Technical note
On the interface shear resistance of a novel geogrid with in-plane drainage capability

https://doi.org/10.1016/j.geotexmem.2007.12.006Get rights and content

Abstract

The enhancement in the short-term interface shear strength (critical case for embankment construction) achieved by a novel geogrid that combines both reinforcement and in-plane drainage functions was studied. Marginal fill (wet gravely clay) was standard Proctor compacted to 92% of its maximum dry density and tested under consolidated-undrained conditions in the large shearbox apparatus. The interface shear resistance (τs−g) values mobilized for the novel geogrid were similar to the undrained shear strength of the surrounding soil. In contrast, the τs−g values mobilized for a conventional geogrid, which had similar physical and tensile strength properties, were only between 82% and 85% of the undrained shear strength of the soil. Overall, the undrained shear resistance mobilized along the soil–geogrid interface was between 20% and 30% greater for the novel geogrid than for the conventional geogrid.

Introduction

Geosynthetics are widely used in reinforced-earth and landfill construction and soft ground improvement (Bergado et al., 2006; Long et al., 2007; Tatsuoka et al., 2007; Rowe and Taechakumthorn, 2008), and have many advantages including speed of construction, flexibility and durability, use of local readily-available soils rather than imported quarry product, and cost effectiveness. More recently, innovative dual-function geosynthetics that combine both reinforcement and drainage functions have been developed (Kempton et al., 2000; Bergado et al., 2002; Lorenzo et al., 2004; Zornberg and Kang, 2005), which can facilitate the use of marginal fill in the construction of reinforced-earth structures. Marginal fill is defined as predominantly granular material that includes high silt and/or clay fractions (more than 15% by dry weight passing the 0.063-mm sieve) and often has high water content, with typically only 90–95% of its maximum dry density achieved under standard Proctor compaction. Dual function geosynthetics included in the earth structures provide reinforcement and preferential drainage channels, thereby increasing the factor of safety against slope instability.

The use of geosynthetics requires a proper understanding of the soil–geosynthetic interaction mechanisms. Utilizing marginal fill would involve considerable savings (Lorenzo et al., 2004) on condition that the intended engineering purpose can be achieved. However, most of the previous research has studied the interaction parameters (pull-out resistance and shear stress–strain characteristics) between geosynthetics and granular soils. Few studies have been carried out in relation to the interaction parameters between cohesive soils and geosynthetics (Bergado et al., 1991; Nagahara et al., 2004; Almohd et al., 2006; Long et al., 2007). For example, the angle of interface friction value for conventional geogrids is lower than the angle of shearing resistance of the surrounding soil and this must be considered in analysing the factor of safety on slope instability where potential slip surfaces can align with the soil–geosynthetic interface. This paper presents a laboratory study of the short-term interface shear resistance (τs−g generally critical case) achieved for using a novel dual-function geogrid in the construction of earth embankments using wet cohesive fill.

Section snippets

Test soil

The test soil was Brown Dublin Boulder clay (Skipper et al., 2005; Long and Menkiti, 2007); a gravely clay of low plasticity (typical liquid limit of 31%; plastic limit of 16% and plasticity index of 15%). The test material had a natural water content value of about 11% and a specific gravity of solids value of 2.70. Standard Proctor compaction tests indicated a maximum dry density of 1.84 tonne/m3 achieved at an optimum water content for compaction value of 13.0%.

Geogrids

The novel geogrid (Paradrain™)

Test programme

Consolidated undrained (CU) shearbox tests were conducted using the large shearbox (300×300 mm2 in plan and 150 mm in depth) in accordance with ASTM D5321 (2002) to measure the development of the shear resistance under medium to high applied normal stresses. The CU shearbox tests simulated in the geotechnical laboratory, the sequence whereby the fill material is placed and compacted in stages onsite, with consolidation occurring during the intervening periods. The test programme included:

  • Five

Experimental results and analysis

The shearbox results were analysed in terms of the total stress condition since the value of the pore pressure during shearing, particularly in the case of the conventional geogrid, was unknown. The shear resistance for all of the interface combinations was found to increase in value with increasing applied stress due to drainage to the pore-air voids, and hence dissipation of the excess pore pressures. Fig. 4, Fig. 5 show the mobilized shear resistance versus shear displacement for the

Discussion

The novel geogrid performed considerably better than the conventional geogrid for the marginal cohesive material tested. The experimental results of this and other studies (Kempton et al., 2000; Zornberg and Kang, 2005) have shown that the undrained shear strength (τs−g) mobilized along the interface is between 20% and 30% greater for the novel geogrid than for conventional geogrids with similar tensile strength properties. The excess pore water pressures generated in the vicinity of the

Summary and conclusions

The enhancement in the short-term interface shear strength achieved by a novel geogrid, which combines both reinforcement and in-plane drainage functions, was studied. The test soil was low-plasticity gravely clay that had been compacted to less than 95% of its maximum dry density achieved under standard Proctor compaction and at a water content value that exceeded the optimum water content for compaction by 3.5%.

The interface shear resistance (τs−g) values mobilized for the novel geogrid were

Acknowledgements

The authors would like to acknowledge the work of Martin Carney, John Kenna and Paul Creaven in performing the tests at the Geotechnical Laboratories, Trinity College Dublin. The paper was written by the first author while on sabbatical leave at the Urban Institute Ireland, University College Dublin.

References (17)

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