Geotechnical Investigation for Slab Settlement: Causes and Mitigation

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GEOLOGIST||ENGINEERING GEOLOGIST||HYDROGEOLOGIST||EXPLORATION GEOLOGIST||RESEARCH GEOLOGIST||ENTREPRENEUR||NATURE ENTHUSIAST "The Enemy of Progress is Perfection"

Geotechnical Investigation for Slab Settlement A geotechnical investigation was undertaken to evaluate the causes of settlement and failure of the concrete slab, approximately 10 metres from the sea. The slab is 0.5m thick and underlain by 1.0m of backfill material, which has been observed to be porous and weakly compacted. Distress has been recorded in the form of sinking and cracking, necessitating a detailed understanding of subsurface conditions and the proposal of suitable mitigation measures to ensure long-term slab stability. Drilling and Sampling Procedures: The investigation included drilling fifteen boreholes to depths of 15 metres, with two additional boreholes extended to 40 metres for profiling the deeper subsurface. Drilling was executed using rotary techniques to recover both disturbed and representative samples for laboratory testing. Disturbed samples were used for classification and index property analysis, while representative samples enabled determination of soil strength and compressibility. In Situ Testing: To characterize the soils in their natural condition, Standard Penetration Tests (SPT) were carried out at 1.5 metre intervals within the boreholes. SPT provided N-values used to assess relative density, shear strength, and stiffness of the soils encountered. Samples retrieved during SPT were correlated with blow counts to refine soil classification and engineering interpretation. An Electrical Resistivity Tomography (ERT) survey was also undertaken to delineate variability in soil stratigraphy and to highlight groundwater influence beneath the slab. Subsurface Conditions: The stratigraphy is dominated by loose to medium dense sands intercalated with silty and clayey horizons and layers of completely to highly weathered sandstone. Marine sands are prevalent, highly pervious, and directly influenced by tidal fluctuations. The shallow groundwater table enhances washout and erosion of fines. The backfill immediately beneath the slab was particularly porous and uncompacted, creating preferential seepage paths and voids. Problem Diagnosis and Mitigation: Slab failure is attributed to uncontrolled backfill, groundwater ingress, and compressible marine sands. To mitigate, systematic grouting is proposed beneath the slab to depths of about 1.0m. Cementitious grouts will fill voids and seal the porous backfill, while microfine or chemical grouts will permeate finer sandy horizons. Compaction grouting may be applied to densify loose layers, and localized soil replacement with engineered fill can be considered. Improved drainage will further reduce tidal groundwater impact. Should settlement persist, micropiles may be installed to transfer loads to deeper sandstone strata.

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Lawrence oode

GEOTECHNICAL INVESTIGATION at GEORAMA Es Ltd

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