A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge

An investigation into the behaviour of artificially produced ions, released from a point source a few metres above the Earth’s surface, is presented. It is shown both experimentally and theoretically that the ions form a plume downwind of the ion source and, moreover, that the nature of this plume i...

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Main Author: Jones, C. D.
Published: Durham University 1974
Subjects:
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.461085
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spelling ndltd-bl.uk-oai-ethos.bl.uk-4610852015-03-19T05:34:13ZA study of turbulent diffusion in the lower atmosphere using artificially produced electric space chargeJones, C. D.1974An investigation into the behaviour of artificially produced ions, released from a point source a few metres above the Earth’s surface, is presented. It is shown both experimentally and theoretically that the ions form a plume downwind of the ion source and, moreover, that the nature of this plume is rather similar to that of a smoke plume. Electric field and ion concentration measurements have been used to deduce certain features about ion plumes and distinct connexions between ion plume behaviour and the local meteorological conditions have been observed. In particular, the use of bidirectional vane techniques has indicated that ions can be used quite successfully as a tracer in short range atmospheric diffusion experiments. The technique does however, possess certain limitations, the details of which are included in the text.530.44Durham Universityhttp://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.461085http://etheses.dur.ac.uk/10447/Electronic Thesis or Dissertation
collection NDLTD
sources NDLTD
topic 530.44
spellingShingle 530.44
Jones, C. D.
A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
description An investigation into the behaviour of artificially produced ions, released from a point source a few metres above the Earth’s surface, is presented. It is shown both experimentally and theoretically that the ions form a plume downwind of the ion source and, moreover, that the nature of this plume is rather similar to that of a smoke plume. Electric field and ion concentration measurements have been used to deduce certain features about ion plumes and distinct connexions between ion plume behaviour and the local meteorological conditions have been observed. In particular, the use of bidirectional vane techniques has indicated that ions can be used quite successfully as a tracer in short range atmospheric diffusion experiments. The technique does however, possess certain limitations, the details of which are included in the text.
author Jones, C. D.
author_facet Jones, C. D.
author_sort Jones, C. D.
title A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
title_short A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
title_full A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
title_fullStr A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
title_full_unstemmed A study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
title_sort study of turbulent diffusion in the lower atmosphere using artificially produced electric space charge
publisher Durham University
publishDate 1974
url http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.461085
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