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When a number is converted into normalized scientific notation, it is scaled down to a number between 1 and 10. All of the significant digits remain, but the placeholding zeroes are no longer required. Thus 1 230 400 would become 1.2304 × 10 6 if it had five significant digits.
One for the transfer of unfolded chains into octanol, which is relevant to the hydrocarbon core of a bilayer. The Stephen H. White website [ 34 ] provides an example of whole residue hydrophobicity scales showing the free energy of transfer ΔG(kcal/mol) from water to POPC interface and to n-octanol. [ 34 ]
In the discrete case, the diversion ratio is naturally interpreted as the fraction of product j demand which treats product i as a second choice, [10] [11] measuring how much of the demand diverting from product j because of a price increase is diverted to product i can be written as the product of the ratio of the cross-elasticity to the own ...
The partitioning of a substance into a solid results in a solid solution. Partition coefficients can be measured experimentally in various ways (by shake-flask, HPLC, etc.) or estimated by calculation based on a variety of methods (fragment-based, atom-based, etc.).
Other measures of the angle used in computing may be based on dividing one whole turn into 2 n equal parts for other values of n. [24] It is 1 / 256 of a turn. [23] π radian: 2: 180° The multiples of π radians (MUL π) unit is implemented in the RPN scientific calculator WP 43S. [25] See also: IEEE 754 recommended operations ...
Density (volumetric mass density or specific mass) is a substance's mass per unit of volume.The symbol most often used for density is ρ (the lower case Greek letter rho), although the Latin letter D can also be used.
Given Enceladus's relatively high rock–mass fraction, the proposed enhancement in 26 Al and 60 Fe would result in a differentiated body, with an icy mantle and a rocky core. [ 89 ] [ 91 ] Subsequent radioactive and tidal heating would raise the temperature of the core to 1,000 K, enough to melt the inner mantle.
The Bond albedo (also called spheric albedo, planetary albedo, and bolometric albedo), named after the American astronomer George Phillips Bond (1825–1865), who originally proposed it, is the fraction of power in the total electromagnetic radiation incident on an astronomical body that is scattered back out into space.