PDF Download

[1]SHEN Huaifei,TIAN Qingjiu,WU Guoxi.Study on Land Use/Cover Change in the Water Supply Area of the Middle-Route of the South-to-North Water Diversion (MR-SNWD) Project[J].Research of Soil and Water Conservation,2015,22(02):204-208.

Copy

Study on Land Use/Cover Change in the Water Supply Area of the Middle-Route of the South-to-North Water Diversion (MR-SNWD) Project

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 22 Number of periods: 2015 02 Page number: 204-208 Column: Public date: 2015-04-28

Title:: Study on Land Use/Cover Change in the Water Supply Area of the Middle-Route of the South-to-North Water Diversion (MR-SNWD) Project

Author(s):: SHEN Huaifei^1,2,3, TIAN Qingjiu^1,3, WU Guoxi²; 1. Collaborative Innovation Center of South China Sea Studies, Nanjing University, Nanjing 210023, China;
2. School of Urban & Rural Planning and Landscape Architecture, Xuchang University, Xuchang, He’nan 461000, China;
3. International Institute for Earth System Science, Nanjing University, Nanjing 210023, China

Keywords:: land use/cover change; land use dynamic degree; Middle-Route of the South-to-North Water Diversion Project

CLC:: TV697.4⁺4;TP79

DOI:: -

Abstract:: There was an obvious spatial difference in spatial patterns of land use/cover change in the water resource district of Middle-Route of the South-to-North Water Diversion Project. The spatial pattern of land use/cover change in the study area was quantitatively analyzed by using RS and GIS. The results showed that: 1) the land use types were mainly forestland, agricultural land and grassland, indicating that the matrix of landscape is forest; 2) the land use change mainly occurred in forestland, cultivated land, and grassland, the forestland had showed the first increasing and then the stability, the areas of construction land increased drastically, and the growth rate accelerated, land use changes mainly occurred in the gully regions with low altitude and gentle slope where human activity was active; 3) the land use dynamic degree was about 1.20%, the overall changes of land use were slight, and the structure of land was more stable.

References:: [1] 陈佑启,杨鹏.国际上土地利用/土地覆盖变化研究的新进展[J].经济地理,2001,21(1):95-100.
[2] 申怀飞,吴国玺,丁圣彦.豫西黄河流域土地利用空间格局地形梯度特征分析[J].地域研究与开发,2012,31(3):159-162.
[3] 张本昀,申怀飞,郑敬刚,等.河南省土地利用景观格局分析[J].资源科学,2009(2):317-323.
[4] 刘纪远,张增祥.中国近期土地利用变化的空间格局分析[J].中国科学:D辑,2002,32(12):1031-1040.
[5] Geist H J, Lambin E F. What drives tropical deforestation[R]. LUCC Report Series,2001.
[6] Turner B L, Lambin E F, Reenberg A. The emergence of land change science for global environmental change and sustainability[J]. Proceedings of the National Academy of Sciences,2007,104(52):20666-20671.
[7] 高志强,刘纪远.基于遥感和GIS的中国土地利用土地覆盖的现状研究[J].遥感学报,1999,3(2):134-138.
[8] 王思远,刘纪远.中国土地利用时空特征分析[J].地理学报,2001,56(6):631-639.
[9] 王根绪,丁永建,王建,等.近15年来长江黄河源区的土地覆被变化[J].地理学报,2004,59(2):163-173.
[10] 王秀兰,包玉海.土地利用动态变化研究方法探讨[J].地理科学进展,1999,18(1):81-87.
[11] Luijten J C. A systematic method for generating land use patterns using stochastic rules and basic landscape characteristics:results for a Colombian hillside watershed[J]. Agriculture, Ecosystems & Environment,2003,95(2):427-441.
[12] 孙丹峰,李红,张凤荣.基于动态统计规则和景观格局特征的土地利用覆被空间模拟预测[J].农业工程学报,2005,21(3):121-125.
[13] 解修平,周杰,张海龙,等.基于景观生态和马尔可夫过程的西安地区土地利用变化分析[J].资源科学,2006,28(6):175-181.
[14] 沈泽昊,张全发,岳超,等.南水北调中线水源区土地利用/土地覆被的空间格局[J].地理学报,2006,61(6):633-644.
[15] 申怀飞,侯刚,翟书梅,等.南水北调中线水源区土地利用/覆被变化及其驱动因素分析[J].贵州农业科学,2013,41(6):167-171.
[16] 朱会义,李秀彬,何书金,等.环渤海地区土地利用的时空变化分析[J].地理学报,2001,56(3):253-260.
[17] 吴秀芹,蔡运龙.塔里木河下游典型区景观生态质量评价[J].干旱区资源与环境,2003,17(2):12-17.

Similar References:

Memo

Last Update: 1900-01-01