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Pressure chamber and air flow porometer for rapid field indication of water status and stomatal condition in wheat

By: Contributor(s): Material type: ArticleArticleLanguage: English Publication details: Cambridge (United Kingdom) : Cambridge University Press, 1977.ISSN:
  • 1469-4441 (Online)
  • 0014-4797
Subject(s): Online resources: In: Experimental Agriculture v. 13, no. 4, p. 341-351602726, 611411Summary: Plant water potential and leaf diffusive conductance, key features of plant responses to water stress in field experiments, can be estimated, respectively, by xylem pressure potential measured with the pressure chamber apparatus, and leaf permeability measured with the air flow porometer. This paper describes modifications to these two techniques in order to increase the rapidity of measurements in wheat to 60/h with the pressure chamber, and 200/h with the porometer. Rapid measurements are needed because of the large within-and between-plot errors encountered with daytime measurements in typical field experiments, examples of which are presented.
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Item type Current library Collection Call number Copy number Status Date due Barcode Item holds
Article CIMMYT Knowledge Center: John Woolston Library CIMMYT Staff Publications Collection CIS-427 (Browse shelf(Opens below)) 1 Available 602726
Article CIMMYT Knowledge Center: John Woolston Library CIMMYT Staff Publications Collection CIS-427 (Browse shelf(Opens below)) 2 Available 611411
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Peer review

Graphs, references p. 351

Peer-review: Yes - Open Access: Yes|http://science.thomsonreuters.com/cgi-bin/jrnlst/jlresults.cgi?PC=MASTER&ISSN=0014-4797

Plant water potential and leaf diffusive conductance, key features of plant responses to water stress in field experiments, can be estimated, respectively, by xylem pressure potential measured with the pressure chamber apparatus, and leaf permeability measured with the air flow porometer. This paper describes modifications to these two techniques in order to increase the rapidity of measurements in wheat to 60/h with the pressure chamber, and 200/h with the porometer. Rapid measurements are needed because of the large within-and between-plot errors encountered with daytime measurements in typical field experiments, examples of which are presented.

Text in English

CMP|MIC 7165-R|3

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