[1]王少军,张志.湖北武当山区土壤侵蚀景观成因机理研究[J].水土保持研究,2003,10(04):113-116.
WANG Shao-jun,ZHANG Zhi.Study the Mechanism on Soil Erosion Landscape in Wudangshan District of Hubei Province[J].Research of Soil and Water Conservation,2003,10(04):113-116.
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WANG Shao-jun,ZHANG Zhi.Study the Mechanism on Soil Erosion Landscape in Wudangshan District of Hubei Province[J].Research of Soil and Water Conservation,2003,10(04):113-116.
湖北武当山区土壤侵蚀景观成因机理研究
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
10
期数:
2003年04期
页码:
113-116
栏目:
出版日期:
1900-01-01
- Title:
- Study the Mechanism on Soil Erosion Landscape in Wudangshan District of Hubei Province
- 分类号:
- S157.1
- 摘要:
- 尽管"长治工程"在丹江口市有较大的投入，从多时相的遥感影像上发现，武当山区土壤侵蚀景观结构为斑散布型，斑的分布具有明显的空间地带性，斑与基间进行了强烈的土壤流交换，局部地区水土流失仍在加强。人类活动与水土流失间的关系复杂，具体表现为缓变性与突变性、可避防性。人类活动是影响武当山区水土流失的主要因子。
- Abstract:
- Though a great deal of engineering has been dived into Danjiangkou city in the course of "Project for Regulating the Yangtse River", the following facts based on multi-time remote sensing image were discovered.The framework of soil erosion landscape in Wudangshan district is the patch scattering, the patch is only scattering in some special spatial zone, the soil current has been exchanged between the patch with matrix, a specific part of the Wudangshan district soil erosion intensified.The relation of human action and soil erosion is complex,the complexity of representation is slowly and abruptly, and avoidance.The human action is the primary factor to bring on soil erosion.
参考文献/References:
[1] 湖北省地图集编纂委员会.湖北省地图集[M].北京:中国地图出版社, 1998.
[2] 许慧, 王家骥.景观生态学的理论与应用[M].北京:中国环境科学出版社, 1993.
[3] 沈清基.城市生态与城市环境[M].上海:同济大学出版社, 1998.
[4] 王少军, 张志.湖北省丹江口市土壤侵蚀景观形成机理[J].水土保持通报, 2001, 21(5):34-36.
[5] 张志, 王少军, 华学理.湖北省"土壤侵蚀内城现象"及景观格局[J].水土保持通报, 2001, 21(4):30-33.
[6] 关君蔚.水土保持原理[M].北京:中国林业出版社, 1996.
备注/Memo
收稿日期:2003-1-5。
基金项目:“全国土壤侵蚀动态遥感调查与数据库更新”项目湖北省部分的成果。
作者简介:王少军（1965- ），女，1993年硕士毕业于中国地质大学研究生院，现从事地理学的教学及科研工作.
更新日期/Last Update:
1900-01-01