Abstract
In the monitoring of air for /sup 14/C and /sup 3/H the necessary sensitivity cannot be achieved by direct measurement, but only through continuous sampling and scintillation spectroscopy. The two radionuclides are separated from each other at the time of sampling. In addition, by a catalytic reaction over CuO at 600/sup 0/C, a differentiation is achieved between tritiated atmospheric water vapor (HTO), /sup 14/CO/sub 2/ and other isotopically labeled substances contained in the air. Tritium is obtained in the form of water and /sup 14/C as Na/sub 2//sup 14/CO/sub 3/. Radioactivity is measured in a scintillation spectrometer. For tritium this method has a detection limit of 0.8 pCi/m/sup 3/ or air, and for C/sup 14/ 0.6 pCi/m/sup 3/ of air. These values correspond to 15 to 30% of the mean background concentration for HTO and /sup 14/CO/sub 2/ observed up to the present.
Citation Formats
Rudolph, J., and Weiss, W.
Sensitive method for continuous air monitoring for /sup 14/C and /sup 3/H. Empfindliches verfahren zur koninuierlichen C-14 und H-3 luftueberwachung.
Germany: N. p.,
1976.
Web.
Rudolph, J., & Weiss, W.
Sensitive method for continuous air monitoring for /sup 14/C and /sup 3/H. Empfindliches verfahren zur koninuierlichen C-14 und H-3 luftueberwachung.
Germany.
Rudolph, J., and Weiss, W.
1976.
"Sensitive method for continuous air monitoring for /sup 14/C and /sup 3/H. Empfindliches verfahren zur koninuierlichen C-14 und H-3 luftueberwachung."
Germany.
@misc{etde_8181341,
title = {Sensitive method for continuous air monitoring for /sup 14/C and /sup 3/H. Empfindliches verfahren zur koninuierlichen C-14 und H-3 luftueberwachung}
author = {Rudolph, J., and Weiss, W.}
abstractNote = {In the monitoring of air for /sup 14/C and /sup 3/H the necessary sensitivity cannot be achieved by direct measurement, but only through continuous sampling and scintillation spectroscopy. The two radionuclides are separated from each other at the time of sampling. In addition, by a catalytic reaction over CuO at 600/sup 0/C, a differentiation is achieved between tritiated atmospheric water vapor (HTO), /sup 14/CO/sub 2/ and other isotopically labeled substances contained in the air. Tritium is obtained in the form of water and /sup 14/C as Na/sub 2//sup 14/CO/sub 3/. Radioactivity is measured in a scintillation spectrometer. For tritium this method has a detection limit of 0.8 pCi/m/sup 3/ or air, and for C/sup 14/ 0.6 pCi/m/sup 3/ of air. These values correspond to 15 to 30% of the mean background concentration for HTO and /sup 14/CO/sub 2/ observed up to the present.}
place = {Germany}
year = {1976}
month = {Jul}
}
title = {Sensitive method for continuous air monitoring for /sup 14/C and /sup 3/H. Empfindliches verfahren zur koninuierlichen C-14 und H-3 luftueberwachung}
author = {Rudolph, J., and Weiss, W.}
abstractNote = {In the monitoring of air for /sup 14/C and /sup 3/H the necessary sensitivity cannot be achieved by direct measurement, but only through continuous sampling and scintillation spectroscopy. The two radionuclides are separated from each other at the time of sampling. In addition, by a catalytic reaction over CuO at 600/sup 0/C, a differentiation is achieved between tritiated atmospheric water vapor (HTO), /sup 14/CO/sub 2/ and other isotopically labeled substances contained in the air. Tritium is obtained in the form of water and /sup 14/C as Na/sub 2//sup 14/CO/sub 3/. Radioactivity is measured in a scintillation spectrometer. For tritium this method has a detection limit of 0.8 pCi/m/sup 3/ or air, and for C/sup 14/ 0.6 pCi/m/sup 3/ of air. These values correspond to 15 to 30% of the mean background concentration for HTO and /sup 14/CO/sub 2/ observed up to the present.}
place = {Germany}
year = {1976}
month = {Jul}
}