Kk. Nielson et Vc. Rogers, A SENSITIVE EFFLUENT METHOD FOR MEASURING RADON GAS EMANATION FROM LOW-EMANATING MATERIALS, Nuclear instruments & methods in physics research. Section A, Accelerators, spectrometers, detectors and associated equipment, 353(1-3), 1994, pp. 519-523
The fraction of radon (Rn-222) gas emanated from soils and building ma
terials is critical in estimating radiation source strengths for human
dosimetry. A sensitive method has been developed to measure emanation
fractions (E) from sample radon effluents. The method equilibrates sa
mples with their emanated radon in sealed cans for 24-30 days. Samples
are then assayed for radium (Ra-226) by high-efficiency gamma scintil
lation spectrometry that eliminates thorium (Th-232) interferences. Ra
don in the can head space is then measured, and E is calculated as the
ratio of emanated radon activity to sample radium activity. Values of
E measured by the effluent method were compared with corresponding me
asurements by the differential gamma assay method. Precisions evaluate
d on 259 Florida soil samples indicated 1000-s detection limits for em
anating radium of Ra(.)E = 0.02 pCi g(-1) by the effluent method and R
a(.)E = 0.5 pCi g(-1) by the differential gamma method. The effluent m
ethod has superior precision by a factor of eight for background soils
containing Ra(.)E = 0.25 pCi g(-1). The effluent method averaged abou
t 8% lower than the differential gamma method on 21 comparison samples
. Twenty were within a +/-20% data accuracy objective.