Morphology of Gas Bubbles in Mud: A Microcomputed Tomographic Evaluation
Morphology of Gas Bubbles in Mud: A Microcomputed Tomographic Evaluation
复制标题
泥浆中气泡的形态:微计算机断层扫描评估
DOI:
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发表时间:
2005
期刊:
影响因子:
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通讯作者:
Y. Furukawa
中科院分区:
文献类型:
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作者:
A. Reed;B. Boudreau;C. Algar;Y. Furukawa
Abstract : Free gas in surficial sediments commonly forms gas bubbles that attenuate and dampen acoustic waves, influence slope stability, and contribute to greenhouse gas concentrations. Therefore, determining the mechanisms that control bubble shape, size, growth, and migration is important to acoustic sediment characterization and other disciplines. Previously, gas bubble shape, size, and distribution was quantified using "low-resolution" (~500 micron) medical computed tomography (CT). Recently, "high-resolution" (to 30 microns. In several MR cores, gas bubbles formed as vertically oriented oblate spheroids with SARs of ~1.6 (5:1 ratio of length to width), yet in other MR cores, gas bubbles formed elongated fractures that spanned the core width, consequently, a SAR could not be accurately determined. In the CH mud, a gas bubble formed as an oblate spheroid (i.e., coin-shape) with a SAR of ~5.0 (30:1 ratio of length to width) as air was injected incrementally through a capillary tube. It appears that bubble shape (i.e., SAR) and orientation are correlated with sediment physical properties and localized heterogeneity. XMCT images show that gas bubbles grow by fracture mechanics rather than by elastic expansion of the sediments. The images also show that the bubbles exist at sizes that are not resolvable with medical CT and often grow with the principal axis oriented vertically. XMCT has enabled the characterization of gas bubbles that are significantly smaller than those evaluated previously, thus furthering our mechanistic understanding of gas bubble formation and growth.