Chemical and isotopic variations in fumarolic discharge and thermal waters at Vulcano Island (Aeolian Islands, Italy) during 1996: evidence of resumed volcanic activity

被引:95
作者
Capasso, G [1 ]
Favara, R [1 ]
Francofonte, S [1 ]
Inguaggiato, S [1 ]
机构
[1] CNR, Ist Geochim Fluidi, I-90146 Palermo, Italy
关键词
chemical and isotopic variations; fumarolic discharge and thermal waters; Vulcano Island;
D O I
10.1016/S0377-0273(98)00111-5
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Gas samples from some fumaroles at 'La Fossa' crater and Baia di Levante on Vulcano Island and from a diffuse soil gas emission were analysed during 1995-1996, along with water samples from thermal wells in the area of Vulcano Porto. During 1996, we observed a significant increase both in the gas/steam ratio and in the CO2 concentration, as well as strong variations in delta(13)C(CO2), delta D-H2O and delta(18)OH(2)O of fumarolic gases. These variations are probably related to an increased inflow of deep fluids of magmatic origin. The temperatures of fumaroles did not show remarkable variations except for fumarole F11. In this case, temperature increased by about 80 degrees C from February to August 1996. During the same period, remarkable variations in temperature, phreatic level and chemical and isotopic composition of water were also recorded in one of the geothermal wells in the Vulcano Porto area (Camping Sicilia; T similar to 60 degrees C). The observed variations in this well are probably related to a pressure build-up, occurring at least in the surficial part of the system, because of increased gas flux and/or decreased permeability of the fumarolic degassing system. Chemical and isotopic composition of the water showed that during this evolutionary phase, the content of fumarolic condensate in this well was about 80 to 90%. Based on the observation of physical and chemical variables of the Camping Sicilia fluids, during this phase of activity, it is concluded that this area is affected by a phreatic eruption hazard if a volcanic episode with high energy discharge in a limited time span occurs. It follows that this well may be considered as a preferential point for volcanic activity monitoring, both in the case of normal routine surveillance and in the case of inaccessibility to the crater area. (C) 1999 Elsevier Science B.V. All rights reserved.
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页码:167 / 175
页数:9
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