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Geotechnical Stability Assessment · MCU19/0008
The test results are reported in the following resistance and friction ratios are only inferred
form: and must not be considered as exact.
In the case where full penetration is Stratification can be inferred from the cone
obtained with successive blow counts and friction traces and from experience and
for each 150mm of , say, 4, 6 and 7 information from nearby boreholes, etc. Where
blows, as shown, this information is presented for general
N = 13 guidance, but must be regarded as
4, 6, 7 interpretive.
In a case where the test is discontinued
short of full penetration, say after 15 Dynamic Cone Penetrometers:
blows for the first 150mm and 30 blows
Dynamic Cone Penetrometer (DCP) tests are
for the next 40mm, as
carried out by driving a 16mm diameter rod
N > 30
into the ground with a 9kg sliding hammer
15, 30/40mm
dropping 510mm and counting the blows for
Cone Penetrometer Testing (CPT): Cone
successive 100mm increments of penetration.
Penetrometer Testing with or without pore
pressure measurement (CPTu) is carried out
Logs
using a Cone Penetrometer in general
accordance with AS 1289 6.5.1, 1999. The borehole or test pit logs are an
interpretation of the subsurface conditions, and
In the tests, a 36mm diameter rod with a
their reliability will depend to some extent on
conical tip is pushed continuously into the soil,
the frequency of sampling and the method of
the reaction being provided by a hydraulic
drilling or excavation.
ram system. Measurements are made of the
end bearing resistance on the cone and the Interpretation of the information shown on the
fractional resistance on a separate 135mm logs, and its application to design and
long sleeve, immediately behind the cone. construction, should therefore take into
Pore Pressure is recovered through a pore ring account the spacing of the boreholes or test
located either within, or more usually pits, the method of drilling or excavation, the
immediately behind the cone/tip. frequency of sampling and testing and the
possibility of other than “straight line” variations
As penetration occurs (at a rate of
between the boreholes or test pits. Subsurface
approximately 20mm per second) and data is
conditions between boreholes or test pits may
recorded every 20mm of penetration, the
vary significantly from conditions encountered
results are presented graphically.
at the borehole or test pit locations.
The information provided on the plot
Groundwater
comprises:
Where groundwater levels are measured in
Cone resistance – expressed in mPa
boreholes, there are several potential
Sleeve friction – expressed in kPa
problems:
Friction ratio – the ratio of sleeve
friction to cone resistance expressed as Although groundwater may be
a percentage. present, in low permeability soils it may
Pore pressure in kPa enter the hole slowly or perhaps not at
Tilt of probe (in degrees). all during the time it is left open.
The ratios of the sleeve resistance to cone A localised perched water table may
resistance will vary with the type of soil lead to an erroneous indication of the
encountered, with higher relative friction in true water table.
clays than in sands. Friction ratios of 1% to 2% Water table levels will vary from time to
are commonly encountered in sands and rising time with seasons or recent weather
to 2% to as high as 8%, and higher in organic changes and may not be the same at
soils. Soil descriptions based on cone the time of construction.
October 2017 pg. 3
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