›› 1986, Vol. 6 ›› Issue (2): 163-169.

• 特区地理 • 上一篇    下一篇

深圳市水土流失问题

李小彬   

  1. 广州地理研究所
  • 出版日期:1986-04-30 发布日期:1986-04-30

ON THE PROBLEM OF SOIL EROSION IN SHENZHEN

LI Xiaobin   

  1. Guangzhou Institute of Geography
  • Online:1986-04-30 Published:1986-04-30

摘要: 深圳市位于南亚热带南部,地势为东高西低,东部山地,山高坡陡,构成岩石以火山岩和石英岩为主,西部滨海平原,组成物质以冲积洪积物为主,中部为低丘台地,以花岗岩和砂页岩为主.深圳水土流失区主要分布在中部的花岗岩低丘台地上.研究水土流失问题,对于山地合理利用、环境保护及当地农业生产,有现实意义.本文以1982—1983年在深圳土地资源调查中所获得的资料,通过对水土流失现状的剖析,探讨其引起侵蚀的原因,并提出整治意见.

Abstract: Soil erosion occurred in the low granite hills and flatforms in middle Shenzhen area.It is divided into intensity(9100T/KM2.year),moderate(6500-9100T/KM2.year) and light(2600-6500T/KM2.year),based on the erosion modulus calculated by observing the tree roots laid bare above the ground,in combination with the present conditions o f soil erosion.The distribution of main severe erosion areas and their characteristics were described in this paper.It is considered that the improper human activities,such as deforestation and cultivation on the steep slopes in hilly areas,as "well as excavation in constructing highways and dams are the main factors to cause severe erosion.Natural conditions such as the weathering layers,rainfall and topograporaplay an important part in this process.