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ABSTRACT
The Sinai series comprises well-drained Chernozem soils developed in calcareous, finely stratified, glaciolacustrine, silty clay loam and silty clay sediments. These soils occupy the nearly level to gently sloping tops of mesa-like hills interlaced with a more or less continuous, moat-like pattern of colluvial-alluvial drains and swales. The profile has some characteristics of youthful grumusols. It consists of a black, granular A1 horizon; dark grayish-brown or olive brown, compound prismatic-subangular blocky B2 horizons; mottled light olive brown, prismatic B3ca horizons; and mottled light olive brown, laminated Cca or Dca horizons. Many vertical, dark-colored tongues of A1 material extend into the B3ca horizons. Laboratory analyses of three profiles sampled in the northern, central, and southern areas of the Prairie Coteau of eastern South Dakota indicate that the northern samples contain greater quantities of organic carbon and total nitrogen than the southern samples. Field studies indicate that the southern soils have browner Ap and B2 horizons, more strongly developed B2 and B2ca horizons, and structural development to greater depths than the central or northern Sinai soils. These morphological and chemical differences are attributed to climatic and vegetative variations during their genesis.
1 Approved for publication by the Director of the South Dakota Agr. Exp. Sta. as Journal Series No. 495. Presented before Div. V, Soil Science Society of America, Nov. 19, 1959, at Cincinnati, Ohio.
2 Formerly Assistant in Agronomy, South Dakota State College, now Graduate Fellow, University of Illinois; and Professor of Agronomy, South Dakota State College, respectively.
Received for publication October 24, 1960. Accepted for publication April 7, 1961.
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