The behaviour of a low-to-medium density chalk under a wide range of pressure conditions

Tingfa Liu, Pedro M. V. Ferreira, Ken Vinck*, Matthew R. Coop, Richard J. Jardine, Stavroula Kontoe

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

9 Citations (Scopus)
45 Downloads (Pure)

Abstract

Experiments are described which provided the basis for advanced numerical modelling of large-scale axial and lateral pile tests undertaken chalk to assist the design of offshore wind and other projects in northern Europe. The research explored the mechanical behaviour of chalk from a UK research site under effective cell pressures up to 12.8 MPa. When sheared from low confining pressures the chalk’s interparticle bonds contribute a large proportion of the peak deviator stresses available to specimens that crack, bifurcate and dilate markedly after failing at relatively small strains. Progressively more ductile behaviour is seen as pressures are raised, with failures being delayed until increasingly large strains and stable critical states are attained. Loading invokes very stiff responses within the chalk’s (Y1) linear elastic limits and behaviour remains stiff, although non-linear, up to large-scale (Y3) yield points. Near-elliptical Y1 and Y3 yield loci can be defined in q-p′ stress space and a critical state v-p′ curve is identified. The chalk’s initially bonded, high porosity, structure is explored by normalising the shearing and compression state paths with reference to both critical state and intrinsic compression lines. The results have important implications for pile test analysis and practical design in this challenging geomaterial.

Original languageEnglish
Article number101268
Number of pages16
JournalSoils and Foundations
Volume63
Issue number1
Early online date26 Dec 2022
DOIs
Publication statusPublished - 1 Feb 2023

Bibliographical note

Funding Information:
The joint study between Imperial College and University College London was supported by the ALPACA and APLACA Plus projects funded by the Engineering and Physical Science Research Council grant EP/P033091/1 held by Imperial College and University of Oxford (led by Professor Byron Byrne), with additional support from Atkins, Cathie Associates, Equinor, Fugro, Geotechnical Consulting Group (GCG), Iberdrola, Innogy, LEMS, Ørsted, Parkwind, Siemens and Vattenfall. Imperial College’s EPSRC Centre for Doctoral Training (CDT) in Sustainable Civil Engineering (EPSRC EP/L016826/1) and the DEME Group (Belgium) supported Ken Vinck’s doctoral study. Field sampling was conducted by Fugro and Socotec UK Ltd and invaluable technical support provided by Ben Boorman and Matt Wilkinson at University College London and Steve Ackerley, Graham Keefe, Prash Hirani, Stef Karapanagiotidis, Graham Nash, Gary Jones at Imperial College London.

Funding Information:
The joint study between Imperial College and University College London was supported by the ALPACA and APLACA Plus projects funded by the Engineering and Physical Science Research Council grant EP/P033091/1 held by Imperial College and University of Oxford (led by Professor Byron Byrne), with additional support from Atkins, Cathie Associates, Equinor, Fugro, Geotechnical Consulting Group (GCG), Iberdrola, Innogy, LEMS, Ørsted, Parkwind, Siemens and Vattenfall. Imperial College's EPSRC Centre for Doctoral Training (CDT) in Sustainable Civil Engineering (EPSRC EP/L016826/1) and the DEME Group (Belgium) supported Ken Vinck's doctoral study. Field sampling was conducted by Fugro and Socotec UK Ltd and invaluable technical support provided by Ben Boorman and Matt Wilkinson at University College London and Steve Ackerley, Graham Keefe, Prash Hirani, Stef Karapanagiotidis, Graham Nash, Gary Jones at Imperial College London.

Publisher Copyright:
© 2022

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