Soil heat flow investigations in the Chilton Valley

The heat flow meter method of measurement of soil heat flow is shown to be the most suitable of available techniques for the investigation of the spatial variation of soil heat flow within the Chilton Valley. A procedure for the calibration of heat flow meters is developed that permits the minimizat...

Full description

Bibliographic Details
Main Author: Moran, R. J.
Language:en
Published: University of Canterbury. Geography 2012
Online Access:http://hdl.handle.net/10092/7076
id ndltd-canterbury.ac.nz-oai-ir.canterbury.ac.nz-10092-7076
record_format oai_dc
spelling ndltd-canterbury.ac.nz-oai-ir.canterbury.ac.nz-10092-70762015-03-30T15:31:03ZSoil heat flow investigations in the Chilton ValleyMoran, R. J.The heat flow meter method of measurement of soil heat flow is shown to be the most suitable of available techniques for the investigation of the spatial variation of soil heat flow within the Chilton Valley. A procedure for the calibration of heat flow meters is developed that permits the minimization of meter measurement errors due to the distortion of the natural soil heat flow. The most significant measurement errors are shown to be those resulting from inaccurate installation of the meters. It is shown that a major factor in determining the spatial variability of soil heat flow within a defined area in the Chilton Valley is the differential shading of the surface by the taller vegetation, and that the spatial sampling density required for the evaluation of the soil heat flow paramenter is detailed micrometeorological studies is considerably greater than that required for the evaluation of this parameter in general studies dealing with longer-term climatological averages.University of Canterbury. Geography2012-09-25T00:43:20Z2012-09-25T00:43:20Z1971Electronic thesis or dissertationTexthttp://hdl.handle.net/10092/7076enNZCUCopyright R. J. Moranhttp://library.canterbury.ac.nz/thesis/etheses_copyright.shtml
collection NDLTD
language en
sources NDLTD
description The heat flow meter method of measurement of soil heat flow is shown to be the most suitable of available techniques for the investigation of the spatial variation of soil heat flow within the Chilton Valley. A procedure for the calibration of heat flow meters is developed that permits the minimization of meter measurement errors due to the distortion of the natural soil heat flow. The most significant measurement errors are shown to be those resulting from inaccurate installation of the meters. It is shown that a major factor in determining the spatial variability of soil heat flow within a defined area in the Chilton Valley is the differential shading of the surface by the taller vegetation, and that the spatial sampling density required for the evaluation of the soil heat flow paramenter is detailed micrometeorological studies is considerably greater than that required for the evaluation of this parameter in general studies dealing with longer-term climatological averages.
author Moran, R. J.
spellingShingle Moran, R. J.
Soil heat flow investigations in the Chilton Valley
author_facet Moran, R. J.
author_sort Moran, R. J.
title Soil heat flow investigations in the Chilton Valley
title_short Soil heat flow investigations in the Chilton Valley
title_full Soil heat flow investigations in the Chilton Valley
title_fullStr Soil heat flow investigations in the Chilton Valley
title_full_unstemmed Soil heat flow investigations in the Chilton Valley
title_sort soil heat flow investigations in the chilton valley
publisher University of Canterbury. Geography
publishDate 2012
url http://hdl.handle.net/10092/7076
work_keys_str_mv AT moranrj soilheatflowinvestigationsinthechiltonvalley
_version_ 1716799566240546816