利用遥感数据估算盐度

M. Gad, M. A., M. Mohamed
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引用次数: 1

摘要

遥感数据已被证明是估算土地覆盖土壤盐分的有效方法。遥感数据用于土壤盐度研究,因为它对预测土壤变化既快速又有用。土壤盐化给农业带来了许多问题,因为它会影响植物的吸水,从而导致产量下降。本研究在埃及吉萨省El-Sheikh进行,了解TDS (Total Dissolved Salts,总溶解盐)田间实况数据与土壤盐渍化指数之间的相关性。在这项研究中,使用了2009年10月Landsat-7拍摄的经过辐射和大气校正的图像。真值数据与盐渍化指数之间采用简单线性回归(SLR)。研究区最具代表性的指数为SI6,相关系数为0.78,RMSE(均方根误差)最小。该方法将遥感数据、GIS数据和实地实况数据相结合,可以精确监测土壤盐分的空间分布,特别是在填海地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ESTIMATING SALINITY USING REMOTE SENSING DATA
Remote sensing data has proved to be an effective method of estimating soil salinity in land cover. Remote sensing data is used in soil salinity studies as it is quick and useful for making soil changes predictions. Soil salinity causes many problems for agriculture as it has bad effects on water absorption of the plants, which results in yield reduction. This study was conducted in El-Sheikh in Giza governorate in Egypt, to understand the correlation between field truth data of soil salinity in terms of TDS (Total Dissolved Salts) and soil salinization indices. In this study, a Landsat-7 image taken in October 2009 was used after radiometric and atmospheric corrections. SLR (Simple Linear Regression) was applied between truth data and salinization indices. The best representative index for the study area was SI6, which achieved a correlation 0.78 and the minimum value of RMSE (Root Mean Square Error). This approach enables precise monitoring of the spatial distribution of soil salinity, especially in the reclaimed areas, by the combination of remotely sensed data, GIS, and field truth data.
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