RESEARCH METHODS IN STUDY OF FOREST ENVIRONMENT. 99 
The conditions under which the hygroscopic coefficient should be 
determined, as most recently worked out by Alway, Kline, and 
McDole (103), are briefly as follows: 
1. The absorption box is of wood, 12 by 9 by 8 inches, the interior 
surfaces being paraffined to prevent absorption of water and warp- 
ing. Larger boxes were found to be more difficult to keep saturated, 
2. In the bottom of this box is placed a snug-fitting galvanized-iron 
tray, 3 to 4 inches high, to hold the water. The walls of the box are 
then lined with blotting paper, the edges of which project into the 
vessel of water. This insures rapid dissemination of vapor through 
the interior. 
3. A wooden table is held by metal supports, 1 to 2 inches above the 
surface of the water in the tray. On this table are placed the two 
trays which hold the soil samples. 
4. Metal trays are accepted as most satisfactory, because they ab- 
sorb no moisture and hence do not retard absorption by the soil. 
These trays are of aluminum or copper, 7 inches long, 5 inches wide, 
and 0.75 inch deep. 
5. The soil is carefully sifted over the bottom of the tray to a depth 
of 1 millimeter. This naturally precludes the use of coarser material. 
It was found that there was little Or no change in soils from careful 
grinding which would barely permit the coarser particles to pass a 
1-millimeter sieve. . It was also found that oven drying at 105° to 
110° C. did not appreciably affect the absorbing capacity of any of 
the soils tested. In any case, however, previous drying should be 
avoided when possible. 
6. The exposure to vapor in the boxes is for 24 hours. At the end 
of this period the soil tray is removed from the box as quickly as 
possible and emptied into a stoppered weighing bottle, since exposure 
to the air beyond a few seconds would cause appreciable loss of mois- 
ture. 
7. Undoubtedly the most important consideration in securing re- 
liable results is a suitable room. This must be, in most cases, a cellar 
room not subject to daily fluctuations of temperature or heating from 
one side, or even to localized heating from bright light. These pre- 
cautions are absolutely vital, if condensation is to be prevented. As 
a matter of theory, it is altogether probable that the need is to pre- 
vent even momentary complete saturation of the vapor in proximity 
to the soils, since this might give rise to the creation of liquid moisture 
in them, and entirely alter their condition. 
8. A temperature of about 60° F. may be considered a standard. 
At a lower temperature there will be fewer water molecules reaching 
the soil, and, necessarily, a slower rate of absorption. 
Under these circumstances fairly constant results may be expected 
in hygroscopic coefficient determinations. In the absence of any other 
