Carnegie Institution of Washington Publication No. 50
Carnegie Institution of Washington Publication No. 50
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In order to eliminate the effects of variations in the humidity of the air and of such slight air currents as might occur in the room, the rates of water loss have been calculated in terms of the evaporimeter rate for the same period. These rates are presented in the form of curves in figure 7 (p. 31), the actual quantities given being the quotients of the rate per hour of evaporation from the soil divided by the corresponding rate per hour of the evapori- meter. These ratios are plotted, as in... other cases, at the middle of the time periods which they represent.
An inspection of these curves shows a curious initial behavior of the 10 per cent soiL Its rate at the start was exceedingly high, but it fell to a position below the other soils within the first three hours.
This is probably due to the fact that in this soil there was not enough water present to even approximately fill the spaces, so that the actual evaporating surface was very large, extending down into the soil for some distance.
What to read after Carnegie Institution of Washington Publication No. 50?
You can find similar books in the "Read Also" column, or choose other free books by Carnegie Institution of Washington to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
In order to eliminate the effects of variations in the humidity of the air and of such slight air currents as might occur in the room, the rates of water loss have been calculated in terms of the evaporimeter rate for the same period. These rates are presented in the form of curves in figure 7 (p. 31), the actual quantities given being the quotients of the rate per hour of evaporation from the soil divided by the corresponding rate per hour of the evapori- meter. These ratios are plotted, as in... other cases, at the middle of the time periods which they represent.
An inspection of these curves shows a curious initial behavior of the 10 per cent soiL Its rate at the start was exceedingly high, but it fell to a position below the other soils within the first three hours.
This is probably due to the fact that in this soil there was not enough water present to even approximately fill the spaces, so that the actual evaporating surface was very large, extending down into the soil for some distance.
What to read after Carnegie Institution of Washington Publication No. 50?
You can find similar books in the "Read Also" column, or choose other free books by Carnegie Institution of Washington to read onlineMoreLess
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