Chemical and isotopic assessment in volcanic thermal waters: Cases of Ischia (Italy) and São Miguel (Azores, Portugal)

Isotopic fractionation of 10B/11B provides a sound tool for identifying hydrogeochemical processes in complex areas, owing to its ability to discriminate between various scenarios. In addition, the occurrence of boron as a minor element in areas of active volcanism allows its use in comparison with concentrations of other conservative or non‐conservative ions. This allows the detection of water mixtures of diverse origin and temperature, deep or shallow, including fresh water, seawater and even brines. This tool was applied in studies of the volcanic islands of Ischia and São Miguel, across widely differing geographical and climatic contexts. Five groups of waters have been identified in Ischia Island: marine, transition, hot carbonated, cold carbonated and fresh waters. For São Miguel Island the identified groups are cold carbonic, hot carbonic, boiling and acidic boiling waters. Copyright © 2008 John Wiley & Sons, Ltd.

[1]  C. Almeida,et al.  Chemical composition of deep hydrothermal fluids in the Ribeira Grande geothermal field (São Miguel, Azores) , 2006 .

[2]  G. Chiodini,et al.  Mineral control of arsenic content in thermal waters from volcano-hosted hydrothermal systems: Insights from island of Ischia and Phlegrean Fields (Campanian Volcanic Province, Italy) , 2006 .

[3]  G. Ferrara,et al.  Boron isotopic variations in fumarolic condensates and thermal waters from Vulcano Island, Italy: Implications for evolution of volcanic fluids , 2005 .

[4]  J. Erzinger,et al.  Boron isotope composition of geothermal fluids and borate minerals from salar deposits (central Andes/NW Argentina) , 2004 .

[5]  G. Ventura,et al.  Fumarolic and diffuse soil degassing west of Mount Epomeo, Ischia, Italy , 2004 .

[6]  L. Civetta,et al.  B/Nb and δ11B systematics in the Phlegrean Volcanic District, Italy , 2004 .

[7]  J. Cruz,et al.  Major ion chemistry of groundwater from perched-water bodies of the Azores (Portugal) volcanic archipelago , 2004 .

[8]  J. Cruz Groundwater and volcanoes: examples from the Azores archipelago , 2003 .

[9]  R. Barnes,et al.  Intercomparison of boron isotope and concentration measurements : Part II: Evaluation of results , 2003 .

[10]  A. Vengosh,et al.  Geochemical constraints for the origin of thermal waters from western Turkey , 2002 .

[11]  Virgilio Cruz,et al.  Hydrogeologic framework of Pico Island, Azores, Portugal , 2001 .

[12]  F. D'amore,et al.  Chemical and isotopical characterisation of fluid manifestations of Ischia Island (Italy) , 2000 .

[13]  P. Nabelek,et al.  Boron, Sr, O, and H isotope geochemistry of groundwaters from Mt. Etna (Sicily)—hydrologic implications , 2000 .

[14]  S. Arnórsson,et al.  The boron isotope systematics of Icelandic geothermal waters: 1. Meteoric water charged systems , 2000 .

[15]  N. Óskarsson,et al.  Chemistry and isotopic composition of fumarole discharges of Furnas caldera , 1999 .

[16]  J. Pacheco,et al.  Volcanic geology of Furnas Volcano, São Miguel, Azores , 1999 .

[17]  Sigurdur R. Gislason,et al.  Chemistry of waters from Furnas volcano, São Miguel, Azores: fluxes of volcanic carbon dioxide and leached material , 1999 .

[18]  S. Caliro,et al.  Variation in the total dissolved carbon isotope composition of thermal waters of the Island of Ischia (Italy) and its implications for volcanic surveillance , 1999 .

[19]  V. Acocella,et al.  The interaction between regional and local tectonics during resurgent doming: the case of the island of Ischia, Italy , 1999 .

[20]  A. Spivack,et al.  THE B ISOTOPIC COMPOSITION OF ARC LAVAS FROM MARTINIQUE, LESSER ANTILLES , 1997 .

[21]  D. Tedesco Chemical and isotopic investigations of fumarolic gases from Ischia island (southern Italy): Evidences of magmatic and crustal contribution , 1996 .

[22]  K. Murray Hydrology and Geochemistry of Thermal Waters in the Upper Napa Valley, California , 1996 .

[23]  M. Nakano,et al.  Boron isotope geochemistry of hot spring waters in Ibusuki and adjacent areas, Kagoshima, Japan , 1996 .

[24]  G. Davidson,et al.  Identification of groundwater solute sources using boron isotopic composition. , 1995, Environmental science & technology.

[25]  S. Arnórsson,et al.  Processes controlling the distribution of boron and chlorine in natural waters in Iceland , 1995 .

[26]  A. Vengosh,et al.  Boron isotope application for tracing sources of contamination in groundwater. , 1994, Environmental science & technology.

[27]  E. Nakamura,et al.  Origin of the slab component in arc lavas from across-arc variation of B and Pb isotopes , 1994, Nature.

[28]  S. Barth Boron isotope variations in nature: a synthesis , 1993 .

[29]  G. Davidson,et al.  Application of Boron Isotopes for Identifying Contaminants such as Fly Ash Leachate in Groundwater , 1993 .

[30]  A. Chivas,et al.  Boron isotope variations during fractional evaporation of sea water: New constraints on the marine vs. nonmarine debate , 1992 .

[31]  L. Bolognesi,et al.  Geothermal assessment of the island of ischia (southern Italy) from isotopic and chemical composition of the delivered fluids , 1992 .

[32]  A. Chivas,et al.  Boron isotope geochemistry of Australian salt lakes , 1991 .

[33]  A. Zanchi,et al.  Simple-shearing block resurgence in caldera depressions. A model from Pantelleria and Ischia , 1991 .

[34]  L. Civetta,et al.  Sr- and Nd-isotope and trace-element constraints on the chemical evolution of the magmatic system of Ischia (Italy) in the last 55 ka , 1991 .

[35]  R. Mazzuoli,et al.  Geochemistry of recent volcanics of Ischia Island, Italy: Evidences for fractional crystallization and magma mixing , 1989 .

[36]  M. Gennaro,et al.  Geochemistry of thermal waters on the island of Ischia (Campania, Italy) , 1984 .

[37]  A. J. Ellis,et al.  Chemistry and Geothermal Systems , 1977 .

[38]  L. Civetta,et al.  Volcanic history of the Island of Ischia (South Italy) , 1976 .