摘要
水网区在宏观尺度上可被视为一种连续介质，可用水在多孔介质中的运动来比拟水网中水的运动。在这种概化条件下，推求出水网区水体运动的表述方法。利用这一方法建立的太湖水网区区域水位模型，与实际情况相比，获得了较好的效果。
The water reticulation is regarded as a continuous medium and water movement in the system is analogized with that in porous medium in macro-scopic scale. The expression of water movement in the system has been derived under above conditions. The model in Tat Lake Area has been developed with the method and the results are reasonable.
出处
《水科学进展》
EI
CAS
CSCD
1995年第3期205-210,共6页
Advances in Water Science
关键词
水网
模型化
连续介质
水位模型
water reticulation
modeling
macro-scale
two-dimensional movement
continuum
waterleve
model
terraqueous complex.
