Natural underground coal fires are a world-wide concern,
emitting carbon dioxide and other pollutant gasses into the atmosphere;
one such coal fire is located at Durango, Colorado. We carried out elastic
modeling in order to investigate the potential
of applying P-wave seismic methods to the problem of differentiating
between burned and unburned coal in the upper
30 m of the subsurface at the site
near Durango. This is a
challenging problem for any geophysical method, but preliminary modeling results
show that the problem is tractable under certain circumstances. Our highly simplified model
suggests that imaging the coal layer can potentially be accomplished with adequately
high frequencies (source center frequency
125 Hz); imaging the actual burned zone would be more
difficult. The model neglects the major near-surface heterogeneity known to exist
at the site; features such as fissures would surely result in diffractions and reflections
that could obscure much of the desired signal.