Microbial nitrogen transformations in sediments and inorganic nitrogen fluxes across the sediment/water interface on the South Island West Coast, New Zealand
In January 1982, sediment microbial N transformations and inorganic N fluxes across the sediment/water interface were studied at nine sites off the South Island West Coast, New Zealand. The sediments showed a great variety in physical, chemical and biological properties. The sediment organic matter...
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Veröffentlicht in: | Estuarine, coastal and shelf science coastal and shelf science, 1985-01, Vol.21 (2), p.245-255 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | In January 1982, sediment microbial N transformations and inorganic N fluxes across the sediment/water interface were studied at nine sites off the South Island West Coast, New Zealand. The sediments showed a great variety in physical, chemical and biological properties. The sediment organic matter had a molar
C
N
ratio of 5.9–10.9, and the total
N
P
ratio was 1.2–4.0. The denitrification capacity in the top 7.5 cm of sediment was 0.1–77.2 mmol N m
−2 day
−1 and generally declined with increasing sediment depth. The
in situ denitrification rate was 0.02–1.84 mmol N m
−2 day
−1 and highest activities were generally found in surface sediments and at 6–7.5 cm depth. Denitrification accounted for 82–100% of total nitrate reduction. Net N mineralization was indirectly estimated at 0.6–2.4 mmol N m
−2 day
−1, and the experimental determination of this N transformation gave 0.6–3.2 mmol N m
−2 day
−1. Denitrification accounted for 3–75% of net N mineralization. The diffusive flux of ammonium and nitrate across the sediment/water interface was 0.1–0.7 and 0.1–0.6 mmol N m
−2 day
−1, respectively. |
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ISSN: | 0272-7714 1096-0015 |
DOI: | 10.1016/0272-7714(85)90100-3 |