Mapping Soil Texture of a Plain Area Using Fuzzy-c-Means Clustering Method Based on Land Surface Diurnal Temperature Difference

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• 作者：De-Cai WANG^a ; ^b ; Gan-Lin ZHANG^a ; ^{glzhang@issas.ac.cn} ; Xian-Zhang PAN^a ; Yu-Guo ZHAO^a ; Ming-Song ZHAO^a ; ^b ; Gai-Fen WANG^a ; ^b
• 关键词：digital soil mapping ; land surface temperature ; low relief area ; MODIS ; remote sensing
• 刊名：Pedosphere
• 出版年：2012
• 期刊代码：16_10020160
• 类别：abs
• 出版时间：June, 2012
• 卷：22
• 期：3
• 页码：394-403
• 文件大小：888 K

摘要

The use of landscape covariates to estimate soil properties is not suitable for the areas of low relief due to the high variability of soil properties in similar topographic and vegetation conditions. A new method was implemented to map regional soil texture (in terms of sand, silt and clay contents) by hypothesizing that the change in the land surface diurnal temperature difference (DTD) is related to soil texture in case of a relatively homogeneous rainfall input. To examine this hypothesis, the DTDs from moderate resolution imagine spectroradiometer (MODIS) during a selected time period, i.e., after a heavy rainfall between autumn harvest and autumn sowing, were classified using fuzzy-c-means (FCM) clustering. Six classes were generated, and for each class, the sand (> 0.05 mm), silt (0.002-0.05 mm) and clay (< 0.002 mm) contents at the location of maximum membership value were considered as the typical values of that class. A weighted average model was then used to digitally map soil texture. The results showed that the predicted map quite accurately reflected the regional soil variation. A validation dataset produced estimates of error for the predicted maps of sand, silt and clay contents at root mean of squared error values of 8.4%, 7.8%and 2.3%, respectively, which is satisfactory in a practical context. This study thus provided a methodology that can help improve the accuracy and efficiency of soil texture mapping in plain areas using easily available data sources.