How Batch-0042-024 Resolves the Mechanism Behind Diurnal Variability in Groundwater Arsenic Mobilization Driven by Redox Oscillations in Shallow Aquifers

批次0042-024如何解析浅层含水层中氧化还原振荡驱动地下水砷迁移的日变化机制

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Diurnal groundwater arsenic spikes correlate precisely with nocturnal O₂ depletion and subsequent Fe(III) oxide reductive dissolution in shallow alluvial aquifers.
High-frequency in-situ sensors capture synchronized pH drops, dissolved Fe²⁺ surges, and As(III) concentration peaks within two hours of sunset.

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