Conductive Backfill for Improving Electrical Grounding in Frozen Soils.

This report is an extension of the authors' earlier resistance-to-ground experiments. Here they supply additional information on the influence of salt-treated backfills around grounding electrodes for reducing resistance to ground. The results are based on observations made over several seasons...

Full description

Bibliographic Details
Main Authors: Sellmann,P V, Delaney,A J, Arcone,S A
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1984
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA144861
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA144861
id ftdtic:ADA144861
record_format openpolar
spelling ftdtic:ADA144861 2023-05-15T15:07:07+02:00 Conductive Backfill for Improving Electrical Grounding in Frozen Soils. Sellmann,P V Delaney,A J Arcone,S A COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1984-06 text/html http://www.dtic.mil/docs/citations/ADA144861 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA144861 en eng http://www.dtic.mil/docs/citations/ADA144861 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *ELECTRICAL GROUNDING ALASKA SOILS SALTS PERMAFROST BACKFILLS PE62730A WU001 Text 1984 ftdtic 2016-02-20T23:08:30Z This report is an extension of the authors' earlier resistance-to-ground experiments. Here they supply additional information on the influence of salt-treated backfills around grounding electrodes for reducing resistance to ground. The results are based on observations made over several seasons of freezing and thawing at sites selected for their variations in grain size, ice content, and ground temperature. More than 20 test electrodes were monitored at two silt sites and one alluvial site. The diameter of the backfilled zones, the salt content, and the backfill material were varied for the electrode installations. In all cases salt backfilling reduced the resistance to ground, with 175 ohms being the lowest value obtained. Reductions varied from very small to an order of magnitude. Resistance also decreased over several seasons. Generally the greatest improvement and lowest values were obtained in the perennially frozen silt in interior Alaska. Data from colder silt suggest that salt backfilling will not be effective in arctic settings. Measurements at a partially thawed, coarse-grained site indicate that salt was moving much more rapidly (approximately give times as fast) away from the treated backfill than at the silt site in the CRREL permafrost tunnel. (Author) Text Arctic Ice permafrost Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
*ELECTRICAL GROUNDING
ALASKA
SOILS
SALTS
PERMAFROST
BACKFILLS
PE62730A
WU001
spellingShingle Snow
Ice and Permafrost
*ELECTRICAL GROUNDING
ALASKA
SOILS
SALTS
PERMAFROST
BACKFILLS
PE62730A
WU001
Sellmann,P V
Delaney,A J
Arcone,S A
Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
topic_facet Snow
Ice and Permafrost
*ELECTRICAL GROUNDING
ALASKA
SOILS
SALTS
PERMAFROST
BACKFILLS
PE62730A
WU001
description This report is an extension of the authors' earlier resistance-to-ground experiments. Here they supply additional information on the influence of salt-treated backfills around grounding electrodes for reducing resistance to ground. The results are based on observations made over several seasons of freezing and thawing at sites selected for their variations in grain size, ice content, and ground temperature. More than 20 test electrodes were monitored at two silt sites and one alluvial site. The diameter of the backfilled zones, the salt content, and the backfill material were varied for the electrode installations. In all cases salt backfilling reduced the resistance to ground, with 175 ohms being the lowest value obtained. Reductions varied from very small to an order of magnitude. Resistance also decreased over several seasons. Generally the greatest improvement and lowest values were obtained in the perennially frozen silt in interior Alaska. Data from colder silt suggest that salt backfilling will not be effective in arctic settings. Measurements at a partially thawed, coarse-grained site indicate that salt was moving much more rapidly (approximately give times as fast) away from the treated backfill than at the silt site in the CRREL permafrost tunnel. (Author)
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
format Text
author Sellmann,P V
Delaney,A J
Arcone,S A
author_facet Sellmann,P V
Delaney,A J
Arcone,S A
author_sort Sellmann,P V
title Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
title_short Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
title_full Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
title_fullStr Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
title_full_unstemmed Conductive Backfill for Improving Electrical Grounding in Frozen Soils.
title_sort conductive backfill for improving electrical grounding in frozen soils.
publishDate 1984
url http://www.dtic.mil/docs/citations/ADA144861
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA144861
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Alaska
genre_facet Arctic
Ice
permafrost
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA144861
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766338676315389952