EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS.
A 3-year program of laboratory testing led to some correlations between the mineralogical composition and the frost susceptibility of soils. Freezing tests were performed on about 400 artificially blended specimens with various amounts and different kinds of mineral fines mixed with a clean sand, a...
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ftdtic:AD0697134 2023-05-15T16:37:28+02:00 EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. Lambe,T. W. Kaplar,C. W. Lambie,T. J. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1969-09 text/html http://www.dtic.mil/docs/citations/AD0697134 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697134 en eng http://www.dtic.mil/docs/citations/AD0697134 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost (*SOILS FROST HEAVE) (*SOIL MECHANICS COLD WEATHER TESTS) FREEZING MINERALS PARTICLE SIZE CLAY SAND SILT TEST METHODS CORRELATION TECHNIQUES IONS FROST SUSCEPTIBILITY Text 1969 ftdtic 2016-02-18T22:37:47Z A 3-year program of laboratory testing led to some correlations between the mineralogical composition and the frost susceptibility of soils. Freezing tests were performed on about 400 artificially blended specimens with various amounts and different kinds of mineral fines mixed with a clean sand, a silt, a lean clay and a heavy clay. The tests demonstrate the frost heave effects of various fines. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
institution |
Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Soil Mechanics Snow Ice and Permafrost (*SOILS FROST HEAVE) (*SOIL MECHANICS COLD WEATHER TESTS) FREEZING MINERALS PARTICLE SIZE CLAY SAND SILT TEST METHODS CORRELATION TECHNIQUES IONS FROST SUSCEPTIBILITY |
spellingShingle |
Soil Mechanics Snow Ice and Permafrost (*SOILS FROST HEAVE) (*SOIL MECHANICS COLD WEATHER TESTS) FREEZING MINERALS PARTICLE SIZE CLAY SAND SILT TEST METHODS CORRELATION TECHNIQUES IONS FROST SUSCEPTIBILITY Lambe,T. W. Kaplar,C. W. Lambie,T. J. EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
topic_facet |
Soil Mechanics Snow Ice and Permafrost (*SOILS FROST HEAVE) (*SOIL MECHANICS COLD WEATHER TESTS) FREEZING MINERALS PARTICLE SIZE CLAY SAND SILT TEST METHODS CORRELATION TECHNIQUES IONS FROST SUSCEPTIBILITY |
description |
A 3-year program of laboratory testing led to some correlations between the mineralogical composition and the frost susceptibility of soils. Freezing tests were performed on about 400 artificially blended specimens with various amounts and different kinds of mineral fines mixed with a clean sand, a silt, a lean clay and a heavy clay. The tests demonstrate the frost heave effects of various fines. (Author) |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Lambe,T. W. Kaplar,C. W. Lambie,T. J. |
author_facet |
Lambe,T. W. Kaplar,C. W. Lambie,T. J. |
author_sort |
Lambe,T. W. |
title |
EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
title_short |
EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
title_full |
EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
title_fullStr |
EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
title_full_unstemmed |
EFFECT OF MINERALOGICAL COMPOSITION OF FINES ON FROST SUSCEPTIBILITY OF SOILS. |
title_sort |
effect of mineralogical composition of fines on frost susceptibility of soils. |
publishDate |
1969 |
url |
http://www.dtic.mil/docs/citations/AD0697134 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697134 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0697134 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027769864519680 |