13.07.2015 Views

Handbook for Methane Control in Mining - AMMSA

Handbook for Methane Control in Mining - AMMSA

Handbook for Methane Control in Mining - AMMSA

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

CHAPTER 7.—MANAGING EXCESS GAS EMISSIONS ASSOCIATEDWITH COAL MINE GEOLOGIC FEATURESBy James P. Ulery 197In This Chapter Geologic features associated with anomalous methane emissions Gas outbursts and blowers <strong>Methane</strong> dra<strong>in</strong>age strategies <strong>for</strong> mitigat<strong>in</strong>g anomalous methane emissionsand General considerations <strong>for</strong> a methane dra<strong>in</strong>age programThis chapter summarizes how certa<strong>in</strong> geologic features may be associated with unexpected<strong>in</strong>creases <strong>in</strong> gas emissions dur<strong>in</strong>g coal m<strong>in</strong><strong>in</strong>g. These unexpected emissions have the potential tocreate explosive conditions <strong>in</strong> the underground workplace. Also discussed are the generally usedpractices to alleviate potential hazards caused by gas emissions associated with these geologicfeatures.INTRODUCTIONUn<strong>for</strong>eseen m<strong>in</strong>e gas emissions <strong>in</strong> quantities sufficient to create hazardous conditions have beenattributed to sources outside the m<strong>in</strong>ed coalbed s<strong>in</strong>ce the first documentation of methane explosions<strong>in</strong> coal m<strong>in</strong>es [Payman and Statham 1930]. Geologic features such as faults have longbeen recognized as conduits <strong>for</strong> gas flow from strata adjacent to m<strong>in</strong>ed coalbeds [Moss 1927;Payman and Statham 1930]. Other features such as sandstone paleochannels, clay ve<strong>in</strong>s, andlocalized fold<strong>in</strong>g have also been recognized <strong>for</strong> their impact on gas emissions <strong>in</strong>to m<strong>in</strong>e work<strong>in</strong>gs[Darton 1915; Price and Headlee 1943; McCulloch et al. 1975; Ulery and Mol<strong>in</strong>da 1984].The fact that strata adjacent to m<strong>in</strong>ed coalbeds can emit large quantities of methane gas <strong>in</strong>to m<strong>in</strong>ework<strong>in</strong>gs is not surpris<strong>in</strong>g from a theoretical perspective. Many researchers have recognized thatdur<strong>in</strong>g the burial and diagenesis of the organic matter <strong>for</strong>m<strong>in</strong>g today’s m<strong>in</strong>able coalbeds, similardispersed organic matter <strong>in</strong> adjacent strata has produced methane <strong>in</strong> quantities far exceed<strong>in</strong>g thestorage capacity of the coal and surround<strong>in</strong>g rock [Juntgen and Kle<strong>in</strong> 1975]. It is not surpris<strong>in</strong>gthen that large quantities of methane can rema<strong>in</strong> trapped <strong>in</strong> these strata. A potential hazardoccurs when m<strong>in</strong><strong>in</strong>g of a nearby coalbed causes pressure differentials and m<strong>in</strong><strong>in</strong>g-<strong>in</strong>duced fracturesconducive to gas flow <strong>in</strong>to the m<strong>in</strong>e work<strong>in</strong>gs from these strata. This gas flow may befacilitated or temporarily impeded by the presence of geologic structures or anomalies.1 Research geologist, Pittsburgh Research Laboratory, National Institute <strong>for</strong> Occupational Safety and Health,Pittsburgh, PA.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!