RESEARCH METHODS IN STUDY OF FOREST ENVIRONMENT. 115 



It should be borne in mind that the ideal temperature conditions 

 were not attained in this test, and, as has been stated, that at no time 

 has complete saturation of the vapor existed, except possibly for 

 short periods during cooling. This ideal has, however, probably been 

 approached more closely than in any previous test, and the long- 

 period employed gives us a new insight into the phenomena of 

 absorption. 



The following comments on Table 5 may assist in an understand- 

 ing of these results. The comparative behavior of various soil com- 

 binations will not be discussed, as these merely substantiate the ob- 

 servations of others. 



1. The amount absorbed b} 7 the unwashed fine sand in 382 days 

 is only one-third more than the absorption in 5 days. It is, however, 

 evident that even at the end of the longer period the unwashed sand 

 was not in an atmosphere of saturated vapor, but rather in one whose 

 pressure was quite as much controlled by the presence of soils still 

 absorbing vapor, and particularly by the sample containing the 

 largest amount of potassium nitrate. Assuming that all the moisture 

 absorbed by the last entered into the salt solution, the latter would 

 be a 22 per cent solution and would stand for an osmotic pressure of 

 more than 45 atmospheres. It is therefore not surprising to find that 

 a soil which contains not over 20 parts per million of soluble mat- 

 ter should make little gain in this atmosphere. 



2. On the other hand, the amount absorbed by the fine sand in 382 

 •lays is just about equal to the wilting coefficient for this sand, as 

 nearly as can be estimated from a test on the original soil, which 

 r-ontained about equal proportions of material finer and coarser than 

 the fine sand. 



3. The continued and relatively large absorption, especially by 

 the soils containing active salts, might be ascribed to the low tem- 

 peratures under which the test was conducted. It is believed, how- 

 ever, that the evidence of a condition slowly approaching saturation 

 vapor pressure, and never quite up to it, is convincing, and that this 

 explains not only the present results but nearly all the phenomena 

 that have been reported in a similar connection. 



A number of other tests somewhat similar to the above were made 

 during 1918, but for short periods only. Several attempts were 

 made to compare the osmotic pressures of soil samples in their 

 natural moisture conditions, by placing the fresh samples under a 

 _<!<■ bell jar without a control solution, to note whether the samples 

 gained or lost moisture in the common atmosphere. While these 

 gains or losses indicated the relative dryness of the several samples. 

 the tests were not continued long enough to produce any results of 



value. K \v:i- found thai period of two or three week-; was ina<la- 



quate to bring about equilibrium between the many samples, whose 



