Leaf surface wetness and evaporation studies with a β-ray gauge

Surface wetness duration was measured by a β-ray gauge as a function of wind velocity in the laboratory. The instrument was field-tested as a dewmeter over a wax bean canopy. Diurnal variations of the net count rate through a turgid tobacco leaf measured by a β-ray gauge system corresponded with the stomatal movement. The approximate exponential relationship of the transmission of β-particles with absorber thickness was found acceptable to study rates of evaporation from free water and through pores. The cumulative rate of evaporation of free water varied linearly with time. Three distinct stages of evaporation rates were observed through a porous medium. (author)