The Relation of Desert Plants to Soil Moisture And to Evaporation
The Relation of Desert Plants to Soil Moisture And to Evaporation
Burton E Burton Edward Livingston
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That of relative trans- piration is seen to be very similar to the same curve for the AUionia of Experiment VI. The first point is probably a maximum, so that here we have to consider two maxima and one minimum. The first maximum is 0.785 and occurs at ll^'SO" a.m. with a temperature of 79.5"* F. and an evaporation rate of 0.046 gram; the second is 0.609 and occurs at 10 a.m., with the same temperature as Fio. 18.— Carve of relative traiiBpiraUon for plant of BoerhaviOf Aagost 16-17, 1904. 60 T...HE RELATION OF DESERT PLANTS TO the other and an evaporation rate of 0.35 gram. The minimum is 0.054 and occurs at 8 p.m., with a temperature of 75° F. and an evaporation rate of 0.029 gram. It appears here again that temperature rather than intensity of evap- oration is possibly the controlling factor in the regulation of relative transpiration, and that the light intensity is not important. The tem- peratures for the maxima are again about 10 degrees higher than those for the minima. The variation in rate of relative transpiration due to Fig.
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