Daly K R, Keyes S D, Roose T
School of Engineering Science, University of Southampton, Southampton SO17 1BJ, England, UK.
Proc Math Phys Eng Sci. 2018 Jul;474(2215):20170745. doi: 10.1098/rspa.2017.0745. Epub 2018 Jul 11.
We show how a combination of X-ray computed tomography (X-CT) and image-based modelling can be used to calculate the effect of moisture content and compaction on the macroscopic structural properties of soil. Our method is based on the equations derived in Daly & Roose (2018 , 20170141. (doi:10.1098/rspa.2017.0141)), which we have extended so they can be directly applied to the segmented images obtained from X-CT. We assume that the soils are composed of air-filled pore space, solid mineral grains and a mixed phase composed of both clay particles and water. We considered three different initial soil treatments, composed of two different compaction levels and two different moisture contents. We found that the effective properties of the soils were unaffected by compaction over the range tested in this paper. However, changing the moisture content significantly altered the hydraulic and mechanical properties of the soils. A key strength of this method is that it enables the optimization or even design of soils composed from different constituents, with specific mechanical and hydraulic properties.
我们展示了如何结合X射线计算机断层扫描(X-CT)和基于图像的建模来计算含水量和压实度对土壤宏观结构特性的影响。我们的方法基于戴利和罗斯(2018年,20170141。(doi:10.1098/rspa.2017.0141))推导的方程,我们对其进行了扩展,使其能够直接应用于从X-CT获得的分割图像。我们假设土壤由充满空气的孔隙空间、固体矿物颗粒以及由粘土颗粒和水组成的混合相组成。我们考虑了三种不同的初始土壤处理方式,由两种不同的压实水平和两种不同的含水量组成。我们发现,在本文测试的范围内,压实度对土壤的有效特性没有影响。然而,改变含水量会显著改变土壤的水力和力学特性。这种方法的一个关键优势在于,它能够对由不同成分组成、具有特定力学和水力特性的土壤进行优化甚至设计。