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K. W. Lo

Researcher at National University of Singapore

Publications -  15
Citations -  372

K. W. Lo is an academic researcher from National University of Singapore. The author has contributed to research in topics: Plane stress & Fracture mechanics. The author has an hindex of 8, co-authored 15 publications receiving 333 citations.

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Tension Crack Development in Soils

TL;DR: In this article, a model for finite-element modeling of tension crack propagation in soils is proposed, based on the splitting of a single node into two distinct nodes in the wake of an advancing crack tip to replicate separation of material on either side of the crack.
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Steady‐State Vibration of Subway‐Soil‐Building System

TL;DR: In this paper, the steady state vibration of a subway-soil-building system is determined using an appropriate finite element model using two different track support systems: direct fixation and a floating slab.
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Groundborne vibrations due to trains in tunnels

TL;DR: In this paper, an analytical procedure for determining groundborne vibrations in buildings due to subway trains is presented, which involves a finite element idealization of the subway-soil-structure interaction problem, using an analytical model for the train loading spectrum at the tunnel invert.
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Unified Approach to Ground Improvement by Heavy Tamping

TL;DR: In this paper, a review of heavy tamping projects indicated that highly organic clays which due to their secondary compression characteristics may not be amenable to treatment by surcharge and vertical drain installation alone, may nevertheless be stabilized by applying high energy impact on installed dynamic replacement (DR) sand columns using a conventional dynamic consolidation plant.
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Performance of a Three-Dimensional Hvorslev–Modified Cam Clay Model for Overconsolidated Clay

TL;DR: In this paper, a novel biaxial device has been developed to conduct the plane strain tests and the experimental results were used to formulate Hvorslev-MCC model which has MCC features in the subcritical region and HVorslev surface in the supercritical region.