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1.5.1 Charity fraction. 1.5.2 Property tax. 1.6 Quantile. ... the cost per mille is the rate per £1000 of insured value. ... Per-unit system; Percentile;
For example, in a solution with a 1:5 dilution ratio, entails combining 1 unit volume of solute (the material to be diluted) with 5 unit volumes of the solvent to give 6 total units of total volume. In photographic development, dilutions are normally given in a '1+x' format.
[1] [2] Fractions are collected based on differences in a specific property of the individual components. A common trait in fractionations is the need to find an optimum between the amount of fractions collected and the desired purity in each fraction. Fractionation makes it possible to isolate more than two components in a mixture in a single run.
This was an official unit of measurement in South Africa until the 1970s, and was defined in November 2007 by the South African Law Society as having a conversion factor of 1 morgen = 0.856 532 hectares. [28] This unit of measure was also used in the Dutch colonial province of New Netherland (later New York and parts of New England). [29] [30]
When a real number like .007 is denoted alternatively by 7.0 × 10 —3 then it is said that the number is represented in scientific notation.More generally, to write a number in the form a × 10 b, where 1 <= a < 10 and b is an integer, is to express it in scientific notation, and a is called the significand or the mantissa, and b is its exponent. [3]
The Stoß is a unit of cattle stock density used in the Alps. For each Alm or Alp it is worked out how many Stoß (Swiss: Stössen) can be grazed (bestoßen); one cow equals one Stoß, 3 bulls equal 2 Stöße, a calf is 1 ⁄ 4 Stoß, a horse of 1, 2 or 3 years old is worth 1, 2 or 3 Stöße, a pig equals 1 ⁄ 4, a goat or a sheep is 1 ⁄ 5 ...
Porosity or void fraction is a measure of the void (i.e. "empty") spaces in a material, and is a fraction of the volume of voids over the total volume, between 0 and 1, or as a percentage between 0% and 100%.
i.e., crystallization takes a time that decreases as one over the one-quarter power of the nucleation rate per unit volume, ˙, and one over the three-quarters power of the growth velocity ˙. Typical crystallites grow for some fraction of the crystallization time t X {\displaystyle t_{X}} and so have a linear dimension G ˙ t X {\displaystyle ...
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