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- W2034101346 abstract "The Albani Hills are affected by strong CO2 degassing processes. The amount of CO2, which rises from the depths and subsequently dissolves into shallow groundwater, has been estimated to be more than 4.2×109 mol year−1. Most of the gas is released in localised anomalous spots (Lavinio, Solforata, and Ciampino–Albano–Nemi areas), generated by fluid leakage processes from buried pressurized reservoirs hosted by structural highs of the calcareous–siliceous marly basement. The groundwater circulating in the anomalous areas becomes CO2 oversaturated, generating observable gas manifestations whose composition is mainly controlled by gas–liquid separation processes. A gas flow rate of 6.1×108 mol year−1 has been measured from the two larger manifestations using the accumulation chamber technique. The presence at shallow level of CO2 oversaturated groundwater can explain several episodes of sudden release of gas which was documented by historical chronicles from Roman times, until now." @default.
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- W2034101346 date "2001-07-01" @default.
- W2034101346 modified "2023-10-18" @default.
- W2034101346 title "Carbon dioxide degassing from the Albani Hills volcanic region, Central Italy" @default.
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- W2034101346 doi "https://doi.org/10.1016/s0009-2541(00)00382-x" @default.
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