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INTERNATIONALJOURNALOFCIVILANDSTRUCTURALENGINEERING Volume1,No 4,2011 Copyright2010AllrightsreservedIntegratedPublishingservicesResearcharticleISSN0976 4399Effectofparticlesizeandshapeonthegrainsizedistributionusing
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Grainsize distribution refers to the measurement and representation of the various sizes of grains or particles within a particular material, such as soil, sediment, or crushed rock.
The requirement to file grainsize distribution may vary depending on the context. However, typically geologists, geotechnical engineers, or researchers working with materials like soil or sediment may be required to file grainsize distribution data as part of their analysis or reports.
To fill out grainsize distribution data, one would typically measure the sizes of individual grains or particles using techniques like sieving or laser diffraction. The measurements are then recorded and organized into a distribution table or plot that shows the percentage of grains falling within each size range.
The purpose of grainsize distribution analysis is to provide information about the sediment or material being studied. It can help determine properties such as porosity, permeability, compaction, or the potential for erosion or sediment transport.
The specific information to be reported on grainsize distribution may vary depending on the requirements or objectives of the study or project. However, common information includes the size range or intervals, the percentage of grains falling within each size range, and any other relevant parameters such as mean or median grain size.
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