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These values were all calculated by Method II.
Left: aS0 calculated by Method II (data [73],[73]).
From 250 to 400 m, aS0 was calculated by Method II using data from an April 2007 cruise [66]; salinity = 36.3 and T = 17.5°C.
Similarly, ΣS0 calculated by Method I ranges from 166 down to 22 μM, compared to actual values from 11 to 4 μM determined by three independent analytical methods.
The concentrations of S42−, S52−, S62− and S72− calculated by Method II using chloroform extraction and cyanolysis data for ΣS0 are uniformly below 0.01 μM whereas actual values measured by methyl triflate derivatization are more than 10-fold higher.
As shown in Additional file 1: Table S-3 (and more extensively in [52]), ΣS0 measured by alternate methods varies by nearly 4-fold, giving rise to a similar range in most of the concentrations calculated by Method II.
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Non-forest biomass in the FIA dataset was calculated by methods described in [28].
It was not long before Avogadro's number could be calculated by methods not closely tied to the kinetic theory of gases.
Non-forest biomass in the FIA dataset was calculated by methods described in [ 28 ].
Total leisure-time physical activity (hours/day) was calculated by methods previously described (4).
Partial charges were calculated by Gasteiger method.
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