Evaluating The Effectiveness of Radon Measurement Techniques in Soil Gas: Impact of Hole Depth and Measurement Time
Main Article Content
Abstract
Radon measurement methodologies are critical for accurate risk assessment and resource optimization, yet challenges persist in determining the optimal sampling depth and measurement duration. These factors significantly influence radon concentration readings, and their impact still needs to be explored in systematic evaluations, particularly in balancing efficiency and accuracy. This study evaluates the effectiveness of radon measurement methodologies by experimenting with how sampling hole depth and measurement duration affect radon concentration in soil gas. Radon experiments were conducted at depths of 0.5 m, 1.0 m, and 1.2 m over a 39-day period in soft tuff rock formations at Institut Teknologi Sumatera. Measurements were taken on Days 0, 6, 12, 18, 27, and 39 using the RAD7 Radon Detector, with multiple cycles to ensure stability. The results indicate that radon concentrations varied significantly with both depth and time, with the highest concentrations observed at 1.2 m on Day 18 (1,089 Bq/m³). A noticeable “lag effect” was observed following rainfall events, where radon levels initially decreased due to soil saturation but spiked as the soil dried. The depth of 0.5 m provided the most consistent measurements, with the lowest coefficient of variation (CV = 31%), making it the most reliable and practical depth for routine radon assessments. Overall, this study highlights the importance of considering environmental conditions, such as rainfall and soil moisture, when interpreting radon data and provides insights into optimizing radon measurement practices for accuracy and efficiency.
Article Details

This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
1. Introduction
By using or sharing content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir ("the Journal"), you agree to follow these Terms and Conditions. The Journal's content is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike (CC BY-NC-SA) license. If you do not agree to these terms, please do not use the content.
2. How You Can Use the Content
-
Share: You can copy, share, and distribute the work, but only for non-commercial purposes.
-
Adapt: You can change, remix, or build on the work, as long as it is for non-commercial purposes and you share it under the same license (CC BY-NC-SA).
3. Attribution (Giving Credit)
When you use or share the content, you must:
-
Give proper credit to the author(s).
-
Mention the title of the work and the journal name.
-
Provide a link to the license (https://creativecommons.org/licenses/by-nc-sa/4.0/).
-
Indicate if you made any changes to the work.
4. Non-Commercial Use
You cannot use the work to make money or for any commercial activities. For example, you cannot sell or use the content in advertisements.
If you want to use the content for commercial purposes, you need to get permission from the author(s) or the publisher.
5. ShareAlike
If you make changes to the content (like creating a new version or remixing it), you must share your new version under the same CC BY-NC-SA license.
6. Exclusions
Some materials in the Journal may have different licenses or restrictions, such as third-party content (like images or datasets). You must respect the rules for those materials.
7. No Warranty
The content is provided "as is." The authors and publisher do not guarantee that the content is error-free or suitable for any specific purpose. Use the content at your own risk.
8. Modifications and Withdrawal of Content
The publisher and authors can update or remove content at any time. If content is removed, the previous versions will still follow these terms.
9. Ethical Use
You must use the content ethically and follow all relevant laws. This includes properly citing the original authors and not misusing the content.
10. Legal Compliance
You are responsible for making sure your use of the content follows the laws of your country. If you believe content violates your rights, please contact us.
11. Changes to Terms
These Terms and Conditions may be updated from time to time. Any changes will be posted on the Journal's website.
12. Contact Information
For questions about these Terms or for permission to use content commercially, please contact us at:
-
Email: eksplorium@brin.go.id
-
Website: https://ejournal.brin.go.id/eksplorium
Conclusion
By using the content from EKSPLORIUM - Buletin Pusat Pengembangan Bahan Galian Nuklir, you agree to follow these Terms and Conditions and the CC BY-NC-SA 4.0 International License.
References
[1] M. Baskaran, Radon: A Tracer for Geological, Geophysical and Geochemical Studies. Springer, 2016.
[2] WHO, WHO Handbook on Indoor Radon: A Public Health Perspective. in WHO Guidelines Approved by the Guidelines Review Committee. Geneva: World Health Organization, 2009. Accessed: Oct. 18, 2024. [Online]. Available: https://www.ncbi.nlm.nih.gov/books/NBK143216/.
