VOLCANIC STEAM OUTPUT DIRECTLY MEASURED IN FUMAROLES - THE OBSERVED VARIATIONS AT VULCANO-ISLAND, ITALY, BETWEEN 1983 AND 1987

被引:30
作者
ITALIANO, F
NUCCIO, PM
机构
[1] Istituto di Geochimica dei Fluidi, CNR, Palermo
[2] Istituto di Mineralogia, Petrografia e Geochimica, University of Palermo
关键词
D O I
10.1007/BF00430775
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The mass of steam emitted by the fumaroles of the crater of Vulcano (Aeolian Islands, Italy) was evaluated by using a direct measuring method. Measurements were effected with this method between 1983 and 1987 in nine field campaigns, the results of which are given in this paper. The steam flux measurements were performed by an instrument expressly designed for steam condensation. The estimates of the thermal energy transported daily by the steam gave values of up to 10E12 J. The sharp variations in the total mass outputs recorded in 1984 and 1985 are here interpreted as being a consequence of the probable accumulation of fluid pressure at depth, during the evolution of volcanic activity. The different results obtained from the various areas of the fumarolic field during the evolutionary phases have led to the hypothesis that different subsystems exist that feed the fumaroles, and that their activity is triggered by volcano-tectonics. This method can be applied in the evaluation of both fumarolic steam and thermal energy outputs, and therefore it is particularly useful in geothermal exploration, in the evaluation of the environmental impact of volcanic degassing, and in the forecasting of volcanic eruptions. The evaluation of the steam output is also useful for quantifying the release of other gaseous species and giving univocal interpretations regarding their variations in concentrations. Furthermore this direct method provides a new way of calibrating the flux estimates effected by other telemetric techniques (Lidar, Cospec, etc.).
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页码:623 / 630
页数:8
相关论文
共 30 条
[1]  
Badalamenti B., Falsaperla S., Neri G., Nuccio P.M., Valenza M., Confronto preliminare tra dati sismici e geochimici nell'area Lipar-Vulcano, CNR-GNV Boll, 1986, pp. 37-47, (1986)
[2]  
Badalamenti B., Gurrieri S., Hauser S., Parello F., Valenza M., Soil CO<sub>2</sub> output in the island of Vulcano during the period 1984–1988: surveillance of gas hazard and volcanic activity, Rend Soc Ital Miner Petrol special volume, 43, pp. 893-899, (1988)
[3]  
Berresheim F.D., Jaeschke W., The contribution of volcanoes to the global atmospheric sulphur budget, J Geophys Res, 88, pp. 3732-3740, (1983)
[4]  
Capasso G., Dongarra' G., Favara R., Hauser S., Valenza M., Isotope compositions of rain water, well water and steam on the island of Vulcano, and their implications for volcanic surveillance, J Volcanol Geoth Res, 49, pp. 147-155, (1992)
[5]  
Casadevall T.J., Rose W., Gerlach T., Greenland L.P., Ewert J., Wunderman R., Symonds R., Gas emissions and eruptions at Mount St Helens trough 1982, Science, 221, pp. 1383-1385, (1983)
[6]  
Casadevall T.J., Rose W.I., Fuller W.H., Hunt W.H., Hart M.A., Moyers J.L., Woods D.C., Chuan R.L., Friend J.P., Sulfur dioxide and particles in volcanic plumes from Poas, Arenal and Colima volcanoes, Costa Rica and Mexico, J Geophys Res, 89, pp. 9633-9641, (1984)
[7]  
De Fiore O., I fenomeni eruttivi avvenuti a Volcano (Isole Eolie) nel 1916, Boll Soc Sism Ital XXII, 56, pp. 1-19, (1920)
[8]  
Del Pezzo E., Martini M., Seismic events under Vulcano, Aeolian Islands, Bull Volcanol, 44, 3, pp. 521-525, (1981)
[9]  
Dessau G., Un rilievo topografico del cratere di Vulcano, Boll Soc Geol It, 53, pp. 232-234, (1934)
[10]  
Falsaperla S., Neri G., Contributi sismologici alla sorveglianza vulcanica di Vulcano, CNR-GNV Boll, 1986, pp. 243-254, (1986)