Seed-Time And Harvest;
Seed-Time And Harvest;
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In other words, the actual loss of the evaporimeter is taken to be equivalent to the loss from a water sur- face of one square decimeter.
On the instrument above described readings were taken at conven- ient intervals from July 24 to August 16. Unfortunately the instru- ment was not installed until after the beginning of the rainy season, so that a rate of evaporation approaching the maximum for the year was probably not observed. Since reliable records of evaporation are exceedingly rare, and ...especially on account of the fact that the pres- ent observations were made at a station whose atmospheric phenomena are especially interesting to botanists, a table of the daily increments of water loss for the above-named period is worthy of its space here.
Table V presents the daily evaporation and also the rainfall from July 25 to August 22. In the first column are given the dates; in the second, the actual losses of the evaporimeter in cubic centimeters; in the third, centimeters of evaporation, being the loss from a single square centimeter of free water surface, derived from the evapori- meter losses by means of the coefficient 100 above d^ved; and in the Digitized by Google SOIL MOISTURE AND TO EVAPORATIOK.
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You can find similar books in the "Read Also" column, or choose other free books by Arthur Timothy Shay to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
In other words, the actual loss of the evaporimeter is taken to be equivalent to the loss from a water sur- face of one square decimeter.
On the instrument above described readings were taken at conven- ient intervals from July 24 to August 16. Unfortunately the instru- ment was not installed until after the beginning of the rainy season, so that a rate of evaporation approaching the maximum for the year was probably not observed. Since reliable records of evaporation are exceedingly rare, and ...especially on account of the fact that the pres- ent observations were made at a station whose atmospheric phenomena are especially interesting to botanists, a table of the daily increments of water loss for the above-named period is worthy of its space here.
Table V presents the daily evaporation and also the rainfall from July 25 to August 22. In the first column are given the dates; in the second, the actual losses of the evaporimeter in cubic centimeters; in the third, centimeters of evaporation, being the loss from a single square centimeter of free water surface, derived from the evapori- meter losses by means of the coefficient 100 above d^ved; and in the Digitized by Google SOIL MOISTURE AND TO EVAPORATIOK.
What to read after Seed-Time And Harvest;?
You can find similar books in the "Read Also" column, or choose other free books by Arthur Timothy Shay to read onlineMoreLess
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