论文标题
孔隙率控制生物保化空间砖中的故障
Porosity governs failure in bioconsolidated space bricks
论文作者
论文摘要
了解合并外部土壤的机械响应和失败需要分析传播裂纹之间的相互作用,这是材料固有的孔结构。在这项工作中,我们研究了使用微生物诱导的方解石沉淀(MICP)进行巩固的月球土壤模拟剂的断裂行为。我们基于带有局部光束元素的晶格网络开发一个数值框架,以模拟样品中多个裂纹的成核,传播,分支和合并。我们的模拟捕获了局部孔对裂纹路径的影响,并提供了一种方法,以预测局部材料刚度的全球孔隙率和/或不确定性不同的样品的行为。我们确定了编码单个或多个裂纹生长事件的签名的多个统计晶格参数。我们的结果揭示了与多孔脆性固体中断裂过程中涉及的复杂性,并且可以很容易地适应其他巩固结构中的故障机理和微/宏裂纹的演变。
Understanding the mechanical response and failure of consolidated extra-terrestrial soils requires analyses of the interactions between propagating cracks the material's inherent pore structure. In this work, we investigate the fracture behaviour of lunar soil simulant consolidated using microbially induced calcite precipitation (MICP). We develop a numerical framework, based on a lattice network with local beam elements, to simulate the nucleation, propagation, branching and merging of multiple cracks within the sample. Our simulations capture the effects of local pores on crack paths as well as provides a means to predict the behaviour of samples with varying global porosity and/or uncertainties in local material stiffness. We identify multiple statistical lattice parameters that encode signatures of single or multiple crack growth events. Our results reveal the complexities involved in the fracture process with porous brittle solids and may easily be adapted to understand failure mechanisms and micro/macro crack evolution in other consolidated structures.