Soil compaction
Assessing the magnitude of soil compaction
Soil compaction measures
Natural factors influencing soil compaction
Most land-based recreational activities carried
out in the vicinity of marine features, whether carried out
on foot, horseback or vehicle, exert forces on the surface of
that feature which can result in compaction. The magnitude of
the pressure and the characteristics of the feature will determine
the nature of any impact.
Impacts can include:
-
erosion of soils and upper levels of less
durable marine features
-
changes in the level and diversity of vegetation
within a site or feature
-
changes in feature density, porosity and
penetrability
Changes to a feature associated with soil compaction
do not necessarily imply a significant adverse impact. There
is an important difference between change and impact and this
can only be determined at the specific site-level.
Assessing the Magnitude of Soil Compaction
It is possible to make an assessment of the
magnitude of soil compaction caused by different activities
by reviewing the different static ground pressures exerted by
activities. This involves dividing the weight exerted by an
activity on the ground by the area in contact with the ground.
Soil
Activity
|
Average of total Weight (g)
|
Ground contact area (cm2)
|
Pressure (g/cm2)
|
Source of data
|
Human
|
|
|
|
|
Bare footed
|
73,000
|
262
|
279
|
Liddle (unpublished)
|
Shoes
|
73,000
|
406
|
180
|
Liddle & Grieg-Smith (1975)
|
Animal
|
|
|
|
|
Horse & rider (shoes only)
|
613,000
|
140
|
4,380
|
Liddle (unpublished)
|
Vehicle
|
|
|
|
|
Trail-bike
|
229,000
|
114
|
2,008
|
Eckert et al (1979)
|
Quad bike
|
140,000
|
1,400
|
100
|
Slaughter et al (1990)
|
Saloon car and driver
|
1,282,000
|
855
|
1,500
|
Liddle & Greig-Smith (1975)
|
Four wheel drive Toyota, loaded four people and gear
|
2,500,000
|
1,483
|
1,686
|
Liddle (unpublished)
|
Compaction Measures
Liddle (1997)
The greatest static pressure is exerted by
horse and rider, mainly because of the small ground area over
which the weight is spread, followed by motorised vehicles.
This has implications for those features which are particularly
sensitive to compaction, such as sand dunes, where activities
such as horses riding are likely to occur.
In those areas where wildfowling takes place,
there may be observable trampling effects on vegetation, although
because the activities tend to take place in tidal areas, compaction
impacts are likely to be minimal. Wildfowling is likely to cause
less overall trampling-related impacts than an activity such
as dog walking for example, as levels of participation in wildfowling
are at a much lower level.
Natural Factors Influencing
Soil Compaction
Marine features are supported by underlying
layers of rock and soil which determine their overall resilience
to ground pressure. The different natural characteristics are
just as important in determining the impact of recreational
activities, as are the relative ground pressures exerted by
those activities. Uneven, stony or rocky ground, as found on
rocky shores, results in a person’s weight being distributed
over a much smaller area. In such an area, the static pressure
of a person can be greater than that of a vehicle, with associated
implications for sensitive rocky shore vegetation.
For example, in areas where underwater reefs
extend to the shore, people who go ‘rock pooling’ or gathering
rock pool species at low tide can exert a significant static
ground pressure, with consequential implications for density
and diversity of species.
Conversely, soft ground such as mudflats, sandflats
and saltmarsh enables the load of a person to be spread over
a greater area and therefore results in lower ground pressure.
However, communities found in such habitats can be very vulnerable
to even low pressure activities, particularly if they live in
the upper layers of the mud or sand flat. Heavy vehicles accessing
these areas therefore have the potential to cause significant
damage to such communities.
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