基于HYDRUS—2D的负压灌溉土壤水分入渗数值模拟
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国家自然科学基金资助项目(31101609)和中国农业大学基本科研业务经费资助项目(2011JS144)


Numerical Simulation of Soil Moisture Infiltration under Negative Pressure Irrigation Based on HYDRUS—2D
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    摘要:

    依据土壤水动力学理论,结合负压灌溉条件下土壤水分运动特征,建立了土壤水分入渗模型。利用HYDRUS—2D对所建模型求解,并模拟在负压地下灌溉下,水分在土壤垂直剖面随时间的入渗变化规律。将模拟结果与试验测量结果进行对比验证,结果表明,两者相对误差为2%~4%,所建模型可以有效描述负压地下灌溉条件下土壤水分入渗规律。利用该模型模拟研究了不同灌水器半径(8、10、12cm)和不同土质(北京地区土壤和基质)下土壤水分的入渗情况。结果表明:灌水器半径是影响土壤水分入渗的显著性因素。灌水器半径越大,水分入渗速率越快。灌水器尺寸对入渗起始时的入渗延迟有较大影响,灌水器半径越大,延迟越小。土壤水分入渗速率与灌水器半径呈正相关。

    Abstract:

    Based on the theory of unsaturated soil water dynamics and characteristics of soil moisture movement under negative pressure irrigation, a moisture infiltration model was proposed. The time-varying rules of moisture infiltration at the vertical soil profile on condition of negative pressure irrigation were simulated by moisture infiltration model of HYDRUS—2D. Result showed that the relative error between simulated and measured value was 2%~4%, which was within a reasonable range. The soil moisture infiltration rules under the negative pressure irrigation can be described effectively by the model. Moisture infiltration with different soils (soil and matrix in Beijing area) and different sizes of emitters (radius varied 8, 10 and 12cm) were simulated. The simulation results indicated that emitter size was a significant influence factor for soil moisture infiltration. The initial moisture migration rate was faster with larger emitter than that with smaller emitter. Meanwhile, the delay at the beginning of infiltration was shorter with larger emitter. There was a positive correlation between infiltration rate and emitter size, and water infiltration rate increased with the increase of the radius of emitter.

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冀荣华,王婷婷,祁力钧,杨知伦.基于HYDRUS—2D的负压灌溉土壤水分入渗数值模拟[J].农业机械学报,2015,46(4):113-119.

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  • 收稿日期:2014-07-12
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  • 在线发布日期: 2015-04-10
  • 出版日期: 2015-04-10