...icNer B.D.,BaumgaRner J.v., Wigington&,et at,1997)等;水力学方法主要代表方法有湿周法(wetted perimeter method)(Ubertini L,Manebla P.Casadei S.,1 996)和R2CROSS法(Mosley M. P.,1982)等。
基于20个网页-相关网页
改进湿周法 improved wetted perimeter method
Shortcoming that ’inflection’ point in wet perimeter method always determined subjectively by eye from a graph is analyzed. The subjectivity is overcome by defining the break in shape using mathematical techniques that was put forward by Gippel.
由于河道湿周法在确定突变点中存在主观性的缺陷,而最大曲率法可以客观的确定河流生态环境需水,避免了主观性。
参考来源 - 南方地区生态环境需水研究Secondly, we introduce some methods to estimate water right of ecological environment such as Montana method, Wetted perimeter method, Maintain flow in Japan and Water demand in China.
在生态水权的计算方法中,重点介绍了Montana法、湿周法、日本的维持流量及我国的河道内和河道外两类生态和环境需水。
参考来源 - 生态水权的理论与实践·2,447,543篇论文数据,部分数据来源于NoteExpress
应用推荐