1962Agronomy JournalRequires access

Availability of Soil Water to Plants as Affected by Soil Moisture Content and Meteorological Conditions1

O. T. Denmead, R. H. Shaw

Open publisher page 582 citations

Abstract

Synopsis Actual transpiration decreased with decreasing soil moisture content and increasing potential transpiration. Average soil suction in the root zone when the actual transpiration rate fell below the potential rate varied from 12 bars when the potential transpiration rate was 1.4 mm. per day to 0.3 bar when the potential rate was 6 to 7 mm. per day.

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Synopsis Actual transpiration decreased with decreasing soil moisture content and increasing potential transpiration. Average soil suction in the root zone when the actual transpiration rate fell below the potential rate varied from 12 bars when the potential transpiration rate was 1.4 mm. per day to 0.3 bar when the potential rate was 6 to 7 mm. per day.

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Available abstract

Synopsis Actual transpiration decreased with decreasing soil moisture content and increasing potential transpiration. Average soil suction in the root zone when the actual transpiration rate fell below the potential rate varied from 12 bars when the potential transpiration rate was 1.4 mm. per day to 0.3 bar when the potential rate was 6 to 7 mm. per day.

Key concepts: Transpiration, Water content, Environmental science, Agronomy, Soil water, DNS root zone, Soil science, Biology

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Availability of Soil Water to Plants as Affected by Soil Moisture Content and Meteorological Conditions1 — Research Paper | ScholarLens