2011
DOI: 10.1016/j.geoderma.2011.01.017
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Mineralogical and physico-chemical properties of Ferralic Arenosols derived from unconsolidated Plio-Pleistocenic deposits in the coastal plains of Congo

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Cited by 50 publications
(26 citation statements)
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“…The soil is a deep Ferralic Arenosol, overlaying geological bedrock of thick detritic layers (continental origin from Plio-Pleistocene). Soil fertility is low, with a low CEC (< 0.5 cmol+ kg −1 ), high sand content (> 90 % of mineral soil), very low clay and silt content ( 2 to 6 % according to depth, respectively) and low iron oxides content (< 1.5 % of the bulk soil, Mareschal et al 2011). The climate is subequatorial with a cool dry season extending typically from May to September, with the mean annual rainfall of 1,250 mm and more than 85 % of atmospheric moisture.…”
Section: Methodsmentioning
confidence: 99%
“…The soil is a deep Ferralic Arenosol, overlaying geological bedrock of thick detritic layers (continental origin from Plio-Pleistocene). Soil fertility is low, with a low CEC (< 0.5 cmol+ kg −1 ), high sand content (> 90 % of mineral soil), very low clay and silt content ( 2 to 6 % according to depth, respectively) and low iron oxides content (< 1.5 % of the bulk soil, Mareschal et al 2011). The climate is subequatorial with a cool dry season extending typically from May to September, with the mean annual rainfall of 1,250 mm and more than 85 % of atmospheric moisture.…”
Section: Methodsmentioning
confidence: 99%
“…A reason for this discrepancy could be the larger range of pedoclimatic conditions covered by the studies described above (e.g., region and national scales compared to our woodland scale). Furthermore, the soils addressed in our study have an identical geologic origin (Cosson, 1955;Jamet and Rieffel, 1976;Mareschal et al, 2011), which probably increased the difficulty of observing differences using classical soil analyses.…”
Section: Measured Dominant Height (M)mentioning
confidence: 92%
“…The soils in the area developed from continental sediment depositions dating from the plio-pleistocene (Jamet and Rieffel, 1976;Mareschal et al, 2011) and originated from the erosion of the Mayombe mountains (Cosson, 1955). The soils are thick, ranging from 80 to 300 m, and belong to the Ferralic Arenosol class (FAO, 1998).…”
Section: Study Sitementioning
confidence: 99%
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