The Variety of Runoff and Sediment and the Sustainable Development in Fenhe Valley

Fenhe valley located in the region of soil erosion in the middle Yellow River, water resources is always very short. Especially in recent decades, plentiful human activities affected the change of runoff. The negative function brought by the change to Fenhe valley is unexpected. In order to survive and develop, the people destroyed forest and reclaimed wasteland excessively, which made ecological environment breach. Water and soil losses, waterlog, drought disaster, pollution of water quality and soil salinification etc. restricted the development in Fenhe valley. In recent decades, the days that the observed discharge of Hejin hydrology station in Fenhe less than 1m 3 /s is up to more than 100 days. It became almost intermittent river due to long time near break-off. Under the condition of same rainfall, runoff decreased largely and concentration of water quality pollution increased. It is very disadvantage to the Yellow River that runoff decreased in Fenhe valley. Owing to excessive population, high degree of water resources exploitation and utilization, and finite local water resources, we must strengthen the management of utilization of exist local water resources, heighten the ratio of water usage, save water usage, and protect water-soil resources for the great development of socio-economic in Fenhe valley.