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The gram (10 −3 kg) is an SI derived unit of mass. However, the names of all SI mass units are based on gram, rather than on kilogram; thus 10 3 kg is a megagram (10 6 g), not a *kilokilogram. The tonne (t) is an SI-compatible unit of mass equal to a megagram (Mg), or 10 3 kg.
Mass; system unit unit-code symbol or abbrev. notes sample default conversion combinations SI: kilogram: kg kg 1.0 kg (2.2 lb) kg lb. kg lb st; kg st. kg st lb; gram: g g 1.0 g (0.035 oz) g oz; milligram: mg mg 1.0 mg (0.015 gr) mg gr; microgram: μg (ug or mcg) μg 1.0 μg (1.5 × 10 −5 gr) non-SI metric: tonne: t t 1.0 t (0.98 long tons; 1. ...
The scale is a value or expression that is used as a factor to convert a value to its corresponding base unit. Commas may be used as a thousand separator (e.g. 1,000,000 ) or e notation may be used (e.g. 1e6 ).
Pressure due to direct impact of a strong breeze (~28 mph or 45 km/h) [27] [28] [31] 120 Pa Pressure from the weight of a U.S. quarter lying flat [32] [33] 133 Pa 1 torr ≈ 1 mmHg [34] ±200 Pa ~140 dB: Threshold of pain pressure level for sound where prolonged exposure may lead to hearing loss [citation needed] ±300 Pa ±0.043 psi
For example, the conversion factor between a mass fraction of 1 ppb and a mole fraction of 1 ppb is about 4.7 for the greenhouse gas CFC-11 in air (Molar mass of CFC-11 / Mean molar mass of air = 137.368 / 28.97 = 4.74). For volume fraction, the suffix "V" or "v" is sometimes appended to the parts-per notation (e.g. ppmV, ppbv, pptv).
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Atmospheric pollutant concentrations expressed as mass per unit volume of atmospheric air (e.g., mg/m 3, μg/m 3, etc.) at sea level will decrease with increasing altitude because the atmospheric pressure decreases with increasing altitude. The change of atmospheric pressure with altitude can be obtained from this equation: [2]
In Earth's atmosphere, the pressure at sea level P 0 averages about 1.01 × 10 5 Pa, the mean molecular mass of dry air is 28.964 Da, and hence m = 28.964 Da × 1.660 × 10 −27 kg/Da = 4.808 × 10 −26 kg. As a function of temperature, the scale height of Earth's atmosphere is therefore H/T = k/mg = 1.381 × 10 −23 J⋅K −1 / (4.808 × ...