Pregled bibliografske jedinice broj: 829728
Vertical distribution of shallow ground thermal properties in different geological settings in Croatia
Vertical distribution of shallow ground thermal properties in different geological settings in Croatia // Renewable energy, 99 (2016), 1202-1212 doi:10.1016/j.renene.2016.08.022 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 829728 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Vertical distribution of shallow ground thermal properties in different geological settings in Croatia
Autori
Soldo, Vladimir ; Boban, Luka ; Borović, Staša
Izvornik
Renewable energy (0960-1481) 99
(2016);
1202-1212
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Ground thermal properties ; Geological settings ; Distributed thermal response test ; Ground source heat pumps
Sažetak
Heat pumps combined with vertical borehole heat exchangers utilize the ground as a heat source or sink for the purpose of heating or cooling. The proper dimensioning of the borehole heat exchanger requires understanding of the thermophysical properties of the ground surrounding boreholes. Presented research was carried out in two geologically different regions with varying thermal parameters relevant for the utilization of ground-coupled heat pumps: Pannonian Basin System and the Dinarides. Eight different sites were selected based on characteristic geological settings and climate in order to include inland, seaside and mountainous regions. In boreholes, 100 and 130 m deep, double Upipe borehole heat exchangers were installed. The improved method for evaluation of the ground thermal conductivity and thermal resistance of a borehole heat exchanger known as distributed thermal response test was used. This method employs optic fiber cables for the measurement of temperature profiles along the borehole heat exchangers. Measurements conducted at different locations show great variability of thermal properties and undisturbed ground temperatures. Obtained results indicate that the average thermal conductivity of sediments in the Pannonian part varies between 1.62 and 2.10 W/(m K), compared to Dinaridic carbonate and evaporite rocks' values between 2.01 and 3.19 W/(m K).
Izvorni jezik
Engleski
Znanstvena područja
Rudarstvo, nafta i geološko inženjerstvo, Strojarstvo
POVEZANOST RADA
Ustanove:
Hrvatski geološki institut
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus