Fig. 1 | Nature Communications

Fig. 1

From: Acceleration of dolomitization by zinc in saline waters

Fig. 1The alternative text for this image may have been generated using AI.

Powder X-ray diffractograms (selected 20–70 °2θ) of reaction products in the main experiment series at selected time intervals of 4, 8, and 12 h. The dolomite and calcite characteristic reflections are indicated in a and b, respectively. The peak at 31.7 °2θ in some diffractograms is due to minor halite that was not entirely dissolved during the rinsing process of the product or developed during drying of the samples

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