Remotely sensed estimation of root-zone salinity in salinized farmland based on soil-crop water relations

IF 5.7 Q1 ENVIRONMENTAL SCIENCES Science of Remote Sensing Pub Date : 2023-10-10 DOI:10.1016/j.srs.2023.100104
Guang Yang , Xuejin Qiao , Qiang Zuo , Jianchu Shi , Xun Wu , Lining Liu , Alon Ben-Gal
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Abstract

Accurate monitoring and evaluation of root-zone soil salt content (SSC) are critical for sustainable development of irrigated agriculture in arid and semi-arid areas. Based on soil-crop water relations and farmland evapotranspiration (ET) fused through remote sensing data, this study developed an inversion method to estimate root-zone SSC using a case study from cotton fields under film mulched drip irrigation (CFFMDI) in the Manas River Basin (MRB) over 21 years (2000–2020). Two hypotheses were set as: (1) relative transpiration can be approximated by relative ET; and (2) the soil water stress response function is linearly proportional to the ratio of relative water supply. Measured data from a field experiment and collected data from regional survey and literature retrieval were used to optimize parameters and verify the hypotheses and method. The method was then applied to analyze the spatial and temporal distribution characteristics and cumulative effects of root-zone SSC. Results showed that the hypotheses and the method were reasonable and reliable in estimating root-zone SSC (with coefficient of determination R2 > 0.50). Along with the popularization of film-mulched drip irrigation and the expansion of CFFMDI over the past 21 years, regional-scale root-zone SSC declined significantly with an annual attenuation rate of about 0.09 g kg−1. Due to the gradual reduction of irrigation amount per unit area, the decline was more rapid before 2011 (0.18 g kg−1), but slightly slowed down or even reversed at the end of the second decade (2015–2020). By 2020, the mean regional root-zone SSC reached 3.93 g kg−1. At the beginning of this century, MRB was mainly composed of mildly- (59.8%) and moderately-salinized CFFMDI (39.9%). However, by 2020, non- (69.7%) and mildly-salinized cotton field (28.2%) dominated the basin. The inversion method of root-zone SSC fully considers the water consumption mechanism of soil-crop system, thus shows great potential in effective planning and management of soil and water resources in arid salinized areas such as MRB.

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基于土壤-作物水分关系的盐渍化农田根区盐度遥感估算
准确监测和评价根区土壤含盐量对干旱和半干旱地区灌溉农业的可持续发展至关重要。基于遥感数据融合的土壤-作物-水分关系和农田蒸散量(ET),本研究开发了一种反演方法,通过对马纳斯河流域21年(2000-2020)棉田膜下滴灌(CFFMDI)的案例研究,估算根区SSC。两个假设是:(1)相对蒸腾作用可以用相对ET近似;(2)土壤水分应力响应函数与相对供水比成线性关系。利用现场实验的测量数据和区域调查和文献检索的收集数据来优化参数并验证假设和方法。然后应用该方法分析了根区SSC的时空分布特征和累积效应。结果表明,这些假设和方法在估算根区SSC方面是合理可靠的(决定系数R2>;0.50)。21年来,随着覆膜滴灌的推广和CFFMDI的扩大,区域尺度根区SSC显著下降,年衰减率约为0.09g kg−1。由于单位面积灌溉量的逐渐减少,2011年之前的下降速度更快(0.18 g kg−1),但在第二个十年(2015-2020)结束时略有放缓甚至逆转。到2020年,平均区域根区SSC达到3.93 g kg−1。本世纪初,MRB主要由轻度(59.8%)和中度盐碱化CFFMDI(39.9%)组成。然而,到2020年,非(69.7%)和轻度盐碱化棉田(28.2%)占据了盆地的主导地位。根区SSC反演方法充分考虑了土壤-作物系统的耗水机制,在MRB等干旱盐碱区水土资源的有效规划和管理中显示出巨大的潜力。
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