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Measurement and zonation of soil surface moisture in arid and semi-arid regions using Landsat 8 images

机译:利用Landsat 8图像中干旱和半干旱区土壤面积水分的测量与区划

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摘要

Monitoring of soil surface moisture is an imperative factor in water and energy cycle. Due to the variability of soil characteristics such as topography, vegetation, and climate dynamics, this important factor varies with respect to time and place. Measuring methods can provide soil moisture information in a wide range of short intervals with reasonable accuracy. In present research, Landsat 8 satellite data with various soil moisture content estimation methods were tested. In order to evaluate the accuracy of each method, the real-field data used 80 samples of volumetric soil moisture content in suburban areas of Semnan city that were collected at the time of satellite passage of the area. Some of the indicators used in this study are normalized vegetation index, NDTI index, NDMI index, PSMI index (use full form of these indices), surface temperature, and SMSWIR index. The SMSWIR index with correlation coefficient was 0.78, and the correlation coefficient of regression model was 0.61, and RMSE was 3.69. The results of the regression model and real data were estimated to be 3.69, which are recommended for assessing surface soil moisture in arid and desert regions. Three indicators of SMSWIR index, NDTI index, and NDMI index with a small difference are not suitable indices for measuring soil moisture content in desert areas with vegetation cover. By employing multivariable regression models, soil moisture model was also prepared by using the studied indices. The findings of this research indicate that the simultaneous correlation model is superior to the surface soil moisture mapping.
机译:监测土壤表面水分是水和能量循环中的势不关量。由于地形,植被和气候动态等土壤特征的变化,这一重要因素相对于时间和地点而异。测量方法可以以合理的准确度提供各种短间隔的土壤湿度信息。目前研究,对具有各种土壤水分含量估计方法的Landsat 8卫星数据进行了测试。为了评估每种方法的准确性,在该地区卫星通道的郊区收集的半南市郊区的80个体积土壤水分含量的实地数据。本研究中使用的一些指标是标准化的植被指数,NDTI指数,NDMI指数,PSMI指数(使用这些指数的全文),表面温度和SMSWIR指数。具有相关系数的SMSWIR指数为0.78,回归模型的相关系数为0.61,RMSE为3.69。回归模型和实际数据的结果估计为3.69,建议评估干旱和沙漠地区的表面土壤水分。 SMSWIR指数,NDTI指数和NDMI指数的三个指标,具有较小差异,不适合用植被覆盖测量沙漠地区土壤水分含量的索引。通过采用多变量回归模型,还通过使用研究指标制备土壤水分模型。该研究的结果表明,同时相关模型优于地面土壤水分测绘。

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