http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28465
Variation of geochemical risk associated with the use of ophiolitic washing muds as refilling material in a basalt quarry of the Northern Appennine (Italy). (Articolo in rivista)
- Type
- Label
- Variation of geochemical risk associated with the use of ophiolitic washing muds as refilling material in a basalt quarry of the Northern Appennine (Italy). (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00254-007-0657-2 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Voltaggio Mario; Spadoni Massimo (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Voltaggio Mario - istituto di geologia ambientale e geoingegneria
Spadoni Massimo - Istituto di geologia ambientale e geoingegneria (literal)
- Titolo
- Variation of geochemical risk associated with the use of ophiolitic washing muds as refilling material in a basalt quarry of the Northern Appennine (Italy). (literal)
- Abstract
- Ophiolitic sequences in Northern Apennines
are usually exploited as source of raw material
for civil engineering works. Grinding procedures of
basalts imply the production of dusts with relatively
high concentration of PHES. This paper studied the
increase of geochemical risk when washing mud produced
at Sasso di Castro quarry site (Tuscany) is reused
as rock keeper in a near dismissed quarry and
highlighted geochemical fractionation produced on the
base of different mineral hardness. Co, Cr, Ni and V
concentration measured in washing mud were higher
than the limits fixed by the Italian law but compatible
with background values. The mobility of these four
elements during future weathering processes were
estimated by considering the element transfer coefficients
and assuming weathered rocks and soils as two
different natural analogues of the future state of
washing mud. The future concentration was estimated
by considering the average lifetime of mineral grains
calculated through their dissolution rate, molar volume
and grain diameter. The variations of geochemical
concentrations were used to estimate the percentage
increase of the geochemical risk at the displacement
place. After 50 years the associated geochemical risk is
still considerably lower than the probability to be
damaged by a single landslide event. (literal)
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- Autore CNR
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