hrcak mascot   Srce   HID

Izvorni znanstveni članak

Radon Concentration in Thermal Water as an Indicator of Seismic Activity

Asta Gregorič
Boris Zmazek
Janja Vaupotič

Puni tekst: engleski, pdf (145 KB) str. 95-98 preuzimanja: 739* citiraj
APA 6th Edition
Gregorič, A., Zmazek, B. i Vaupotič, J. (2008). Radon Concentration in Thermal Water as an Indicator of Seismic Activity. Collegium antropologicum, 32 - Supplement 2 (2), 95-98. Preuzeto s https://hrcak.srce.hr/34548
MLA 8th Edition
Gregorič, Asta, et al. "Radon Concentration in Thermal Water as an Indicator of Seismic Activity." Collegium antropologicum, vol. 32 - Supplement 2, br. 2, 2008, str. 95-98. https://hrcak.srce.hr/34548. Citirano 16.06.2021.
Chicago 17th Edition
Gregorič, Asta, Boris Zmazek i Janja Vaupotič. "Radon Concentration in Thermal Water as an Indicator of Seismic Activity." Collegium antropologicum 32 - Supplement 2, br. 2 (2008): 95-98. https://hrcak.srce.hr/34548
Harvard
Gregorič, A., Zmazek, B., i Vaupotič, J. (2008). 'Radon Concentration in Thermal Water as an Indicator of Seismic Activity', Collegium antropologicum, 32 - Supplement 2(2), str. 95-98. Preuzeto s: https://hrcak.srce.hr/34548 (Datum pristupa: 16.06.2021.)
Vancouver
Gregorič A, Zmazek B, Vaupotič J. Radon Concentration in Thermal Water as an Indicator of Seismic Activity. Collegium antropologicum [Internet]. 2008 [pristupljeno 16.06.2021.];32 - Supplement 2(2):95-98. Dostupno na: https://hrcak.srce.hr/34548
IEEE
A. Gregorič, B. Zmazek i J. Vaupotič, "Radon Concentration in Thermal Water as an Indicator of Seismic Activity", Collegium antropologicum, vol.32 - Supplement 2, br. 2, str. 95-98, 2008. [Online]. Dostupno na: https://hrcak.srce.hr/34548. [Citirano: 16.06.2021.]

Sažetak
Radon concentration in thermal springs at Hotavlje and Bled has been measured from October 2005 to June 2008
and from October 2005 to September 2007, respectively. At both locations several anomalies in radon concentration were
observed, that might have been caused by seismic events. In this study all earthquakes with ratio (D/R) between strain radius
(D) and distance to the epicenter (R) greater than 0.5 were taken into account. Five earthquakes occurred in the vicinity
of Bled in this period, the strongest at a distance of 17 km with the magnitude ML=3.8 and four radon anomalies
were observed. At Hotavlje fourteen earthquakes occurred in the vicinity with D/R ratio from 0.5 to 2.9. During this period
three radon anomalies were observed.

Ključne riječi
radon; anomalous radon level; thermal water; earthquakes

Hrčak ID: 34548

URI
https://hrcak.srce.hr/34548

Posjeta: 905 *