吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (6): 1810-1818.doi: 10.13278/j.cnki.jjuese.201706204
黄星1, 路莹2, 刘肖1, 段晓飞1, 朱利民1
Huang Xing1, Lu Ying2, Liu Xiao1, Duan XiaoFei1, Zhu Limin1
摘要: 为了研究人工回灌条件下地下水位抬升对悬浮颗粒在含水层中的迁移-沉积的影响机理,在室内模拟实验中,采用100 mg/L的金刚砂悬浊水回灌中粒石英砂介质,分别研究了不同抬升速率(0、2、4 cm/h)条件下人工回灌过程中的悬浮物堵塞规律。实验结果表明:地下水位抬升速率对堵塞位置和堵塞位置处悬浮物的级配影响不大,悬浮物主要淤积在0~2 cm深度处;在26 h前地下水位抬升引起的入渗量比地下水位固定的入渗量小,在26 h后二者相反;水位抬升使介质表层堵塞发展速度减慢,非堵塞层渗流状态出现非饱和时刻滞后;在堵塞层0~2 cm处地下水位抬升使堵塞速率小于地下水位固定的堵塞速率。
中图分类号:
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