Comparative Study for Regional Terrain Factors in Coarse Sand Source Area of Loess Plateau
|更新时间:2025-03-12
|
Comparative Study for Regional Terrain Factors in Coarse Sand Source Area of Loess Plateau
Bulletin of Soiland Water ConservationVol. 31, Issue 1, Pages: 111-114(2012)
作者机构:
1. 北京师范大学地理学与遥感科学学院,北京,100875
2. 水利部水土保持监测中心,北京,100055
3. 黄河水土保持生态环境监测中心,陕西,西安,710021
作者简介:
基金信息:
DOI:
CLC:
Published:2012
稿件说明:
移动端阅览
GAO Yun-fei, LI Zhi-guang, YANG Sheng-tian, et al. Comparative Study for Regional Terrain Factors in Coarse Sand Source Area of Loess Plateau[J]. Bulletin of Soiland Water Conservation, 2012, 31(1): 111-114.
DOI:
GAO Yun-fei, LI Zhi-guang, YANG Sheng-tian, et al. Comparative Study for Regional Terrain Factors in Coarse Sand Source Area of Loess Plateau[J]. Bulletin of Soiland Water Conservation, 2012, 31(1): 111-114.DOI:
Comparative Study for Regional Terrain Factors in Coarse Sand Source Area of Loess Plateau
By taking small watershed on the 1∶10 000 scaled topographic map of Qingshuichuan basin in the coarse sand source area of the Loess Plateau as a basic cell
terrain factors for regional soil erosion
including surface relief
variance coefficient
and contour line density
are extracted from 1∶250 000 scaled digital elevation model.The terrain factors calculated from the 1∶10 000 scaled map are regarded as truth values to fit the calculation method of terrain factors for soil erosion in each region.Results showed that only the contour line density is an appropriate index of terrain factors for regional soil erosion.The method has been applied in the lower reaches of Huangpuchuan River
with the deviation less than 10%.Such a good simulation result indicates that the method can be used as a reference to index determination in the calculation of regional terrain factor for soil erosion.