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作 者:雷米 周金龙[1,2] 魏兴 张杰[1,2] 范薇 LEI Mi;ZHOU Jinlong;WEI Xing;ZHANG Jie;FAN Wei(College of Water Conservancy and Civil Engineering,Xinjiang Agricultural University,Urumqi 830052,China;Xinjiang Hydrology and Water Resources Engineering Research Center,Urumqi 830052,China)
机构地区:[1]新疆农业大学水利与土木工程学院,新疆乌鲁木齐830052 [2]新疆水文水资源工程技术研究中心,新疆乌鲁木齐830052
出 处:《人民黄河》2021年第2期100-105,共6页Yellow River
基 金:新疆农业大学研究生“水利工程”重点学科研究项目(SLXK-YJS-2018-04)。
摘 要:为了解库尔勒市地下水超采区综合治理效果,采用层次分析法构建库尔勒市地下水超采区综合治理评价指标体系,同时采用回归模型对地下水水位、水量进行相关分析,结果表明:库尔勒市地下水超采区综合治理方案制定合理,综合治理效果基本达到要求;地下水水位回升区主要位于山前倾斜平原的沙依东园艺场、英下乡、库尔楚园艺场、上户镇、塔什店镇、兰干乡和恰尔巴格乡以及冲积平原的哈拉玉宫乡和普惠地区,影响地下水水位动态变化的主要因素为人类活动(地下水压采)和地质因素,水文因素对地下水水位影响存在一定滞后性。In order to understand the comprehensive control effect of groundwater over⁃exploitation areas in Korla City,the assessment system of groundwater over⁃exploitation areas was constructed by analytic hierarchy process.At the same time,the regression method was used to an⁃alyze the correlation of groundwater level and quantity.The results show that the comprehensive control plan of the groundwater over⁃exploita⁃tion areas is reasonable and the comprehensive control effect basically can meet the requirements.Rising areas of groundwater level are mainly located in piedmont sloping plain such as Shayidong Garden Spot,Yingxia Township,Kuerchu Garden Spot,Shanghu Township,Tashidian Township,Langan Township and Qiaerbage Township and it also includes Halayugong Township and Puhui Town in the alluvial plain.It is found that the main factors affecting groundwater dynamics are human activities(groundwater restricted mining)and geological factors,the depth of groundwater has lagged reaction to the effect of hydrologic factors.
分 类 号:P641[天文地球—地质矿产勘探] X523[天文地球—地质学]
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