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Soil salinization and critical shallow groundwater depth under saline irrigation condition in a Saharan irrigated land

机译:撒哈拉灌区盐水冲洗条件下的土壤盐渍化与临界浅地下水深度

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摘要

In the arid irrigated lands, understanding the impact of shallow groundwater fluctuation on soil salinization has become crucial. Thus, investigation of the possible options for maintaining the groundwater depth for improving land productivity is of great importance. In this study, under saline irrigation condition, the effects of shallow groundwater depth on water and salt dynamics in the root-zone of date palms were analyzed through a particular field and modeling (SWAP) investigation in a Tunisian Saharan oasis (Dergine Oasis). The model was calibrated and validated against the measured soil water content through the date palm root-zone. The good agreement between measured and estimated soil water content demonstrated that the SWAP model is an effective tool to accurately simulate the water and salt dynamics in the root-zone of date palm. Multiple groundwater depth scenarios were performed, using the calibrated SWAP model, to achieve the optimal groundwater depth. The simulation results revealed that the shallow groundwater with a depth of similar to 80 cm coupled with frequent irrigation ( 20 days interval) during the summer season is the best practice to maintain the adequate soil water content (> 0.035 ( cm(3) cm(-3)) and safe salinity level (< 4 dS m(-1)) in the root- zone layer. The results of field investigation and numerical simulation in the present study can lead to a better management of lands with shallow water table in the Saharan irrigated areas.
机译:在干旱的灌溉土地中,了解浅层地下水波动对土壤盐渍化的影响变得至关重要。因此,调查维持地下水深度以改善土地生产力的可能选择具有重要意义。在这项研究中,通过在突尼斯撒哈拉绿洲(Dergne Oasis)中的特定领域和建模(SWAP)调查分析了浅地下水深度对枣树水和盐动力学对水和盐动力学的影响。通过日期棕榈根区校准该模型并验证测量的土壤水含量。测量和估计土壤含水量之间的良好一致性表明,交换模型是一种有效的工具,可以精确地模拟枣棕榈根区中的水和盐动力学。使用校准的交换模型进行多种地下水深度场景,实现最佳地下水深度。仿真结果表明,夏季期间,具有频繁灌溉(20天间隔20天)的浅地下水的浅层地下水是保持足够土壤含水量的最佳做法(> 0.035(cm(3)厘米( -3))和根系层中的安全盐度水平(<4ds m(-1))。现场调查和本研究数值模拟的结果可能导致与浅水桌的陆地进行更好的管理撒哈拉灌溉区域。

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