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中国黄土高原泾河流域的土地利用变化及其与地形因素的关系。

The land use changes and its relationship with topographic factors in the Jing river catchment on the Loess Plateau of China.

作者信息

Li Zhi, Liu Wenzhao, Zheng Fenli

机构信息

College of Natural Resources and Environment, Northwest A & F University, Yangling, Shaanxi 712100 China.

Institute of Soil and Water Conservation, CAS & MWR, Yangling, Shaanxi China.

出版信息

Springerplus. 2013 Dec 11;2(Suppl 1):S3. doi: 10.1186/2193-1801-2-S1-S3. eCollection 2013.

Abstract

A series of soil conservation measures have been carried out to reduce soil loss on the Loess Plateau of China since 1950s, and the biologic measures were implemented according to topographic factors such as slope and elevation; therefore, the changes in topographic factors of land use can indicate the effects of the biologic measures. The objectives of this study were to (i) analyze the land use changes in the Jing River catchment during 1986-2000 and to (ii) examine the effects of biologic measures through relating land use changes with topographic factors. During 1986-2000, the dominant land use types were farmland and grassland (88% of the whole catchment). Compared with 1986, farmland and forest decreased while grassland and construction land increased with little changes in water and unused land. Three main conversion types occurred, i.e. the mutual conversion between forest and grassland, the mutual conversion between farmland and grassland, and farmland converted to other types. The elevation of farmland, forest, construction land and water increased, while that of grassland and unused land decreased. The mean slope gradient of each land use type changed little except for unused land. The above results suggested farmland has greatly decreased on tableland region due to the increase in construction land, forest has moved to gully region while grassland has increased despite elevation and slope. The land use in the Jing River catchment during 1986-2000 was changing to a more reasonable spatial pattern.

摘要

自20世纪50年代以来,中国黄土高原开展了一系列水土保持措施以减少土壤流失,生物措施根据坡度和海拔等地形因素实施;因此,土地利用地形因素的变化可以表明生物措施的效果。本研究的目的是:(i)分析1986-2000年泾河流域的土地利用变化;(ii)通过将土地利用变化与地形因素相关联来检验生物措施的效果。1986-2000年期间,主要土地利用类型为农田和草地(占整个流域的88%)。与1986年相比,农田和林地减少,草地和建设用地增加,水域和未利用地变化不大。发生了三种主要的转换类型,即林地和草地之间的相互转换、农田和草地之间的相互转换以及农田转换为其他类型。农田、林地、建设用地和水域的海拔升高,而草地和未利用地的海拔降低。除未利用地外,各土地利用类型的平均坡度变化不大。上述结果表明,由于建设用地增加,塬区农田大幅减少,林地向沟谷区转移,而草地尽管海拔和坡度有所变化但仍有所增加。1986-2000年期间,泾河流域的土地利用正转变为更合理的空间格局。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2f16/3973418/2b2e91f39efe/40064_2013_712_Fig1_HTML.jpg

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