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Measuring radon by collecting its progeny is an old technique
Title: Measuring radon by collecting its progeny is an
old te
>>> "North, David"
<DNorth@LIFESPAN.ORG> 11/15/02 11:09AM >>>
wrote about a science project for his
daughter involving collecting progeny of radon (we no longer use
"daughters" as it implies discrimination!)
It
would be nice if a student reproduced the basic technique used by
Marie Curie for measuring radioactivity, including the radioactivity
of radon progeny. She used a quadrant electrometer to measure
collected charge from natural radioactivity on a flat plate which was
biased positive or negative and was one side of an open air
capacitor. The other side of the capacitor is electrically isolated
and connected electrically to one side of a quadrant electrometer.
The same side of the electrometer is connected to one electrode on
one side of a piezo electric crystal (probably quartz). A piezo
electric potential can be produced by placing small weights on a pan
attached to the end of the crystal. The position of the mirror
attached to the supporting fiber of the quadrant electroscope to view
any change in potential of the capacitor plate that collects the air
ions produced by the radioactivity on the lower plate. The initial
position of the electroscope is viewed by a small telescope to read
the reflection of a scale some distance from the mirror. That
is, the initial position of the electrometer fiber can be shown with
great sensitivity by viewing the scale with the telescope. As the
collector plate collects air ions, the potential of the plate causes
the electrometer fiber to move. At a suitable elapsed time, weights
are added to the pan to produce a piezo potential that
cancels the potential collected by the air ions. The weight needed to
balance the collected ion charge is a measure of the charge and thus
of the radioactivity.
To
measure radon progeny, a long wire was biased negative to attract
positive recoil atoms which lose electrons after it ejects an alpha
particle. After some period of time the wire is disconnected
from its voltage source an coiled up to fit on the bottom plate of
the "ion chamber". By this means the early workers
found that there was more emanation (radon) near water falls. There
is also more radon over a freshly plowed field. I wonder if the EPA
knows about this.
With
her technique Madame Curie could measure an ion current equivalent to
10 picoamperes (10^-11 A). I have always been
impressed at the cleverness of many of our physics predecessors.
I hope
to place this description with an appropriate diagram on the Virtual
Radiation Museum (VRM) which is under construction at
http://www.medphysics.wisc.edu/~vrm Your help and suggestions are
solicited to have the VRM help educate the public and the radiation
professionals about ionizing radiation. Best wishes,
John Cameron
My personal web site at
http://www.medphysics.wisc.edu/~jrc/ is also under construction.
--
John R. Cameron (jrcamero@wisc.edu)
2678 SW 14th Dr. Gainesville, FL 32608
(352) 371-9865 Fax (352) 371-9866
(winters until about May 15)
PO Box 405, Lone Rock,WI 53556
(for UPS, etc. use: E2571 Porter Rd.)
(608) 583-2160; Fax (608) 583-2269
(summer: until about Oct. 15)