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. Author manuscript; available in PMC: 2015 Dec 1.
Published in final edited form as: Water Res. 2014 Aug 24;66:242–253. doi: 10.1016/j.watres.2014.08.016

Table 2.

Experimental results at different times for the precipitation of As-S mineral treatments at different pH (6.1, 6.45 and 7.1)

Experiment texp (d) pHt [TotAs]t (mM) [SO42−]t (mM) [H2S]t (mM) Sloss/ASloss
pH = 6.1 0 6.17 0.55±0.01 0.81±0.03 0.00±0.00 --
6 5.93 0.05±0.02 0.12±0.01 0.01±0.00 1.34
9 5.97 0.00±0.00 0.07±0.01 0.02±0.01 1.32
12 5.90 0.00±0.00 0.09±0.01 0.03±0.01 1.25
35 5.96 0.00±0.00 0.05±0.00 0.05±0.00 1.29

pH = 6.45 0 6.44 0.51±0.00 0.78±0.02 0.00±0.00 --
6 6.49 0.25±0.03 0.35±0.02 0.05±0.01 1.47
9 6.49 0.10±0.00 0.20±0.02 0.04±0.01 1.31
12 6.47 0.07±0.02 0.17±0.04 0.04±0.01 1.31
34 6.49 0.03±0.00 0.14±0.01 0.03±0.00 1.27

pH = 7.1 0 7.13 0.51±0.01 1.09±0.05 0.00±0.00 --
6 7.15 0.39±0.01 0.87±0.05 0.08±0.01 1.27
9 7.15 0.27±0.03 0.57±0.01 0.11±0.00 1.80
12 7.19 0.24±0.00 0.38±0.03 0.26±0.02 1.72
33 7.15 0.12±0.00 0.38±0.00 0.25±0.04 1.19

S and As losses are defined as the difference between the total initial concentration and the concentration at time t:

Sloss = (SO42− + H2S)0 − (SO42− + H2S)t

Asloss = (TotAs)0 − (TotAs)t