Tensiometers and blocks are in common use to measure soil water suctio
n. The working range of tensiometers is only 0.7 to 0.8 bar. To measur
e higher values of soil water tensions psychrometric methods are appli
cable, but for tensions more than 0.7 to 0.8 bar only block methods ma
y be used. Some sources of errors may restrict the accuracy to measure
soil water tension or soil water content. Under favorable conditions
a range of the measured parameters can be given. At no account the blo
ck. method should be accepted uncritically.