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m^^iz$$m&'f - HKU Libraries - The University of Hong Kong

m^^iz$$m&'f - HKU Libraries - The University of Hong Kong

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<strong>The</strong> steep terrain and thin weathered mantle may make many areas <strong>of</strong> volcanic rock unsuitable forintensive development. Large volumes <strong>of</strong> excavation, much <strong>of</strong> it requiring blasting, would be necessary forsite formation, and the resulting slopes may be subject to joint-controlled instability. However, where theserocks occur on flat to gently sloping terrain, their foundation depths are fairly shallow. Recent developmentson Tsing Yi Island have been carried out partly in coarse tuff and shallow stripping depths have beenencountered.Site investigations in the volcanic rocks should be designed to determine the depth and degree <strong>of</strong>weathering, the frequency and orientation <strong>of</strong> jointing and the position and seasonal fluctuations <strong>of</strong> the watertable. <strong>The</strong> Standard Penetration Test can be a useful indicator <strong>of</strong> the depth <strong>of</strong> successive zones <strong>of</strong>decomposition <strong>of</strong> the rock mass. Direct shear tests on the discontinuities <strong>of</strong> Zone C/D rocks, and direct shearand triaxial tests on Zone A/B rocks, can be used to determine the shear strengths <strong>of</strong> joints and soil matrix. Itshould be noted that, because most failures <strong>of</strong> insstu material are shallow, the overburden pressure on a failureplane is probably quite low. Representative shear strength parameters should therefore be obtained fromlaboratory triaxial tests carried out at appropriately low confining pressures.3.1H Characteristics <strong>of</strong> the Metamorphic RocksVery Sittle is known about these rocks within the study area. Dark metamorphosed sulphurous shales andquartzites occur <strong>of</strong>fshore in an area planned for reclamation. <strong>The</strong>se rocks are deeply weathered and occurbeneath, up to 40 m <strong>of</strong> marine deposits and old alluvium. <strong>The</strong>y decompose to a very dense clayey silt that hasSPT values ranging from 20 up to 120. <strong>The</strong> upper value indicates that driven piles may terminate within it.It should be noted that the sulphur derived from pyrites may produce an acid groundwater that could reactwith steel piles or concrete. Chemical analysis <strong>of</strong> the groundwater may indicate the nature and extent <strong>of</strong> thispotential problem.34

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