Frame-like actions for massless mixed-symmetry fields in Minkowski space. Fermions

A frame-like action for massless mixed-symmetry fermionic fields in Minkowski space is constructed. The action is uniquely determined by gauge invariance.     

Mass Number Dependence of the Forward Production of Charged Hadrons and Nuclear Fragments in Carbon–Lead and Carbon–Carbon Interaction at a Beam Energy of 19.6 GeV per Nucleon

Physics of Atomic Nuclei - The inclusive differential cross sections for the production of $$\pi^{\pm}$$ and $$k^{-}$$ mesons, protons, and antiprotons with momenta between 6 and 50 GeV/c and...     

Hydrosilylation of Allyl Ethers in the Presence of Supported Sulfur-Containing Platinum(II) Complexes

Hydrosilylation of allyl ethyl, allyl butyl, allyl glycidyl, allyl benzyl, and allyl phenyl ethers by 1,1,3,3-tetramethyldisiloxane in the presence of supported sulfur-containing platinum(II) complexes with the general formula [{SiO₂}O_2Si(Me)(CH₂)₃SR]₂PtCl₂ (R = Bu, Hex, Bn; {SiO₂} is silica surface) and side processes have been studied.     

Standard enthalpies of formation for crystalline serine and isoserine and products of their dissociation in aqueous solutions

The heats of solution of crystalline serine and isoserine in water and potassium hydroxide solutions are measured via direct calorimetry at 298.15 K. The standard enthalpies of formations of amino acids and products of their dissociation in aqueous solution are calculated.     

Water Loss and Deformation of an Argillaceous Stratum During Well Operation in an Aquifer

The axisymmetric problem of flow through a porous medium to a well and deformation in a system consisting of rocks, a saturated argillaceous stratum, and an aquifer is investigated. An integrodifferential equation describing the evolution of the pressure field in the aquifer is obtained with allowance for fluid crossflow from the stratum. The crossflow distributions and the ground surface subsidence at various instants of time are found. The limiting subsidence is expressed in closed form. It is shown that over a fairly long time the well production rate is almost completely ensured by water loss from the clay.