| 临淄地区水资源特征 |
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| 引用本文： | 贾贵廷,牛平山.临淄地区水资源特征[J].石家庄经济学院学报,1995(2). |
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| 作者姓名： | 贾贵廷 牛平山 |
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| 作者单位： | 河北地质学院水工系 |
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| 摘 要： | 临淄地区水资源丰富，地表水、地下水已得到充分利用。地下水主要赋存在寒武—奥陶系碳酸盐岩裂隙岩溶含水岩组和第四系孔隙含水岩组，二者在山前形成越流系统。地表水与地下水联系密切，互相转化，现有地表蓄水工程和地下水开采水源地布置合理，不易再增加地表蓄水工程和地下水开采量。
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| 关 键 词： | 临淄地区，水资源，含水岩组，边界条件 |
The Characteristics of the Water Resource in Linzhi Region |
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| Jia Guiting, Niu pingshan.The Characteristics of the Water Resource in Linzhi Region[J].Journal of Shijiazhuang University of Economics,1995(2). |
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| Authors: | Jia Guiting Niu pingshan |
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| Abstract: | The water resource in Linzhi region is abundant, and the surface water and the groundwater have made of full use. The groundwater exists mainly in fissure-karst aquifer system of carbonafite of cambrain system of & Ordovician system and pore aquiter system of Quternary system, which form a leakage system in front of mountains. The relation between the surface water and the groundwater is close and can transform each other. The distribution of the present water storage projects and the groundwater-supply bases is proper, so it should not increase the surface water storage projects and the groundwater mining. |
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| Keywords: | Linzhi Region water resource aquiter system boundary condition |
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