Pietro Sirianni
Biographic Data
| ID | 7861149 |
|---|---|
| NAME | Pietro Sirianni |
| GIVEN NAMES | Pietro |
| FAMILY NAME | Sirianni |
| SIGNATURE | SIRIANNI P |
| AFFILIATIONS | Institute of Environmental Geology and Geoengineering |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2019 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 0 |
Radon Hazard in Central Italy
Radon ( 222 Rn) is a natural radioactive gas formed in rocks and soil by the decay of its parent nuclide (238-Uranium). The rate at which radon migrates to the surface, be it along faults or directly emanated from shallow soil, represents the Geogenic Radon Potential (GRP) of an area. Considering that the GRP is often linked to indoor radon risk levels, we have conducted multi-disciplinary research to: (i) define local GRPs and investigate their …
Geology of the central part of the Amatrice Basin (Central Apennines, Italy)
A 1:5,000 scale geological map and 31 geological cross-sections are presented for the surroundings of Amatrice village (central Apennines, Italy), epicentral area of the first damaging earthquake of the 2016–2017 seismic sequence. This detailed geological dataset focuses on: (i) the extent, the thickness, and the internal stratigraphic architecture of the Quaternary continental deposits; (ii) the bedding and the thickness of the Miocene substratu…
No prominent works on this page.
Geology of the central part of the Amatrice Basin (Central Apennines, Italy)
A 1:5,000 scale geological map and 31 geological cross-sections are presented for the surroundings of Amatrice village (central Apennines, Italy), epicentral area of the first damaging earthquake of the 2016–2017 seismic sequence. This detailed geological dataset focuses on: (i) the extent, the thickness, and the internal stratigraphic architecture of the Quaternary continental deposits; (ii) the bedding and the thickness of the Miocene substratu…
Radon Hazard in Central Italy
Radon ( 222 Rn) is a natural radioactive gas formed in rocks and soil by the decay of its parent nuclide (238-Uranium). The rate at which radon migrates to the surface, be it along faults or directly emanated from shallow soil, represents the Geogenic Radon Potential (GRP) of an area. Considering that the GRP is often linked to indoor radon risk levels, we have conducted multi-disciplinary research to: (i) define local GRPs and investigate their …
Geology (2 works) · Bedding (1 work) · Earth science (1 work) · earthquake and tectonic studies (1 work) · Effective dose (radiation) (1 work) · Environmental Science (1 work) · Geochemistry (1 work) · Geologic map (1 work) · Geological and Geochemical Analysis (1 work) · Geological and Geophysical Studies Worldwide (1 work)