首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Time-lapse 3D imaging of calcite precipitation in a microporous column
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Time-lapse 3D imaging of calcite precipitation in a microporous column

机译:微孔柱中方解石沉淀的时间流逝3D成像

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摘要

Time-lapse X-ray computed tomography is used to image the evolution of calcite precipitation during flow through microporous quartz over the course of 400 h. The growth rate decreases by more than seven times, which is linked to the clogging of flow paths that restricts flow to some regions of the column. Fewer precipitates are observed as a function of column depth, which is found to be related to a differential nucleation density along the sample. A higher nucleation density closer to the inlet implies more crystal volume increase per unit of time without affecting the rate if normalized to the surface area of crystals. Our overall growth rates measured in porous media are orders of magnitude slower than growth rates derived from traditional precipitation experiments on free surfaces.
机译:时间间隔X射线计算机断层扫描用于通过微孔石英在400小时内通过微孔石英进行图像的演化。 生长速率降低了超过七次,这与限制柱子的某些区域的流动路径的堵塞有关。 观察到较少的沉淀物作为柱深度的函数,该函数被发现与沿着样品的差分成核密度有关。 更近于入口的成核密度暗示每单位时间的更多晶体体积增加,而不会影响到晶体表面区域的速率。 我们在多孔介质中测量的整体增长率是比自由表面上传统降水实验的生长速率慢的数量级。

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