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Response to Information Request - OPW13/0669
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Tree Inspection Report -
Manyaii Chan
Site Address: 4 Habitat Place, Noosa Heads
orl’
roots during the repairs (approximately 150mm in diameter). There are no visible signs of canopy decline
result ng from this root pruning; however the onset of decay often takes several years to become apparent.
Root growth and development excelled within the excavated area as a result of back filling the rain water
harvesting tanks area with Mary Valley Sand.
WhilSl
beco
investigating the site characteristics on Sunshine Coast Regional Council My Maps website, it has
e apparent that the immediate environment surrounding 4 Habitat Place has been mapped under the
Noos Plan as a Flood Hazard Area, Minimum Floor Height, Acid Sulphate Soils & Bushfire Hazard. The
adjoi ng allotment Weyba Creek Bushland Reserve South is mapped as a Biodiversity I Environmental Area.
Despi e being mapped as a Bush Fire Hazard area, there is no fire contaminant line (buffer) between the rear
boun aries of Habitat Place properties which adjoin this Weyba Creek Bushland Reserve South Environmental
area.
Acid ulphate Soils will only become an issue in the event that soil is excavated, exposed to the air, which is
highly unlikely considering the fact that the construction phase is complete.
There is a sewer main contained within an easement, (apex in shape) which runs through 4 Habitat Place
(refer 0 aerial imagery on page 2). Image 7 on page 4 shows an estimated projection of this easement with the
manh Ie cover positioned beneath the pool deck. This easement runs through the structural Root Zone of this
Eucal ptus tereticornis (Forest Red Gum) thus making it difficult to maintain easement infrastructure. Based
upon ite projections ArborCare Queensland believes the centre of this easement to be situated approx. 2.2m
to 2.7 from edge of the tree.
A su y drawing of 4 Habitat Place, Noosa Heads classifies the soil type as a Silt Clay Soil. Typically clay soil
types re associated with a
phenomena called expandable clays (Shrink Swells)
Shrink Swell occurs as a result of changes in the moisture content of clay-rich soils. This is reflected in a
chang in volume of the ground through shrinking or swelling. Swelling pressures can cause heaving, or lifting,
of stru tures whilst shrinkage can cause differential settlement.
The by which the ground can shrink and I or swell is determined by the water content in the near
and th
arount
surfac and the type of clay. Considering the size and stature of this Eucalyptus tereticornis (Forest Red Gum)
current environmental weather conditions there is the possibility that this phenomena may become a
proble as the tree matures and weather patterns change.
Consultin Arborist: Phillip Best
Dip. Arb, Nat. Cert. Hort Page 8/10
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