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ABSTRACT
Calcium Carbonate Solonchaks occur in close association with Chernozems and Humic-Gley soils. Profiles have A1-Cca-C horizon sequence and form in calcareous parent materials. Evidence is presented to show that the prominent Cca horizon results form the precipitation of lime out of capillary water rising or moving laterally from a zone of water saturation.
1 Joint contribution of North Dakota Agr. Exp. Sta. and USDA, SCS. The material is taken from a thesis submitted by the senior author in partial fulfillment for the M.S. degree. Presented before Div. V., Soil Science Society of America, Atlanta, Ga., Nov. 21, 1957.
2 Former graduate student, North Dakota Agricultural College, now Assistant in Soil Survey, North Dakota Agr. Exp. Sta.; former Soil Scientist, North Dakota Agr. Exp. Sta. and SCS now Soil Scientist, SCS, USDA, Berkeley, Calif., respectively.
Received for publication May 23, 1958. Accepted for publication September 2, 1958.
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