干旱区生态环境知识资源中心(Arid): 靖边县四柏树海则引水回渗试验

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	靖边县四柏树海则引水回渗试验
其他题名	Analysis of Experiment about Diversion Recharge in Sibaishuhaize Lake of Jingbian County
	宋寿鹏 1; 杨涛 2; 康卫东 3
来源期刊	水土保持研究
ISSN	1005-3409
出版年	2010
卷号	17 期号:4 页码:195-197
中文摘要	该文以四柏树海则野外回渗试验为基础,取得引水回渗入渗系数0.01m/d,并据此确定四柏树海则全年有水的最小引水量;通过建立地下水数值模拟模型,预测现状开采条件下,四柏树海则引水回渗引起的地下水位升幅变化. 结果表明:保证四柏树海则全年有水,引水回灌量需达到20万m~3/a,入渗补给地下水量为16万m~3/a,可增加海则面积42623m~2,水位增幅大于1m. 显然,引水回渗对营造沙漠绿洲及回补地下水源,实现绿洲生态的恢复和人居环境的改善具有重要意义
英文摘要	Based on field diversion recharge experiment in Sibaishuhaize Lake, the infiltration coefficient is 0.01m/d, and then minimal diversion with water all the year round was confirmed. Variable amplitude of groundwater level in the current condition of exploitation was predicts through the establishment of groundwater numerical simulated mode. The results showed water quantity of diversion recharge should achieve 2010~4 m~3/a, and infiltration is 16 10~4 m~3/a in order to ensure that Sibaishuhaize has water all the year round, increasing area of Sibaishuhaize by 42 623m~2, the increasing amplitude of groundwater level is more than 1m. Obviously, diversion recharge is of great significance for recovering the oasis and supplementary water sources, realizing the improvement of restoration of oasis ecology and living environment for human beings
中文关键词	引水回渗 ; 入渗系数 ; 数值模拟
英文关键词	diversion recharge infiltration coefficient numerical simulation
语种	中文
国家	中国
收录类别	CSCD
WOS类目	MINERALOGY
WOS研究方向	Mineralogy
CSCD记录号	CSCD:3979266
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/225685
作者单位	1.同济大学地下建筑与工程系, 上海 200092, 中国; 2.石家庄经济学院, 石家庄, 河北 050031, 中国; 3.西北大学地质学系, 西安, 陕西 710029, 中国
推荐引用方式 GB/T 7714	宋寿鹏,杨涛,康卫东. 靖边县四柏树海则引水回渗试验[J],2010,17(4):195-197.
APA	宋寿鹏,杨涛,&康卫东.(2010).靖边县四柏树海则引水回渗试验.水土保持研究,17(4),195-197.
MLA	宋寿鹏,et al."靖边县四柏树海则引水回渗试验".水土保持研究 17.4(2010):195-197.