Observation



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meteorological elements
to develop this method.


27
2.8.22 Mesurement of soil moisture potential
2.8.221 The tensiometer method
Tensiometers are used for direct mesurements of soil-moisture
suction in the range of 0 to 100 KPa. The instrument consists
of a porous oup filled with water and buried in the soil. The
movement of the water to the soil creates a negative pressure
or suction, the equilibrium value of which can be measured by
a vacuum gauge. This vacuum gauge can either be a directly
read manometer (e.g. Bourdon or mercury type) or ab bstrain-gauge based pressure transducer used together with an
electrical indicator or recording device. When the matric
suction approaches the value of the atmospheric pressure, air
enters the porous cups and useful readings can no longer be
made. Therefore, tensiometers maybe useful in irrigation

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