Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/120
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dc.contributor.authorWilson, DJen_AU
dc.date.accessioned2007-11-22T04:13:03Zen_AU
dc.date.accessioned2010-04-30T04:27:55Z-
dc.date.available2007-11-22T04:13:03Zen_AU
dc.date.available2010-04-30T04:27:55Z-
dc.date.issued1988-03en_AU
dc.identifier.citationWilson, D. J. (1988). Correcting the error in neutron moisture probe measurements caused by a water density gradient. (ANSTO/E674). Lucas Heigts, NSW: Australian Nuclear Science and Technology Organisation.-
dc.identifier.govdoc80-
dc.identifier.isbn0642598843en_AU
dc.identifier.issn10307745en_AU
dc.identifier.otherANSTO-E-674en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/120en_AU
dc.description.abstractIf a neutron probe lies in or near a water density gradient the probe may register a water density different to that at the measuring point. The effect of a thin stratum of soil containing an excess or depletion of water at various distances from a probe in an otherwise homogeneous system has been calculated producing an 'importance' curve. The effect of these strata can be integrated over the soil region in close proximity to the probe resulting in the net effect of the presence of a water density gradient. In practice the probe is scanned through the point of interest and the count rate at that point is corrected for the influence of the water density on each side of it. An example shows that the technique can reduce an error of 10 per cent to about 2 per cent.en_AU
dc.language.isoen_auen_AU
dc.publisherAustralian Nuclear Science and Technology Organisationen_AU
dc.subjectCorrections-
dc.subjectNeutron probes-
dc.subjectMeasuring methods-
dc.subjectMoisture gages-
dc.titleCorrecting the error in neutron moisture probe measurements caused by a water density gradienten_AU
Appears in Collections:Scientific and Technical Reports

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