黄土区长武塬地下水埋深动态特征及影响因素分析
【目的】明确地下水补给机制并指导地下水资源合理开发。【方法】基于1976—2017年长武塬区5眼监测井的地下水埋深数据,分析了地下水埋深动态变化,并利用互相关和多元线性回归等方法识别地下水埋深的影响因素。【结果】长武塬区地下水埋深介于25~95 m之间,各井因水文地质和人为干扰程度等差异表现出不同的波动特征。地下水埋深总体呈波动下降趋势,降幅介于0.08~0.21 m/a。气象因子、植被和人为因素在年内或年际尺度对地下水埋深都有一定影响,但主导性不同。年际尺度,人为因素主导地下水埋深变化,贡献率达74%。年内尺度,植被是影响地下水埋深的主要因素,贡献率为40%。【结论】人口、GDP和苹果园面积...
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description | 【目的】明确地下水补给机制并指导地下水资源合理开发。【方法】基于1976—2017年长武塬区5眼监测井的地下水埋深数据,分析了地下水埋深动态变化,并利用互相关和多元线性回归等方法识别地下水埋深的影响因素。【结果】长武塬区地下水埋深介于25~95 m之间,各井因水文地质和人为干扰程度等差异表现出不同的波动特征。地下水埋深总体呈波动下降趋势,降幅介于0.08~0.21 m/a。气象因子、植被和人为因素在年内或年际尺度对地下水埋深都有一定影响,但主导性不同。年际尺度,人为因素主导地下水埋深变化,贡献率达74%。年内尺度,植被是影响地下水埋深的主要因素,贡献率为40%。【结论】人口、GDP和苹果园面积的增加对地下水埋深影响较大,需要考虑人类活动与水资源间的可持续性。 |
doi_str_mv | 10.13522/j.cnki.ggps.2021656 |
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WANG, Wanzhou ; YAN, Xin ; LI, Bingbing ; LI, Zhi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p1282-455d72951df05ef6bdd6963578241b0bb447e7e1761b040dfac3e2c00daeee663</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi ; eng</language><creationdate>2022</creationdate><topic>Agricultural development</topic><topic>Anthropogenic factors</topic><topic>Boreholes</topic><topic>Cross correlation</topic><topic>Economic development</topic><topic>Environmental changes</topic><topic>Environmental management</topic><topic>Geology</topic><topic>Groundwater</topic><topic>Groundwater levels</topic><topic>Groundwater management</topic><topic>Groundwater recharge</topic><topic>Human influences</topic><topic>Hydrogeology</topic><topic>Loess</topic><topic>Orchards</topic><topic>Population studies</topic><topic>Resource management</topic><topic>Sustainable development</topic><topic>Vegetation</topic><topic>Water resources</topic><topic>Water table</topic><toplevel>online_resources</toplevel><creatorcontrib>SUN Jineng</creatorcontrib><creatorcontrib>WANG, Wanzhou</creatorcontrib><creatorcontrib>YAN, Xin</creatorcontrib><creatorcontrib>LI, Bingbing</creatorcontrib><creatorcontrib>LI, Zhi</creatorcontrib><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>Agricultural 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 China</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Guanʻgai paishui xuebao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>SUN Jineng</au><au>WANG, Wanzhou</au><au>YAN, Xin</au><au>LI, Bingbing</au><au>LI, Zhi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>黄土区长武塬地下水埋深动态特征及影响因素分析</atitle><jtitle>Guanʻgai paishui xuebao</jtitle><date>2022-10-01</date><risdate>2022</risdate><volume>41</volume><issue>10</issue><spage>90</spage><epage>97</epage><pages>90-97</pages><issn>1672-3317</issn><abstract>【目的】明确地下水补给机制并指导地下水资源合理开发。【方法】基于1976—2017年长武塬区5眼监测井的地下水埋深数据,分析了地下水埋深动态变化,并利用互相关和多元线性回归等方法识别地下水埋深的影响因素。【结果】长武塬区地下水埋深介于25~95 m之间,各井因水文地质和人为干扰程度等差异表现出不同的波动特征。地下水埋深总体呈波动下降趋势,降幅介于0.08~0.21 m/a。气象因子、植被和人为因素在年内或年际尺度对地下水埋深都有一定影响,但主导性不同。年际尺度,人为因素主导地下水埋深变化,贡献率达74%。年内尺度,植被是影响地下水埋深的主要因素,贡献率为40%。【结论】人口、GDP和苹果园面积的增加对地下水埋深影响较大,需要考虑人类活动与水资源间的可持续性。</abstract><cop>Xinxiang City</cop><pub>Chinese Academy of Agricultural Sciences (CAAS) Farmland Irrigation Research Institute Editorial Office of Journal of Irrigation and Drainage</pub><doi>10.13522/j.cnki.ggps.2021656</doi><tpages>8</tpages></addata></record> |
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subjects | Agricultural development Anthropogenic factors Boreholes Cross correlation Economic development Environmental changes Environmental management Geology Groundwater Groundwater levels Groundwater management Groundwater recharge Human influences Hydrogeology Loess Orchards Population studies Resource management Sustainable development Vegetation Water resources Water table |
title | 黄土区长武塬地下水埋深动态特征及影响因素分析 |
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