TY - JOUR
T1 - Time series analysis of CO concentrations from an Eastern Kentucky coal fire
AU - Hower, James C.
AU - O'Keefe, Jennifer M.K.
AU - Henke, Kevin R.
AU - Bagherieh, Amirhossein
PY - 2011/12/1
Y1 - 2011/12/1
N2 - Coal fires in natural outcrops, in abandoned and active coal mines, and in coal and coal-refuse piles are responsible for the uncontrolled emissions of gases, including CO, CO2, H2S, hydrocarbons, and volatile aromatics. Typically, measurements of gases at a mine vent are made over a short time interval, perhaps no more than 10min, including the time for replicate measurements. Such timing provides little information on longer-term variations in emissions, although comparisons of seasonal measurements suggest such changes do occur. To address this problem, we placed temperature and CO data loggers in coal fire vents to collect time series measurements for a period of up to three weeks. For one experiment, 11days of data at one-minute intervals indicated that the CO emissions were generally in the 400-550ppmv range. However near daily depressions in CO concentrations occurred and in some cases fell below 50ppmv; followed by an increase to ~700-800ppmv; in turn followed by a return to the ambient conditions. Data for a separate 21-day collection period in a different vent of the same fire exhibited similar trends, albeit at a higher CO concentration. The drop in CO concentration may be associated with a meteorologically-driven inhalation cycle of the fire, whereby air diluted the combustion generated CO. We propose this was followed by an increase in the intensity of the fire due to increased O2 from the inhaled air, producing increased CO concentrations, before settling back to the ambient conditions.
AB - Coal fires in natural outcrops, in abandoned and active coal mines, and in coal and coal-refuse piles are responsible for the uncontrolled emissions of gases, including CO, CO2, H2S, hydrocarbons, and volatile aromatics. Typically, measurements of gases at a mine vent are made over a short time interval, perhaps no more than 10min, including the time for replicate measurements. Such timing provides little information on longer-term variations in emissions, although comparisons of seasonal measurements suggest such changes do occur. To address this problem, we placed temperature and CO data loggers in coal fire vents to collect time series measurements for a period of up to three weeks. For one experiment, 11days of data at one-minute intervals indicated that the CO emissions were generally in the 400-550ppmv range. However near daily depressions in CO concentrations occurred and in some cases fell below 50ppmv; followed by an increase to ~700-800ppmv; in turn followed by a return to the ambient conditions. Data for a separate 21-day collection period in a different vent of the same fire exhibited similar trends, albeit at a higher CO concentration. The drop in CO concentration may be associated with a meteorologically-driven inhalation cycle of the fire, whereby air diluted the combustion generated CO. We propose this was followed by an increase in the intensity of the fire due to increased O2 from the inhaled air, producing increased CO concentrations, before settling back to the ambient conditions.
KW - Carbon monoxide
KW - Coal fire
KW - Data logger
KW - Markov
KW - Mercury
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U2 - 10.1016/j.coal.2011.10.001
DO - 10.1016/j.coal.2011.10.001
M3 - Article
AN - SCOPUS:82955187819
SN - 0166-5162
VL - 88
SP - 227
EP - 231
JO - International Journal of Coal Geology
JF - International Journal of Coal Geology
IS - 4
ER -