Abstract
IN recent years it has become a practice to deduce the radioactivity of the air (that is, its radon content) from the sampling and measurement of the short-lived radon daughter products. This method dates from the beginning of the present century1. The unique difference between the early measurements and the recent ones consists in the method of sampling the active deposit of radon; while nowadays deposition on filter paper is almost exclusively used, in the early experiments the transmutation products of radon were collected on the electrode by a strong electric field.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
