Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods
The results of a laboratory testing program, carried out to compare two independent methods for determining the unfrozen water content of soils, are described. With the time domain reflectometry method, the unfrozen water content is inferred from a calibration curve of apparent dielectric constant v...
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ftdtic:ADA203082 2023-05-15T16:37:54+02:00 Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods Smith, Michael W. Tice, Allen R. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1988-10 text/html http://www.dtic.mil/docs/citations/ADA203082 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA203082 en eng http://www.dtic.mil/docs/citations/ADA203082 Approved for public release; distribution is unlimited. DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost *SOIL TESTS *MOISTURE CONTENT *SOILS LABORATORY TESTS NUCLEAR MAGNETIC RESONANCE WATER COMPARISON TEST METHODS ESTIMATES DIELECTRIC PROPERTIES FREEZING CONSTANTS ERRORS PRECISION CALIBRATION ABSORPTION EQUATIONS RANGE(EXTREMES) REFLECTOMETERS TEXTURE TIME DOMAIN VOLUME CURVED PROFILES PROBES TEMPERATURE TIME DOMAIN REFLECTOMETRY DIELECTRIC CONSTANT FROZEN SOILS PE62730A WU002 Text 1988 ftdtic 2016-02-23T06:15:48Z The results of a laboratory testing program, carried out to compare two independent methods for determining the unfrozen water content of soils, are described. With the time domain reflectometry method, the unfrozen water content is inferred from a calibration curve of apparent dielectric constant vs volumetric water content, determined by experiment. Previously, precise calibration of the TDR technique was hindered by the lack of a reference comparison method, which nuclear magnetic resonance now offers. This has provided a much greater scope for calibration, including a wide range of soil types and temperature (unfrozen water content). The results of the testing program yielded a relationship between dielectric constant and volumetric unfrozen water content that is largely unaffected by soil type, although a subtle but apparent dependency on the texture of the soil was noted. It is suggested that this effect originates from the lower valued dielectric constant for absorbed soil water. In spite of this, the general equation presented may be considered adequate for most practical purposes. The standard error of estimate is 0.015 cc/cc, although this may be reduced by calibrating for individual soils. Brief guidelines on system and probe design are offered to help ensure that use of the TDR method will give results consistent with the relationship presented. Keywords: Dielectric constant; Frozen soils; Soils tests; Time domain reflectometry. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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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 *SOIL TESTS *MOISTURE CONTENT *SOILS LABORATORY TESTS NUCLEAR MAGNETIC RESONANCE WATER COMPARISON TEST METHODS ESTIMATES DIELECTRIC PROPERTIES FREEZING CONSTANTS ERRORS PRECISION CALIBRATION ABSORPTION EQUATIONS RANGE(EXTREMES) REFLECTOMETERS TEXTURE TIME DOMAIN VOLUME CURVED PROFILES PROBES TEMPERATURE TIME DOMAIN REFLECTOMETRY DIELECTRIC CONSTANT FROZEN SOILS PE62730A WU002 |
spellingShingle |
Soil Mechanics Snow Ice and Permafrost *SOIL TESTS *MOISTURE CONTENT *SOILS LABORATORY TESTS NUCLEAR MAGNETIC RESONANCE WATER COMPARISON TEST METHODS ESTIMATES DIELECTRIC PROPERTIES FREEZING CONSTANTS ERRORS PRECISION CALIBRATION ABSORPTION EQUATIONS RANGE(EXTREMES) REFLECTOMETERS TEXTURE TIME DOMAIN VOLUME CURVED PROFILES PROBES TEMPERATURE TIME DOMAIN REFLECTOMETRY DIELECTRIC CONSTANT FROZEN SOILS PE62730A WU002 Smith, Michael W. Tice, Allen R. Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
topic_facet |
Soil Mechanics Snow Ice and Permafrost *SOIL TESTS *MOISTURE CONTENT *SOILS LABORATORY TESTS NUCLEAR MAGNETIC RESONANCE WATER COMPARISON TEST METHODS ESTIMATES DIELECTRIC PROPERTIES FREEZING CONSTANTS ERRORS PRECISION CALIBRATION ABSORPTION EQUATIONS RANGE(EXTREMES) REFLECTOMETERS TEXTURE TIME DOMAIN VOLUME CURVED PROFILES PROBES TEMPERATURE TIME DOMAIN REFLECTOMETRY DIELECTRIC CONSTANT FROZEN SOILS PE62730A WU002 |
description |
The results of a laboratory testing program, carried out to compare two independent methods for determining the unfrozen water content of soils, are described. With the time domain reflectometry method, the unfrozen water content is inferred from a calibration curve of apparent dielectric constant vs volumetric water content, determined by experiment. Previously, precise calibration of the TDR technique was hindered by the lack of a reference comparison method, which nuclear magnetic resonance now offers. This has provided a much greater scope for calibration, including a wide range of soil types and temperature (unfrozen water content). The results of the testing program yielded a relationship between dielectric constant and volumetric unfrozen water content that is largely unaffected by soil type, although a subtle but apparent dependency on the texture of the soil was noted. It is suggested that this effect originates from the lower valued dielectric constant for absorbed soil water. In spite of this, the general equation presented may be considered adequate for most practical purposes. The standard error of estimate is 0.015 cc/cc, although this may be reduced by calibrating for individual soils. Brief guidelines on system and probe design are offered to help ensure that use of the TDR method will give results consistent with the relationship presented. Keywords: Dielectric constant; Frozen soils; Soils tests; Time domain reflectometry. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Smith, Michael W. Tice, Allen R. |
author_facet |
Smith, Michael W. Tice, Allen R. |
author_sort |
Smith, Michael W. |
title |
Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
title_short |
Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
title_full |
Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
title_fullStr |
Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
title_full_unstemmed |
Measurement of the Unfrozen Water Content of Soils. Comparison of NMR (Nuclear Magnetic Resonance) and TDR (Time Domain Reflectometry) Methods |
title_sort |
measurement of the unfrozen water content of soils. comparison of nmr (nuclear magnetic resonance) and tdr (time domain reflectometry) methods |
publishDate |
1988 |
url |
http://www.dtic.mil/docs/citations/ADA203082 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA203082 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA203082 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766028195197353984 |