在Ca2+溶液环境中对不和红色粘土的分解进行实验研究
Hongming Wang1,2, Zhikui Liu3, Shanmei Li1
1College of Civil Engineering and Architecture, Guilin University of Technology, Guilin, 541004, China.
Scientific reports
|December 2, 2024
概括
地下水中的 (Ca2+) 显著影响了吉林的红土瓦解. 低矩阵吸收加剧了随着Ca2+度的增加而导致的分解,而高矩阵吸收导致了不论Ca2+水平的强烈分解.
科学领域:
- 地质技术工程 地质技术工程
- 环境科学 环境科学
- 土壤力学 土壤力学
背景情况:
- 吉林的地景观具有高度 (Ca2+) 的地下水.
- 红色粘土的解体是岩地区土壤洞穴崩的关键因素.
研究的目的:
- 为了研究Ca2+溶液中不和红色粘土的分解机制.
- 量化矩阵吸收和Ca2+度对红色粘土分解率的影响.
主要方法:
- 使用实时质量变化记录的自制装置进行分解试验.
- 用于矿物成分分析的X射线衍射 (XRD).
- 纸方法用于确定矩阵吸收.
主要成果:
- 矩阵吸入量随着水分含量而降低,随着空隙比率而增加.
- 在矩阵吸收> 965 kPa时,分解是强烈的,独立于Ca2+度.
- 在矩阵吸量<965kPa时,分解速度随着Ca2+度 (0.057到3.027g/s) 的增加而增加.
结论:
- 高矩阵吸收会通过水的进入和空气压缩导致分解,产生拉伸应力.
- 低矩阵吸收诱导的分解是由于Ca2+减少了粘土颗粒的吸引力和扩散层.
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