[3] M. N. Heriawan, A. A. Syafi’i, A. Saepuloh, T. Kubo, and K. Koike, “Detection of Near-Surface Permeable Zones Based on Spatial Correlation Between Radon Gas Concentration and DTM-Derived Lineament Density,” Nat Resour Res, vol. 30, no. 4, pp. 2989–3015, Aug. 2021, doi: 10.1007/s11053-020-09718-z.
[4] K. Koike, T. Yoshinaga, and H. Asaue, “Characterizing Long-term Radon Concentration Changes in A Geothermal Area for Correlation with Volcanic Earthquakes and Reservoir Temperatures: A Case Study from Mt. Aso, Southwestern Japan,” Journal of Volcanology and Geothermal Research, vol. 275, pp. 85–102, Apr. 2014, doi: 10.1016/j.jvolgeores.2014.02.007.
[5] S. Sukanya, J. Noble, and S. Joseph, “Application of Radon (222Rn) as An Environmental Tracer in Hydrogeological and Geological Investigations: An Overview,” Chemosphere, vol. 303, p. 135141, Sep. 2022,
doi: 10.1016/j.chemosphere.2022.135141.
[6] R. Prasetio, N. Laksminingpuri, S. Satrio, E. R. Pujiindiyati, B. Pratikno, and P. Sidauruk, “The 222Rn and CO2 Soil Gas Distribution at Lembang Fault Zone, West Java - Indonesia,” Journal of Environmental Radioactivity, vol. 257, p. 107079, Feb. 2023, doi: 10.1016/j.jenvrad.2022.107079.
[7] R. Prasetio, J. Hutabarat, Y. Daud, and H. Hendarmawan, “Distribution of 222Rn and CO2 Across Faults and Its Origin in Wayang Windu Geothermal Area, West Java - Indonesia,” Geothermics, vol. 110, p. 102691, May 2023, doi: 10.1016/j.geothermics.2023.102691.
[8] I. A. E. Agency, “Measurement and Calculation of Radon Releases from NORM Residues,” International Atomic Energy Agency, Text, 2013. Accessed: Oct. 18, 2024. [Online]. Available: https://www.iaea.org/publications/10369/measurement-and-calculation-of-radon-releases-from-norm-residues.
[9] W. W. Nazaroff, Radon and Its Decay Products in Indoor Air, United States: John Wiley and Sons, Incorporated, 1988. [Online]. Available: http://inis.iaea.org/search/search.aspx?orig_q=RN:21058186.
[10] N. M. Hassan, M. Hosoda, T. Ishikawa, A. Sorimachi, S. K. Sahoo, S. Tokonami, and M. Fukushi “Radon Migration Process and Its Influence Factors; Review,” Japanese Journal of Health Physics, vol. 44, no. 2, pp. 218–231, 2009, doi: 10.5453/jhps.44.218.
[11] J. C. Miles, “Temporal Variation of Radon Levels in Houses and Implications for Radon Measurement Strategies,” Radiat Prot Dosimetry, vol. 93, no. 4, pp. 369–376, 2001, doi: 10.1093/oxfordjournals.rpd.a006449.
[12] S. D. Schery, D. H. Gaeddert, and M. H. Wilkening, “Factors Affecting Exhalation of Radon from A Gravelly Sandy Loam,” Journal of Geophysical Research: Atmospheres, vol. 89, no. D5, pp. 7299–7309, 1984, doi: 10.1029/JD089iD05p07299.
[13] S. A. Mangga, Amirudin, T. Suwarti, S. Gafoer, and Sidarto, Geological Map of The Tanjungkarang Quadrangle, Sumatera, Scale 1:250000, Geological Research and Development Centre, Bandung, 1993.
[14] M. Iqbal, B. R. Juliarka, W. Ashuri, and B. A. Farishi, “Hydrogeochemistry of Natar and Cisarua Hot Springs in South Lampung, Indonesia,” Journal of Geoscience, Engineering, Environment, and Technology, vol. 4, no. 3, pp. 178–185, Sep. 2019, doi: 10.25299/jgeet.2019.4.3.2959.