Reference soil Nigeria 11: Phaeozem
Phaeozems occur all over the world, but especially on the more moist side of the steppe regions, bordering Chernozems.
Characteristics
Soils having a mollic horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation); a base saturation of 50 percent or more between 25 and 100 cm from the soil surface; a calcium carbonate-free soil matrix at least to a depth of 100 cm from the soil surface, or to a contrasting layer between 25 and 100 cm; no diagnostic horizons other than an albic, argic, cambic or vertic horizon, or a petrocalcic horizon in the substratum.
Reference soil NG011: Phaeozems
Brief description of the soil: A deep, poorly drained clayey soil with common cracks, pressure faces and slickensides; faint mottling occurs throughout the soil; horizontation is gradual, structure is moderate to strong developed. Physiographic unit: Seasonally inundated, almost flat to sloping region towards Niger river. Permeability: moderate before Niger was dammed up. Vegetation cover: grasses like Echinochlora pyramidalis, Vossia cuspidata. Flooding: Profile flooded 3 months a year during rainy season June to August/September. Additional notes to profile description: A11: Mottles appear also along rootchannels; cracks 0,5 cm wide. A12, B21, B22: Mottles discontinuous; common pressure faces. B3: Many interseckting slickensides with 60° angle with the horizontal; many pressure faces; few soft whitish accumulations. 2C: Weathered piece of schist, underlain by a fairly homogeneous clay layer. 3C: common white weathered rock (10 Yr 8/1). References: - Siderius, W.; Soil-vegetation relationships in the Borgu Game reserve. Wildlife Technical Report No.8. Kainji Lake Research Project, Jan. 1974. "vertic" (USDA) is a tentative subgroup. Climate data source: Agroclimatological data Africa 1, FAO. Rome 1984.