Meeting
with Associate Professor Brian Finlayson 16/3/01
Centre for environmental applied hydrology School of anthropology
and applied environmental studies The Melbourne University Margy
Dockray (Mt. Arthur Environment Management Group) and Frank Strie
(Private Forestry Consultant) met with Prof. Brian Finlayson from
9.30am to 6.00pm on site at coupe LI 126C on Mt. Arthur on Friday
16th March.
We were joined by Jonno Pedley (Mt Arthur Environment Management
Group) for some of this time. The purpose of Brian's visit was to
outline the likely impacts from an hydrological point of view regarding
the consequences of clearfelling/plantation establishment across
the coupe, as well as in areas adjacent to the coupe.
We took Brian to several sites within the coupe, including the variation,
where he examined logging practices, definition of streams and reserves,
roading, drainage, geological form and soil types. From these observations,
he drew the following conclusions.
The effects of clearing native forest and replacing with plantation:
Water Yield Relevant Data: The scale of the clearing and replacement
plantations in this area is so large that the effects on the water
yield have the potential to be tremendous. This extensive clearing
has been conducted without sufficient data and study, ie no small
scale pilot areas established and monitored for changes in water
yield. Therefore, any conclusions drawn, (including those Forestry
Tasmania, and Brian Finlayson) as to the effects on water yield,
of such large scale plantation establishment, could only be speculation.
Given the nature of the operation, (clearing of forest which has
taken millennia to establish) any impact on water yield will be
long term and one way (as good as irreversible). Therefore, Brian
suggested that the continued clearing and replacement with plantation
is both foolish and dangerous, as the effects on water yield although
unknown, could be catastrophic.
He described the operation as "flying blind" in relation to water
yield. Brian based his conclusions on data available through smaller
scale clearing of areas of Eucalyptus Regnans forest in central
Victoria, which has both similarities and differences to the area
on Mt. Arthur.
On the basis of extrapolation of data from these studies, Brian
guesses that there will be a reduction in water yield. Brian stressed
that although others may form different conclusions, their conclusions
would not be based on alternative evidence.
There just is no data on which to make reliable conclusions.
Water Quality The effect on water quality by clearing and plantation
establishment in this operation will take two forms - impact from
run-off (carrying sediment thereby increasing turbidity) and impact
from use of chemicals and sprayed herbicides.
RunOff. Preamble:
Unidentified streams Throughout the coupe and surrounding areas,
there was evidence that streams and water carrying depressions had
been ignored and disturbed. This was particularly noticeable in
the area known as the variation to the FPP for Coupe LI 126C. In
the section above the Mt. Arthur Road, at least 4 streams, currently
flowing (after prolonged dry period) were identified. According
to the FPC 2000, these streams were at least class 4, and probably
even class 3 (for definition, see p56). That they existed should
have been evident by the vegetation, which was rainforest, with
no eucalypti. Two of these streams, although running, are not defined
by significant depressions, and could not have been noted through
contours in aerial survey, although the other two were defined by
depression.
The variation to the FPP made no mention of any of these streams,
indicating that the hydrological survey was inadequate in assessment
for the coupe. The operator had therefore cleared the entire area,
with major disturbance to the streams.
Still in the variation, in the area below the Mt. Arthur Road, depressions
were noted, having been entirely cleared, and used as snig tracks
for the removal of logs. These depressions were identified as class
4 streams, leading directly into the class 3 stream marked as being
at the head of the Shepherd's Rivulet, on the edge of the coupe.
Insufficient Buffer Zones in streamside reserves. Throughout the
coupe, streams identified on the FPP were not afforded appropriate
exclusion zones. The nature of these streams high in the catchment
is that they cover a broad area, with ill-defined banks and boundaries.
Again, the boundaries of the streams can be ascertained through
studying the vegetation. Stream boundaries change according to the
seasonal conditions. As the soils become saturated during wet periods,
the water table rises and the boundaries of the water courses expand
and widen. In some cases the stream itself grows in width from a
narrow channel to 20 or 30 meters wide. (For example, the stream
on lower side of road before the intersection to Lone Star Road).
According to the FPC 2000, streams will be afforded exclusion zones
according to their classification, which extend from both edges
or banks of the stream as it runs during the wettest periods. It
is these non-disturbed exclusion zones which are supposed to absorb
any sediment caught up in the run-off, before it reaches the stream
system itself. In the coupe however, exclusion zones were inadequate,
being measured from the middle of the streams assessed in the dryest
season rather than from their extremities in the wettest conditions.
Roading, and provision of drains for run-off. The Mt. Arthur Road
was not adequately constructed, being flat, with no table drains.
