Introduction to Shale Gas Classification, Formation, & Extraction
Abstract
The production of conventional gas has been declining over the last few years due to dwindling reserves. To counter-act this decline, companies are quickly turning to unconventional gas plays that can offer even greater reserves as shown in figure 1. Unfortunately, recovering unconventional gas is a very difficult process that requires advanced stimulation and/or completion methods as compared to conventional gas wells. The various forms of unconventional gas include tight gas, coal bed methane (CBM), shale gas, and gas hydrates. This paper will present a general overview of shale gas while providing insight into specific shale gas plays located in Canada and the United States. Specifically, it will discuss how the increase in shale gas production in the United States has validated the commercial viability of shale gas drilling through the use of new technological processes including hydraulic fractures in horizontal wells. This technology is then being applied to Canada where according to the NEB, over 1000 tcf of shale gas has been discovered to date.
Introduction
Shale rock is considered by the ERCB as “lithostratigraphic unit having less than 50% by weight organic matter, with: less than 10% of the sedimentary clasts having a grain size greater than 62.5 micrometers; and more than 10% of the sedimentary clasts having a grain size less than 4 micrometers”(Section 1.020(2)(27.1), Oil and Gas Conservation Regulations(OGCR)). In conventional terms this means, a shale gas reservoir consists of very fine grained particles that are filled with organic-rich material. Shale reservoirs are able to store gas in numerous ways. According to Centre for Energy, natural gas can be adsorbed onto insoluble organic matter called kerogen, trapped in pore spaces of fine grained sediments interbedded with shale and
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