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碳酸从无形转化为晶体的转变会在封闭的流体中驱动复杂的降水模式
Jianping Xu1, Matthew T Balhoff2
1Hildebrand Department of Petroleum and Geosystems Engineering, The University of Texas at Austin, Austin, TX 78712, USA; Center for Subsurface Energy and the Environment, The University of Texas at Austin, Austin, TX 78712, USA; John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, USA.
碳酸在降水过程中从无形转化为晶体的过程,在狭窄的微流体系统中驱动复杂的流体动力学和独特的降水模式. 这一发现为矿物沉和反应运输提供了新的见解.
科学领域:
- 地质化学 地质化学
- 流体动力学 流体动力学
- 材料科学 材料科学 材料科学
背景情况:
- 碳酸沉涉及无形到晶体的过渡,改变沉形态.
- 虽然在生物矿物化和合成方面进行了研究,但其对流体动力学的影响仍未得到充分研究.
研究的目的:
- 为了研究碳酸从无形转化为晶体转化的影响,碳酸在混合诱导的沉在微流体的流体动力学.
- 描述由此产生的降水模式及其与流动行为的关系.
主要方法:
- 微流体实验包括同时注射碳酸 (Na2CO3) 和化 (CaCl2) 溶液.
- 格子博尔兹曼模拟用于模拟膜演变,流体压力和降水模式.
主要成果:
- 在混合界面形成无形碳酸薄膜,随后溶解和再结晶.
- 薄膜的稀薄和破裂导致各种流体的移位,混合和二次薄膜的生长.
- 显而易见的降水模式 (局部化,间歇性,均) 出现,由合膜动态和流体压力驱动.
结论:
- 形态到晶体的转变是限制系统中规范降水模式和流体动力学的关键因素.
- 这些发现为地质碳捕集,反应运输和生物矿物化相关的矿物沉提供了新的见解.
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