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. 2011 May;77(9):3132–3136. doi: 10.1128/AEM.02085-10

Fig. 3.

Fig. 3.

Fe(II) formation rates obtained in anoxic soil microcosms in relation to the initial Fe(II) concentrations. Initial Fe(II) formation rates were determined in carbon-unamended soil microcosms of horizons Btlc, Br1, and Br2, whereas biostimulated Fe(II) formation rates were determined in carbon-amended Btlc microcosms.