Analysis of salinization dynamics by remote sensing in Hetao Irrigation District of North China

被引:145
|
作者
Yu, Ruihong [2 ]
Liu, Tingxi [1 ]
Xu, Youpeng [3 ]
Zhu, Chao [2 ]
Zhang, Qing [4 ]
Qu, Zhongyi [1 ]
Liu, Xiaomin [1 ]
Li, Changyou [1 ]
机构
[1] Inner Mongolia Agr Univ, Coll Water Conservancy & Civil Engn, Hohhot 010018, Inner Mongolia, Peoples R China
[2] Inner Mongolia Univ, Coll Environm & Resources, Hohhot 010021, Inner Mongolia, Peoples R China
[3] Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210093, Jiangsu Prov, Peoples R China
[4] Inner Mongolia Univ, Coll Life Sci, Hohhot 010021, Inner Mongolia, Peoples R China
基金
中国国家自然科学基金;
关键词
Salinization; Spatial-temporal analysis; Remote sensing; Hetao Irrigation District; SOILS; VEGETATION;
D O I
10.1016/j.agwat.2010.03.009
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Remote sensing can provide base information for documenting salinity change and for predicting its future evolution trend. The spatial and temporal distributions of soil salinization of Jiefangzha Irrigation Sub-district, the western part of Hetao Irrigation District of Inner Mongolia in northern China, were determined through analysis of satellite-based remote sensing images. Three Landsat TM/ETM+ satellite images taken during 14 years (1991 similar to 2005) coupled with field observations were chosen as the basic data sources. Supervised classification and visual interpretation were used to analyze salinity classification and statistical method was applied to analyze the relationship between salinity and groundwater depth. From 1991 to 2005 the area of heavy saline land decreased from 191 to 136 km(2), or 3.9 km(2) per year; the moderate saline land decreased from 318 to 284 km(2), or 2.5 km(2) per year; the slight saline land decreased from 510 to 394 km(2), or 8.2 km(2) per year. Therefore, soil salinization in Jiefangzha Irrigation Sub-district is decreasing in general. The electrical conductivity (EC) values measured from field have the following relationship with the reflectance composition obtained from LANDSAT Enhanced Thematic Mapper Plus (ETM+) data: EC = 5.653(band5 - band7)/(band5 + band7) + 0.246. In addition, an r(2) value between EC values and groundwater depth is 0.72, which indicates groundwater depth is the major factor for the regional soil salinity control. The paper can serve as a theoretical reference for optimal allocation of irrigation water resource and salinization control in Hetao Irrigation District. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:1952 / 1960
页数:9
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