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福建省水土流失的时空变化

曾舒娇 汪小钦 陈贤干 王振平 林敬兰 陈善沐

水土保持通报2017,Vol.37Issue(6):305-312,320,9.
水土保持通报2017,Vol.37Issue(6):305-312,320,9.DOI:10.13961/j.cnki.stbctb.2017.06.050

福建省水土流失的时空变化

Temporal and Spatial Variation of Soil Erosion in Fujian Province

曾舒娇 1汪小钦 1陈贤干 1王振平 1林敬兰 2陈善沐2

作者信息

  • 1. 福州大学空间数据挖掘与信息共享教育部重点实验室福建省空间信息工程研究中心,福建福州350002
  • 2. 福建省水土保持试验站,福建福州350003
  • 折叠

摘要

Abstract

[Objective] To provide scientific basis for soil and water conservation,the dynamic monitoring and temporal and spatial variations of soil erosion in Fujian Province from 1990 to 2015 were studied.[Methods] Choosing Fujian Province as a study area,combined with GIS and RS technologies,the research was carried out based on USLE model.[Results] ① The soil erosion intensity of Fujian Province was general light.The soil erosion areas were found primarily in the western and southeastern of Fujian Province and less in central and northern parts,As to the spatial variation of soil erosion,a decreasing trend from the southeast coastal area to the northwest inland area was found existed.During the past 25 years,the transfer of soil erosion intensity mainly occurred between the light/moderate erosion and slight erosion.② From 1990 to 2015,the area of soil erosion reduced by 3 825.55 km2 totally,which was mainly covered by light erosion intensity.Especially after 2010,the area of soil erosion showed a faster shrink.Meanwhile,soil erosion in coastal areas got improvement more evidently than the erosion in inland areas.[Conclusion] The improvement of soil erosion in Fujian Province was obvious during the past 25 years,which showed significant benefits in soil erosion control,

关键词

水土流失/时空变化/USLE/福建省

Key words

soil erosion/temporal and spatial variation/USLE/Fujian Province

分类

农业科技

引用本文复制引用

曾舒娇,汪小钦,陈贤干,王振平,林敬兰,陈善沐..福建省水土流失的时空变化[J].水土保持通报,2017,37(6):305-312,320,9.

基金项目

国家科技支撑计划课题“南方红壤水土流失综合监测”(2013BAC08B01) (2013BAC08B01)

福建省高校产学研重点项目“集成多重时空分辨率的县域水土流失遥感协同监测”(2017Y4010) (2017Y4010)

中央引导地方发展专项(2017L3012) (2017L3012)

水土保持通报

OA北大核心CSCDCSTPCD

1000-288X

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