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pro vyhledávání: '"Guglielmo Federico Antonio Brunetti"'
Autor:
Guglielmo Federico Antonio Brunetti, Christine Stumpp, Carmine Fallico, Gerardo Severino, Samuele De Bartolo
Anomalous transport processes are frequently observed in radial flow to wells in highly heterogeneous aquifers. This is generally related to the presence of preferential flow pathways that bypass the sediment matrix, thus leading to the formation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cefe86f0e541e2d6dd08600ac876c680
https://doi.org/10.5194/egusphere-egu23-6934
https://doi.org/10.5194/egusphere-egu23-6934
Autor:
Guglielmo Federico Antonio Brunetti, Samuele De Bartolo, Carmine Fallico, Ferdinando Frega, Maria Fernanda Rivera Velásquez, Gerardo Severino
The spatial variability of the aquifers' hydraulic properties can be satisfactorily described by means of scaling laws. The latter enable one to relate the small (typically laboratory) scale to the larger (typically formation/regional) ones, therefor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40b3e05766faa6a12254e00cfc6ed328
https://hdl.handle.net/11587/455513
https://hdl.handle.net/11587/455513
Autor:
A. Sommella, Gerardo Severino, S. De Bartolo, Carmine Fallico, Guglielmo Federico Antonio Brunetti
Publikováno v:
Stochastic Environmental Research and Risk Assessment. 33:1651-1657
We deal with the spatial distribution of the hydraulic conductivity K within heterogeneous porous formations where a radial flow (typical of pumping and slug tests) is taking place. In particular, the study provides a wide data-set which is instrumen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d85f04c0bae073e701872778e9fbc363
https://doi.org/10.1007/s00477-019-01704-z
https://doi.org/10.1007/s00477-019-01704-z
Autor:
Maria Fernanda Rivera Velasquez, Carmine Fallico, Ferdinando Frega, Gerardo Severino, Samuele De Bartolo, Guglielmo Federico Antonio Brunetti
The spatial variability of the hydraulic properties of aquifers can be satisfactory described by means of scaling law(s). The latter enables one, among the others, to relate the small (typically laboraory) scale to the larger (typically formation/reg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d73eca08ff89d9f5a6e6209ae3ed4ca0
https://hdl.handle.net/11588/920566
https://hdl.handle.net/11588/920566
We present an experimental study aiming at the identification of the hydraulic conductivity in an aquifer which was packed according to four different configurations. The conductivity was estimated by means of slug tests, whereas the other parameters
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d3a5113c9e05330ae6291c8878b6423
https://hdl.handle.net/11588/832188
https://hdl.handle.net/11588/832188
Autor:
Guglielmo Federico Antonio Brunetti, Samuele De Bartolo, Carmine Fallico, Gerardo Severino, Giuseppe Tripepi
Groundwater flow and contaminant transport are strongly influenced by the aquifer’s heterogeneity (Chao et al., 2000; Fernàndez-Garcia et al., 2004). Generally, the flow (and transport) variables, such as the effective conductivity Keff, can be mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::026d6d716672934f35ab96be9fccc5a7
https://doi.org/10.5194/egusphere-egu2020-4782
https://doi.org/10.5194/egusphere-egu2020-4782