Detecting soil salinity with arid fraction integrated index and salinity index in feature space using Landsat TM imagery

被引:26
|
作者
Wang, Fei [1 ,2 ]
Chen, Xi [1 ]
Luo, GePing [1 ]
Ding, JianLi [3 ]
Chen, XianFeng [1 ,4 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Xinjiang Univ, Coll Resources & Environm Sci, Urumqi 830046, Peoples R China
[4] Slippery Rock Univ Penn, Slippery Rock, PA 16057 USA
基金
中国国家自然科学基金;
关键词
soil salinity; spectrum; halophytes; Landsat TM; spectral mixture analysis; feature space; model; SPECTRAL REFLECTANCE; VEGETATION COVER; NDVI; INDICATORS; OASIS;
D O I
10.1007/s40333-013-0183-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Modeling soil salinity in an arid salt-affected ecosystem is a difficult task when using remote sensing data because of the complicated soil context (vegetation cover, moisture, surface roughness, and organic matter) and the weak spectral features of salinized soil. Therefore, an index such as the salinity index (SI) that only uses soil spectra may not detect soil salinity effectively and quantitatively. The use of vegetation reflectance as an indirect indicator can avoid limitations associated with the direct use of soil reflectance. The normalized difference vegetation index (NDVI), as the most common vegetation index, was found to be responsive to salinity but may not be available for retrieving sparse vegetation due to its sensitivity to background soil in arid areas. Therefore, the arid fraction integrated index (AFII) was created as supported by the spectral mixture analysis (SMA), which is more appropriate for analyzing variations in vegetation cover (particularly halophytes) than NDVI in the study area. Using soil and vegetation separately for detecting salinity perhaps is not feasible. Then, we developed a new and operational model, the soil salinity detecting model (SDM) that combines AFII and SI to quantitatively estimate the salt content in the surface soil. SDMs, including SDM1 and SDM2, were constructed through analyzing the spatial characteristics of soils with different salinization degree by integrating AFII and SI using a scatterplot. The SDMs were then compared to the combined spectral response index (COSRI) from field measurements with respect to the soil salt content. The results indicate that the SDM values are highly correlated with soil salinity, in contrast to the performance of COSRI. Strong exponential relationships were observed between soil salinity and SDMs (R (2)> 0.86, RMSE < 6.86) compared to COSRI (R (2)=0.71, RMSE=16.21). These results suggest that the feature space related to biophysical properties combined with AFII and SI can effectively provide information on soil salinity.
引用
收藏
页码:340 / 353
页数:14
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