信号与信息处理

探地雷达波振幅与土壤含水量关系的数值模拟

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  • 1. 首都师范大学资源环境与地理信息系统北京市重点实验室,北京10048
    2. 首都师范大学城市环境过程与数字模拟国家重点实验室培育基地,北京10048
    3. 首都师范大学三维信息获取与应用教育部重点实验室,北京100048

收稿日期: 2014-12-02

  修回日期: 2014-12-28

  网络出版日期: 2015-01-04

基金资助

国家科技支撑计划课题基金(No.2012BAH34B01);国家自然科学基金(No.41371434)

Numerical Study on the Relationship between Amplitudes of Ground Penetrating Radar Wave and Water Content in Soil

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Received date: 2014-12-02

  Revised date: 2014-12-28

  Online published: 2015-01-04

摘要

通过建立探地雷达波振幅与土壤介电常数之间的定量关系可反演土壤含水量. 在采用时间域有限差分法建立土壤分层模型的基础上,模拟探地雷达电磁波在均匀分层土壤介质中的传播特性,分析土壤介电常数与雷达回波振幅之间的变化规律,证实了回波振幅随着介电常数的增大而减小,总结出介电常数与振幅之间的幂函数关系式. 最后通过室内土壤模型对此关系式进行了验证,结果表明由此关系式反演出的土壤含水量值与土壤三参数仪测定的含水量值相一致.

本文引用格式

李蕙君1,2,3, 钟若飞1,2,3 . 探地雷达波振幅与土壤含水量关系的数值模拟[J]. 应用科学学报, 2015 , 33(1) : 41 -49 . DOI: 10.3969/j.issn.0255-8297.2015.01.005

Abstract

Water content in soil can be derived from the relation between changes in ground penetrating radar signals and the soil’s dielectric constant. Using the finite difference time domain (FDTD) method, a model of layered soil is established to simulate ground penetrating radar electromagnetic waves in the soil. The transmission characteristics of layered soil are analyzed using the model. The results indicate that a functional relation exists between the soil dielectric constant and the amplitude, i.e., the wave amplitude decreases with the increased electric constant. With an indoor soil model, the obtained relationship
is verified: the computed water content agrees with the wet sensor data.
 

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