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Land susceptibility to soil erosion in Orashi Catchment, Nnewi South, Anambra State, Nigeria
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Abstract. Soil erosion is one of the most critical environmental hazards that causes
land degradation and water quality challenges. Specifically, this phenomenon
has been linked, among other problems, to river sedimentation, groundwater
pollution and flooding. This paper assesses the susceptibility of Orashi
River Basin (ORB) to soil erosion for the purpose of erosion control
measures. Located in the South Eastern part of Nigeria, the ORB which covers
approximately 413.61 km2 is currently experiencing one of the
fastest population growth rate in the region. Analysis of the soil erosion
susceptibility of the basin was based on four factors including; rainfall,
Land use/Land cover change (LULC), slope and soil erodibility factor (k).
The rainfall was assumed to be a constant and independent variable, slope and
soil types were categorised into ten (10) classes each while the landuse was
categorised into five classes. Weight was assigned to the classes based on
the degree of susceptibility to erosion. An overlay of the four variables in
a GIS environment was used to produce the basin susceptibility to soil
erosion. This was based on the weight index of each factors. The LULC
analysis revealed that built-up land use increased from 26.49 km2
(6.4 %) in year 1980 to 79.24 km2 (19.16 %) in 2015 at an
average growth rate of 1.51 km2 per annum while the light forest
decreased from 336.41 km2 (81.33 %) in 1980 to
280.82 km2 (67.89 %) in 2015 at an average rate
1.59 km2 per annum. The light forest was adjudged to have the
highest land cover soil erosion susceptibility. The steepest slope ranges
between 70 and 82∘ (14.34 % of the total land area) and was
adjudged to have the highest soil susceptibility to erosion. The total area
covered of the loamy soil is 112.37 km2 (27.07 %) with
erodibility of 0.7. In all, the overlay of all the variables revealed that
106.66 km2 (25.70 %) and 164.80 km2 (39.7 %) of the
basin has a high and very high susceptibility to soil erosion. The over
50 % high susceptibility of catchment has serious negative implications
on the surface water in terms of water quality and downstream siltation with
great consequences on biodiversity and ecosystem services including domestic
and industrial usage.
Title: Land susceptibility to soil erosion in Orashi Catchment, Nnewi South, Anambra State, Nigeria
Description:
Abstract.
Soil erosion is one of the most critical environmental hazards that causes
land degradation and water quality challenges.
Specifically, this phenomenon
has been linked, among other problems, to river sedimentation, groundwater
pollution and flooding.
This paper assesses the susceptibility of Orashi
River Basin (ORB) to soil erosion for the purpose of erosion control
measures.
Located in the South Eastern part of Nigeria, the ORB which covers
approximately 413.
61 km2 is currently experiencing one of the
fastest population growth rate in the region.
Analysis of the soil erosion
susceptibility of the basin was based on four factors including; rainfall,
Land use/Land cover change (LULC), slope and soil erodibility factor (k).
The rainfall was assumed to be a constant and independent variable, slope and
soil types were categorised into ten (10) classes each while the landuse was
categorised into five classes.
Weight was assigned to the classes based on
the degree of susceptibility to erosion.
An overlay of the four variables in
a GIS environment was used to produce the basin susceptibility to soil
erosion.
This was based on the weight index of each factors.
The LULC
analysis revealed that built-up land use increased from 26.
49 km2
(6.
4 %) in year 1980 to 79.
24 km2 (19.
16 %) in 2015 at an
average growth rate of 1.
51 km2 per annum while the light forest
decreased from 336.
41 km2 (81.
33 %) in 1980 to
280.
82 km2 (67.
89 %) in 2015 at an average rate
1.
59 km2 per annum.
The light forest was adjudged to have the
highest land cover soil erosion susceptibility.
The steepest slope ranges
between 70 and 82∘ (14.
34 % of the total land area) and was
adjudged to have the highest soil susceptibility to erosion.
The total area
covered of the loamy soil is 112.
37 km2 (27.
07 %) with
erodibility of 0.
7.
In all, the overlay of all the variables revealed that
106.
66 km2 (25.
70 %) and 164.
80 km2 (39.
7 %) of the
basin has a high and very high susceptibility to soil erosion.
The over
50 % high susceptibility of catchment has serious negative implications
on the surface water in terms of water quality and downstream siltation with
great consequences on biodiversity and ecosystem services including domestic
and industrial usage.
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