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An apparatus for the measurement of the rates of emanation of radon from rock specimens and powders

 

作者: R. H. McCorkell,   M. P. Brameld,  

 

期刊: Review of Scientific Instruments  (AIP Available online 1980)
卷期: Volume 51, issue 4  

页码: 459-463

 

ISSN:0034-6748

 

年代: 1980

 

DOI:10.1063/1.1136245

 

出版商: AIP

 

数据来源: AIP

 

摘要:

Specimens are placed in sealed chambers to which scintillation cells are attached and radon concentrations,R, are measured in the air of the chambers at intervals thereafter by inserting the cells into scintillation counters. The Rn emanation rate is calculated from the rate at whichRincreases, or from the maximumRreached. Uncertainties are estimated to be 10%–25%, detection limits 10−19Ci cm−2s−1or 5×10−19Ci g−1s−1. Effects of disequlibrium in the Rn decay chain, or the diffusion rate of Rn, and of Rn leakage are considered. Powdering a rock usually has little effect on its emanation rate per gram.

 

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