程海

程海是一个微碱性的闭口湖，pH9.1，DO9.01mg／L，总硬度17.10德国度，总碱度30.41德国度。

Chenghai lake is a alkalescence lake , has not outlet . pH is 9.1 , total hardness is 17.10 Germanic degrees , total basicity is 30.41 Germanic degrees .

研究结果表明，程海是一个由淡水湖向咸水湖过渡的苏打湖，并且不再届贫营养湖。

The research shows that the Chenghai Lake is a tsoda lake which is in transition from freshwater lake to saltwater lake and no longer an oligotrophic lake .

程海断裂带断层泥中石英碎砾表面SEM特征及断层活动状态的分析

The SEM Characteristics of the Surface of Quartz Grains in the Gouge of Chenghai Fault and Evaluation of Its Activity State Painting

程海螺旋藻养殖废水拟在对其COD、pH、SS进行初级处理后，抽入黄泥田水库稀释，降低其含盐量后用于农灌。

After the primary treatment on its COD , pH and SS , the wastewater from the Spirulina raising is used in agricultural fields after infusing into the reservoir for dilution and reducing its salt content .

程海断裂带挽近期活动性研究

Neoid activity on the Chenghai fracture

程海的环境及保护

The environment and protection of Chenghai

程海断裂控制下的次级块体&滇西北块体与滇中块体的边界沿程海断裂作相向运动。

The Chenghai fault , as a boundary of tectonic sub blocks , makes the Northwestern Yunnan block and Middle Yunnan block move clockwise , and their margins move oppositely along the Chenghai fault .

提出祥云推覆构造是在古近纪印度欧亚板块俯冲、碰撞导致金沙江红河断裂带和程海断裂带走滑运动的区域构造背景下形成的。

This paper proposed that Xiangyun nappe was formed at the regional tectonic settings of the Paleogene India-Eurasian plate subduction , collision resulted in the Jinsha River-Red River fault zone and Chenghai fault zone strike-slip movement .