Cycling of redox-sensitive elements in a sandy subterranean estuary of the southern North Sea
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文摘
Trace metal concentrations in beach pore water deviate from conservative mixing. S and O isotope ratios of dissolved sulfate indicate a cryptic sulfur cycle. Dissolved reactive Mn may accelerate redox reactions in shallow suboxic pore waters. The subterranean estuary is a source of Fe, Mn, and Mo, but a sink for V, U, and Re. The tidal flat area is more important for trace element budgets than the beach.

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