从粘土和地先驱物中对形热石进行实验性结晶
Abdulwahab Muhammad Bello1, Anas Muhammad Salisu1, Abduljamiu O Amao1
1College of Petroleum Engineering & Geosciences, Center for Integrative Petroleum Research, King Fahd University of Petroleum & Minerals, Dhahran, Saudi Arabia.
Scientific reports
|March 5, 2026
概括
砂岩中的形岩形成涉及地和粘土溶解. 合成的analcime可以通过孔隙创建来改善砂岩的机械稳定性和水库质量.
科学领域:
- 地质地质地质地质地质地
- 矿物学是一门学科.
- 地质化学 地质化学
背景情况:
- Analcime 是工业用途的状岩石中一个关键的外原性矿物.
- 它的形成来自粘土矿物和田前体并未得到充分理解.
- 之前的研究集中在火山玻璃作为前体.
研究的目的:
- 研究从阿尔科斯砂岩中形成的热水形形成.
- 确定粘土矿物质和地在的起源中的作用.
- 探索对砂岩特性和水库质量的潜在影响.
主要方法:
- 使用Na2CO3溶液 (0.1M,0.5M) 的热水合成.
- 实验在80°C至250°C的温度下进行了336小时.
- 使用显微镜和化学分析分析矿物质溶解和沉.
主要成果:
- 从溶解的地,高岩,石岩和石岩中结晶的 Analcime.
- 立方到梯形形状的形晶体形成.
- 在≥200°C时出现了轻微的热带石阶段 (摩登石,沙巴石).
- Analcime 沉为颗粒涂层,替代剂和毛孔填充水泥.
- 观察到孔径高达9.7微米的孔径.
结论:
- 田和粘土矿物是水热形形成的可行的前体.
- 合成的analcime可以增强砂岩的机械稳定性.
- Analcime 的溶解可以创建二次多孔性,改善水库质量.
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