考虑煤储层自调节效应的物质平衡方程的推导
erivation for material-balance equation based on the consideration of coal seam’s self-adjusting function
煤储层在排水采气的过程中,一方面随着流体压力的降低,基质发生膨胀,基质之间的裂隙缩小;另一方面,随着煤层气的解吸,煤基质会收缩,储层裂隙会增大(自调节效应)。裂隙的变化最终取决于两种作用的差值。目前国内外对于煤储层自调节效应的研究,多集中在渗透率动态变化研究方面,而在煤层气藏的物质平衡研究中,没有考虑自调节效应。本文在考虑了降压-解吸对储层裂隙的双重作用的前提下,推导了煤层气藏的物质平衡方程。另外,本文对如何提高物质平衡法的实际应用效果做了初步的理论探讨。
uring the water draining and gas production in the coal seam,the hydrodynamic pressure will decrease, and the matrixes will expand, so the crannies will be compressed; And at the same time, the matrixes will shrink in response to gas desorption, so the crannies will be splayed (self-adjusting function). The variance of crannies will be decided by the difference of the two effects. At present, researches on this matter mainly converge in the aspect of permeability’s performance analysis, while in the aspect of material-balance research, this matter has not been considered. This article has taken account of this matter, and derived material –balance equation for coal seam. In addition, the article has made preliminary research on how to use well the material-balance techniques.
胡素明、李相方
矿业工程理论与方法论
煤层气物质平衡解吸自调节水侵
coalbed methanematerial-balancedesorptionself-adjustmentwater influx
胡素明,李相方.考虑煤储层自调节效应的物质平衡方程的推导[EB/OL].(2009-06-05)[2025-08-18].http://www.paper.edu.cn/releasepaper/content/200906-188.点此复制
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