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Not AvailableTHE PAPER DEALS WITH A LABORATORY STUDY IN WHICH A SOIL AMELIORANT OF HYDROXY ALUMINIUM POLYMERS KNOWN AS HYDRAL , WAS TESTED TO IMPROVE SOME OF THE PHYSICAL PROPERTIES OF A HEAVY CLAY SOIL BELONGING TO GREY UPLAND SOIL GROUP. IN INDIA, SUCH SOILS KNOWN AS 'KABAR' AND 'MAR' ARE FOUND IN BUNDELKHAND REGION... THE ADDITION OF HYDRAL ( 0 TO 5% ON THE WEIGHT BASIS) TO THE SOIL RESULTED IN SIGNIFICANT DECREASE IN HARDNESS AND ADHESION . SIGNIFICANT INCREASE OF WATER PERMEABILITY WAS OBSERVED , ALTHOUGH THE EFFECT OF HYDRAL TREATMENT ON POROSITY WAS RATHER SLIGHT.Not Availabl

Coherent resonance stop bands in alternating gradient beam transport

An extensive experimental study is performed to confirm fundamental resonance bands of an intense hadron beam propagating through an alternating gradient linear transport channel. The present work focuses on the most common lattice geometry called “FODO” or “doublet” that consists of two quadrupoles of opposite polarities. The tabletop ion-trap system “S-POD” (Simulator of Particle Orbit Dynamics) developed at Hiroshima University is employed to clarify the parameter-dependence of coherent beam instability. S-POD can provide a non-neutral plasma physically equivalent to a charged-particle beam in a periodic focusing potential. In contrast with conventional experimental approaches relying on large-scale machines, it is straightforward in S-POD to control the doublet geometry characterized by the quadrupole filling factor and drift-space ratio. We verify that the resonance feature does not essentially change depending on these geometric factors. A few clear stop bands of low-order resonances always appear in the same pattern as previously found with the sinusoidal focusing model. All stop bands become widened and shift to the higher-tune side as the beam density is increased. In the space-charge-dominated regime, the most dangerous stop band is located at the bare betatron phase advance slightly above 90 degrees. Experimental data from S-POD suggest that this severe resonance is driven mainly by the linear self-field potential rather than by nonlinear external imperfections and, therefore, unavoidable at high beam density. The instability of the third-order coherent mode generates relatively weak but noticeable stop bands near the phase advances of 60 and 120 degrees. The latter sextupole stop band is considerably enhanced by lattice imperfections. In a strongly asymmetric focusing channel, extra attention may have to be paid to some coupling resonance lines induced by the Coulomb potential. Our interpretations of experimental data are supported by theoretical predictions and systematic multiparticle simulations

Response and stability of underground structures in rock mass during earthquakes

Underground structures are well known to be earthquake resistant. However, the recent earthquakes showed that underground structures are also vulnerable to seismic damage. There may be several reasons such as high ground motions and permanent ground movements. This study attempts to describe various forms of damage to underground structures such as tunnels, caverns, natural caves and abandoned mines during major earthquakes. Results of various model tests on shaking table are also presented to show the effect of ground shaking on the response and collapse of underground structures in continuum and discontinuum. Furthermore, some empirical equations are proposed to assess the damage to underground structures, which may be useful for quick assessments of possible damage. © 2010 Springer-Verlag

Earthquakes as a rock dynami problem and their effects on rock engineering structures

An earthquake is an instability problem of the Earth’s crust and it is a subject of geoscience and geo-engineering. An earthquake is caused by varying crustal stresses and it is a product of rock fracturing and/or slippage of major discontinuities such as faults and fracture zones. © 2012 by Taylor & Francis Group, LLC

Earthquakes as a rock dynami problem and their effects on rock engineering structures

An earthquake is an instability problem of the Earth’s crust and it is a subject of geoscience and geo-engineering. An earthquake is caused by varying crustal stresses and it is a product of rock fracturing and/or slippage of major discontinuities such as faults and fracture zones. © 2012 by Taylor & Francis Group, LLC