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Quick Methods for Determining Plant Available Water. Gaylon S. Campbell, Ph. D. Decagon Devices, Inc. Pullman, WA www.decagon.com. Volume Fractions: a “Typical” Soil at Field Capacity. Field capacity or Drained upper limit. Air 24%. Plant Available Water 13%.
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Quick Methods for Determining Plant Available Water Gaylon S. Campbell, Ph. D. Decagon Devices, Inc. Pullman, WA www.decagon.com
Volume Fractions: a “Typical” Soil at Field Capacity Field capacity or Drained upper limit Air 24% Plant Available Water 13% Unavailable Water 13% Permanent wilt point or lower limit Solid 50%
Our Task Demonstrate a quick method for determining plant available water by • Showing how to find the -1.5 MPa water content of a soil sample • Showing how to find the -33 kPa water content of a soil
WP4 Dew Point Potentiameter Range is 0 to -300 MPa Accuracy is 0.1 MPa Read time is 5 minutes or less Water Potential Measurement in the Dry Range (for PWP)
Chilled Mirror Dew Point • Cool mirror until dew forms • Detect dew optically • Measure mirror temperature • Measure sample temperature with IR thermometer • Water potential is approximately linearly related to Ts - Td Fan Optical Sensor Mirror Infrared Sensor Sample
Equilibrates water under tension with soil water through a porous cup Measures pressure of water Highest accuracy, but limited range (0 to -70 kPa) Water Potential Measurement in the Wet Range (for FC)
Steps for Quick -1.5 MPa Water Content • Air dry, crush and sieve the soil sample • Determine the soil texture • Find the approximate -1.5 MPa and air dry water content for that texture • Calculate the amount of water to add
Steps Continued • Add water, mix and equilibrate • Measure water potential and water content • Compute -1.5 MPa water content • Convert to volumetric water content
How Much Water to Add Silt loam soil: w-1.5 = 0.098 g/g wad= 0.033 g/g 50 g. sample Add 3.15 ml. of water to 50 g of air dry soil
Reading the Water Potential Insert sample Seal chamber Wait 3-5 min. and read the result
Computing the -1.5 MPa Water Content Wm = 0.109 m = -1.01
Convert to Volumetric Water Content • Probes measure volumetric wc • Soil stores in terms of volumetric wc If bulk density were 1.4 g/cm3
Quick Determination of the -33 kPa Water Content • Do it in the field or take field samples after heavy rain or irrigation • Measure water potential with a tensiometer • Measure water content with a probe (volumetric) • Calculate -33 kPa water content
Measuring Water Potential Remove cap from tensiometer Insert the probe and read
Calculating the -33 kPa water content Assume • Sandy loam • Water potential reading is -18 kPa • Water content reading is 0.25 m3 m-3
Conclusions • Upper and lower limits for plant available water are soil specific • They are approximated by the -33 kPa and -1.5 MPa water contents • Quick methods for determining these values are available
Conclusions • The -1.5 MPa water content is found by measuring water content and potential on a sample near -1.5 MPa and extrapolating • The -33 kPa water content is found by measuring water content and potential on a sample near -33 kPa and extrapolating