Land surface in gravity points classification by a complete system of curvatures

A general theory of land surface in a gravitational field is being developed. The four classes of topographic variables are defined: local (class A) and global (class B) that have no sense without gravity, and local (class C) and global (class D) which are gravity invariant. A complete system of curvatures is introduced for a general situation of nonuniform gravity. The curvatures refer to classes A and C, the latter being subject of the differential geometry of surfaces, the former being subject of this work in a special section of mathematics concerned with surfaces in a vector field. The svstem of curvatures consists of 7 known ones of the classes A and C and 5 new curvatures of the class A (difference, horizontal excess, vertical excess, total ring, and total accumulation curvatures). Seven new theorems show in which way curvatures can reflect landforms and their ability to influence substance flows, and the relationship between them. Land surface in gravity-points classification is constructed based on signs of curvatures, which includes known curvature-based classifications as partial situations, and 12 main types (from total 48) are shown to form open subsets of the surface with equal probability to meet them for the land surface as indicated by a new statistical hypothesis. A central-point method for local variables calculation in uniform gravity approximation is described for a computer Digital Elevation Models treatment.

[1]  Jozef Krcho,et al.  Morphometric analysis of relief on the basis of geometric aspect of field theory , 1973 .

[2]  S. K. Jenson,et al.  Extracting topographic structure from digital elevation data for geographic information-system analysis , 1988 .

[3]  A. Sard,et al.  The measure of the critical values of differentiable maps , 1942 .

[4]  I. Evans Statistical Characterization of Altitude Matrices by Computer. Report 6. An Integrated System of Terrain Analysis and Slope Mapping. , 1979 .

[5]  Dan Pennock,et al.  Landform classification and soil distribution in hummocky terrain , 1987 .

[6]  Keith C. Clarke,et al.  Scale-Based Simulation of Topographic Relief , 1988 .

[7]  P. V. Sharma,et al.  Geophysical Methods in Geology , 1942, Nature.

[8]  A. R. Aandahl,et al.  The Characterization of Slope Positions and Their Influence on the Total Nitrogen Content of a Few Virgin Soils of Western Iowa , 1949 .

[9]  T. A. Elkins The second derivative method of gravity interpretation , 1951 .

[10]  L. Martz,et al.  CATCH: a FORTRAN program for measuring catchment area from digital elevation models , 1988 .

[11]  Carl Friedrich Gauss Disquisitiones generales circa superficies curvas , 1981 .

[12]  B. Mandelbrot How Long Is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension , 1967, Science.

[13]  F. R. Troeh,et al.  Landform Parameters Correlated to Soil Drainage 1 , 1964 .

[14]  M. B. Dobrin Introduction to Geophysical Prospecting , 1976 .

[15]  Robert Finn,et al.  Equilibrium Capillary Surfaces , 1985 .