grain size distribution वाक्य
उदाहरण वाक्य
मोबाइल
- Gradation of a soil is determined by reading the grain size distribution curve produced from the results of laboratory tests on the soil.
- Its grain size distribution is : 52 % under 10 microns; 33 % 10 microns to 30 microns, 15 % above 30 microns.
- This change will introduce some form of grain size distribution, which will have a significant impact on the ultimate physical properties of the material.
- The results of a sieve analysis are plotted as a grain size distribution curve, which is then analyzed to determine the soil gradation of the particular soil.
- The engineering properties of soils are affected by four main factors : the predominant size of the mineral particles, the type of mineral particles, the grain size distribution, and the relative quantities of mineral, water and air present in the soil matrix.
- If the soil has 5 12 % by weight of fines passing a # 200 sieve ( 5 % # 200 < 12 % ), both grain size distribution and plasticity have a significant effect on the engineering properties of the soil, and dual notation may be used for the group symbol.
- "' Abnormal "'or "'discontinuous grain growth "', also referred to as "'exaggerated "'or "'secondary recrystallisation grain growth "', is a grain growth phenomenon through which certain energetically favorable grains ( crystallites ) grow rapidly in a bimodal grain size distribution.
- A disturbed sample is one in which the structure of the soil has been changed sufficiently that tests of structural properties of the soil will not be representative of in-situ conditions, and only properties of the soil grains ( e . g ., grain size distribution, Atterberg limits, and possibly the water content ) can be accurately determined.
- In addition, because the source of sediment ( i . e . land, ocean, or organically ) is often correlated with how coarse or fine sediment grain sizes that characterize an area are on average, grain size distribution of sediment will shift according to relative input of land ( typically fine ), marine ( typically coarse ), and organically-derived ( variable with age ) sediment.
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