Laboratory study of NO flux from agricultural soil: Effects of soil moisture, pH, and temperature

Unique laboratory test chambers with attendant procedures are described, and the results of a comprehensive test protocol are discussed in terms of the mechanical, chemical and biological factors contributing to NO flux from agricultural soil to the lower levels of the troposphere. Soil moisture con...

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Veröffentlicht in:Journal of Geophysical Research 1999-01, Vol.104 (D1), p.1621-1629
Hauptverfasser: Ormeci, Banu, Sanin, Selim L., Peirce, J. Jeffrey
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container_issue D1
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container_title Journal of Geophysical Research
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creator Ormeci, Banu
Sanin, Selim L.
Peirce, J. Jeffrey
description Unique laboratory test chambers with attendant procedures are described, and the results of a comprehensive test protocol are discussed in terms of the mechanical, chemical and biological factors contributing to NO flux from agricultural soil to the lower levels of the troposphere. Soil moisture content, pH, and temperature are investigated to determine the effects of these important variables on NO flux. The flux is seen to increase with temperature and is greatest at pH 8 for the ranges studied. Further, NO flux is seen to decrease as soil moisture content is 45% water filled pore space. Mechanical, chemical, and biological factors in the soil which contribute to these observed fluxes are addressed.
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source Wiley Journals; Wiley-Blackwell AGU Digital Library; Wiley Online Library (Open Access Collection); Alma/SFX Local Collection
subjects Chemical composition and interactions. Ionic interactions and processes
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
title Laboratory study of NO flux from agricultural soil: Effects of soil moisture, pH, and temperature
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