Crop Science Grow Your Career with CSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Comstock, J.P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Comstock, J.P.
Agricola
Right arrow Articles by Comstock, J.P.
Crop Science 40:709-712 (2000)
© 2000 Crop Science Society of America

CROP ECOLOGY, MANAGEMENT & QUALITY

Correction of Thermocouple Psychrometer Readings for the Interaction of Temperature and Actual Water Potential

J.P. Comstock

Boyce Thompson Institute for Plant Research, Tower Road, Ithaca, NY 14853 USA

jpc8{at}cornell.edu

The standard method of temperature correction for a thermocouple psychrometer only yields satisfactory results for a limited range of water potential and temperature. Contrary to assumptions in standard practices, there is an interaction between the actual water potential under measurement and the temperature correction. Fortunately, the errors associated with ignoring this interaction are often small, and data are presented here that permit an assessment of whether the error is within acceptable limits under specific experimental conditions. More elaborate algorithms are given that can be used more robustly across a wide range of measurement conditions if needed. The temperature responses of two commonly used commercial psychrometers were examined, and it was found that this interaction resulted in model-specific correction algorithms. More specifically, it was found that the frequently made assumption of a correction factor that changes linearly with temperature is a satisfactory approximation across a range of at least 15 to 35°C. However, it was also found that the slope describing how this correction factor changes with temperature itself changes as a function of the actual water potential being measured. The details and magnitude of this effect were model specific.

Abbreviations: RH, relative humidity • µV, microvolt







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Vadose Zone Journal
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2000 by the Crop Science Society of America.