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赵忠义, 王健, 申景转, 张立海, 钱慧英. 颗粒分析中密度计法土粒粒径计算公式研究[J]. 岩土工程学报, 2001, 23(2): 247-249.
引用本文: 赵忠义, 王健, 申景转, 张立海, 钱慧英. 颗粒分析中密度计法土粒粒径计算公式研究[J]. 岩土工程学报, 2001, 23(2): 247-249.
ZHAO Zhongyi, WANG Jian, SHEN Jingzhuan, ZHANG Lihai, QIAN Huiying. Research on formula for calculating grain diameter in densimeter method of granulometric analysis[J]. Chinese Journal of Geotechnical Engineering, 2001, 23(2): 247-249.
Citation: ZHAO Zhongyi, WANG Jian, SHEN Jingzhuan, ZHANG Lihai, QIAN Huiying. Research on formula for calculating grain diameter in densimeter method of granulometric analysis[J]. Chinese Journal of Geotechnical Engineering, 2001, 23(2): 247-249.

颗粒分析中密度计法土粒粒径计算公式研究

Research on formula for calculating grain diameter in densimeter method of granulometric analysis

  • 摘要: GB/T 5 0 12 3— 1999《土工试验方法标准》中采用密度计法进行颗粒分析时 ,土粒粒径计算公式 (斯托克斯公式 )是在层流条件下 ,对低速运动的微小球形颗粒仅考虑介质粘性阻力和有效重力条件下导出的。试验的土颗粒都具有不规则的形状 ,颗粒在下沉过程中由于周围颗粒的存在而引起附加作用 (即干涉沉降 ) ,这些因素会使颗粒沉降速度大为降低。此外颗粒沉降速度较大时悬液中将产生紊流 ,超出斯托克斯公式适用范围。上述因素都会使试验结果与实际产生一定偏差。通过对上述因素的剖析 ,得出了斯托克斯公式的修正方法及适用范围。

     

    Abstract: The use of the formula for calculating the grain diameter in densimeter method prescribed in “Standard for soil test method” GB/T 50123—1999 is limited to the small global grains with low velocity in a layer flow considering only the viscous resistance and effective gravity. The soil grains tested all have irregular shape.The surrounding granules cause additional action to the settling granules (namely, intervenient settling). These factors will reduce the settling velocity of granules greatly. In addition, there will be a turbulent flow in the suspending liquid when the settling velocity of granule is bigger. This will outstep the applicable range of Stokes formula. The above-mentioned factors will cause that the calculated results deviate from reality. This paper dissects the above-mentioned factors,and proposes the corrected Stokes formula and its applicable range.

     

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