steep water change
1.Wave off into shallow waters, seabed by the friction effect change steep wave front, trough ice, water points trajectory showed reciprocating flow, but also to the shore into the flow speed usually return rate greater than offshore, the net result of sediment at the bottom to the shore handling, and was the shock waves on the shore with the water current - Riviera Online accumulation.
2.According as the density change in operation has a characteristic of expansion by steep lead, and as data analysis of pore pressure at drawdown on the earth dams built by dumping soils into the ponded water suggested as well, the author has proposed that one must adopt the consolidation model of Biot to calculate the pore pressure at drawdown on those dams because it has considered for the deformation of skeleton.
