Tisza

Over the last two years the method has been used to examine more than 3,000 bolts on several bridges. The traditional method and the new one are compared with the help of the results of a measurement carried out on a bridge built over the Tisza 24 years ago. 

Luttinger-Tisza method is burdened by independent minimization variables, while analysis of the values of the Fourier components F k) makes it possible to immediately exclude no less than half of the variable set and to obtain a result much more quickly. Degeneracy of the ground state occurs either due to coincidence of minimal values of Vt (k) at two boundary points of the first Brillouin zone k = b]/2 and k = b2/2, or as a result of the equality Fj (k) = F2 (k) at the same point k = h/2. The natural consequence of the ground state degeneracy is the presence of a Goldstone mode in the spectrum of orientational vibrations.53... 

Let us present the ground state characteristics of dipoles (interacting as defined by Eq. (2.2.2)) on square, triangular, rectangular, and rhombic lattices. The ground state of a square dipole lattice was first determined by the Luttinger-Tisza method in... 

Lieb EH (1982) In Feshbach H, Shimony A (eds) Physics as natural philosophy Essays in honor of Laszlo Tisza on his 75th Birthday, MIT Press, Cambridge, MA, pill... 

E. H. Lieb, in Physics as Natural Philosophy Essays in Honor of Laszlo Tisza on His Seventy-Fifth Birthday, edited by A. Shimony and H. Fesh-bach (MIT, Cambridge, 1982), p. Ill revised as Int. J. Quantum Chem. 24, 243 (1983) and further extended in Ref. [II], p. 31. 

Department of Theoretical Physics, University of Szeged, Szeged, Hungary, H-6720 Tisza L. krt. 84-86... 

Tisza, S., Molnar-Perl, I., Friedman, M., Sass, P. (1996). Simultaneous capillary GC of acids and sugars as their silyl(oxime) derivatives Quantitation of chlorogenic acid, raffinose, and pectin substances. J. High Resolut. Chromatogr, 19, 54-58. 

This chapter deals with the thermodynamics of one-phase systems, and it is understood that the phase is homogeneous and at uniform temperature. The basic structure of thermodynamics provides the tools for the treatment of more complicated systems in later chapters. This book starts with the fundamentals of thermodynamics, but the reader really needs some prior experience with thermodynamics at the level of undergraduate thermodynamics (Silbey and Alberty, 2001). Legendre transforms play an important role in this chapter, and the best single reference on Legendre transforms is Callen (1960, 1985). Other useful references for basic thermodynamics are Tisza (1966), Beattie and Oppenheim (1979), Bailyn (1994), and Greiner, Neise, and Stocker (1995). 

Alkaloida Vegy, Gyar, Tisza-vasvari H. U. 304 Alkaysi, H. N. vgl. Smissman,... 

Tisza theorem states If the solution of equation 133 subject to the single weak constraint, equaiion 135, also satisfies the strong constraints of equation 134, then the solution of the simpler weak constraint problem is a rigorous solution of the strong constraint problem. With simple choices of the anv, it happens that rigorous solutions of many physically interesting problems can be solved. 

Mineral Composition of Soil Samples3 Collected Along River Tisza (Hungary)... 

The results of Table 3.14 show that there is a relation between the concentration of surface sites and composition (Table 3.12). The number of silanol sites is proportional to the sand content, except for freshly deposited alluvial soils with high primary silicate content (e.g., Tiszalok, Zahony). The sandy soils from wetland areas (soils near River Tisza) do not fit the usual tendencies that is, the concentrations of silanol and aluminol sites are significantly lower, as expected from similar data of other sandy soils. 

We have seen in this work that most of the regional Pleistocene sediments have yielded mammalian fossils originating from the Upper Pleistocene, i.e. the no. II terrace surfaces and the Upper Pleistocene loess. In addition, the upper layers (down to ca. 40-50 m) of the filling material of the Great Hungarian Plain—just like the swamp loess of the Tisza, or its bluish clay —have been found to contain fossils dated to the Lower Wiirm (Janossy and Voros, 1979). 

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