SURVEYING
AND MONITORING OF EROSION SITE
SURVEY
INVOLVEMENT IN EROSION CONTROL
Erosion has
been described as the washing away of the top soil as a result of the actions
of agents such as water and wind. Gully erosion, being the predominant in
Southern Nigeria, is also a type of environmental degradation with a lot of
disastrous consequences caused mainly by flood as a result of high
precipitation, which is fallout of climate change. It can be determined,
especially in terms of extent and scope, monitored and controlled.
Soil erosion is the detachment of
soil particles and it occurs by the action of water, wind and glacial ice as
the case may be. Soil erosion may be gradual process that continues relatively
unnoticed, or it may occur at an alarming rate causing serious loss of top
soil, which in some cases advance further into gullies of unimaginable
magnitude and consequence.
Generally
erosion occurs when raindrops, rainy seasons’ runoff, or floodwaters wear away
and transport soil particles. It is a complex natural process that has often
been accelerated by human activities such as land clearance, agriculture,
construction, surface mining, and urbanization.
Types of Erosion:
There are many types of erosion and mentioned
here are a few of them, which include: Sheet erosion, Rill erosion, Valley or
stream erosion and Gully erosion. Gully erosion, being the main topic of the
discus, results where water flows along a linear depression eroding a trench or
gully.. It is particularly noticeable in the formation of hollow ways where
prior to being tracked, an old rural road has over many years become
significantly lower than the surrounding fields. It usually begins gradually, being initially
insignificant, and graduates into an unimaginable monstrous dimension of
momentous consequences when ignored. In its developmental stage, it might be in
form of a shallow depression following the line of a footpath, but would sooner
grow and expand in both depth and bounds into a gruesome gully.
Causes of
gully erosion:
The likely causative factors of gully erosion
could be either natural or anthropogenic sources Natural factors include:
1. Nature of soil. Some soils have high
erodibilty factors hence susceptible to high rate of erosion while some soils
have very low erodibilty factors and as such low rate of erosion.
2. Topography of terrain. Rugged and steep
terrains with high slope are more likely to experience high gully erosion rate
than flat terrain. This is so because flood, which is an agent of soil erosion
increases in velocity with high slope than on flat terrain thereby acquiring
greater momentum to move displaced soil particles from one place to another.
3. Amount of precipitation results in high
volume of rainfall, which is one of the major factors of gully erosion. The
higher the amount of rainfall, the higher the quantity of soil particles that
are dissolved, displaced and moved away. High precipitation amounts to high
level of flood in most areas. Some areas experience higher precipitation than
others.
4. Land
cover. Availability of tree canopies and some plants naturally break the
effects of direct raindrops on the soil on the one hand and reduce the velocity
of flood and its consequences on the soil on the other.
Areas without these natural protections, experience
high level of erosion and subsequent gullies.
Anthropogenic factors include:
1.
Construction projects. Actions carried out both during and after construction
such as grading, clearing, and other activities that disturb the surface of the
soil, alter existing topography, and remove existing vegetation, can increase
erosion potential during construction.
2. Urbanization involving road construction,
building development, etc., contribute immensely to gully sites development.
3. Sand excavation. Sand excavation along the
sides of the roads by individuals who obtain permission to carry out such
excavation contribute to gully developments within the region of study.
4. Quarrying and mining activities. Abandoned
pits as a result of mining activities over a long period of time develop into
gullies.
5. Increase in the areas covered by pavements
and structures and a failure to incorporate into the construction design,
control measures that adequately stabilize slopes, re-establish cover on
exposed soils, or convey runoffs, can increase erosion long after construction
is completed.
6. Poor construction e.g. of roads without
adequate provision of drainage to rightly direct the runoffs.
7. Some other causative factors are cattle
grazing, deforestation, and bad farming habits of the people and so on.
Effects of erosion:
The overbearing effects of erosion on the
environment of the host areas cannot be emphasized. Apart from being a major
source of land degradation, it has been categorized as one of the major causes
of environmental disaster in the state and its environs. One of these effects
includes the formation of gullies. As the erosion continues to remove soil
along drainage lines, the affected areas continue to deepen. The end results
over a long period of years are deep gullies, which continue to enlarge if no
measure is taken to check it. The monstrous nature of gullies are such that
they continue to enlarge and deepen that some have gone as deep as over 100m
and these have resulted in the following.
i.
Displacement
of communities/settlements.
ii.
Destruction of Natural Habitat. Gullies are so
devastating that they destroy the natural habitat thereby affecting the flora
and fauna in the area.
iii.
Destruction of houses. Cracking of houses and
falling of buildings into gully sites are common features in the area. People
have lost their investments to gully expansion in areas like Agulu, Nanka,
Nnewi, etc., including the study erosion site at Omagba II Onitsha.
iv.
Sedimentation. One of the consequences of
gully erosion is the resultant sedimentation. This is because as the soil is
being eroded from one area caused by water runoff, it is being deposited in
other areas as sediments This has resulted in the disappearance of some streams
and rivers within the zone.
v.
Land Degradation: this is one of the worst
environmental problems facing many people worldwide. Over 40million are
affected in Nigeria (Uchegbu, 2002). It is the general and gradual reduction of
land value mainly as a result of some unhealthy anthropogenic activities on the
land. When top soils are washed away by erosion, the soil looses values due to
the washing away of soil nutrients by water. Also gullies on their own part
create trenches and deep holes that suddenly cut off large portions of lands
thereby degrading the values of such lands.
vi.
Damage to Infrastructure. Some infrastructures
such as roads and concrete drainages have been broken down and some communities
completely cut off.
The role of
surveying and mapping in the management and control of gully erosion.
The surveys carried out for gully control and remediation
included:
• Mapping of catchment basin and location of rills and secondary
gullies contributing run off to the main gully.
• Detailed surveys of
existing control infrastructure including gutters, culverts, catch pits,
drainage channels e.t.c
• Longitudinal bed profile from head to outlet of the main
gully.
• Planimetric survey
of the gully head at large scale.
• Cross sectional
surveys of the gully to determine the nature of the stage of gully development
i.e whether V or U shaped.
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