水闸沿江、沿海侧潮位的变化规律不拒绝正态分布、对数正态分布和极值I型分布，但极值I型分布最优。
Along Yangtze river and Yellow sea side it doesn't refuse normal school, logarithm normal school, and extremum I distributing, but coincides with extremum I distributing best.
极值I型分布不适宜作为坡残积黏土质围岩黏聚力、内摩擦角的概率分布；
Extreme type I isn′t equal to be probability distribution of cohesion and internal friction angle of clinosol and residual cohesive soil surrounding rock.
极值I型分布不适宜作为坡残积黏土质围岩黏聚力、内摩擦角的概率分布；
Extreme type I isn′t equal to be probability distribution of cohesion and internal friction angle of clinosol and residual cohesive soil surrounding rock.
应用推荐