马东豪, 张佳宝, 黄平. 确定Brooks-Corey土壤水力特性模型参数的垂直入渗方法[J]. 水科学进展, 2011, 22(2): 235-241.
引用本文: 马东豪, 张佳宝, 黄平. 确定Brooks-Corey土壤水力特性模型参数的垂直入渗方法[J]. 水科学进展, 2011, 22(2): 235-241.
MA Dong-hao, ZHANG Jia-bao, HUANG Ping. Determination of Brooks-Corey soil hydraulic parameters through vertical infiltration experiments[J]. Advances in Water Science, 2011, 22(2): 235-241.
Citation: MA Dong-hao, ZHANG Jia-bao, HUANG Ping. Determination of Brooks-Corey soil hydraulic parameters through vertical infiltration experiments[J]. Advances in Water Science, 2011, 22(2): 235-241.

确定Brooks-Corey土壤水力特性模型参数的垂直入渗方法

Determination of Brooks-Corey soil hydraulic parameters through vertical infiltration experiments

  • 摘要: 在水平入渗方法的基础上,提出了一种不需测定饱和导水率,仅利用一维垂直入渗试验即可确定Brooks-Corey模型参数的新方法.利用封丘县两种质地土壤的入渗资料,对所提出的方法进行了检验.结果表明,只要入渗历时足够长,基质势和重力势作用相当,垂直入渗方法确定的土壤水力参数与水平吸渗方法的预测结果相近;利用预测的参数,数值解和提出的近似解均能很好模拟土壤水分入渗过程.相对于水平吸渗方法和反推参数法,垂直入渗方法省时省力,且能避免数值弥散和参数不唯一问题.

     

    Abstract: A new method is proposed for estimating soil hydraulic parameters in the Brooks-Corey model.The method uses only one-dimensional vertical infiltration experiments,thus,measurement of saturated hydraulic conductivity is not required.The method is tested in two soil textures in Fengqiu County.The result shows that the Brooks-Corey soil parameters estimated by the new method are quite comparable to those of using the horizontal absorption method when the gravitational potential is balanced by the matric potential(capillary potential) and the soil stays wet long enough.Using the estimated parameters,the infiltration process simulated by the Brooks-Corey model is in good agreement with the observation.The new method saves time and effort,and can help to avoid the numerical dispersion problems as well as multiple solutions compared to other methods such as the horizontal absorption method and the inverse parameter method.

     

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