在温度-压力合下研究花岩的实时子释放模式
Penghua Hu1, Yuan Xin2, Peng Ji2
1School of Resources and Safety Engineering, Central South University, Changsha, 410083, China; Beijing Research Institute of Chemical Engineering Metallurgy, Beijing, 101149, China.
Journal of environmental radioactivity
|July 11, 2025
概括
从花岩中释放的气随着压力增加而加剧,在裂传播期间达到峰值. 温度-压力合显著影响这种释放,特别是在高温下,影响花岩.
科学领域:
- 地质科学 地质科学
- 环境科学 环境科学
- 核工程 核工程是指核工程.
背景情况:
- 矿开采会释放出放射性气.
- 了解在深层条件下从花岩中释放的非常重要,这对安全至关重要.
- 温度-压力合对花岩中子释放的影响需要研究.
研究的目的:
- 为了研究温度-压力合下花岩中气释放的规律.
- 探索不同温度对花岩中子释放行为的影响.
- 为科学预防和控制释放的战略提供基础.
主要方法:
- 在不同温度梯度 (25°C至300°C) 下对花岩进行单轴压缩实验.
- 在实验期间实时监测释放变化.
- 分析释放模式与应变和温度的关系.
主要成果:
- 花岩的子释放量随着应变而增加,裂传播期间达到峰值,然后减少,然后再次增加.
- 在100-150°C时,排气量减少了28.45% (压缩/密集),在150-200°C时增加了29.33% (裂扩张).
- 高温降低花岩的机械性能,加速水蒸发,促进热膨胀,增强释放.
结论:
- 温度-压力合显著影响花岩中的子释放行为.
- 在高温下微裂的产生和扩张为子迁移创造了新的途径.
- 这些发现对于理解释放动态和开发深度采矿环境中的减缓策略至关重要.
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