ABSTRACT
Soil survey
and land evaluation for selected crops in Ibiono Ibom Local Government Area of
Akwa Ibom State (LGA), Nigeria were carried out. The objectives were to survey,
characterize, classify and evaluate the suitability of the soils for the
cultivation of four arable crops (cassava, maize, plantain/banana, wetland
rice) and three permanent crops (cocoa, oil palm and rubber). Topographic map
of the study area at the scale of 1:50,000 was acquired from the office of the
Surveyor General of Akwa Ibom State. A digital elevation model (DEM)
of the study area was also acquired from United State Geological Survey (USGS)
at 30m resolution. Elevation map was
generated from both the topographic map and digital elevation model and
superimposed on each other to generate the final base map of the study. The
base map was made up of three mapping units based on elevation gradient of 0-50
masl (soil mapping unit 1), 51-100 masl (soil mapping unit 2) and 101 masl and
above (soil mapping unit 3). with the help of Hand held Global
Positioning System (GPS), the
latitudes, longitudes and elevation on
the base map were cross-checked in the field (ground truthing). Profile pits
were sunk in representative locations within each soil mapping unit. A total of nine profile pits were sunk with
three in each mapping unit. Each pit was described in accordance with FAO
guidelines for soil profile description. Soil samples were collected based on
genetic horizons for laboratory analysis. Undisturbed bulk soil samples were
also collected using core ring for bulk density and saturated hydraulic
conductivity determinations. The results showed that soil mapping unit 1 is located
in the poorly drained, nearly level to level topography with elevation gradient
of 0 – 50 masl. Soil texture was sand in the Ap-horizon and
sandy clay loam in the B-horizon. Soil pH was moderately acid in both Ap and
B-horizon. Organic carbon was high in
the Ap -horizon and moderate in the B-horizon. Total N was low in both Ap and B
-horizon. Available P was moderate in both Ap and B -horizon. Exchangeable Ca
was moderate in the Ap- horizon and low in the B -horizon. Exchangeable Mg was
moderate in both Ap and B-horizon. Exchangeable K was very high in the Ap-
horizon and high in the B-horizon. The ECEC was moderate in the Ap- horizon and
low in the B-horizon. Soil mapping unit 2 is located partly within the
imperfectly drained and partly within somewhat well-drained with gently sloping
topography. The elevation varied from 51 to 100 masl. Soil texture was sand in the Ap-horizon and sandy clay loam in the
B-horizon. Soil pH was moderately acid in the Ap-horizon and strongly acid in
the B-horizon. Organic carbon was high
in the Ap -horizon and moderate in the B-horizon. Total N was moderately low in
both Ap and B -horizon. Available P was moderate in the Ap-horizon and low in
the B -horizon. Exchangeable Ca was low in the Ap- horizon and moderate in the
B -horizon. Exchangeable Mg was moderate in both Ap and B-horizon. Exchangeable
K was very low in both the Ap and B- horizon. Effective Cation Exchange Capacity (ECEC) was
low in both the Ap and the B- horizon. Soil mapping Unit 3 is located
within the well-drained, gently sloping topography. The elevation varied from
101 masl and above. Soil texture was
sand in the Ap-horizon and sandy clay loam in the B-horizon. Soil pH was
strongly acid in both Ap and B-horizon. Organic carbon was moderate in the Ap
-horizon and low in the B-horizon. Total N was low in both Ap and B -horizon.
Available P was moderate in both Ap and B -horizon. Exchangeable Ca was low in
both the Ap and B -horizon. Exchangeable Mg was moderate in both Ap and
B-horizon. Exchangeable K was very high in
the Ap- horizon and low in the B-horizon. The Effective Cation Exchange
Capacity (ECEC) was moderate in the Ap-
horizon and low in the B-horizon. Soil mapping unit 1 was classified as
Typic Epiaquept or Gleyic Cambisol. In
soil mapping unit 2, the imperfectly drained area was classified as Aeric Epiaquept
or Gleyic Cambisol. Soil mapping unit 3
was classified as Typic Hapludult or Haplic Acrisol. The results of land
suitability evaluation showed that, soil mapping unit 1 (Ibom 1) .was
marginally suitable (S3) for maize cultivation, moderately suitable (S2) for
wetland rice, marginally suitable (S3) for cassava, marginally suitable (S3)
for plantain/banana cultivation, not suitable (N1) for cocoa cultivation, not
suitable (N1) for rubber cultivation but marginally suitable (S3) for oil palm
cultivation,
Soil mapping unit 2 was moderately suitable (S2) for maize cultivation, marginally
suitable (S3) for wetland rice, marginally suitable (S3) for cassava
cultivation, marginally suitable (S3) for plantain/banana cultivation, not
suitable (N1) for cocoa cultivation, not suitable (N1) for rubber cultivation
but marginally suitable (S3) for oil palm cultivation. Soil mapping
unit 3, was.
Highly suitable (S1) for maize cultivation, not suitable (N1) for wetland rice,
moderately suitable (S2) for cassava cultivation, marginally suitable (S3) for
plantain/banana cultivation., not suitable (N1) for cocoa cultivation and
marginally suitable (S3) for rubber and oil palm cultivations. Major limitations
for all the crops in the three mapping units were fertility, soil physical
characteristics and wetness. Climatic variables were optimum or suboptimal for
most of the crops under consideration in all the mapping units.