. The zone above 120 m a.s.l. is not optimal for karst groundwater exploitation because of its high karst cave filling rate (82.89%) and low water-filling cavity ratio (16.95–30.08%), in which the karst groundwater is easily connected with surface water, therefore, an increase of possibility of collapse when abstracting groundwater. The zone between 120 and 90 m a.s.l. could be more optimal for groundwater extraction due to its medium scale of karst caves, relatively low karst cave filling rate (62.07%), and high water-filling cavity rate (30.43–62.10%) relatively. Meanwhile, a favorable groundwater exploitation and utilization region is located in the eastern study area, which has the highest underground karst development, with the highest percentage of boreholes encountering caverns (80.21%), linear karst rates (8.58%), and the medium karst cave filling rate (65.61%). This study provides a scientific basis for the exploitation of karst groundwater and construction of a backup emergency water sources for Guilin City.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s13146-024-00939-4</doi></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0891-2556 |
| ispartof | Carbonates and evaporites, 2024-06, Vol.39 (2), p.34, Article 34 |
| issn | 0891-2556 1878-5212 |
| language | eng |
| recordid | cdi_proquest_journals_2955977025 |
| source | Springer Nature - Complete Springer Journals |
| subjects | Aquifers Boreholes Caves Earth and Environmental Science Earth Sciences Exploitation Geology Groundwater Karst Limestone Mineral Resources Mineralogy Original Article Surface water Underground caverns Water resources |
| title | Underground karst development characteristics and their influence on exploitation of karst groundwater in Guilin City, southwestern China |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-13T08%3A57%3A56IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Underground%20karst%20development%20characteristics%20and%20their%20influence%20on%20exploitation%20of%20karst%20groundwater%20in%20Guilin%20City,%20southwestern%20China&rft.jtitle=Carbonates%20and%20evaporites&rft.au=Pu,%20Zhenggong&rft.date=2024-06-01&rft.volume=39&rft.issue=2&rft.spage=34&rft.pages=34-&rft.artnum=34&rft.issn=0891-2556&rft.eissn=1878-5212&rft_id=info:doi/10.1007/s13146-024-00939-4&rft_dat=%3Cproquest_cross%3E2955977025%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2955977025&rft_id=info:pmid/&rfr_iscdi=true |