Abstract

This research examines the simultaneous retrieval of surface soil moisture and salt concentrations using hyperspectral reflectance data in an arid environment. We conducted laboratory and outdoor field experiments in which we examined three key soil variables: soil moisture, salt and texture (silty loam, clay and silty clay). The soil moisture content models for multiple textures (M_SMC models) were based on selected hyperspectral reflectance data located around 1460, 1900 and 2010 nm and resulted in R2 values higher than 0.933. Meanwhile, the soil salt concentrations were also accurately (R2 > 0.748) modeled (M_SSC models) based on wavebands located at 540, 1740, 2010 and 2350 nm. When the different texture samples were mixed (SL + C + SC models), soil moisture was still accurately retrieved (R2 = 0.937) but the soil salt not as well (R2 = 0.47). After stratifying the samples by retrieved soil moisture levels, the R2 of calibrated M_SSCSMC models for soil salt concentrations improved to 0.951. This two-step method also showed applicability for analyzing soil-salt samples in the field. The M_SSCSMC models resulted in R2 values equal to 0.912 when moisture is lower than 0.15, and R2 values equal to 0.481 when soil moisture is between 0.15 and 0.2.

Highlights

  • An irrigation monitoring program is often required to maintain soil moisture at a reasonable range to grow crops while reducing salinity risks and ecological concerns

  • Waveband Selections Sensitive to Soil Moisture and Salt

  • Based ranking (PCAr) applied to the silty loam (SL) + to silty clay (SC) data setdevelop for R, N, A1 and A”.models, Sensitive wavebands were system selected according to was applied to the SL + C + SC data set for R, N, A′ and A′′

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Summary

Introduction

An irrigation monitoring program is often required to maintain soil moisture at a reasonable range to grow crops while reducing salinity risks and ecological concerns. Identification and monitoring of Soil Moisture Content (SMC) and Soil Salt Concentration (SSC) are important for setting up a sustainable and economically beneficial irrigation program. Precise and accurate measurements of SMC and SSC can be performed in a laboratory. One robust SMC indicator is gravimetric water content (GWC) [1], but it is restricted to a small volume of soil. For SSC measurements, electrical conductivity (EC), total soluble salts (TSS) [2], sodium adsorption ratio (SAR) and exchangeable sodium percentage (ESP) [3] are typical indicators. Some more practical in situ measurements of SMC and SSC, such as time domain reflectometry (TDR), electromagnetic induction, e.g., EM38 [4], Hydra-probe [5] and SCT-10, employ probes or sensors

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