文章摘要
董亚维,吴永红,马卫星,陈桂荣.基于遥感监测的河龙区间水土保持效果分析Journal of Water Resources and Water Engineering[J].,2012,23(1):157-160
基于遥感监测的河龙区间水土保持效果分析
Analysis on effectiveness of soil and water conservation in Hekou Town - Longmen sector based on remote sensing monitoring
Received:August 23, 2011  Revised:November 07, 2011
DOI:
中文关键词: 水土流失  动态监测  遥感监测  水土保持成效
英文关键词: soil and water erosion  dynamic monitoring  remote sensing monitoring  effectiveness of soil and water conservation
基金项目:
Author NameAffiliation
DONG Yawei Yellow River Soil and Water Conservation Eco-Environment Monitoring Center,Xi’an 710021, China 
WU Yonghong XifengSoil and Water Conservation Experimental Station under Yellow River Water Conservancy Committee, Qingyang 745000, China 
MA Weixing Yellow River Soil and Water Conservation Eco-Environment Monitoring Center,Xi’an 710021, China 
CHEN Guirong Yellow River Soil and Water Conservation Eco-Environment Monitoring Center,Xi’an 710021, China 
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中文摘要:
      以遥感影像为主要信息源,通过大量的野外调查,建立了河龙区间土地利用、植被覆盖度影像解译标志,在地理信息系统支持下,采用计算机辅助下的人工解译,对河龙区间水土流失进行了动态监测。结果显示:河龙区间80.40%的土壤侵蚀为水蚀,19.60%为风蚀。土壤侵蚀强度以中度侵蚀、强度侵蚀为主,其次是微度侵蚀,再次是轻度和极强度侵蚀,剧烈侵蚀所占比例最小。与2000年相比,2008年土壤侵蚀强度整体下降,微度、轻度、中度侵蚀面积逐渐增大,极强度、剧烈侵蚀面积逐渐减少,说明河龙区间的生态环境逐渐变好,侵蚀正向着良性趋势发展。其原因除了梯田、林地、坝地越来越发挥较大的效益外,草地面积的增加,尤其是封禁治理、生态修复等措施的大面积实施,可能是河龙区间近期土壤侵蚀强度减弱的一个原因。
英文摘要:
      Taking remote sensing data as the main information source, through massive field investigation, the paper established the image translation signs of different types of land utilization and vegetation coverage. Under the support of geographic information system, by the method of computer assistanted artificial translation, it has carried on the soil erosion dynamic monitoring to the Hekou town-Longmen sector. The result show: About 80.40% of total soil erosion was water erosion; about 19.60% was wind erosion. The soil erosion intensity is mainly determined by moderate erosion and intensive erosion, the micro-degree erosion take second part, the third is mild erosion and extremely intensitive erosion, the acute erosion accounts for the smallest proportion. Compared with the soil erosion in 2000 the total soil erosion intensity reduced in 2008. The areas of micro-degree erosion, mild erosion and moderate erosion increased gradually; the areas of extremely intensitive erosion and acute erosion decreased accordingly. It shows that the eco-environment improves gradually in this area. The erosion is turning toward the benign tendency. Except for the reason that terraced field, forest land and dam land takes more and more environmental benefit, perhaps the increase of grass land, especially the implementation of large area closing measures and ecological restoration is the main reason that weakened the soil erosion intensity in this sector in recent years.
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