论文部分内容阅读
依据新疆地矿局昌吉地下水均衡试验场 1 998~ 2 0 0 0年不同水位埋深粘土试筒 (2 .0m2 或 4 .0m2 )内负压计监测资料 ,得出天山北坡平原区粘土包气带零通量面仅在潜水位埋深≥ 6m的条件下稳定存在的结论
According to the monitoring data of the negative pressure gauge in the buried depth clay test tube (2.0m2 or 4.0m2) from 1998 to 2001 in Changji Groundwater Balance Test Site of Xinjiang Bureau of Geology and Mineral Resources, the clay package in the northern slope of Tianshan The results show that the zonal with zero flux surface is stable only at the depth of 6 m