基于GNSS反射法的土壤水分估算

Jabir Shabbir Malik, Jingrui Zhang, N. A. Naqvi
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引用次数: 3

摘要

全球导航卫星系统反射测量(GNSS-R)被定义为一种双基地雷达系统。GNSS-R在微波遥感应用中具有独特的潜力。本文重点研究了利用GPS-L1地表散射或反射信号估算土壤含水量的可行性。GPS信号的接收和处理使用4米高的地面平台。本文利用地表功率反射率(即反射信号与直接信号的功率比)估算土壤水分。得到了介电常数的解析解。通过对土壤介电常数的测量,发现土壤介电常数的物理适宜值与一个常数参数的半经验模型有关。土壤水分含量是通过准确地知道土壤的质地组成砂S和粘土C的百分比来获取的。为了验证估算结果,将土壤湿度值与现场测量值进行了比较。最后,使用绝对相对误差、均方根误差(RMSE)和均方根偏差(RMB)三种统计工具进行误差分析。结果表明:降雨发生后,土壤湿度变化显著;然而,也观察到,在某些情况下,在较高的仰角值是不一致的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil moisture content estimation using GNSS reflectometry (GNSS-R)
Global Navigation Satellite System-Reflectometry (GNSS-R) is defined as a bistatic radar system. GNSS-R has a unique potential in microwave remote sensing application. The focus of this paper is the feasibility of estimating soil moisture content using GPS-L1 scattered or reflected signals from the earth's surface. GPS signals are received and processed using ground based platform at 4m height. In this paper soil moisture is estimated from the surface power reflectivity which is the power ratio of the reflected signal and the direct signal. Analytical solution for the dielectric constant is resolved. The dielectric constant is measured and the physically suitable value of soil dielectric constant is related with the semi-empirical model of a constant parameters. Soil moisture content is retrieved by exactly knowing the soil textural composition of sand S and clay C in percentage. To validate the results estimated soil moisture values are compared with the in-situ measurements. Finally for error analysis three statistical tools are used, absolute relative error, Root Mean Square Error (RMSE), and Root Mean Bias (RMB). The results demonstrate that soil moisture varies and changed significantly after rainfalls occurred. However, it is also observed that values are inconsistent at higher elevation angles in some cases.
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