| 青岛地区玄武岩含水层(体)的开发 |
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| 引用本文： | 邱汉学.青岛地区玄武岩含水层(体)的开发[J].中国海洋大学学报(自然科学版),1993(Z1). |
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| 作者姓名： | 邱汉学 |
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| 作者单位： | 青岛海洋大学海洋地质系 |
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| 摘 要： | 研究青岛地区玄武岩地质、水文地质条件,提出玄武岩地下水及其含水层(体)的开发途径:干旱年份尽可能多开采地下水,丰水年份人工回灌以增加水资源可利用量。人工回灌的水源可利用大沽河弃水,通过现有井、钻孔及地下隧道进行。
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| 关 键 词： | 青岛地区 玄武岩含水层(体) 合理开发利用 人工回灌 |
RATIONAL DEVELOPMENT OF BASALTIC AQUIFER IN QINGDAO AREA |
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| Qtu Hanxue.RATIONAL DEVELOPMENT OF BASALTIC AQUIFER IN QINGDAO AREA[J].Periodical of Ocean University of China,1993(Z1). |
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| Authors: | Qtu Hanxue |
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| Institution: | Department of Marine Geology |
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| Abstract: | The groundwater in the basaltic aquifer and the aquifer itself are hopeful resources. It is found that the water in the basaltic aquifer is abundant between 20m and 50m of buried depth in Qingdao area. Adequate and rational development in arid periods and years can make space for artificial recharge in humid seasons or years. This measure can greatly increase the abstraction amount of groundwater. |
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| Keywords: | Qingdao area basaltic aquifer rational development artificial recharge |
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