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Effect of Saline Water Irrigation on Soil Moisture and Salinity and Modeling Transpiration of Greenhouse-Grown Tomato in Response to Salt Stress

机译:盐水冲洗对盐胁迫盐胁迫下温室生长番茄土壤水分和盐度及造型蒸腾的影响

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Fresh water shortage is a major limiting factor for the development of greenhouse agriculture in arid regions. Brackish or saline water irrigation is an important approach to address this issue. However, the salts from irrigation water are also brought into the soil. If the salts accumulate in the crop root zone, it may have a negative effect on crop growth. In this study, a greenhouse experiment was carried out to evaluate the influence of saline water irrigation on soil moisture and salinity and to examine the response of tomato transpiration to salt stress. The treatments comprised of three salinity levels (0.4 g L ?1 (fresh water; control), 3.4 g L ?1 and 6.4 g L ?1 ; denoted as T1, T2 and T3, respectively). Results showed that saline water irrigation significantly increased soil moisture and salinity, while no obvious difference was observed in root length density distribution among the treatments. Further, a method was developed to optimize the parameters in tomato transpiration model using the data from T3 treatment and the results were validated using the data from T2 treatment. We found that the optimized model could well simulate the effects of salt accumulation on tomato transpiration. Overall, our results would provide theoretical and technical support for soil salt regulation and sustainable saline water utilization for greenhouse agricultural production.
机译:淡水短缺是干旱地区温室农业发展的主要限制因素。咸水或盐水灌溉是解决这个问题的重要方法。然而,来自灌溉水的盐也被带入土壤中。如果盐在作物根区积聚,则可能对作物生长产生负面影响。在这项研究中,进行了温室实验,以评估盐水灌溉对土壤水分和盐度的影响,并检查番茄蒸腾对盐胁迫的反应。该治疗包含三个盐度水平(0.4gl≤1(淡水;对照),3.4gl≤1和6.4gl≥1;表示为T1,T2和T3)。结果表明,盐水灌溉显着提高土壤水分和盐度,同时在治疗中的根部长度密度分布中没有观察到明显差异。此外,开发了一种方法以利用来自T3处理的数据来优化番茄蒸腾模型中的参数,并且使用来自T2处理的数据进行验证结果。我们发现优化的模型可以很好地模拟盐积累对番茄蒸腾的影响。总体而言,我们的结果将为温室农业生产的土壤盐调控和可持续盐水利用提供理论和技术支持。

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