http://www.cnr.it/ontology/cnr/individuo/prodotto/ID42386
EVALUATION OF FLOW RATE IN UNSATURATED ROCK: FIELD TEST WITH INTEGRATED APPROACH (Articolo in rivista)
- Type
- Label
- EVALUATION OF FLOW RATE IN UNSATURATED ROCK: FIELD TEST WITH INTEGRATED APPROACH (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- CAPUTO M.C.; DE CARLO L.; DE BENEDICTIS F. (literal)
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- http://www.psp-parlar.de/details_artikel.asp?tabelle=FEBArtikel&artikel_id=3241&jahr=2010 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- Scopus (literal)
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CAPUTO M.C. - Water Research Institute (IRSA), National Research Council (CNR), Viale F. De Blasio N.5, 70123, Bari, Italy
DE CARLO L. - Water Research Institute (IRSA), National Research Council (CNR), Viale F. De Blasio N.5, 70123, Bari, Italy
DE BENEDICTIS F. - Water Research Institute (IRSA), National Research Council (CNR), Viale F. De Blasio N.5, 70123, Bari, Italy (literal)
- Titolo
- EVALUATION OF FLOW RATE IN UNSATURATED ROCK: FIELD TEST WITH INTEGRATED APPROACH (literal)
- Abstract
- The knowledge of the unsaturated flow rate is essential
for both groundwater protection and management, however
it is not easy to determine experimentally, especially
on the rocks and in the field.
This study aims to evaluate the flow rate of potential
contaminants in a porous aquifer using an integrated approach
that combines electrical resistivity measurements
with a large ring infiltrometer test.
Specifically, the field tests were carried out on the outcrop
of sandstone in a quarry, located in Southern Italy,
which has recently been affected by mycelium sludge derived
from pharmaceutical industry waste. The electrical
resistivity tomography was carried out to visualise the infiltration
of water in the subsoil in order to evaluate the unsaturated
water flow in the sandstone. Simultaneously, the
vertical flow into the unsaturated subsoil was investigated
by measuring water levels in a large adjustable ring infiltrometer,
sealed directly on the rock. The results of this
study confirm the efficacy of the combined methodologies
to monitor the vertical flow through unsaturated porous rock. (literal)
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