Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Cultrera M.[1]"'
Publikováno v:
Acque Sotterranee, Vol 7, Iss 3 (2018)
Acque sotterranee 7 (2018): 67–70. doi:10.7343/as-2018-344
info:cnr-pdr/source/autori:Galgaro A.[1,3], Cultrera M.[1], Dalla Santa G.[1], Peron F.[2]/titolo:Laboratory thermal conductivity measurements on gravel samples/doi:10.7343%2Fas-2018-344/rivista:Acque sotterranee/anno:2018/pagina_da:67/pagina_a:70/intervallo_pagine:67–70/volume:7
Acque sotterranee 7 (2018): 67–70. doi:10.7343/as-2018-344
info:cnr-pdr/source/autori:Galgaro A.[1,3], Cultrera M.[1], Dalla Santa G.[1], Peron F.[2]/titolo:Laboratory thermal conductivity measurements on gravel samples/doi:10.7343%2Fas-2018-344/rivista:Acque sotterranee/anno:2018/pagina_da:67/pagina_a:70/intervallo_pagine:67–70/volume:7
Modern Ground Source Heat Pumps (GSHPs) systems must be designed by taking into account the ground thermal properties, in order to properly plan the capability of the heat pumps to transfer calories through the Ground Source Heat Exchangers (GSHE) to
Publikováno v:
Hydrogeology journal 26 (2018): 837–851. doi:10.1007/s10040-017-1700-3
info:cnr-pdr/source/autori:Cultrera M.[1], Boaga J.[1], Di Sipio E.[2], Dalla Santa G.[1], De Seta M.[1], Galgaro A.[1,3]/titolo:Modelling an induced thermal plume with data from electrical resistivity tomography and distributed temperature sensing: a case study in northeast Italy/doi:10.1007%2Fs10040-017-1700-3/rivista:Hydrogeology journal/anno:2018/pagina_da:837/pagina_a:851/intervallo_pagine:837–851/volume:26
info:cnr-pdr/source/autori:Cultrera M.[1], Boaga J.[1], Di Sipio E.[2], Dalla Santa G.[1], De Seta M.[1], Galgaro A.[1,3]/titolo:Modelling an induced thermal plume with data from electrical resistivity tomography and distributed temperature sensing: a case study in northeast Italy/doi:10.1007%2Fs10040-017-1700-3/rivista:Hydrogeology journal/anno:2018/pagina_da:837/pagina_a:851/intervallo_pagine:837–851/volume:26
Groundwater tracer tests are often used to improve aquifer characterization, but they present several disadvantages, such as the need to pour solutions or dyes into the aquifer system and alteration of the water’s chemical properties. Thus, tracers
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e06093c100ce23d39d24b061ff7789e5
http://hdl.handle.net/11577/3253520
http://hdl.handle.net/11577/3253520