Assertion: sediment's concentration | /r/CapableOf | remain elevated
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text: 1999]. Concentrations of SiO 3 2− in the water exiting the salinity‐amended reactors increased shortly after initial salinity intrusion and remained elevated (Figure 2), indicating enhanced dissolution rates of silica minerals due to salinity intrusion was not a transient process, at least on the timescale of this experiment.