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- W2324674788 abstract "Measuring the discharge of water from the field of peat bog we obtained a discharge curve along with periodical daily changes in a drainage.In this experiment, it was found that evapo-transpiration from the surface of peat bog was a major cause of periodical daily change.The evapo-transpiration increased gradually with time after the sunrise and decreased with time after the sunset.The minimum discharge due to evapo-transpiration has occurred at 3-4p. m.The water level reached its maximum just after a rain, and then discharge has decreased gradually and exponentially. The daily loss by evapo-transpiration was superposed on the exponential function.Thus these are expressed by the following formulaQ=Ae-λ(t-3)-Be-λ′(t-3){1-sin-π/12(t+3)}Here λ denotes the coefficient of decrease of discharge (-0.0015--0.0016), λ′ the coefficient of decrease of amplitude of evapo-transpiration (-0.0012--0.0013)The quantity of evapo-transpiration for 24hrs. was 15-27% of the daily total discharge. (see Fig. 3(c))And the maximum quantity at 3-4p. m. was 34-70% of the total discharge at that time. (see Fig. 3 (d))" @default.
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- W2324674788 date "1959-01-01" @default.
- W2324674788 modified "2023-10-02" @default.
- W2324674788 title "Studies on the Evapo-transpiration" @default.
- W2324674788 doi "https://doi.org/10.2480/agrmet.15.21" @default.
- W2324674788 hasPublicationYear "1959" @default.
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