PEDOGENESIS OF ANCIENT DUNE SOILS IN THE SOKOTO SEDIMENTARY BASIN, NORTHWESTERN NIGERIA
PEDOGENESIS OF ANCIENT DUNE SOILS IN THE SOKOTO SEDIMENTARY BASIN, NORTHWESTERN NIGERIA
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Date
1995-11
Authors
RAJI, BASHIRU ADEMOLA
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Abstract
The morphological, physical, chemical and mineralogical characteristics of ancient
dune soils of the Sokoto sedimentary basin of northwestern Nigeria were studied with a
view to elucidating their pedogenesis. The phosphorus forms and adsorption characteristics
of the soils were also examined.
The results of the studies show that the dune soils presently are characterized by
a Sudano-Sahelian climate bordering on semi-aridity towards the northern part, that is
around lllela town. The dune soils have similar properties especially in the surface
horizons but expectedly differ mainly in their physical properties since they are mainly
Entisols.
The soils are mainly deep to very deep and have a colour with strong chroma, >
4 throughout their profiles. They are generally sandy except in the Sokoto dunes where
sandy loam textures are encountered. Structurally, the surface horizons exhibit weak
development and are, therefore susceptible to some amount of erosion hazard.
All the soils are characterized by high bulk densities, low total poaisities and high
macroporosities of more than 30 percent. The soils therefore have very low water
retention capacities.
Organic carbon contents are extremely low, being less than 2 g kg-1 in all the
soils. The available phosphorus levels are low to moderate in Sangiwa and Sokoto dunes
and moderate to very high in the lllela dunes.
Soil pH indicates an extremely acid to moderately alkaline soil reaction while the
total exchangeable bases are very low, often less than 1.% cmol(+) kg-1, in all the soils.
Exchange acidity is also low and less than 2.0 cmol(+) kg-1 soil. The soils have very low
CEC, which range from 1.0 to 4.6 cmol(+) kg-1 soil in all the pedons and low to moderate
base saturation reflecting the rather siliceous nature of the parent material.
Electrical conductivity (EC), exchangeable sodium percent (ESP) and free
carbonate values are all very low, with EC values of less than 0.24 dS m-1, ESP of less
than 4 percent and free carbonate contents of less than 10 g CaC03 Kg-1 soil in all the
soils.
The values of DTPA cationic micronutrients, Cu, Zn, Mn and Fe are all well
above the critical limits of 0.2, 0.8, 1.0 and 4.5 µg g-1 respectively. Phosphorus fractions
and adsorption capacities are similar in all the dunes. The soils have a high total-P
content, ranging from 404 to 1881 µg g-1, but the occluded forms account for
proportionately higher percentages than the other forms of P. Adsorb-P followed by Al-P
are the dominant extraclable inorganic-P forms. The soils have very low P sorption
capacities which average about 100 mg kg-1 soil. The P-sorption capacities at standard P
solution concentration of 0.3 mg/1 are low and average about 20 mg kg-1 soil. The soils
also have very low bond energy.
The mineralogy of the soils are similar. Magnetite is the dominant magnetic
mineral while quartz is the dominant non-magnetic mineral in the fine sand fractions. In
the silt fractions, quartz is dominant followed by kaolinite in all the soils. Kaolinite is the
dominant mineral in the clay fraction of all the soils.
Parent material, topo-drainage and paleoclimatology were presumed to have had
the most profound effect on the dune soils. Organic matter mineralization, limited clay
eluviation-illuviation, horizonation, textural and structural differentiation are the main
significant pedogenic processes occurring in the soils but these processes are better
expressed in the Sokoto dunes and in pedon LDS 2 of Illela dunes, thereby producing Bt
horizons.
According to the criteria of the USDA Soil Taxonomy, all the soils on the
Sangiwa and Mela dunes are classified as Ustic Quartzipsamments except pedon LDS 2
on Illela dunes which is classified as Arenic Haplustult. Soils on the Sokoto dunes are
classified as Kanhaplic Haplustults except for pedons SDS 3 and 4 which are classified
as Lithic Haplustult and Ustic Quartzipsamment respectively. In the FAO/UNFSCO soil
map of the world legend, the soils on Sangiwa dunes are placed as Ferralic Arenosols
while those on Sokoto dunes are placed as Haplic Alisols except for pedon SDS 4 which
is placed as Ferralic Arenosol. Pedons LDS 1, 3 and 4 on the Mela dunes are all placed
as Ferralic Arenosols, while pedons LDS 2 is placed as Haplic Acrisols.
Organic matter and related properties, exchangeable cationic bases, especially K.
low water and nutrient holding capacities are the major constraints to productivity in all
the soils. In addition, phosphorus is also a constraint to productivity in the Sangiwa dunes.
Micronutrients are however, adequate for most crops.
Description
Thesis submitted to The Post-Graduate School in partial
fulfillment of the Requirement for the award of the Degree of
Doctor of Philosophy (Pedology).
IN
The Department of Soil Science
Ahmadu Bello University
Zaria, Nigeria
Keywords
PEDOGENESIS,, ANCIENT, DUNE,, SOILS,, SOKOTO,, SEDIMENTARY, BASIN,, NORTHWESTERN, NIGERIA