Electrical Properties of Ice.

An experimental and phenomenological study was made of the charge separation at the advancing surface of growing ice (Workman-Reynolds effect). The charge separation is fundamentally ascribed to anions and cations of an electrolyte solute crossing the phase boundary at different rates. The sign of t...

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Bibliographic Details
Main Author: Gross,Gerardo Wolfgang
Other Authors: NEW MEXICO INST OF MINING AND TECHNOLOGY SOCORRO
Format: Text
Language:English
Published: 1970
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0718359
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718359
id ftdtic:AD0718359
record_format openpolar
spelling ftdtic:AD0718359 2023-05-15T16:37:07+02:00 Electrical Properties of Ice. Gross,Gerardo Wolfgang NEW MEXICO INST OF MINING AND TECHNOLOGY SOCORRO 1970-12 text/html http://www.dtic.mil/docs/citations/AD0718359 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718359 en eng http://www.dtic.mil/docs/citations/AD0718359 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Atmospheric Physics Snow Ice and Permafrost (*ICE ELECTRICAL PROPERTIES) (*CLOUDS ICE) FREEZING IMPURITIES HALIDES ALKALI METAL COMPOUNDS ELECTROLYTES AMMONIUM COMPOUNDS FLUORIDES PH FACTOR CARBON DIOXIDE ALKALI HALIDES Text 1970 ftdtic 2016-02-19T00:24:45Z An experimental and phenomenological study was made of the charge separation at the advancing surface of growing ice (Workman-Reynolds effect). The charge separation is fundamentally ascribed to anions and cations of an electrolyte solute crossing the phase boundary at different rates. The sign of the charge on the ice is determined by the preferentially incorporated ion constituent. The magnitude is determined by solute species, solute concentrations, and freezing rate. The process is very sensitive to hydrogen-ion concentration. Solutes widely present in meteoric waters, ammonium, bicarbonate, sodium, and chloride, give rise to large charge separations. Although the present results suggest that water free of impurities will not show appreciable charge separation upon freezing, this question, of paramount importance for an understanding of cloud processes, requires further investigation. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Workman ENVELOPE(-65.683,-65.683,-66.392,-66.392)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Atmospheric Physics
Snow
Ice and Permafrost
(*ICE
ELECTRICAL PROPERTIES)
(*CLOUDS
ICE)
FREEZING
IMPURITIES
HALIDES
ALKALI METAL COMPOUNDS
ELECTROLYTES
AMMONIUM COMPOUNDS
FLUORIDES
PH FACTOR
CARBON DIOXIDE
ALKALI HALIDES
spellingShingle Atmospheric Physics
Snow
Ice and Permafrost
(*ICE
ELECTRICAL PROPERTIES)
(*CLOUDS
ICE)
FREEZING
IMPURITIES
HALIDES
ALKALI METAL COMPOUNDS
ELECTROLYTES
AMMONIUM COMPOUNDS
FLUORIDES
PH FACTOR
CARBON DIOXIDE
ALKALI HALIDES
Gross,Gerardo Wolfgang
Electrical Properties of Ice.
topic_facet Atmospheric Physics
Snow
Ice and Permafrost
(*ICE
ELECTRICAL PROPERTIES)
(*CLOUDS
ICE)
FREEZING
IMPURITIES
HALIDES
ALKALI METAL COMPOUNDS
ELECTROLYTES
AMMONIUM COMPOUNDS
FLUORIDES
PH FACTOR
CARBON DIOXIDE
ALKALI HALIDES
description An experimental and phenomenological study was made of the charge separation at the advancing surface of growing ice (Workman-Reynolds effect). The charge separation is fundamentally ascribed to anions and cations of an electrolyte solute crossing the phase boundary at different rates. The sign of the charge on the ice is determined by the preferentially incorporated ion constituent. The magnitude is determined by solute species, solute concentrations, and freezing rate. The process is very sensitive to hydrogen-ion concentration. Solutes widely present in meteoric waters, ammonium, bicarbonate, sodium, and chloride, give rise to large charge separations. Although the present results suggest that water free of impurities will not show appreciable charge separation upon freezing, this question, of paramount importance for an understanding of cloud processes, requires further investigation. (Author)
author2 NEW MEXICO INST OF MINING AND TECHNOLOGY SOCORRO
format Text
author Gross,Gerardo Wolfgang
author_facet Gross,Gerardo Wolfgang
author_sort Gross,Gerardo Wolfgang
title Electrical Properties of Ice.
title_short Electrical Properties of Ice.
title_full Electrical Properties of Ice.
title_fullStr Electrical Properties of Ice.
title_full_unstemmed Electrical Properties of Ice.
title_sort electrical properties of ice.
publishDate 1970
url http://www.dtic.mil/docs/citations/AD0718359
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718359
long_lat ENVELOPE(-65.683,-65.683,-66.392,-66.392)
geographic Workman
geographic_facet Workman
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0718359
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027419003650048