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. 2017 Oct 19;18:6. doi: 10.1186/s12932-017-0044-1

Table 2.

Fe-normalized electrons transferred over 28 days relative to the redox state measured (a) directly after addition of HS or RHS, i.e. t = 0, in the HS or RHS magnetite sample and (b) t = 28 days bicarbonate control sample

Sample meq e Fe−1 a meq e Fe−1 b
Biogenic magnetite + HS 0.5 − 12.4
Biogenic magnetite + RHS − 47.7 − 67.5
13 nm magnetite + HS 17.9 − 6.3
13 nm magnetite + RHS 10.7 − 16.8
7 nm magnetite + HS 0.2 − 7.8
7 nm magnetite + RHS − 0.7 − 11.7
500 nm magnetite + HS 2.9 3.1
500 nm magnetite + RHS 2.0 2.6

Positive numbers are net-oxidation reactions and negative numbers are net-reduction reactions with respect to Fe

Using the values in Additional file 1: Table S5, the electrons transferred (z) were calculated as

z=(Fe2+(%)+Fe(II)(%))ref.-(Fe2+(%)+Fe(II)(%))sample100×Fe(II)tot.avgFetot.avg where Fe(II)tot.avg=[Fe(II)]tot.ref.+[Fe(II)]tot.sample2 and Fetot.avg=Fetotref.+Fetotsample2, Fe2+ represents dissolved Fe2+, Fe(II) represents solid phase Fe(II), [Fe(II)]tot is the sum of dissolved Fe2+ and solid phase Fe(II), [Fetot] is the total concentration of Fe (i.e. the sum of Fe2+, Fe(II), Fe3+ and Fe(III)) and ref. is (a) the t = 0 sample of the HS or RHS sample as indicated on the lines in the table or (b) the bicarbonate control at t = 28 days