2008
DOI: 10.1016/j.jenvrad.2007.08.022
|View full text |Cite
|
Sign up to set email alerts
|

Determination of specific activity of 226Ra, 232Th and 40K for assessment of radiation hazards from Turkish pumice samples

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
30
0
4

Year Published

2008
2008
2018
2018

Publication Types

Select...
7
2
1

Relationship

0
10

Authors

Journals

citations
Cited by 68 publications
(34 citation statements)
references
References 21 publications
(18 reference statements)
0
30
0
4
Order By: Relevance
“…The same geometry and size are used for both measured and reference material samples. The measurements are collected for 20 to 24 hours [5]. …”
Section: Radioactivity Measurementsmentioning
confidence: 99%
“…The same geometry and size are used for both measured and reference material samples. The measurements are collected for 20 to 24 hours [5]. …”
Section: Radioactivity Measurementsmentioning
confidence: 99%
“…15 It is a solidified frothy lava typically created when superheated, highly pressurized rock is violently ejected from a volcano. The pumice block is a highly porous material, when the pores in pumice are filled with air, it can be buoyant in water.…”
Section: Introductionmentioning
confidence: 99%
“…This radium equivalent activity is a weighted sum of activities of the above named radionuclides. The estimation of Ra eq is based on the assumptions that 10 Bq kg -1 of 226 Ra, 7 Bq kg -1 of 232 Th and 130 Bq kg -1 of 40 K produce the same gamma dose rate (Turhan and Gunduz, 2007). The Ra eq is defined as: The mean values of the radium equivalent activity and the associated uncertainties calculated (using Eq.…”
Section: Resultsmentioning
confidence: 99%