Titlebook: Optimal Control Problems Related to the Robinson–Solow–Srinivasan Model; Alexander J. Zaslavski Book 2021 The Editor(s) (if applicable) an

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Alexander J. Zaslavskiep-like coseismic changes?in the near field. A new mechanism has emerged that suggests that coseismic release of pore water from unsaturated soils may also cause step-like increases of water level. Laboratory experiments show that both ?the?undrained?consolidation and the?release of water from unsat

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the seismic waves, where the current results from the field and laboratory studies are in conflict. Finally, while in most cases the liquefied sediments are sand or silty sand, well-graded gravel has increasingly been witnessed to liquefy during earthquakes and is not simply the result of entrainmen

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