1989
DOI: 10.1007/bf01121081
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14C emission from RBMK-1500 reactors and features determining it

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Cited by 11 publications
(6 citation statements)
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“…During the initial period of reactor operation, pure nitrogen is used instead of the nitrogen-helium mixture. During this period (approximately 18 months), the formation of 14 C is about 10 times higher than during the subsequent normal operation at rated power (Konstantinov 1989). Measurements performed in 1985-1986 of atmospheric 14 C release at the high-altitude pipe gave a value of 1.4 ± 0.3 TBq/GW e ⋅yr (Konstantinov 1989).…”
Section: Ignalina Lithuaniamentioning
confidence: 90%
See 1 more Smart Citation
“…During the initial period of reactor operation, pure nitrogen is used instead of the nitrogen-helium mixture. During this period (approximately 18 months), the formation of 14 C is about 10 times higher than during the subsequent normal operation at rated power (Konstantinov 1989). Measurements performed in 1985-1986 of atmospheric 14 C release at the high-altitude pipe gave a value of 1.4 ± 0.3 TBq/GW e ⋅yr (Konstantinov 1989).…”
Section: Ignalina Lithuaniamentioning
confidence: 90%
“…During this period (approximately 18 months), the formation of 14 C is about 10 times higher than during the subsequent normal operation at rated power (Konstantinov 1989). Measurements performed in 1985-1986 of atmospheric 14 C release at the high-altitude pipe gave a value of 1.4 ± 0.3 TBq/GW e ⋅yr (Konstantinov 1989). Mikhajlov et al (1999) measured the 14 C distribution near the Ignalina NPP, and the highest value found corresponds to a 14 C specific activity of 430 Bq/kg C recorded in 2-yr-old pine cones that were collected at a distance of 5 km east of the location.…”
Section: Ignalina Lithuaniamentioning
confidence: 90%
“…As it was mentioned before, DIC samples in the lake were collected once or twice a year only from 1979 to 2009. In other temperate lakes, it was observed that during the warm period, when there is a high intensity of photosynthesis, the daily 13 C/ 12 C values of DIC as well as DIC concentration itself could be highly variable [28][29][30][31][32]. This means that not only seasonal [33] but also diurnal changes in 14 C specific activity values in DIC are also possible.…”
Section: Model Assumptionsmentioning
confidence: 99%
“…The boiling water reactors (BWRs) and heavy water reactors (HWRs, CANDU type) as well as gas cooled reactors (HTGR, AGR, Magnox) release 14 C mainly as carbon dioxide; whereas discharges from pressurized water reactors (PWRs) are dominated by hydrocarbons such as methane or ethane [1, [3][4][5][6][7][8][9][10]. The discharges from light-water-cooled graphite-moderated reactors (RBMK), which operated at the Ignalina Nuclear Power Plant (INPP), are of carbon dioxide form 14 C [11,12] and are similar to other BWRs. The INPP located in north-eastern Lithuania operated two RBMK-1500 units (design electric power 1500 MW e ).…”
Section: Introductionmentioning
confidence: 99%
“…The boiling water reactors (BWRs) and heavy water reactors (HWRs, CANDU type) as well as gas cooled reactors (HTGR, AGR, Magnox) release 14 C mainly as carbon dioxide 14 CO 2 , whereas discharges from pressurized water reactors (PWRs) are dominated by hydrocarbons such as methane or ethane (Kunz 1985; Veres et al 1995; Stenström et al 2000; Yim and Caron 2006; Mazeika et al 2007). In light-water-cooled, graphite-moderated reactors (RBMK) 14 C is released mainly in the form of 14 CO 2 (Gaiko et al 1985; Konstantinov et al 1989) as typical for the BWRs. Gaiko et al (1985) reported that ~90% of the total 14 C was produced in the graphite moderator of the RBMK reactor, however, is not expected to be available for release during normal operation of the reactor.…”
Section: Introductionmentioning
confidence: 99%