Stability of dissolved and soluble Fe(II) in shelf sediment pore waters and release to an oxic water column
Shelf sediments underlying temperate and oxic waters of the Celtic Sea (NW European Shelf) were found to have shallow oxygen penetrations depths from late spring to late summer (2.2–5.8 mm below seafloor) with the shallowest during/after the spring-bloom (mid-April to mid-May) when the organic carbo...
| Những tác giả chính: | , , , , , , , , , , , , |
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| Định dạng: | Journal article |
| Được phát hành: |
Springer International Publishing
2017
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