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HYPROP 2

HYPROP 2

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    • More precise and robust
    • Low time, cost, and effort
    • Easy to handle and flexible
    • Simultaneous measurement of water retention function and hydraulic conductivity
    • High validity of the water retention function, especially in the area close to saturation
    • The hydraulic functions are consistently verified by a large number of measuring values
    • Reliable determination of unsaturated conductivity in the medium water potential range—independent of model assumptions
    • Tensiometers measure beyond typical cavitation point down to -240 kPa
    • Tensiometers are positioned upside down in the soil sample (undisturbed evaporation and no impact on the tensiometer shafts)
    • Reduced tensiometer water loss after reaching the cavitation phase
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