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construction and refurbishment of earthen irrigation channel banks

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Natural moisture content should also be measured. This will give an indication <strong>of</strong> howclose the borrow material is to optimum moisture content <strong>and</strong> whether it requirestreatment before <strong>construction</strong>. Refer Section 16.11, Moisture Content Control Tests <strong>and</strong>Procedures.Soil Classification may be achieved by Australian St<strong>and</strong>ard tests or by field identificationmethods.Australian St<strong>and</strong>ard tests should be used wherever possible. However, many <strong>of</strong> thesetesting procedures need to be conducted by experienced staff with appropriate equipmentin a laboratory, <strong>and</strong> are <strong>of</strong>ten time-consuming <strong>and</strong> expensive. For small projects, fieldidentification procedures may be adequate as described in section 15.10. Where staff areexperienced in <strong>channel</strong> bank <strong>construction</strong> in a particular area, they can become reasonablyaccurate at determining soil classification <strong>and</strong> estimating shrinkage <strong>and</strong> dispersion, byfield methods.When determining the level <strong>of</strong> testing required for a particular project, consideration mustbe given to the risk rating <strong>of</strong> the <strong>channel</strong> bank. Refer Section 14, Risk Analysis. Wherethe Risk is determined to be Medium to High, more care will be required in soil testing.Consideration should be given to using Australian St<strong>and</strong>ard tests for Soil Classification,Shrinkage <strong>and</strong> Dispersion. If the Risk is assessed as Low, field identification methodsmay be appropriate.15.4 Soil ClassificationTo measure soil properties like permeability, shear strength <strong>and</strong> erosion resistance can bedifficult, time consuming <strong>and</strong> expensive. It can therefore be very useful to sort soils intogroups showing similar behaviour. Such sorting is soil classification. Soil Classificationis thus the process by which a soil sample is classified into a group <strong>of</strong> soils all <strong>of</strong> whichexhibit similar behaviour. The aim <strong>of</strong> a classification system is to provide a set <strong>of</strong>common definitions which will permit useful comparisons to be made between differentsoils. Soil behaviour <strong>and</strong> suitability for various <strong>construction</strong> purposes can then bepredicted by using the classification system.The two classification criteria relevant to <strong>channel</strong> bank <strong>construction</strong> are:1. a broad classification into the five fundamental soil groups; gravel, s<strong>and</strong>, silt, clay <strong>and</strong>organic material, as shown in Figure 15.2.2. the plasticity <strong>of</strong> the fine-grained fraction <strong>of</strong> the materialSoilGravel (G)Coarse grainedS<strong>and</strong> (S)Silt (M)Fine grainedInorganic clay (C)PeatOrganic siltor clay (O)Figure 15.2Broad Classification <strong>of</strong> SoilsGravels <strong>and</strong> s<strong>and</strong>s can be readily identified by appearance <strong>and</strong> feel, but silts <strong>and</strong> clays areindistinguishable when dry.Construction <strong>and</strong> Refurbishment <strong>of</strong> Earthen Channel Banks August 2002 - Edition 1.0 15-7

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