pF value

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In soil science , the dimensionless pF value (p of power , F of free energy of the water) characterizes the energy with which the soil water is held against gravity in the soil matrix. The higher the pF value, the drier the soil or the lower its water content .

definition

Conversion table
pF value Soil water
tension in hPa
Soil water
tension in mWS
Soil moisture
0 −1 hPa = −10 0 hPa −0.01 mWS
1 −10 hPa = −10 1 hPa −0.1 mWS wet
2 −100 hPa = −10 2 hPa −1 mWS wet
3 −1,000 hPa = −10 3 hPa −10 mWS fresh
4th −10,000 hPa = −10 4 hPa −100 mWS dry
5 −100,000 hPa = −10 5 hPa −1000 mWS dry

The pF value is defined as the decadic logarithm of the amount of soil water tension in hectopascals (this is also called suction tension or matrix potential  ):

If the soil water tension is not given as pressure in hectopascals, but

it must first be converted into hectopascals to determine the pF value.

Under hydrostatic conditions, the pF value corresponds to the decadic logarithm of the vertical distance to the water table in centimeters.

Application examples

  • In the hydrostatic state, a groundwater level of 60 cm below the soil surface corresponds to a soil water tension at the soil surface of −60 hPa and thus a pF value of 1.8.

See also

literature

  • Karl Heinrich Hartge: Introduction to Soil Physics. E. Schweizerbart'sche Verlagsbuchhandlung oHG, Stuttgart 1978, ISBN 3-432-89681-6 , pp. 132-140.
  • Diedrich Schroeder: Soil science in brief. Hirt Verlag, Unterägeri 1984, ISBN 3-266-00192-3 .

Web links

  • Christine Alewell: Soil Water: Capillarity, Potentials, Darcy, nFK , Chapter 8 in Fundamentals of Soil Science . Institute for Environmental Geosciences, University of Basel (PDF file; 1.69 MB).
  • M. Schöniger, J. Dietrich: Matrix potential and water content . In: HydroSkript - lectures on hydrology and water management.