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Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions

Note 71 — Chapter XI · THE WATER OF SOILS.

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The partial saturation to a definite extent was effected by means of solutions of calcium chlorid of different degrees of concentration, according to the determinations of Wüllner (Pogg. Ann.). These solutions were placed in a wide, flat dish, over which a layer of soil 1 mm. in thickness was exposed, all being covered with a bell glass lined inside with the same solution, so as to insure equal saturation.

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