The B horizon has hue of 7.5YR or 10YR, value of 3 to 6, and chroma of 2 to 6. It is sand, fine sand, loamy fine sand, or loamy sand. Reaction ranges from moderately acid to neutral. The C horizon has hue of 7.5YR or 10YR, value of 3 to 7, and chroma of 2 to 6. It is stratified layers of sand, fine sand, loamy fine sand, coarse sand, or gravelly coarse sand.
Reaction ranges from moderately acid to neutral.
The Acquango, Biltmore, Caesar, Chute, Dabney, Hodge, Pahuk , Penwood, Pinegrove, Plainfield, Sardak, Sarpy, Spessard, Suncook, Tyner, Wesport and Windsor soils lack redoximorphic features at depths of 40 to 60 inches and saturation for 1 month or less per year in 6 or more out of 10 years. The Aldo, Oakville and Osolo soils are saturated for more than 1 month per year and lack an irregular decrease in organic carbon and lack stratification in the lower part of the series control section. Boplain series has a paralithic contact at depths less than 40 inches. Perks soils have free carbonates in the lower part of the series control section. Scotah soils occupy level or gently undulating high flats and natural levees on flood plains.