Geoscience Reference
In-Depth Information
Table 10.8 ( Continued )
Test type
Test
Coefficient of variation
Compaction
Maximum dry density
1-7%
Optimum moisture content
200-300%
Durability
Absorption
25%
Crushing value
8-14%
Flakiness
13-40%
Los angeles abrasion
31%
Sulphate soundness
92%
Deformation
Compressibility
18-73%
Consolidation coefficient
25-100%
Elastic modulus
2-42%
Flow
Permeability
200-300%
10.9 Distribution functions
Variability can be assessed by distribution functions.
The Normal distribution is the taught fundamental distribution, in maths and
engineering courses. It is the simplest distribution to understand, but is not directly
relevant to soils and rocks.
When applied to soil or rock strength properties, negative values can result
at say lower 5 percentile if a normal distribution used (Look and Griffiths,
2004).
The assumed distribution can affect the results considerably. For example the
probability of failure of a slope can vary by a factor of 10 if a normally distributed
or gamma distribution used.
Table 10.9 Appropriate distribution functions in Rock property assessment (Look and Griffiths,
2004).
Distribution
Overall
Typical application outside of geotechnical engineering
type
rank
Pearson VI
1
Time to perform a task.
Lognormal
2
Measurement errors. Quantities that are the product of a large
number of other quantities. Distribution of physical quantities
such as the size of an oil field.
Gamma
3
Time to complete some task, such as building a facility,
servicing a request.
Weibull
4
Lifetime of a service for reliability index.
Beta
5
Approximate activity time in a PERT network. Used as a rough
model in the absence of data.
Normal
11
Distribution characteristics of a population (height, weight);
size of quantities that are the sum of other quantities (because
of central limit theorem).
Above rank is based on various goodness of fit tests for 25 distribution types.
Due to non normality of distribution, the median is recommended instead of mean
in characterisation of a site.
 
 
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