The daily and seasonal variation of evapotranspiration on the tea field was measured using the chamber method.
The amount of transpiration from tea plant was large on clear days, but it was small on cloudy and rainy days.
Transpiration began at sunrise, but most of it occurred in the middle of the day, and decreased until sunset. And there was very little transpiration at night.
Evaporation from the soil surface also varied with time, amounting from 1/3 to 1/2 of transpiration from tea plant.
There was considerable seasonal variation in the transpiration from tea plant with the largest occurence in mid-summer and the smallest in the winter. The amount of transpiration in a day was 6 or 7 mm in the summer, 2 mm in the winter, and 3 or 4 mm in the spring and autumn.
At the sprouting time, the amount of transpiration from young leaves was relatively little, but that from matured leaves at plucking time was relatively large.
The amount of transpiration from tea plants was related to climatic factors, and it showed the high correlation to solar radiation, air temperature, and air humidity.
It was thought that the seasonal variation of the amount of transpiration was related to the ability of transpiration owing to plant physiological factor.
Eestimating by the evapotranspiration rate, the amount of water consumption on the tea field was 1, 300 mm in a year, and 120 mm during sprouting time to plucking time of each harvesting season.
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