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A PROCESS-BASED MODEL FOR FLUIDIZED BED IN SAND FILLED RESERVOIRS

机译:基于过程的砂岩储层流化床模型

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Arid and semi-arid regions are prone to severe water inadequacies. They are characterized by little rainfall resulting in several seasonal rivers. Seasonal riverbeds provide opportunity for water to be stored in river's sand-beds while their surfaces may appear dry. It is an important source of water in most rural areas under arid conditions. Several numerical models have been developed for solving sediment problems in alluvial rivers. However, rarely if ever were a model applied for sand filled reservoirs. This study presents a model to understand interacting factors through which physical water storage potential can be increased in sand filled reservoirs. Finite different method (FDM) has been applied to numerically solve mass balance continuity equation in sand filled reservoir. There were reasonable agreements between estimated results and experimental measurements from a laboratory setup. The study could provide economic and suitability data for increasing water supplies to a small community.
机译:干旱和半干旱地区容易出现严重的缺水情况。他们的特点是降雨少,导致几条季节性河流。季节性河床为水提供了存储在河沙床中的机会,而河床的表面可能看起来很干。在干旱条件下,它是大多数农村地区的重要水源。已经开发了一些数值模型来解决冲积河流中的沉积物问题。但是,很少有模型被应用到充满沙子的储层中。这项研究提出了一个模型,以了解相互作用的因素,通过这些因素可以在充满沙子的储层中增加物理储水潜力。有限差分法(FDM)已被应用来数值求解砂砾储层的质量平衡连续性方程。估计结果与实验室设置的实验测量值之间存在合理的共识。该研究可以提供经济和适宜性数据,以增加对小社区的供水。

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