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The red circle reports the time of the most elevated HI values.
Each of the SIGNAL2 and SWAMPS scores are mapped linearly to HI values (Figure 1 and Table 1) and the MHI is equal to the geometric mean of the two HI values.
This suggests that a chemical-by-chemical approach would "catch" the mixture exposures with the largest HI values.
For these reasons, the WQHI is calculated from the geometric mean of the 'worst' three HI values.
It is important that the WQHI is not positively biased by large quantities of good HI values, and that very poor HI values (e.g. values of 0 which indicate a need for very urgent attention) are not "lost" through averaging with better HI values.
However, this is because the data cannot be mapped one to one, and the hI values for non-cooperative fluctuations shift to lower values, since the all or no bars in a fluctuating edge increases the heterogeneity index.
The HI values decrease a lot as a function of increasing concentration of hydrophilic SO3H groups.
The experimentally obtained temperatures were used by a numerical technique in order to determine time-varying hi values.
Predictions of HI using the sub-surface topography greatly decreased prediction errors, especially for intermediary HI values at middleslope position.
A numerical technique which compares theoretical and experimental thermal profiles is used for investigating the influence of solute content on hi values.
The total organic carbon (Corg, %) contents of carbonaceous rocks range from 0.21% to 39.61%, and hydrogen index (HI) values are between 25 and 174 mg HC/g rock.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com