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construction and refurbishment of earthen irrigation channel banks

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lose some moisture by evaporation. The specimen is then rolled out by h<strong>and</strong> on asmooth surface or between the palms into a thread about 3mm in diameter. Thethread is then folded <strong>and</strong> re-rolled repeatedly. During this manipulation themoisture content is gradually reduced <strong>and</strong> specimen stiffens, finally loses itsplasticity, <strong>and</strong> crumbles when the plastic limit is reached.After the thread crumbles, the pieces should be lumped together with a slightkneading action continued until the lump crumbles.The tougher the thread near the plastic limit <strong>and</strong> stiffer the lump when it finallycrumbles, the more potent is the colloidal clay fraction in the soil. Weakness <strong>of</strong>the thread at the plastic limit <strong>and</strong> quick loss <strong>of</strong> coherence <strong>of</strong> the lump below theplastic limit indicates either inorganic clay <strong>of</strong> low plasticity, or materials such askaolin-type clays <strong>and</strong> organic clays. Highly organic clays have a very weak <strong>and</strong>spongy feel at the plastic limit.15.11.4 Boundary ClassificationProper boundary classification <strong>of</strong> a soil near the borderline between coarse-grained<strong>and</strong> fine-grained soils is accomplished by classifying it first as a coarse-grained soil<strong>and</strong> then as a fine-grained soil. This type <strong>of</strong> dual classification is done for all soilswhich are visually judged to have between 40% <strong>and</strong> 60% <strong>of</strong> fine (or coarse)material.15.11.5 PlasticityThe h<strong>and</strong> classification method in the Description & Field Identification column inTable 15-10, can be used to determine whether the sample is <strong>of</strong> low, medium orhigh plasticity.Descriptive SymbolDescription & Field IdentificationTermLowPlasticityL May appear cloddy when dry, but dry lumps canreadily be broken by <strong>and</strong> powdered by pressure <strong>of</strong> thefingers <strong>and</strong> thumb. Will roll into a thick s<strong>of</strong>t threadthat is easily broken. When dry will brush from theh<strong>and</strong>s.IntermediatePlasticityI Fine textured soil smooth to the touch. May bemoulded into various shapes, will roll into a thread butbreaks on bending slightly.HighPlasticityH Very fine textured soil, smooth <strong>and</strong> very greasy. Rollsinto a very fine thread without breaking. Thread willbend to about 45° without breaking.Fat Clay H Threads will bend almost in two without breaking.Table 15-10Determination <strong>of</strong> plasticity by Field Identification15.11.6 Rapid Dispersion Test.Fill a clear glass jar half full (100ml) <strong>of</strong> distilled water or rainwater, gently place apea-size crumb (5 to 10 grams) <strong>of</strong> dry soil sample into the jar <strong>and</strong> leave undisturbedfor at least an hour, without shaking. At the end <strong>of</strong> the waiting period, the interfaceConstruction <strong>and</strong> Refurbishment <strong>of</strong> Earthen Channel Banks

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