Site Characterization of Alluvial Silty Sand Soils by Dynamic In-Situ and Laboratory Tests

IF 0.6 Q4 CONSTRUCTION & BUILDING TECHNOLOGY
Ali Ramazan Borujerdi
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Abstract

Soil is normally heterogeneous and non-uniform material since it is made up of diverse types of matter. Understanding of soil parameters is one of the foremost complex assignments in geotechnical design. A few laboratory tests of soil need to carry out for engineering practices. Research facility tests take too much time to achieve and are excessive moreover. There's another elective way to urge soil parameters direct from the soil field investigation report to spare time and fetched. The objective ofthis consideration is to explore the relationships of soil parameters with the most commonly utilized soil investigating apparatuses SPT and CPT and other soil parameters that relate to direct applications in designing practice. In this investigate, four sets of in-situ tests were created in order to study the appropriateness of different existing CPT-SPT relationships to the alluvial silty sand soils. The recouped tests from SPT tests contain a calculable sum of fines (fc) extending from 3.5 to 39.2 percent and mean grain measure (D50) extending from 0.09 to 0.23 mm. Ponder comes about demonstrated that qc/N ratio as a function of D50and fc-based relationships are ineffectively pertinent to the silty sand soils. This paper recommends that q/(N1)60ratio as a function of increasing steadily can be way better related in silty sand soils rather than research facility-based D50or fcrelationships. An exertion has moreover been made to perform a comparative investigation for the compelling point of inside contact gotten from CPT, SPT, direct shear tests, andtriaxial tests.
冲积粉质砂土的动态原位和室内试验研究
土壤通常是异质性和非均匀性的物质,因为它是由不同类型的物质组成的。了解土壤参数是岩土工程设计中最重要的复杂任务之一。为了工程实践,需要进行一些土壤的室内试验。研究设施测试需要花费太多的时间来完成,而且是过度的。还有一种可选的方法,直接从土壤实地调查报告中督促土壤参数,利用空余时间提取。这一考虑的目的是探索土壤参数与最常用的土壤调查仪器SPT和CPT以及与设计实践中直接应用相关的其他土壤参数之间的关系。在本研究中,为了研究不同的CPT-SPT关系对冲积粉砂土的适用性,创建了四组原位试验。从SPT试验中回收的试验含有可计算的细粒(fc),范围从3.5%到39.2%,平均颗粒测量(D50)范围从0.09到0.23毫米。研究表明,qc/N比作为d50和fc关系的函数对粉砂质土没有有效的相关性。本文建议,在粉砂质土壤中,q/(N1)60比作为稳定增长的函数可以比基于研究设施的d50或函数更好地相关。并对CPT试验、SPT试验、直剪试验和三轴试验的内接触强迫点进行了对比研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.90
自引率
20.00%
发文量
25
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