| 滹滏平原地下水系统脆弱性最佳地下水水位埋深探讨 |
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| 引用本文： | 严明疆,张光辉,王金哲,聂振龙,申建梅,郝明亮.滹滏平原地下水系统脆弱性最佳地下水水位埋深探讨[J].地球学报,2009,30(2):243-248. |
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| 作者姓名： | 严明疆 张光辉 王金哲 聂振龙 申建梅 郝明亮 |
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| 作者单位： | 中国地质科学院水文地质环境地质研究所, 河北石家庄 050061;中国地质科学院水文地质环境地质研究所, 河北石家庄 050061;中国地质科学院水文地质环境地质研究所, 河北石家庄 050061;中国地质科学院水文地质环境地质研究所, 河北石家庄 050061;中国地质科学院水文地质环境地质研究所, 河北石家庄 050061;中国地质科学院水文地质环境地质研究所, 河北石家庄 050061 |
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| 基金项目： | 国家重点基础性研究项目(编号: 2006CB403401)、中国地质科学院基本科研业务费专项经费(编号: Ywf060718)、国家科技支撑计划项目 (No. 2007BAD69B02)资助。 |
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| 摘 要： | 笔者以滹滏平原为研究区, 采用统计分析的方法, 分析了地下水防污性与地下水资源脆弱性随地下水位埋深之间的变化关系。结果表明, 当地下水位埋深增大时, 地下水防污性增强的地区, 地下水资源脆弱性也增高；通过二者之间变化关系, 认为受地下水位埋深制约及地下水位埋深对二者的不同影响, 存在使地下水系统脆弱性最佳的地下水位埋深区间；通过地下水位埋深对地下水防污性与地下水资源脆弱性影响及其制约关系, 确定滹滏平原淡水区和咸水区地下水系统脆弱性最佳地下水位埋深分别为27~30 m和15~19 m。
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| 关 键 词： | 地下水系统脆弱性最佳地下水位埋深 地下水资源脆弱性 地下水防污性 变化关系 |
Discussion on the Groundwater Depth of the Optimal Groundwater System Vulnerability in Hufu Plain |
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| YAN Ming-jiang,ZHANG Guang-hui,WANG Jin-zhe,NIE Zhen-long,SHEN Jian-mei and HAO Ming-liang.Discussion on the Groundwater Depth of the Optimal Groundwater System Vulnerability in Hufu Plain[J].Acta Geoscientia Sinica,2009,30(2):243-248. |
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| Authors: | YAN Ming-jiang ZHANG Guang-hui WANG Jin-zhe NIE Zhen-long SHEN Jian-mei and HAO Ming-liang |
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| Institution: | Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061;Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang, Hebei 050061 |
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| Abstract: | The statistical analysis method was used to analyze the relationship between the aquifer sensitivity and the groundwater vulnerability with groundwater depth in Hufu plain. The result demonstrates that the vulnerability of groundwater resources increases and the aquifer sensitivity becomes stronger with the increasing groundwater depth. Based on an analysis of the relationship between the aquifer sensitivity and the groundwater vulnerability, the authors consider that the depth of groundwater is the key factor affecting groundwater resource vulnerability as well as aquifer sensitivity, and there exists a water table range of the optimal groundwater system vulnerability. The range is different in different areas. The water table range of the optimal groundwater vulnerability for fresh water and for saline water is defined at 27~30 m and 15~19 m respectively. |
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| Keywords: | The groundwater depth of the optimal groundwater system vulnerability groundwater resources vulnerability aquifer sensitivity change relationship |
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