By Malcolm Bolton (auth.)
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Extra resources for A Guide to Soil Mechanics
Does a variation in the level of a lake affect the compression of the mud at the bottom of it? 1 Origins Soils and rocks are the naturally occurring fabric of our planet. The individual crystal grains within a beach pebble may have witnessed each of the countless cycles in the 4 500 000 million year drama which has been the unfolding of Earth's history: cycles of mountain building, followed by erosion, transportation of the rock fragments by wind and water, sedimentation, cementation, compression and subsequent upthrust in a later collision of land-masses.
Metamorphic rocks are those whose nature has been altered as a result of the local application of pressure or heat. Soil mechanics concerns itself with sedimentary materials, in particular with those that are not yet cemented, nor very greatly compressed. Soil to the engineer implies any uncemented and badly fitting accumulation of mineral fragments of various size, shape and composition with an appreciable percentage of interconnecting voids. The parallel discipline of rock mechanics, on the other hand, is concerned with intact blocks of a cemented, compressed or crystalline nature, separated by joints and fissures: the blocks themselves may or may not be porous, but the mechanics of the whole assemblage is dominated by the disposition of the joints in the same way as in a child's tower made of wooden blocks.
6) Three flow channels were decided on, and sketched in, starting from the quite uniform EDC region. (7) Starting at ED, equipotentials were sketched in so as to form squares, remembering that boundaries DC, EF and FG were flowlines. Both equipotentials and flowlines were then extended to cover the whole region with square figures of growing size. (8) A rubber can be used to eliminate mistakes, which in this case centred around C and G, and a fair flownet is produced within about half an hour.
A Guide to Soil Mechanics by Malcolm Bolton (auth.)