Temperature and evaporation characteristics of Arizona soils

Nineteen representative Arizona soils plus no. 20 silica sand were studied during May, 1983, to determine the relationship between soil temperature change and evaporation and individual soil characteristics. The soils were placed in 50 x 50 x 28 cm wooden boxes with each soil series occupying two bo...

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Main Author: Poland, John Robert.
Other Authors: Post, Donald F.
Language:en
Published: The University of Arizona. 1984
Online Access:http://hdl.handle.net/10150/191810
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-1918102015-10-23T04:37:46Z Temperature and evaporation characteristics of Arizona soils Poland, John Robert. Post, Donald F. Matthias, Allan D. Tucker, T. C. Nineteen representative Arizona soils plus no. 20 silica sand were studied during May, 1983, to determine the relationship between soil temperature change and evaporation and individual soil characteristics. The soils were placed in 50 x 50 x 28 cm wooden boxes with each soil series occupying two boxes, one which had been wetted with two pore volumes of water and one which was dry. Surface soil temperatures (measured with a hand-held infrared thermometer) were taken six times a day for all soils. The wetted soils were weighed at the beginning and end of a 36 hour run to determine gravimetrically the amount of water lost due to evaporation. Thermal and evaporation measurements were compared to a number of soil characteristics determined on both a volume and weight basis. 1984 Thesis-Reproduction (electronic) text http://hdl.handle.net/10150/191810 213296154 en Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. The University of Arizona.
collection NDLTD
language en
sources NDLTD
description Nineteen representative Arizona soils plus no. 20 silica sand were studied during May, 1983, to determine the relationship between soil temperature change and evaporation and individual soil characteristics. The soils were placed in 50 x 50 x 28 cm wooden boxes with each soil series occupying two boxes, one which had been wetted with two pore volumes of water and one which was dry. Surface soil temperatures (measured with a hand-held infrared thermometer) were taken six times a day for all soils. The wetted soils were weighed at the beginning and end of a 36 hour run to determine gravimetrically the amount of water lost due to evaporation. Thermal and evaporation measurements were compared to a number of soil characteristics determined on both a volume and weight basis.
author2 Post, Donald F.
author_facet Post, Donald F.
Poland, John Robert.
author Poland, John Robert.
spellingShingle Poland, John Robert.
Temperature and evaporation characteristics of Arizona soils
author_sort Poland, John Robert.
title Temperature and evaporation characteristics of Arizona soils
title_short Temperature and evaporation characteristics of Arizona soils
title_full Temperature and evaporation characteristics of Arizona soils
title_fullStr Temperature and evaporation characteristics of Arizona soils
title_full_unstemmed Temperature and evaporation characteristics of Arizona soils
title_sort temperature and evaporation characteristics of arizona soils
publisher The University of Arizona.
publishDate 1984
url http://hdl.handle.net/10150/191810
work_keys_str_mv AT polandjohnrobert temperatureandevaporationcharacteristicsofarizonasoils
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