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1.then the model of groundwater movement is solved for actual velocity of groundwater flow in every unit;
再解地下水运动方程得到各单元的地下水实际流速;收藏指正
2.The Meso Cenozoic palaeohydrodynamic fields in Lanping area was studied by means of sedimentary basinsimulation technique. The results show that groundwater moved from the center and the western part of the basin to the south during Late Cretaceous with a current velocity about 1.85 mm/a~2.93 mm/a and an average about 2.24 mm/a.
本文利用沉积盆地模拟技术对兰坪地区中新生代的古水动力场进行了详细研究 ,结果表明盆地晚白垩世地下水是由中、西部向南部一带流动 ,流速约为 1.85 m m/ a~2 .93mm/ a,平均 2 .2 4mm/ a。收藏指正
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