The Relation of Desert Plants to Soil Moisture And to Evaporation
The Relation of Desert Plants to Soil Moisture And to Evaporation
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To quickly assess the difficulty of the text, read a short excerpt:
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.
What to read after The Relation of Desert Plants to Soil Moisture And to Evaporation?
You can find similar books in the "Read Also" column, or choose other free books by Burton E Burton Edward Livingston to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
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.
What to read after The Relation of Desert Plants to Soil Moisture And to Evaporation?
You can find similar books in the "Read Also" column, or choose other free books by Burton E Burton Edward Livingston to read onlineMoreLess
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