Spring water and CO2 interaction at Popocatépetl volcano, Mexico
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Abstract
Six years of monitoring HCO - and pH at selected springs at Popocatépetl during the present eruptive period are presented. Small peaks in HCO - concentration and P in springs are associated with small magmatic pulses at Popocatépetl volcano. The magma provides CO2-rich fluids into the water system controlled by meteoric recharge. The PCO2 in equilibrium with the springs is two to four orders of magnitude higher than air-saturated water. The high partial pressure of CO2 also suggests a direct interac- tion with the magmatic fluids. The isotopic signature of carbon as well, supports a magmatic origin for dissolved CO2.
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Martin-Del Pozzo, A. L., Inguaggiato, S., Aceves, F., Sáenz, H., & Aguayo, A. (2002). Spring water and CO2 interaction at Popocatépetl volcano, Mexico . Geofisica Internacional, 41(3), 345–351. https://doi.org/10.22201/igeof.00167169p.2002.41.3.354
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