Abstract

The amount of fines in sand greatly influence the permeability of sandy soils. Thus, this research was conducted to study the effect of plastic and non-plastic fines on the permeability of three types of sands (Lawrencepur sand, Chenab sand and Ravi sand). For this purpose, plastic and non-plastic fines were collected from different location of Lahore. Samples were prepared by mixing plastic and non-plastic fines into each type of sand separately, in amounts ranging from 0% to 50% with increments of five percent. Overall 63 samples were prepared. Sieve analysis and hydrometric analysis were performed to obtain particle size distribution for each sample. Atterberg’s limits were also determined and each sample was classified according to the Unified Soil Classification System (USCS). Compaction tests were performed on all samples as per the procedure in a standard Proctor test. The test samples were compacted in permeability molds with optimum moisture contents to obtain the density, as per a standard Proctor test. Hydraulic conductivity tests were performed on all sixty-three samples using a constant head permeameter and a falling head permeameter. Permeability results were plotted against the percentage of fines added. It was noted from the curves that the permeability of sand-fine mixtures shows a decreasing trend with the addition of fine contents. A few trials were performed to formulate a correlation. Validation of the correlation was performed with the results of 52 data sets from the field. Finally, the devised correlation was compared with three empirical equations proposed by Mujtaba, Kozeny–Carman and Hazen.

Highlights

  • Permeability is an important physical property of soil whose understanding is essential in settlement, seepage and stability analyses [1,2]

  • An equation was developed to predict the permeability of sand and fine mixes

  • The study of literature indicates that most equations developed for predicting the permeability are for granular soils with little effort being made for fine-grained soils

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Summary

Introduction

Permeability is an important physical property of soil whose understanding is essential in settlement, seepage and stability analyses [1,2]. The stability of structures depends to a large degree on the interaction of the said soil with water, or in other words, the ability of water to flow through the soil [3,4]. In-depth understanding of soil permeability is needed to estimate the quantity of seepage under and through dams, levees and embankments etc. It helps to plan dewatering methods to facilitate underground construction [5]. Many dam failures have occurred due to insufficient geotechnical and geological investigations. The failure due to seepage through a dam body and/or foundation accounts for almost 30% of total failures [6]

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