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Time step-size on simulation of tree-induced capillary potential in unsaturated soils

机译:模拟非饱和土壤中毛细血管电势的时间步长

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Unreliability in the assumption of soil properties, selection of elapse time, choice of time step size and atmospheric variables causes most inconsistencies in the simulation results. Therefore, time step size studied was based on root water up-take on a single Lime tree on a Boulder Clay. The effects of ¼, ½ and 1 day time step sizes on generated capillary potential at 0.0 m, 1.4 m and 3.0 m from the lime tree for elapse time of 30, 90, 190 and 270 days elapsed time were studied. A straightforward sink term for root water uptake was used and combined with two-dimensional axi-symmetric governing equation for unsaturated soil. The simulated capillary potential was directly proportional to the elapsed time. The time step sizes studied were found to give the same generated capillary potentials at same spacial distances. The idea was to investigate the generated capillary potentials at ¼, ½ and 1 days time steps sizes at a same spatial distance from the Lime tree on a Boulder Clay should be the same. Consequently, the difference in the results generated with the three initial time step sizes were far less than ±5%, which is satisfactory.
机译:在假定土壤性质,经过时间的选择,时间步长的选择和大气变量的选择上的不可靠性导致了模拟结果中的大多数不一致性。因此,研究的时间步长是基于在Boulder粘土上的单个Li树上吸收根系水的量。 ¼,½的影响研究了在距m树0.0 m,1.4 m和3.0 m处经过30、90、190和270天后产生的毛细电势的1天时间步长。使用了直接的根吸收水槽术语,并将其与非饱和土壤的二维轴对称控制方程相结合。模拟的毛细管电势与经过时间成正比。发现研究的时间步长在相同的空间距离下产生相同的毛细管电势。这个想法是研究在¼,½处产生的毛细管电势。和在Boulder粘土上距tree树的空间距离相同的1天时间步长大小应该相同。因此,使用三个初始时间步长大小生成的结果差异远小于±5%,这是令人满意的。

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