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  • 标题:Dissolved Iron Behavior in the Ravenglass Estuary Waters, An Implication on the Early Diagenesis
  • 本地全文:下载
  • 作者:Ehsan Daneshvar
  • 期刊名称:Universal Journal of Geoscience
  • 印刷版ISSN:2331-9593
  • 电子版ISSN:2331-9615
  • 出版年度:2015
  • 卷号:3
  • 期号:1
  • 页码:1-12
  • DOI:10.13189/ujg.2015.030101
  • 语种:English
  • 出版社:Horizon Research Publishing
  • 摘要:Estuaries are suitable places for both clay mineral accumulation and iron trapping. Flocculated and deposited Fe compounds in the estuaries can lead to neo-formed minerals which they have a basic role in reservoir quality estimation. The aqueous geochemistry of the Ravenglass estuary and its feeding rivers has been studied to assess if, where and when aqueous iron is lost from the river water and accumulates as part of the sediment in the estuary. Ravenglass estuary waters are conservative mixtures between river water and seawater in terms of chloride, sodium, potassium and magnesium. Alkalinity (bicarbonate), calcium and sulphate are locally non-conservative and are affected by biological and mineral processes. The River Irt contains twice as much dissolved iron as the River Esk but all iron concentrations are much lower in the estuary samples than in the feeding rivers. Aqueous iron undergoes large-scale accumulation in the Ravenglass estuary. Iron concentrations are lowest at high tide at all sampling sites on the Ravenglass estuary. Iron concentrations are highest at low tide for the Irt arm of the estuary but are highest on the falling tide between high and low tide. Iron concentrations in estuary samples decrease rapidly as salinity increases with low iron concentrations in all estuary samples once salinity exceeds 5,000 mg/lit. Iron concentrations also decrease as pH increases. The loss of iron is presumably due to flocculation of colloidal iron oxides, hydroxides and iron-organic complexes. Fluvial aqueous iron does not behave conservatively on mixing with seawater; most iron is lost from the water column at an early stage of river water mixing with estuary water. The site of primary iron-loss from the water occurs towards the heads of estuaries but this site will move as a function of time within the tide cycle. Given that the Esk has highest iron concentrations between high and low tide, it is likely that iron is swept from the iron-rich Irt arm of the estuary into the iron-poor Esk arm soon after high tide.
  • 关键词:Estuaries; Flocculation; Iron Elimination; Chlorite
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