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relevant micro-concepts of common nigerian civil engineering

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vii)viii)Construction material in caisson foundations and land reclamation schemes as well asdredging and other works.Construction material for buildings <strong>of</strong> mud, compressed earth and burned bricks/firedclay.In all theoretical and practical applications <strong>of</strong> soil, the fundamental considerations and principlesare aimed at assessing the strength (shear) and consolidation/compressibility characteristics <strong>of</strong>the material. It is interesting to have known that when the twin world trade centre towers <strong>of</strong> 110storeys (411.5 metres) collapsed following the terrorist attacks <strong>of</strong> September 11, 2001, thesubstructure supported by the soil was quoted to be undamaged. Indeed the soil has atremendous capacity to take impacts from crushes <strong>of</strong> explosives, plane crashes, shuttle machinesand, <strong>of</strong> course, the world’s structures <strong>of</strong> all sizes and heights. The soil takes the loads imposedby these situations quite comfortably: frequently it does so with very prominent and noticeabledeformations and settlements depending on the material plasticity. Because the strength andconsolidation characteristics <strong>of</strong> the soils are so influential, I have found it convenient to classifythe theorems and principles associated to these properties (i.e. shear and settlement) as macro<strong>concepts</strong>.However, there are certain <strong>micro</strong>-<strong>concepts</strong> related to the behaviour and response <strong>of</strong> thesoils to loading conditions that affect their strengths tremendously but which we frequentlyeasily overlook. One <strong>of</strong> these <strong>micro</strong>-<strong>concepts</strong> deals with the influence <strong>of</strong> water within the voidspaces <strong>of</strong> the soils. The concept is easily explained by the piston and spring analogy.A load (stress), σ is applied on the piston. The loads taken by the spring and water are σ / and u,respectively. At the beginning, as long as the weep hole is closed, σ = 0 and σ = u; i.e. the wholeload is taken up by the water. When the weep hole is opened gradually, stress is transferred fromthe water to the spring so that σ / > 0 so that at any finite time, t, σ = σ / + u and at t = ∞, u = 0 andσ = σ / .9

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