【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。更多还原

【Abstract】 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 ofwater infiltration but also to the accumulative total volume of water which flows into the reservoir under thecondition of pond infiltration, well injection and channel infiltration. The infiltration rate increases with theincreasing of the reservoir depth of surface water and decreases with its decreasing, while the accumulativeamount of infiltrated water increases with the increasing time. The key for underground artificial reserve troughwell injection is to select the high permeable formation.更多还原