Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Ines Krajcar Bronič"'
Publikováno v:
Geologija, Vol 51, Iss 2, Pp 169-180 (2008)
The stable isotopic composition of hydrogen and oxygen (δ2H and δ18O) and tritium activity (3H) are monitored in monthly precipitation at Ljubljana since 1981. Here we present complete set of numerical data and the statistical analysis for period 1
Externí odkaz:
https://doaj.org/article/872009e4694f4b2ab6a3ae616222bc11
Autor:
Jadranka Barešić, Sanja Faivre, Andreja Sironić, Damir Borković, Ivanka Lovrenčić Mikelić, Russel N. Drysdale, Ines Krajcar Bronić
Publikováno v:
Geosciences, Vol 11, Iss 9, p 376 (2021)
Tufa is a fresh-water surface calcium carbonate deposit precipitated at or near ambient temperature, and commonly contains the remains of macro- and microphytes. Many Holocene tufas are found along the Zrmanja River, Dalmatian karst, Croatia. In this
Externí odkaz:
https://doaj.org/article/571591b4c43348fe8de56b2600d3f4c6
Publikováno v:
Geologija, Vol 58, Iss 2, Pp 233-246 (2015)
The stable isotopic composition of oxygen and hydrogen (δ18O and δ2H) and the tritium activity (A) were monitored in precipitation at synoptic station Portorož (Slovenia) during the period 2007–2010. Monthly and yearly isotope variations are d
Externí odkaz:
https://doaj.org/article/ddedb1a3d75e47d49bf7008367692740
Publikováno v:
Geologija, Vol 57, Iss 2, Pp 217-230 (2014)
The stable isotopic composition of hydrogen and oxygen (δ2H and δ18O) and the tritium activity (A) were monitored in monthly collected precipitation at Ljubljana (Reaktor) during the period 2007–2010. Monthly and yearly isotope variations are d
Externí odkaz:
https://doaj.org/article/2f372a2cd2b14e1c96d13becd39cc353
Concentration and stable carbon isotopic composition of CO2 in cave air of Postojnska jama, Slovenia
Publikováno v:
International Journal of Speleology, Vol 42, Iss 3, Pp 279-287 (2013)
Partial pressure of CO2 (pCO2) and its isotopic composition (δ13CairCO2) were measured in Postojnska jama, Slovenia, at 10 locations inside the cave and outside the cave during a one-year period. At all interior locations the pCO2 was higher and δ1
Externí odkaz:
https://doaj.org/article/13c1db4a0c774255ac0cc0664f5f9f24