A simple method to evaluate daily positive soil heat flux.

M. A. Hares; J. Ben-Asher; A. D. Matthias; A. W. Warrick

doi:10.2136/sssaj1985.03615995004900010008x

A simple method to evaluate daily positive soil heat flux.

M. A. Hares, J. Ben-Asher, A. D. Matthias, A. W. Warrick

Department of Life Sciences

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8 Scopus citations

Abstract

Daily positive heat flow into soil is an important component in the energy balance of a soil surface. If surface soil heat flux is assumed to vary diurnally as a sinusoidal function of time, with frequency, the daily positive soil heat flux density can be estimated. This method of estimation requires the measurement of surface soil temperature at about sunrise and at about mid-day to determine Delta T_o.-from Authors

Original language	English
Pages (from-to)	45-47
Number of pages	3
Journal	Soil Science Society of America Journal
Volume	49
Issue number	1
DOIs	https://doi.org/10.2136/sssaj1985.03615995004900010008x
State	Published - 1 Jan 1985

ASJC Scopus subject areas

Soil Science

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10.2136/sssaj1985.03615995004900010008x

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title = "A simple method to evaluate daily positive soil heat flux.",

abstract = "Daily positive heat flow into soil is an important component in the energy balance of a soil surface. If surface soil heat flux is assumed to vary diurnally as a sinusoidal function of time, with frequency, the daily positive soil heat flux density can be estimated. This method of estimation requires the measurement of surface soil temperature at about sunrise and at about mid-day to determine Delta To.-from Authors",

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AU - Matthias, A. D.

AU - Warrick, A. W.

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Y1 - 1985/1/1

N2 - Daily positive heat flow into soil is an important component in the energy balance of a soil surface. If surface soil heat flux is assumed to vary diurnally as a sinusoidal function of time, with frequency, the daily positive soil heat flux density can be estimated. This method of estimation requires the measurement of surface soil temperature at about sunrise and at about mid-day to determine Delta To.-from Authors

AB - Daily positive heat flow into soil is an important component in the energy balance of a soil surface. If surface soil heat flux is assumed to vary diurnally as a sinusoidal function of time, with frequency, the daily positive soil heat flux density can be estimated. This method of estimation requires the measurement of surface soil temperature at about sunrise and at about mid-day to determine Delta To.-from Authors

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A simple method to evaluate daily positive soil heat flux.

Abstract

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