太行山前平原非河道条件下地下调蓄功能实验研究——以滹沱河冲洪积平原为例  

Study on Artificial Underground Reserve Function in the Aquifer away from River Channels in Taihang Piedmont Plain of China:A Case Study in the Alluvial Plain of Hutuohe River

作　　者：张光辉[1] 费宇红[2] 邢开 刘克岩 王金哲[1] 申建梅[1] 聂振龙[1] 

机构地区：[1]中国地质科学院水文地质环境地质研究所,河北石家庄050061 [2]河海大学,江苏南京210098 [3]黑龙江省水文地质勘查院,黑龙江哈尔滨150036 [4]河北省水文水资源勘测局,河北石家庄050031

出　　处：《水文》2004年第2期15-19,共5页Journal of China Hydrology

基　　金：国家科技部公益项目"太行山前平原地下调蓄潜力与效益"(2000-163)资助

摘　　要：通过实验研究探讨了太行山前平原地下调蓄能力,实验研究表明,在汇水坑渗、井灌和引水渠渗条件下,太行山前冲洪积平原地下调蓄功能不仅与地表积水深度、入渗时间有关,而且还与汇水总量的多少有关。单位时间渗漏量的大小与地表蓄水深度呈正相关关系。地表蓄水深度愈大,单位时间渗漏量愈大;累计渗漏量随着入渗时间的延长而增加,渗漏速率随着累计渗漏量的增加而减小。采用井灌方式进行地下调蓄的关键,是选择具有强渗透性的层位。The result of experiments implies that the reserve function of the aquifers from artificial recharge in Taihang piedmont plain of China is related, not only to the reservoir depth of surface water and the time of water infiltration but also to the accumulative total volume of water which flows into the reservoir under the condition of pond infiltration, well injection and channel infiltration. The infiltration rate increases with the increasing of the reservoir depth of surface water and decreases with its decreasing, while the accumulative amount of infiltrated water increases with the increasing time. The key for underground artificial reserve trough well injection is to select the high permeable formation.

关 键 词：山前冲洪积平原 坑渗与井灌 汇水静态入渗 渠系引水 地下调蓄功能 滹沱河冲洪积平原 

分 类 号：P641.2[天文地球—地质矿产勘探]