000 03234nam a22005415i 4500
001 978-3-540-36354-5
003 DE-He213
005 20140220083740.0
007 cr nn 008mamaa
008 110101s2011 gw | s |||| 0|eng d
020 _a9783540363545
_9978-3-540-36354-5
024 7 _a10.1007/978-3-540-36354-5
_2doi
050 4 _aTA703-705.4
050 4 _aTA775-787
050 4 _aTC1-1800
072 7 _aRBP
_2bicssc
072 7 _aRBGK
_2bicssc
072 7 _aSCI042000
_2bisacsh
082 0 4 _a624.15
_223
100 1 _aGudehus, Gerd.
_eauthor.
245 1 0 _aPhysical Soil Mechanics
_h[electronic resource] /
_cby Gerd Gudehus.
264 1 _aBerlin, Heidelberg :
_bSpringer Berlin Heidelberg,
_c2011.
300 _aXIII, 840p. 1000 illus.
_bonline resource.
336 _atext
_btxt
_2rdacontent
337 _acomputer
_bc
_2rdamedia
338 _aonline resource
_bcr
_2rdacarrier
347 _atext file
_bPDF
_2rda
490 1 _aAdvances in Geophysical and Environmental Mechanics and Mathematics,
_x1866-8348
505 0 _aPrologue -- introduction -- simple psammoids -- simple peloids -- psammoids with reversals -- peloids with reversals -- pore fluid -- bridging gaps -- localization -- fabric -- boundary conditions -- one-dimensional evolutions -- plane-parallel evolutions without ssi -- plane-parallel evolutions with ssi -- axi-symmetric evolutions -- less symmetric evolutions -- critical phenomena -- epilogue -- references -- symbols and acronyms.
520 _aSoil is matter in its own right. Its nature can be captured by means of monotonous, cyclic and strange attractors. Thus material properties are defined by the asymptotic response of sand- and clay-like samples to imposed deformations and stresses. This serves to validate and calibrate elastoplastic and hypoplastic relations with comparative plots. Extensions capture thermal and seismic activations, limitations occur due to localizations and skeleton decay.Attractors in the large characterize boundary value problems from model tests via geotechnical operations up to tectonic evolutions. Validations of hypoplastic calculations are shown with many examples, possible further applications are indicated in detail. This approach is energetically justified and limited by critical points where the otherwise legitimate continuity gets lost by localization and decay. You will be fascinated by the fourth element although or just as it is so manifold.
650 0 _aEngineering.
650 0 _aPhysical geography.
650 0 _aEngineering geology.
650 0 _aHydraulic engineering.
650 1 4 _aEngineering.
650 2 4 _aGeoengineering, Foundations, Hydraulics.
650 2 4 _aEngineering, general.
650 2 4 _aGeotechnical Engineering.
650 2 4 _aGeophysics/Geodesy.
650 2 4 _aSoft and Granular Matter, Complex Fluids and Microfluidics.
710 2 _aSpringerLink (Online service)
773 0 _tSpringer eBooks
776 0 8 _iPrinted edition:
_z9783540363538
830 0 _aAdvances in Geophysical and Environmental Mechanics and Mathematics,
_x1866-8348
856 4 0 _uhttp://dx.doi.org/10.1007/978-3-540-36354-5
912 _aZDB-2-EES
999 _c106639
_d106639