The boundary condition at bed surface of diffusion equation of nonuniform sediment is derived based on the concept of exchange intensity of stochastic theory by the author.
The boundary condition at bed surface of diffusion equation of nonuniform sediment is derived based on the concept of exchange intensity of stochastic theory by the author.
摘要文中首先给出了由我们建立的床面泥沙交换理论导出的非均匀沙扩散方程的边界条件。