塔克拉玛干沙漠腹地地下水质的应用评价  

ASSESSMENT OF THE SVITABILITY OF UNDERGROUND WATER FOR IRRIGATION IN THE HINTERLAND OF TAKLIMAKAN DESERT

作　　者：何欣东 丛自立[1] 陈广庭[1] 高前兆[1] 陈国雄[1] 

机构地区：[1]中国科学院兰州沙漠研究所

出　　处：《中国沙漠》1996年第1期24-26,共3页Journal of Desert Research

摘　　要：长期利用高矿化度地下水灌溉造成沙质土壤的次生盐渍化是塔克拉玛干沙漠腹地建立人工生态系统的主导限制因素之一。据１９９２年与１９９４年在塔克拉玛干沙漠腹地满参与中三点２年的试验研究结果认为：在灌溉水的适宜应用条件下，利用矿化度为４ｇ／Ｌ～５ｇ／Ｌ的地下水灌溉种植瓜果蔬菜和固沙植物是能够成功的；生长季内土壤含盐量＜０．１％。With respect to establish artificial ecosystem itself, one of key limiting factors is soil salt stress which caused by irrigating underground water with higher mineralization degree for long term due to local intense evaporation in the hinterland of Taklimakan Desert. The experimental results for two years show: under Suitable application conditions of sprinkling water, it can succeed in making use of underground water with about 4 g/L～5 g/L of mineralization degree to irrigate vegetable and sand-binding plants, and salts content in the soil was lower than 0. 1% within the growth phase of plants.

关 键 词：塔克拉玛干沙漠 地下水 水质评价 

分 类 号：P641.12[天文地球—地质矿产勘探]