Existing culverts had been damaged and/or covered. According to
the code, all forestry roads must be shaped and table drains constructed,
with frequent exits for dispersement of water into areas of undisturbed
vegetation, where most of the sediment from the run-off from disturbed
areas could be trapped and collected.
There were insufficient exits, and undisturbed patches of vegetation,
to enable adequate protection for streams. Instead, all run-off
water would be expected to build up on road edges, collecting at
the lowest points (where there were depressions and streams), and
flow directly into the stream systems. In conclusion: Much of the
disturbed soil and rock, would be picked up and washed into the
streams, causing ongoing sedimentation and increased turbidity.
This has two effects.
Firstly, the water becomes contaminated with silt, requiring filtering
for human consumption downstream, and secondly, a fine layer of
sediment is deposited over stream bed, causing a blanketing of habitat
for macro-invertebrates, at the bottom of the food chain, which
then affects the whole eco-system. Also, the vegetation in these
areas is sensitive and largely intolerant to the build up of sediment
around their roots and buts.
Chemical contamination Preamble:
The argument that the spraying of herbicides, application of fertilisers
and laying of 1080 poison, is of no environmental concern, lies
in the assertion that these rainforest soils have a thick humus
layer, which acts as a filter to chemical contaminants. The surface
water containing contaminants gradually percolates down through
this thick humus layer into the soil where the chemicals are fully
absorbed and bio-degraded. Thus, the soil filters out all contaminants
before the water reaches the water table where it is transported
clean, into the streams and river systems.
Brian explained that while there is some truth in this argument,
it was not true in soils that had been subject to ground preparation
prior to plantation establishment because once the forest had been
cleared, the thick humus layer is dissipated through burning and
ploughing. Also in these forest soils, there are "macro pores" (root
holes, structural cracks, animal burrows etc.) where some of the
surface water is transported directly down, straight through into
the water table, with no opportunity for contaminants in this proportion
of water to be absorbed.
This is further complicated in areas of block fields such as the
higher parts of Mt Arthur (deep cavities carrying water laterally
through conduits below the surface) which transport these contaminants
downstream. So you have a proportion of contaminants being moved
quickly down through the soil in macro pores then laterally through
soil through block fields emerging in springs and streams lower
down the slope. These contaminants all then pass into the food chain.
Diesel contamination:
Diesel and oil will travel through the soil. Where there have been
small spillages, as has happened on the coupe, the worry is that
the operators are carrying out practices that are unsafe, and may
lead to catastophe.
Conclusions:
Contamination of the water table, with chemicals from herbicide
and fertiliser application associated with plantation establishment
will result from the operations in the area.
Contamination of surface water from run-off, and soil erosion, will
occur, increasing particularly as the soil becomes saturated during
prolonged wet peroiods. This surface water will find its way into
streams and rivers because of inadequate buffer zones of undisturbed
vegetation. The impact of this is likely to be to cause damage to
the ecosystems of the rivers and streams through siltation, as well
as increased turbidity in water downstream.
Specific for water catchment areas:
The higher up the mountain you go, the greater the water yield because
of increasing rainfall, and lowering of transpiration due to decreasing
temperatures. This means that the higher up the mountain, the more
fragile and sensitive the area. According to the code, no more than
5% of a town water supply catchment can be felled each year. The
reason being the risk of contaminants to the water supply. The problem
with the code as it stands is that it only mentions town water catchment.
Those outside the towns who are also adversely affected by contaminants
in the water are not afforded the same consideration and protection.
Problems with using maps for assessment of
coupe's water courses:
Often contours on a map will show a depression but not a stream
(blue line). In very wet conditions, the streams extend uphill.
The water is carried down the depressions which would be completely
dry at this time of year. Also, the contour lines on maps themselves
are not necessarily accurate. Most contours are mapped from aerial
photographs, which do not show very small depressions, or streams
which run without a depression or topographical definition, as is
the case high up in this catchment. Also, the forest canopy is uneven
and irregular, therefore it often hides these types of water courses.
Even walking over the ground may not show up water courses, as they
may be covered over with large quantities of rotting vegetation
and leaf litter. Provision is made within the FPP that if one of
these streams is discovered by an operator, he must then contact
a Forestry Tasmania officer. The problem with this is that the operator
may only discover the stream when it is already too late, having
disturbed it with felling and machinery.
Preparation of the land for planting and the
deep ripping of the slopes:
The ripping of rows up and down the slopes acts as tiny class 4
water courses, pulling sediment off the slopes directly into the
streams and rivers and contributing significantly to soil erosion.
This practice was noticed in areas adjacent to the coupe. |