The influence of earthworks construction on porewater pressures in clays and mudstones of the Lias Group

Author:

Briggs Kevin M.1ORCID,Trinidad González Yuderka2ORCID,Meijer Gerrit J.3ORCID,Ridley Andrew4,Powrie William1ORCID,Butler Simon5,Sartain Nick5

Affiliation:

1. Faculty of Engineering and the Environment, University of Southampton, University Road, Highfield, Southampton SO17 1BJ, UK

2. Department of Civil, Construction, and Environmental Engineering, Iowa State University, Town Engineering Building, 394 Town Engineering, Ames, IA 50011, USA

3. Department of Architecture and Civil Engineering, University of Bath, Bath BA2 7AY, UK

4. Geotechnical Observations Ltd, 9 Avro Way, Brooklands, Weybridge KT13 0YF, UK

5. High Speed Two (HS2) Ltd, Two Snowhill, Snow Hill Queensway, Birmingham B4 6GA, UK

Abstract

Monitoring the changes in porewater pressure associated with the construction of earthworks can yield information on the stiffness and permeability of the ground, as well as how the natural groundwater regime might be impacted. This paper presents 3 years of porewater pressure measurements in weathered Lias Group mudstone, obtained from a trial cutting and a trial embankment constructed for the UK's High Speed Two (HS2) railway. The immediate changes in porewater pressure were small in relation to the changes in total stress imposed. This can be explained by the consolidation or swelling during the period of construction, combined with the sensitivity of very stiff clays and mudstones to a very small (0.5%) reduction in the degree of saturation. In the longer term, porewater pressures reduced across the site owing to the reduction in ground level at the trial cutting. Rates of porewater pressure change were accelerated by more permeable limestone within the ground profile reducing drainage path lengths. It was concluded that construction-induced porewater pressure changes may be smaller, and their rate of dissipation more rapid, in weathered clays and mudstones such as those of the Lias Group than in younger, more compressible clay deposits.

Funder

Engineering and Physical Sciences Research Council

Royal Academy of Engineering

Publisher

Geological Society of London

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