首页> 外文会议>International CoalBed and Shale Gas Symposium >Permeability, Elastic, and Carbon Dioxide-Sorption Properties of Upper Freeport Coalbed Cores from a Carbon Dioxide Sequestration/Enhanced Coalbed Methane Field Project
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Permeability, Elastic, and Carbon Dioxide-Sorption Properties of Upper Freeport Coalbed Cores from a Carbon Dioxide Sequestration/Enhanced Coalbed Methane Field Project

机译:来自二氧化碳封存/增强煤层野外工程上部自由口煤层芯的渗透性,弹性和二氧化碳 - 吸附性能

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The National Energy Technology Laboratory (NETL) of the U.S. Department of Energy is aiding its industrial and academic partners in a field project to assess the suitability of unmineable coal seams for sequestration of carbon dioxide and enhanced coalbed methane production. The permeability behavior of bituminous and sub-bituminous coals is know to be quite complex. According to laboratory data and various models, the permeability depends on the fluid composition, the network of cleats in the coal, the fluid pressure, the lithostatic or coriflning pressure, and the Young's modulus and Poisson's ratio of the coal. In the laboratory experiments reported here, steady-state permeabilities to helium, methane, or carbon dioxide were measured for Upper Freeport cores from a field sequestration project. Bulk compressibilities were measured by compressing the sample in an X-ray CT (computer tomography) scanner and calculating changes of sample density. Fluid pressure, confining pressure, history of pressure changes (i.e., pressure hysteresis), and fluid composition were extensively explored and found to have important effects on the permeability. Results were found which appeared to confirm that useful permeabilities depend on flow through the cleats, and that under certain conditions permeabilities can be reduced by several orders of magnitude due to cleat closure. These experiments may suggest additional measurements or models for the permeabilities of various coals and their dependence on elastic, gas sorption, and swelling and shrinkage parameters.
机译:美国能源部的国家能源技术实验室(Netl)正在助攻其工业和学术伙伴在一个领域项目中,以评估未解除的煤层用于隔离二氧化碳和增强的煤层气生产的适用性。沥青和亚沥青煤的渗透行为是非常复杂的。根据实验室数据和各种型号,渗透率取决于流体组成,煤中的砂砾网络,流体压力,岩性或可系源压力,以及幼苗的模量和泊松煤的比例。在这里报道的实验室实验中,测量来自野外封存项目的上自由口核来测量氦,甲烷或二氧化碳的稳态渗透性。通过压缩X射线CT(计算机断层扫描)扫描仪中的样品并计算样品密度的变化来测量块状压缩性。流体压力,限制压力,压力变化史(即,压力滞后)和流体组合物被广泛探索,发现对渗透性具有重要影响。发现结果似乎证实了有用的渗透性取决于流过夹层的流动,并且在某些条件下可以通过夹板闭合而减少几个数量级的渗透率。这些实验可以提示各种煤的渗透性的额外测量或模型及其对弹性,气体吸附和溶胀和收缩参数的依赖性。

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