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Appendix E - Geotechnical site classification report · MCU25/0022
Tree root growth
Trees and shrubs that are allowed to grow in the vicinity of footings
can cause foundation soil movement in two ways:
• Roots that grow under footings may increase in cross-
sectional size, exerting upward pressure on footings.
• Roots in the vicinity of footings will absorb much of the
moisture in the foundation soil, causing shrinkage or
subsidence.
Unevenness of Movement
The types of ground movement described above usually occur
unevenly throughout the building’s foundation soil. Settlement due looting settlement
to construction tends to be uneven because of:
• Differing compaction of foundation soil prior to construction.
• Differing moisture content of foundation soil prior
to construction.
Movement due to non-construction causes is usually more uneven external footings. The doming is accentuated and cracking reduces
still. Erosion can undermine a footing that traverses the flow or can or disappears where it occurred because of dishing, but other
create the conditions for shear failure by eroding soil adjacent to a cracks open up. The roof lines may become convex.
footing that runs in the same direction as the flow. Doming and dishing are also affected by weather in other ways. In
Saturation of clay foundation soil may occur where subfloor walls create areas where warm, wet summers and cooler dry winters prevail,
a dam that makes water pond. It can also occur wherever there is a water migration tends to be toward the interior and doming will be
source of water near footings in clay soil. This leads to a severe accentuated, whereas where summers are dry and winters are cold
reduction in the strength of the soil which may create local shear failure. and wet, migration tends to be toward the exterior and the
Seasonal swelling and shrinkage of clay soil affects the perimeter of the underlying propensity is toward dishing.
building first, then gradually spreads to the interior. The swelling Movement caused by tree roots
process will usually begin at the uphill extreme of the building, or on In general, growing roots will exert an upward pressure on footings,
the weather side where the land is flat. Swelling gradually reaches the whereas soil subject to drying because of tree or shrub roots will tend
interior soil as absorption continues. Shrinkage usually begins where to remove support from under footings by inducing shrinkage.
the sun’s heat is greatest.
Effects of Uneven Soil Movement on Structures Complications caused by the structure itself
Most forces that the soil causes to be exerted on structures are
Erosion and saturation vertical – i.e. either up or down. However, because these forces are
Erosion removes the support from under footings, tending to create seldom spread evenly around the footings, and because the building
subsidence of the part of the structure under which it occurs. resists uneven movement because of its rigidity, forces are exerted
Brickwork walls will resist the stress created by this removal of from one part of the building to another. The net result of all these
support by bridging the gap or cantilevering until the bricks or the forces is usually rotational. This resultant force often complicates
mortar bedding fail. Older masonry has little resistance. Evidence of the diagnosis because the visible symptoms do not simply reflect the
failure varies according to circumstances and symptoms may include: original cause. A common symptom is binding of doors on the
• Step cracking in the mortar beds in the body of the wall or vertical member of the frame.
above/ below openings such as doors or windows. Effects on full masonry structures
• Vertical cracking in the bricks (usually but not necessarily in Brickwork will resist cracking where it can. It will attempt to span
line with the vertical beds or perpends). areas that lose support because of subsided foundations or raised
Isolated piers affected by erosion or saturation of foundations will points. It is therefore usual to see cracking at weak points, such as
eventually lose contact with the bearers they support and may tilt or openings for windows or doors.
fall over. The floors that have lost this support will become bouncy, In the event of construction settlement, cracking will usually remain
sometimes rattling ornaments etc. unchanged after the process of settlement has ceased.
With local shear or erosion, cracking will usually continue to develop
Seasonal swelling/shrinkage in clay until the original cause has been remedied, or until the subsidence
Swelling foundation soil due to rainy periods first lifts the most exposed has completely neutralised the affected portion of footing and the
extremities of the footing system, then the remainder of the perimeter structure has stabilised on other footings that remain effective.
footings while gradually permeating inside the building footprint to lift
internal footings. This swelling first tends to create a dish effect, In the case of swell/shrink effects, the brickwork will in some cases
because the external footings are pushed higher than the internal ones. return to its original position after completion of a cycle, however it
is more likely that the rotational effect will not be exactly reversed,
The first noticeable symptom may be that the floor appears slightly and it is also usual that brickwork will settle in its new position and
dished. This is often accompanied by some doors binding on the will resist the forces trying to return it to its original position. This
floor or the door head, together with some cracking of cornice means that in a case where swelling takes place after construction
mitres. In buildings with timber flooring supported by bearers and and cracking occurs, the cracking is likely to at least partly remain
joists, the floor can be bouncy. Externally there may be visible after the shrink segment of the cycle is complete. Thus, each time the
dishing of the hip or ridge lines. cycle is repeated, the likelihood is that the cracking will become
As the moisture absorption process completes its journey to the wider until the sections of brickwork become virtually independent.
innermost areas of the building, the internal footings will rise. If the With repeated cycles, once the cracking is established, if there is no
spread of moisture is roughly even, it may be that the symptoms will other complication, it is normal for the incidence of cracking to
temporarily disappear, but it is more likely that swelling will be stabilise, as the building has the articulation it needs to cope with the
uneven, creating a difference rather than a disappearance in problem. This is by no means always the case, however, and
symptoms. In buildings with timber flooring supported by bearers and monitoring of cracks in walls and floors should always be treated
joists, the isolated piers will rise more easily than the strip footings or seriously.
piers under walls, creating noticeable doming of flooring.
Upheaval caused by growth of tree roots under footings is not a
As the weather pattern changes and the soil begins to dry out, the simple vertical shear stress. There is a tendency for the root to also
external footings will be first affected, beginning with the locations exert lateral forces that attempt to separate sections of brickwork
where the sun’s effect is strongest. This has the effect of lowering the after initial cracking has occurred.
8894-193 Sankeys Rd-FEDERAL Page 13 of 15 19/07/2023
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