Fig. 4: ΔTA versus ΔCa for the oxic incubations. | Communications Earth & Environment

Fig. 4: ΔTA versus ΔCa for the oxic incubations.

From: Sediment resuspension in muddy sediments enhances pyrite oxidation and carbon dioxide emissions in Kiel Bight

Fig. 4: ΔTA versus ΔCa for the oxic incubations.The alt text for this image may have been generated using AI.

Red, blue, and orange lines show linear correlations at each site. The colour bar represents the change in SO42− concentrations during the incubations. The dashed line represents the theoretical slope for calcium carbonate dissolution. ΔTA and Ca refer to the change in concentrations from the initial values.

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