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Soil columns were used to study the movement of 45Ca by leaching them with salt solutions of various concentrations and ionic combinations. The results showed that the distribution patterns of radio‐calcium within the soil columns varied with the anionic species as well as with the type of cations of the salt solutions. Exchange and movement of radio‐calcium was higher with sulfate than with chloride salt solutions. The difference is explained on the basis of the differential displacement of calcium from the exchange sites caused by the salts present in soil solution. The data obtained may have significance in understanding the development of solonetzic soils.

Clay separated from a Solonetz Bnt horizon was fractionated lnto coarse (2–0.2 µ), medium (0.2–0.14 µ), fine (0.14–0.08 µ) and very fine (<0.08 µ) size fractions. Organic matter from these fractions was obtained by extractions with 0.1M Na4P2O7(pH 11.0), followed by extractions with 0.1N NaOH. The residue was then repeatedly treated with an HF‐HCl mixture and the remaining organic fraction was extracted with 0.1M Na4P2O7(pH 11.0). The organic and clay fractions were analyzed for C and N contents, and by X‐ray diffraction, electron microscopy and infrared spectroscopy. Experimental data indicated that the largest portion of the complexed organic matter was associated with the coarse clay fraction which contained relatively large amounts of kaolinite, whereas a small percentage was associated with the fine clay fraction where kaolinite occurred as traces. The percentage of extractable organic matter increased with decrease in clay particle size. No evidence was found for the adsorption of organic matter in the interlamellar spaces as reported by some previous workers. Study of humic acids isolated from the clay fractions showed that aliphatic structures were more common in humic acids derived from fine clay than in those separated from the coarse clay fraction. Aromatic structures of the humic acids increased in the order of pyrophosphate humic acid→alkali humic acid→residual humic acid. The humic acids unextractable by the solvents commonly employed appeared to be highly humified and aromatic in nature.

The boiling point and density of the phosphines have been correlated by using the quantity M?2. The use of such data permits the classification of these compounds into associated and normal liquids. These conclusions are also supported by the study of the heat of evaporation of the phosphines.