含气水合物沉积物压力岩心分析技术研究进展

Y. Konno, J. Yoneda, Yusuke Jin
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摘要

气体水合物是笼形化合物,其中的客体分子,如甲烷,处于由水分子形成的笼状结构中。大量的碳被认为储存在天然气水合物中。因此,天然气水合物作为一种重要的碳循环储层和一种可能的未来能源备受关注。了解含气水合物沉积物的储层性质对预测水合物解离行为具有重要意义。然而,分析含有天然气水合物的沉积物样品是相当困难的,因为天然气水合物在取心、处理和测量过程中会分解。在本文中,我们回顾了一种压力核分析技术,它是一种在处理和测量过程中保持样品压力在天然气水合物平衡条件下的独特技术。根据技术进步,将压力岩心分析技术分为三代,并对科学发现进行了总结。最后讨论了该技术在国内外天然气水合物研究中的应用前景。
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Current perspectives on pressure-core analysis technology for gas-hydrate-bearing sediments
: Gas hydrates are clathrate compounds in which guest molecule such as methane is in a cage formed by water molecules. Huge amount of carbon is considered to be stored in natural gas hydrates. Thus, gas hydrates attract much attentions as a major reservoir of carbon cycle and a possible future energy resource. It is important to understand reservoir properties of gas-hydrate-bearing sediments for prediction of gas hydrate dissociation behaviors. However, analysis of sediment samples containing gas hydrates is quite difficult because gas hydrates dissociate during coring, handling, and measuring processes. In this paper, we review a pressure-core analysis technology that is a unique technology keeping sample pressure within the equilibrium conditions of gas hydrates during handling and measuring processes. We categorize the pressure-core analysis technology into three generations according to the technological progress and summarize scientific findings. Finally, we discuss perspective of this technology within and beyond gas hydrate research.
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