A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers

he rate of snow deposition at various cold regions on the earth is an important quantity for glaciological and climatological studies. Radioactive debris from above-ground tests of nuclear weapons (mainly 1954–1970) and from the Chernobyl accident (1986) have been deposited on glaciers and snowfield...

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Published in:Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
Main Authors: Dunphy, P. P., Dibb, Jack E., Chupp, E. L.
Format: Text
Language:unknown
Published: University of New Hampshire Scholars' Repository 1994
Subjects:
Online Access:https://scholars.unh.edu/earthsci_facpub/25
https://doi.org/10.1016/0168-9002(94)91704-3
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spelling ftuninhampshire:oai:scholars.unh.edu:earthsci_facpub-1024 2023-05-15T13:41:56+02:00 A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers Dunphy, P. P. Dibb, Jack E. Chupp, E. L. 1994-12-30T08:00:00Z text/html https://scholars.unh.edu/earthsci_facpub/25 https://doi.org/10.1016/0168-9002(94)91704-3 unknown University of New Hampshire Scholars' Repository https://scholars.unh.edu/earthsci_facpub/25 http://dx.doi.org/10.1016/0168-9002(94)91704-3 Copyright © 1994 Published by Elsevier B.V. Earth Sciences Scholarship Atmospheric Sciences text 1994 ftuninhampshire https://doi.org/10.1016/0168-9002(94)91704-3 2023-01-30T21:34:09Z he rate of snow deposition at various cold regions on the earth is an important quantity for glaciological and climatological studies. Radioactive debris from above-ground tests of nuclear weapons (mainly 1954–1970) and from the Chernobyl accident (1986) have been deposited on glaciers and snowfields, where they can be used as time and depth markers to determine the subsequent accumulation of snow. We discuss a technique to locate these markers that has been used just recently — in-situ measurement of γ-rays from 137Cs. These γ-rays, which are associated with radioactive fallout, have a distinctive depth profile and serve as markers of the historical nuclear events. The γ-ray measurement involves lowering a scintillation detector down a borehole in the snow or ice and recording the response to the 137Cs γ-rays as a function of depth. The in-situ measurement can be done relatively quickly and can replace sample retrieval, or it can be used to decide which ice or snow samples should be transported for later analysis in the laboratory. The feasibility of in-situ γ-ray measurement has been demonstrated at sites in the French Alps and Greenland. We report on a portable detector system that is being developed for use in Antarctica. It is based, as much as possible, on inexpensive, commercially available detectors and electronics. The advantages and disadvantages of this approach are discussed. The problems involved with making these measurements in a harsh environment and the steps taken to deal with them are also presented. Text Antarc* Antarctica Greenland University of New Hampshire: Scholars Repository Greenland Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment 353 1-3 482 485
institution Open Polar
collection University of New Hampshire: Scholars Repository
op_collection_id ftuninhampshire
language unknown
topic Atmospheric Sciences
spellingShingle Atmospheric Sciences
Dunphy, P. P.
Dibb, Jack E.
Chupp, E. L.
A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
topic_facet Atmospheric Sciences
description he rate of snow deposition at various cold regions on the earth is an important quantity for glaciological and climatological studies. Radioactive debris from above-ground tests of nuclear weapons (mainly 1954–1970) and from the Chernobyl accident (1986) have been deposited on glaciers and snowfields, where they can be used as time and depth markers to determine the subsequent accumulation of snow. We discuss a technique to locate these markers that has been used just recently — in-situ measurement of γ-rays from 137Cs. These γ-rays, which are associated with radioactive fallout, have a distinctive depth profile and serve as markers of the historical nuclear events. The γ-ray measurement involves lowering a scintillation detector down a borehole in the snow or ice and recording the response to the 137Cs γ-rays as a function of depth. The in-situ measurement can be done relatively quickly and can replace sample retrieval, or it can be used to decide which ice or snow samples should be transported for later analysis in the laboratory. The feasibility of in-situ γ-ray measurement has been demonstrated at sites in the French Alps and Greenland. We report on a portable detector system that is being developed for use in Antarctica. It is based, as much as possible, on inexpensive, commercially available detectors and electronics. The advantages and disadvantages of this approach are discussed. The problems involved with making these measurements in a harsh environment and the steps taken to deal with them are also presented.
format Text
author Dunphy, P. P.
Dibb, Jack E.
Chupp, E. L.
author_facet Dunphy, P. P.
Dibb, Jack E.
Chupp, E. L.
author_sort Dunphy, P. P.
title A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
title_short A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
title_full A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
title_fullStr A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
title_full_unstemmed A gamma-ray detector for in-situ measurement of 137Cs radioactivity in snowfields and glaciers
title_sort gamma-ray detector for in-situ measurement of 137cs radioactivity in snowfields and glaciers
publisher University of New Hampshire Scholars' Repository
publishDate 1994
url https://scholars.unh.edu/earthsci_facpub/25
https://doi.org/10.1016/0168-9002(94)91704-3
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Earth Sciences Scholarship
op_relation https://scholars.unh.edu/earthsci_facpub/25
http://dx.doi.org/10.1016/0168-9002(94)91704-3
op_rights Copyright © 1994 Published by Elsevier B.V.
op_doi https://doi.org/10.1016/0168-9002(94)91704-3
container_title Nuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
container_volume 353
container_issue 1-3
container_start_page 482
op_container_end_page 485
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