Dielectric properties of saline soil based on a modified dobson dielectric model

Nigara Tashpolat, Jianli Ding, Danlin Yu

Research output: Contribution to journalArticlepeer-review

14 Scopus citations

Abstract

Soil salinization is a major concern for agricultural development in arid areas. In this paper, a modified Dobson dielectric model was applied to simulate the dielectric constant of saline soil in the Ugan-Kuqa river delta oasis of Xinjiang Uygur autonomous region, northwestern China. The model performance was examined through analyzing the influences of its parameters on the soil dielectric constant and the relationship between radar backscattering coefficient and the dielectric constant of saline soil. The results of the study indicate that: (1) The real part of the soil dielectric constant is affected by soil water content at low radar frequencies; the imaginary part is closely related with both the soil water content and soil salt content. (2) The soil water and salt contents are related with the coefficient of dialectical loss, which is consistent with the natural conditions of saline soil in arid areas and provides valuable references for the study of soil dielectric properties. (3) The changes of soil water content and soil salt content have instant influences on the dielectric constant of saline soil. Subsequently, the radar backscattering coefficient is affected to respond to the dielectric constant of saline soil. The radar backscattering coefficient is most responsible to the radar’s cross polarization pattern with a correlation coefficient of R2=0.75. This study provides a potential method to monitor soil salinization and soil water content by using a soil dielectric model and radar techniques.

Original languageEnglish
Article numberA013
Pages (from-to)696-705
Number of pages10
JournalJournal of Arid Land
Volume7
Issue number5
DOIs
StatePublished - 1 Oct 2015

Keywords

  • Backscattering coefficient
  • Dielectric constant
  • Dielectric constant model
  • Radarsat-2 images
  • Saline soil

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