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Modeling shallow water table dynamics under subsurface irrigation and drainage

机译:地下排灌条件下浅层地下水动力学模拟

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We develop conceptual and numerical models of water table dynamics under a subsurface irrigation and drainage system. The numerical model is implemented with distinct drainable and fillable porosity parameters that are estimated by accounting for the unsaturated zone fluxes to and from the shallow water table. The model was applied to two field sites under subsurface irrigation and drainage system in northeast Florida to simulate water table dynamics during potato growing seasons in 2010 and 2011. Simulated water table elevations showed a close agreement with the observed water table dynamics in the fields during both growing seasons. Furrows that act as shallow drains in the field facilitated rapid drawdown of the water table after rainfall events, while the outer, deeper ditches provided little drainage of water from the root-zone. Intermittent irrigation regimes, although could substantially reduce surface runoff from the fields, resulted in relatively deeper water tables during the growing season, suggesting a potential trade-off between water deliveries and root-zone soil moisture availability. (C) 2014 Elsevier B.V. All rights reserved.
机译:我们开发了地下灌溉和排水系统下地下水位动力学的概念模型和数值模型。该数值模型采用不同的可排水和可填充孔隙率参数来实现,这些参数通过考虑进出浅水区的非饱和区通量来估算。该模型被应用于佛罗里达州东北部地下灌溉和排水系统下的两个田间场地,以模拟2010年和2011年马铃薯生长季节的地下水位动态。模拟的地下水位高程与实地观测到的两个田间的地下水位动态密切相关生长季节。在降雨事件发生后,犁沟作为田间的浅沟渠促进了地下水位的快速下降,而较深的外部沟渠几乎没有从根部区排出水。间歇灌溉制度虽然可以大大减少田间地表径流,但在生长季节导致地下水位相对较深,这表明水的输送量与根区土壤水分的可利用性之间可能存在权衡。 (C)2014 Elsevier B.V.保留所有权利。

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