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. 2008 Dec 1;75(3):858–861. doi: 10.1128/AEM.01045-08

TABLE 1.

Chemical parameters for the inflowing groundwater and the oxidation basin of the planta

Location pH Eh (mV) Temp (°C) Fe2+ concn (mg/liter) Fe3+ concn (mg/liter) SO42− concn (mg/liter) Total inorganic carbon concn (mg/liter) Total organic carbon concn (mg/liter) NH4 concn (mg/liter) Cl concn (mg/liter)
Inflow 4.9 270 17 630 3 2,700 98 50 0.6 21
Oxidation basin 3 480 17 100 300 2,400 NDb ND ND ND
a

The oxygen concentration 20 cm below the water surface decreased from approximately 8 mg/liter around the inflow area to about 5 mg/liter in the middle of the oxidation basin.

b

ND, not determined.