Analysis on Changes of Land Use Structure in Water Source Area of Middle Route of South to North Water Diversion Project Based on Markov Transfer Matrix

ZHU Jiulong

doi:10.13961/j.cnki.stbctb.2016.02.033

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Analysis on Changes of Land Use Structure in Water Source Area of Middle Route of South to North Water Diversion Project Based on Markov Transfer Matrix

- Analysis on Changes of Land Use Structure in Water Source Area of Middle Route of South to North Water Diversion Project Based on Markov Transfer Matrix
- Bulletin of Soiland Water Conservation Vol. 36, Issue 2, Pages: 171-175(2016)
- 作者机构：
  
  中原工学院经济管理学院,河南,郑州,450007
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2016.02.033
  CLC：
- Published：2016
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ZHU Jiulong. Analysis on Changes of Land Use Structure in Water Source Area of Middle Route of South to North Water Diversion Project Based on Markov Transfer Matrix[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 171-175.
DOI：

ZHU Jiulong. Analysis on Changes of Land Use Structure in Water Source Area of Middle Route of South to North Water Diversion Project Based on Markov Transfer Matrix[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 171-175. DOI： 10.13961/j.cnki.stbctb.2016.02.033.

摘要

[目的] 揭示南水北调中线水源区土地利用结构变化特征

为区域土地规划提供依据。[方法] 根据土地利用现状调查数据及影像资料

测算水源区土地利用结构熵、均衡度和优势度

并利用马尔科夫转移矩阵求解各种类型土地间的数量转换关系。[结果](1) 水源区土地类型转化主要发生在耕地、林地和草地之间;(2) 2010年以前

水源区土地利用结构稳定性较高

2010年以后

由于丹江口水库蓄水而导致水源区土地利用结构波动性较大。[结论] 水源区各种类型的土地面积不断变化

在2008-2010年土地结构较为稳定

2010-2013年土地结构和稳定性出现了波动。

Abstract

[Objective] The characteristics of land use structure in the middle route of the south to north water transfer project was demonstrated to provide the basis for the regional land planning. [Methods] Data was collected by surveying of land use status of water source area and eliciting from image. The entropy

equilibrium degree and dominance degree were measured. The conversional quantity relationship was calculated by Markoff transfer matrix. [Results] Land type conversion mainly occurred among farmland

woodland and grassland. Land use structure of water source area was relatively stable before 2010. However

it had become unstable after 2010 because Danjiangkou reservoir began work from then on. [Conclusion] The land area of various types of water source area was constantly changing. Land structure was comparatively stable in 2008-2010

land structure and stability fluctuated in 2010-2013.

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