F. Goff et al., Passive infrared remote sensing evidence for large, intermittent CO2 emissions at Popocatepetl volcano, Mexico, CHEM GEOL, 177(1-2), 2001, pp. 133-156
Passive infrared (FTIR) and correlation spectrometer (COSPEC) measurements
were conducted at Popocatepetl volcano during February 10 to 26. 1998 from
sites 4 to 17 km distant from the summit. Volcano behavior was relatively q
uiet and SO2 flux averaged 1670 +/- 1420 t/day (51 measurements). relativel
y small for Popocatepetl. Concurrent HCl/SO2 and HF/SO2 ratios were 0.17 +/
- 0.1 and 0.031 +/- 0.003, respectively, about the same as ratios measured
from 1994 to 1997. The amount of CO2 in the volcanic plume was quantified u
sing FASCODE in which atmospheric CO2 is numerically subtracted from the to
tal infrared spectrum to obtain the residual magmatic CO2. Surprisingly, CO
2/SO2 mass ratios rose dramatically to values as high as 140, about 30 time
s higher than typical values of 2 to 8 measured from 1994 to 1996. These ex
cursions in high CO2/SO2 ratios were short-lived, lasting no longer than ab
out 0.5 to 3.0 h but CO2 flux occasionally exceeded 100,000 t/day. We estim
ate that the average CO2/SO2 ratio for the period was about 23, yielding an
average CO2 flux of roughly 38,000 t/day. Chemical and petrographic analys
es of lava and pumice erupted during explosions on June 30, 1997 and Januar
y 1, 1998 show conclusively that Popocatepetl produces mixed products forme
d by injection of mafic magma into a more silicic chamber at temperatures a
nd pressures of roughly 1040 degreesC and 5 kbar. In addition. Popocatepetl
eruptive products include xenoliths of metamorphosed carbonate rocks conta
ining wollastonite and other calc-silicate minerals indicating reaction of
magma with Cretaceous limestone underlying the volcano. Using a normal CO2/
SO2 ratio of 4 for reference. we calculate an average excess CO2 production
of 32,000 t/day for 17 days. This would require assimilation of only 5 x 1
0(-4) km(3) of limestone, an amount easily accessible in the 3-km-thick Cre
taceous section beneath the volcano. We also examine two scenarios in which
excess CO2 is produced by degassing of subjacent basalt magma, but these e
xplanations seem less plausible to us. Because many other Volcanoes are und
erlain by carbonate sequences, short-duration bursts of CO2 flux, and incre
ased CO2/SO2 ratio, might be observed at other sites, if simultaneous, real
-time measurements of major gas species are made. Published by Elsevier Sci
ence B.V.