Abstract

In countries characterized by arid and semi-arid climates, a precise determination of soil moisture conditions on the field scale is critically important, especially in the first crop growth stages, to schedule irrigation and to avoid wasting water. The objective of this study was to apply the operative methodology that allowed surface soil moisture (SSM) content in a semi-arid environment to be estimated. SSM retrieval was carried out by combining two scattering models (IEM and WCM), supplied by backscattering coefficients at the VV polarization obtained from the C-band Synthetic Aperture Radar (SAR), a vegetation descriptor NDVI obtained from the optical sensor, among other essential parameters. The inversion of these models was performed by Neural Networks (NN). The combined models were calibrated by the Sentinel 1 and Sentinel 2 data collected on bare soil, and in cereal, pea and onion crop fields. To retrieve SSM, these scattering models need accurate measurements of the roughness surface parameters, standard deviation of the surface height (hrms) and correlation length (L). This work used a photogrammetric acquisition system carried on Unmanned Aerial Vehicles (UAV) to reconstruct digital surface models (DSM), which allowed these soil roughness parameters to be acquired in a large portion of the studied fields. The obtained results showed that the applied improved methodology effectively estimated SSM on bare and cultivated soils in the principal early growth stages. The bare soil experimentation yielded an R2 = 0.74 between the estimated and observed SSMs. For the cereal field, the relation between the estimated and measured SSMs yielded R2 = 0.71. In the experimental pea fields, the relation between the estimated and measured SSMs revealed R2 = 0.72 and 0.78, respectively, for peas 1 and peas 2. For the onion experimentation, the highest R2 equaled 0.5 in the principal growth stage (leaf development), but the crop R2 drastically decreased to 0.08 in the completed growth phase. The acquired results showed that the applied improved methodology proves to be an effective tool for estimating the SSM on bare and cultivated soils in the principal early growth stages.

Highlights

  • Soil surface moisture (SSM) is the main factor of water and heat fluxes in the soilplant-atmosphere continuum that plays a key role in determining crop water supply, which is crucial for the vegetation health [1]

  • We present the simulation results of the backscatter coefficients of the integral equation model (IEM) comafter applying the methodology described in Figure 6 and using the measured roughness bined with the WCM scattering models at VV polarization on the experimental barley field parameters L and hrms

  • For the purpose of further improving the results of this methodology, we measured the roughness parameters by a photogrammetric acquisition system carried on a Unmanned Aerial Vehicles (UAV) to reconstruct a digital surface models (DSM) that allowed these parameters to be obtained over a large portion of the studied fields

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Summary

Introduction

Soil surface moisture (SSM) is the main factor of water and heat fluxes in the soilplant-atmosphere continuum that plays a key role in determining crop water supply, which is crucial for the vegetation health [1]. Radar measurements are associated with moisture and roughness characteristics of soil surface [3] Many electromagnetic models, such as the Kirchoff Approximations [4], the small perturbation model (SPM) [5] and the integral equation model (IEM) [6], have been created to study backscattering and to simulate radar backscattering coefficient, σ0 , data. The hardest point of developing soil moisture retrieval models is to determine the surface roughness parameters: the standard deviation of the surface height variation (hrms) and the correlation length (L). These parameters significantly affect the relations between radar backscatter and soil moisture [9]

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