Abstract

Soil salinization is one of the most widespread soil degradation processes on Earth, especially in arid and semi-arid areas. The salinized soil in arid to semi-arid Xinjiang Uyghur Autonomous Region in China accounts for 31% of the area of cultivated land, and thus it is pivotal for the sustainable agricultural development of the area to identify reliable and cost-effective methodologies to monitor the spatial and temporal variations in soil salinity. This objective was accomplished over the study area (Keriya River Basin, northwestern China) by adopting technologies that heavily rely on, and integrate information contained in, a readily available suite of remote sensing datasets. The following procedures were conducted: (1) a selective principle component analysis (S-PCA) fusion image was generated using Phased Array Type L-band SAR (PALSAR) backscattering coefficient (σ°) and Landsat Enhanced Thematic Mapper Plus (ETM+) multispectral image of Keriya River Basin; and (2) a support vector machines (SVM) classification method was employed to classify land cover types with a focus on mapping salinized soils; (3) a cross-validation method was adopted to identify the optimum classification parameters, and obtain an optimal SVM classification model; (4) Radarsat-2 (C band) and PALSAR polarimetric images were used to analyze polarimetric backscattering behaviors in relation to the variation in soil salinization; (5) a decision tree (DT) scheme for multi-source optical and polarimetric SAR data integration was proposed to improve the estimation and monitoring accuracies of soil salinization; and (6) detailed field observations and ground truthing were used for validation of the adopted methodology, and quantity and allocation disagreement measures were applied to assess classification outcome. Results showed that the fusion of passive reflective and active microwave remote sensing data provided an effective tool in detecting soil salinization. Overall accuracy of the adopted SVM classifier with optimal parameters for fused image of ETM+ and PALSAR data was 91.25% with a Kappa coefficient of 0.89, which was further improved by the DT data integration and classification method yielding an accuracy of 93.01% with a Kappa coefficient of 0.92 and lower disagreement of quantity and allocation.

Highlights

  • Soil salinization negatively affects crop growth and productivity, especially in arid and semi-arid areas where evaporation exceeds rainfall [1]

  • This was due to the fact that slightly salt affected soil was usually covered with 30% vegetation which consists of Tamarix chinensis Lour, Phragmites communis, Haloxylon ammodendron, Karelinia caspica (Figure 2)

  • We found that salt tolerant vegetation such as Tamarix chinensis Lour, Phragmites communis, Halocnemum strobilaceum, Halostachys caspica, Alhagi pseudalhagi can grow in various salinized soils, especially in slightly and moderately salinized soils

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Summary

Introduction

Soil salinization negatively affects crop growth and productivity, especially in arid and semi-arid areas where evaporation exceeds rainfall [1]. The global extent of primary salt-affected soils is 955 M ha, while secondary salinization affects some 77 M ha, with 58% of these are situated in irrigated areas [2]. It is imperative to detect, monitor, and map soil salinity over space and time to prevent further land degradation, and to ensure the sustainable development of agriculture [4,5]. A growing body of studies, aided by statistical analyses of field spectroscopy data and satellite remote sensing observations demonstrates that both multispectral [10,11,12,13,14,15] and hyperspectral passive reflectance data can be used to map soil salinization at landscape scales [16]. Radar data have the potential for evaluating soil salinity through monitoring and mapping salt-affected areas [20]

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