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The Al-Yahudu tablets are a collection of about 200 clay tablets from the sixth and fifth centuries BCE on the exiled Judean community in Babylonia following the destruction of the First Temple. [ 1 ] [ 2 ] [ 3 ] They contain information on the physical condition of the exiles from Judah and their financial condition in Babylon . [ 4 ]
There is no clear relationship between the size of soil mineral components and their mineralogical nature: sand and silt particles can be calcareous as well as siliceous, [18] while textural clay (0.002 mm (7.9 × 10 −5 in)) can be made of very fine quartz particles as well as of multi-layered secondary minerals. [19]
That is, the distance between two neighboring iodides in the crystal is assumed to be twice the radius of the iodide ion, which was deduced to be 214 pm. This value can be used to determine other radii. For example, the inter-ionic distance in RbI is 356 pm, giving 142 pm for the ionic radius of Rb +. In this way values for the radii of 8 ions ...
The probability to find a particle at the distance from the origin between and + is (/), plus we have kinds of way to choose which particle, while the probability to find a particle outside that sphere is /. The sought-for expression is then
Radius of gyration (in polymer science)(, unit: nm or SI unit: m): For a macromolecule composed of mass elements, of masses , =1,2,…,, located at fixed distances from the centre of mass, the radius of gyration is the square-root of the mass average of over all mass elements, i.e.,
Badenhorst was born in Pietermaritzburg in the then Natal Province on 6 December 1967. He was one of four children. Badenhorst completed high school at Hoërskool Waterkloof, Pretoria, in 1985 and subsequently went to work for the South African Government Printing Works.
The average distance between points inside a disk of radius r is [10] 128 45 π r ≈ 0.905414787 … r . {\displaystyle {\frac {128}{45\pi }}r\approx 0.905414787\ldots r.} The values for a half disk and quarter disk are also known.
The geodesic distance between opposite umbilical points is the same regardless of the initial direction of the geodesic. Whereas the closed geodesics on the ellipses X = 0 and Z = 0 are stable (a geodesic initially close to and nearly parallel to the ellipse remains close to the ellipse), the closed geodesic on the ellipse Y = 0 , which goes ...