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首页> 外文期刊>Journal of the Indian Society of Soil Science >Simulation of Water and Heat Transport in Drip-irrigated Sandy Soil under Mulched Conditions
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Simulation of Water and Heat Transport in Drip-irrigated Sandy Soil under Mulched Conditions

机译:覆盖条件下滴灌沙土水热传递的模拟

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摘要

Extremely high temperatures during summer and limited water availability are characteristics of arid and semi-arid regions. Drip irrigation offers a great potential for getting high water use efficiency under such situations. Therefore, a field experiment was carried out to quantify the effects of wheat straw mulch on soil water and thermal regime in the drip-irrigated sandy soil under uncropped condition at Regional Research Station Balsamand (29 deg 07/N 75 deg 28/E, 225 m elevation) of CCS HaryanaAgricultural University, Hisar. The field experiment consisted of two treatments, namely 1) control (no mulch), and 2) wheat straw mulch. Two-dimensional Hydras-2D numerical model was used to estimate hydraulic parameters using inverse modeling for simulating water and heat transport under control and mulch field conditions. Soil water content and hourly temperature were measured at different depths. Wheat straw mulch increased the soil water storage by 1.9 L m~(-2) compared to control. The mulch decreased the daily soil temperature amplitude and average temperatures measured at 0.05, 0.10 and 0.20 m depths than those in control. Hydrus-2D model performed well for simulating water flow in control with RMSE values ranging from 0.008 to 0.012 m~3 m~(-3), and in mulch with RMSE values of 0.010 to 0.012 m~3 m~(-3). The model predicted that soil water storage decreased and evaporation increased by increasing the drip irrigation frequency under both the treatments. The Hydrus-2D also simulated diurnal soiltemperatures reasonably well under control and mulch treatments with RMSE values ranging from 0.8 to 1.9 deg C. Thus, mulching is beneficial in conserving soil moisture and moderating soil temperature in arid regions. The Hydrus-2D model was found to bea useful tool for simulating water and heat flow in the drip-irrigated sandy soil under field conditions.
机译:夏季和极端干旱地区的特征是夏季极高的温度和有限的水供应。在这种情况下,滴灌技术具有很高的用水效率。因此,在Balsamand地区研究站(29 deg 07 / N 75 deg 28 / E,225)进行了田间试验,以定量研究未覆盖条件下滴灌沙质土壤中麦草覆盖对土壤水分和热状况的影响。米高度),CCS哈里亚纳邦农业大学,希萨尔。田间试验由两种处理组成,即1)对照(无覆盖)和2)小麦秸秆覆盖。使用二维Hydras-2D数值模型通过逆模型估算水力参数,以模拟控制和覆盖条件下的水和热传输。在不同深度下测量土壤含水量和小时温度。与对照相比,麦草覆盖提高了土壤蓄水量1.9 L m〜(-2)。与对照相比,覆盖物降低了每日土壤温度幅度和在0.05、0.10和0.20 m深度处测得的平均温度。 Hydrus-2D模型在RMSE值介于0.008至0.012 m〜3 m〜(-3)的控制范围内以及RMSE值介于0.010至0.012 m〜3 m〜(-3)的覆盖范围内模拟水流效果良好。该模型预测,在两种处理方式下,通过增加滴灌频率,土壤储水量减少,蒸发增加。 Hydrus-2D还可以在RMSE值介于0.8到1.9℃的控制和覆盖条件下合理地模拟昼夜土壤温度。因此,覆盖有利于保存干旱地区的土壤水分和调节土壤温度。 Hydrus-2D模型被发现是用于模拟田间条件下滴灌沙土中水和热流的有用工具。

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