煤矿土壤的分解机制基于颗粒度和水空气两相流量
Guanji Lyu1,2, Mingxin Zheng1, Lu Xiong1
1College of Transportation Engineering, East China Jiaotong University, Nanchang, Jiangxi 330013, China.
ACS omega
|January 20, 2025
概括
碳含土壤 (CBS) 在干湿周期下分解. 标准基本 (A) 的增加与分解率 (DR) 的降低相关,表明土壤的结构稳定性. 伊利特和水空气流也影响了CBS的分解.
科学领域:
- 地质技术工程 地质技术工程
- 土壤科学 土壤科学
- 环境科学 环境科学
背景情况:
- 含煤土壤 (CBS) 容易因周期性干湿条件而解体.
- 了解CBS分解对于坡道工程安全至关重要.
研究的目的:
- 研究CBS在干湿周期下的分解特性和机制.
- 分析颗粒度和分解率之间的关系.
- 检查矿物学和水空气双相流在CBS分解中的作用.
主要方法:
- 静态水分解试验. 静态水分解试验.
- 环境扫描电子显微镜 (ESEM).环境扫描电子显微镜.
- 矿物质化学组成分析.
主要成果:
- 标准基本 (A) 和分解率 (DR) 之间存在显著的指数关系,较高的A表示较低的DR.
- 在CBS的解体过程中,粒度进化,反映了干湿周期的粒子大小分布变化.
- 伊利特通过水化排斥促进裂纹形成;水空气双相流 (WTF) 通过压力波动驱动分解.
结论:
- 标准基本是CBS在循环湿和干燥下稳定的关键指标.
- 矿物成分 (伊利特) 和水力机械过程 (WTF) 是CBS分解的关键因素.
- 这些发现增强了对CBS行为的理解,以改善斜坡工程实践.
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