自然杂志 ›› 2008, Vol. 30 ›› Issue (1): 28-31.

• 专题综述 • 上一篇    下一篇

黄土丘陵区不同土地利用方式产沙规律研究

连振龙①,刘普灵②,徐学选③,贺萍④   

  1. ①硕士研究生,②③研究员,中国科学院水利部 水土保持研究所 黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西 杨陵, 712100; ④ 安塞县农业经济管理站,陕西 安 , 717400)
  • 收稿日期:2007-12-13 修回日期:2007-12-13 出版日期:2008-02-20 发布日期:2008-02-20

Study on Sediment-yield Characteristics of Different Land Use in Loess Hilly Region

Lian Zhenlong①,Liu Puling②,Xu Xuexuan③,He Ping④   

  1. ①Graduate Student,②③Professor,Institute of Soil and Water Conservation, Chinese Academy of Science and Ministry of Water Resources,
    State Key Laboratory of Soil Erosion and Dryland Farming On the Losse Plateau, YangLing,712100 Shaanxi,China ;
    ④Asistont Engineer,AnSai Agro-economy Administration, AnSai, 717400,Shaanxi,China
  • Received:2007-12-13 Revised:2007-12-13 Online:2008-02-20 Published:2008-02-20

摘要: 通过对黄土丘陵区退耕还林(草)坡地的人工模拟降雨实验资料的分析,认为区分导致该区草灌坡地不同产流方式的临界降雨强度为1.40~1.45mm/min,裸露坡耕地产沙强度产生明显变化的临界降雨强度为1.50~1.53mm/min。同时讨论了该区不同土地利用方式的产沙规律,给出了其相关方程。研究结果表明植被通过改变坡面产水产沙规律,对减少坡面侵蚀产沙作用显著。

Abstract: By analysis of the data of field simulated rainfalls, this paper makes the conclusion that in the Loess Hilly Region, the critical rainfall intensity that can distiguish the two main runoff-production modes on grass and bushes ranges from 1.40 mm/min to 1.45mm/min. And on bare sloping field, the critical rainfall intensity that make sharp transfomation of sediment-yield intensity ranges from 1.50mm/min to 1.53mm/min. At the same time, this paper talks over the sediment-yield charicterdistics of different land use, and finds their corelative equation. Results indicate the great benefits of vegetation on decreasing slope soil erosion.