Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/4390
DC Field | Value | Language |
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dc.contributor.authorall | Paternoster, M.; Department of Geological Sciences, University of Basilicata, Campus Macchia Romana, I-85100 Potenza, Italy | en |
dc.contributor.authorall | Liotta, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Favara, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.date.accessioned | 2008-12-01T13:20:47Z | en |
dc.date.available | 2008-12-01T13:20:47Z | en |
dc.date.issued | 2008-01-01 | en |
dc.identifier.uri | http://hdl.handle.net/2122/4390 | en |
dc.description.abstract | A rain gauge network consisting of five sites located at different altitudes, ranging from 320 to 1285 m.a.s.l., was installed at Mt. Vulture volcano (southern Italy). Rain water samples were collected monthly over a two-year period and their isotopic composition (d18O and dD) was analyzed. During the same period, circulating groundwater was sampled from 24 springs and wells distributed throughout the study area. Monthly isotopic composition values were used to determine the local meteoric water line (LMWL). Its slope is slightly lower than the relationship defined by Longinelli and Selmo (Longinelli, A., Selmo, E., 2003. Isotopic composition of precipitation in Italy: a first overall map. J. Hydrol. 270, 75–88) for southern Italy. The groundwater samples analyzed were distributed essentially along the LMWL. The weighted local meteoric water line (WLMWL), defined through the mean values weighted by the rainfall amount, however, may define in a short range the meteoric end-member in the local hydrological cycle more precisely. Since most of the groundwater sampling locations do not show seasonal variations in their stable isotope values, the flow system appears to be relatively homogeneous. The mean altitude of the recharge by rainfall infiltration was estimated on the basis of the local vertical isotopic gradient d18O. A few springs, which show anomalous isotopic values, reveal more regional circulation systems, associated with tectonic structures responsible for the ascent of deeper water. | en |
dc.language.iso | English | en |
dc.publisher.name | Elsevier | en |
dc.relation.ispartof | Journal of Hydrology | en |
dc.relation.ispartofseries | /348 (2008) | en |
dc.relation.isversionof | http://hdl.handle.net/2122/3212 | en |
dc.subject | Isotopic composition | en |
dc.title | Stable isotope ratios in meteoric recharge and groundwater at Mt. Vulture volcano, southern Italy | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 87-97 | en |
dc.identifier.URL | http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V6C-4PRYG9K-8&_user=5381242&_rdoc=1&_fmt=&_orig=search&_sort=d&view=c&_acct=C000067082&_version=1&_urlVersion=0&_userid=5381242&md5=fe900a43b1d7ed7ece7ac4d148395698 | en |
dc.subject.INGV | 03. Hydrosphere::03.02. Hydrology::03.02.02. Hydrological processes: interaction, transport, dynamics | en |
dc.identifier.doi | 10.1016/j.jhydrol.2007.09.038 | en |
dc.description.obiettivoSpecifico | 1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attive | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Paternoster, M. | en |
dc.contributor.author | Liotta, M. | en |
dc.contributor.author | Favara, R. | en |
dc.contributor.department | Department of Geological Sciences, University of Basilicata, Campus Macchia Romana, I-85100 Potenza, Italy | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Università della Basilicata, Potenza, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
crisitem.author.orcid | 0000-0002-7203-1565 | - |
crisitem.author.orcid | 0000-0003-4588-2935 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 03. Hydrosphere | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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Paternoster et al 2008.pdf | Main article | 914.58 kB | Adobe PDF |
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