基于CT图像的土壤孔隙结构三维重建及水力学性质预测

    Three-dimensional reconstruction of soil pore structure and prediction of soil hydraulic properties based on CT images

    • 摘要: 为了更好地了解土壤孔隙结构对水分运动过程的影响机制,该文利用黄淮海平原原状潮土CT扫描图像,通过数字图像分析和计算机重建技术对孔隙结构进行三维重建,根据图像分析获得的孔隙大小分布和连通性等形态学参数建立了用于描述孔隙尺度结构特征对水分运动影响机制的网络模型,据此预测了样本尺度(样本体积为385.84 cm3)的土壤水力学性质。结果表明,模型预测的水力学性质和实测值基本吻合,变化趋势基本一致,二者的决定系数达0.94以上。结果表明相关网络模型可以较好地模拟孔隙尺度的水分运动过程,可用于预测土壤的非饱和水力学性质。

       

      Abstract: In order to better understand the effects of soil pore structure on water movement, the three-dimensional structure of soil pore was constructed using CT images of fluvor-aquic soil in Huang-Huai-Hai Plain. Pore size distribution and connectivity parameters were determined by digital image analysis. A spatially-correlated network model was set up to describe the effects of pore-scale structure on water flow in soils, and predict the hydraulic properties of soil samples. The results showed that the predicted hydraulic properties agreed well with the measured values and the correlation coefficients were above 0.94. It indicated that correlated network model could simulate pore-scale water movement process, which provides reference for predicting the unsaturated hydraulic properties of soil.

       

    /

    返回文章
    返回