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Modelling macro-nutrient release and fate resulting from sediment resuspension in shelf seas

Modelling macro-nutrient release and fate resulting from sediment resuspension in shelf seas
Modelling macro-nutrient release and fate resulting from sediment resuspension in shelf seas
Early diagenesis (ED), the physical and biogeochemical changes undergone in surficial sediments, plays an important role in the biogeochemical cycles of key elements (carbon, nitrogen and oxygen) in highly productive shelf-seas. Modelling the process uses a relatively simple set of mathematical equations to represent the transport and reaction terms. We have calibrated an existing steady-state ED model, which we have expanded to include more processes and variables (e.g. mineralisation of organic matter using iron oxide and sulphate) to examine the fate of the nutrients through sediment water exchanges. Biogeochemical cycles can be affected by resuspension as a result of release or uptake of nutrients, which can also have a considerable effect on primary productivity. Resuspension is a wide-spread transport process in shallow seas due to winds, tides and biological activity. In contrast to previous diagenetic modelling, we aim to model resuspension and its effect on nutrient cycling. We will also study the resuspension effects on reactions such as the reoxidation or burial of reduced compounds and associated nutrients.We will present results from the modelling experiments, showing the relative role of various oxidising agents (oxygen, nitrate, iron oxide and sulphate) during the degradation of organic matter in the sediments. Observations made in the North Sea provide suitable data to calibrate the model. Current results show that the model is able to give realistic representations of sedimentary nutrient profiles from the North Sea.We aim to present
preliminary results showing the effect of resuspension on the transport processes of nutrients across the sediment-water interface, and will discuss the implications that this may have on the calculation of nutrient budgets in continental shelf seas
Wood, C.C.
cce67086-fb31-4cfa-8cd7-ee1463d6310d
Kelly-Gerreyn, B.A.
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Statham, P.J.
51458f15-d6e2-4231-8bba-d0567f9e440c
Aldridge, J.N.
d1dd87c8-516a-48ee-a59e-2541fff26a34
Fones, G.R.
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Couceiro, F
fefd7ac4-e7d3-46cf-988d-8ecd2e18b7d4
Thompson, C.E.L.
2a304aa6-761e-4d99-b227-cedb67129bfb
Wood, C.C.
cce67086-fb31-4cfa-8cd7-ee1463d6310d
Kelly-Gerreyn, B.A.
1434d5fd-49f7-4774-b5ff-ddf334a3dcc2
Statham, P.J.
51458f15-d6e2-4231-8bba-d0567f9e440c
Aldridge, J.N.
d1dd87c8-516a-48ee-a59e-2541fff26a34
Fones, G.R.
5b71916c-4859-4a6f-b9ad-b6b1f541cbfa
Couceiro, F
fefd7ac4-e7d3-46cf-988d-8ecd2e18b7d4
Thompson, C.E.L.
2a304aa6-761e-4d99-b227-cedb67129bfb

Wood, C.C., Kelly-Gerreyn, B.A., Statham, P.J., Aldridge, J.N., Fones, G.R., Couceiro, F and Thompson, C.E.L. (2010) Modelling macro-nutrient release and fate resulting from sediment resuspension in shelf seas. 14th Biennial Challenger Conference for Marine Science, Southampton, United Kingdom. 06 - 09 Sep 2010.

Record type: Conference or Workshop Item (Other)

Abstract

Early diagenesis (ED), the physical and biogeochemical changes undergone in surficial sediments, plays an important role in the biogeochemical cycles of key elements (carbon, nitrogen and oxygen) in highly productive shelf-seas. Modelling the process uses a relatively simple set of mathematical equations to represent the transport and reaction terms. We have calibrated an existing steady-state ED model, which we have expanded to include more processes and variables (e.g. mineralisation of organic matter using iron oxide and sulphate) to examine the fate of the nutrients through sediment water exchanges. Biogeochemical cycles can be affected by resuspension as a result of release or uptake of nutrients, which can also have a considerable effect on primary productivity. Resuspension is a wide-spread transport process in shallow seas due to winds, tides and biological activity. In contrast to previous diagenetic modelling, we aim to model resuspension and its effect on nutrient cycling. We will also study the resuspension effects on reactions such as the reoxidation or burial of reduced compounds and associated nutrients.We will present results from the modelling experiments, showing the relative role of various oxidising agents (oxygen, nitrate, iron oxide and sulphate) during the degradation of organic matter in the sediments. Observations made in the North Sea provide suitable data to calibrate the model. Current results show that the model is able to give realistic representations of sedimentary nutrient profiles from the North Sea.We aim to present
preliminary results showing the effect of resuspension on the transport processes of nutrients across the sediment-water interface, and will discuss the implications that this may have on the calculation of nutrient budgets in continental shelf seas

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More information

Published date: 9 September 2010
Venue - Dates: 14th Biennial Challenger Conference for Marine Science, Southampton, United Kingdom, 2010-09-06 - 2010-09-09
Organisations: Ocean Biochemistry & Ecosystems, Coastal & Shelf Research, National Oceanography Centre

Identifiers

Local EPrints ID: 64861
URI: http://eprints.soton.ac.uk/id/eprint/64861
PURE UUID: 16374eea-3c6b-4393-af0f-e72cc8961ca2
ORCID for C.E.L. Thompson: ORCID iD orcid.org/0000-0003-1105-6838

Catalogue record

Date deposited: 26 Mar 2010
Last modified: 23 Jul 2022 01:47

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Contributors

Author: C.C. Wood
Author: B.A. Kelly-Gerreyn
Author: P.J. Statham
Author: J.N. Aldridge
Author: G.R. Fones
Author: F Couceiro
Author: C.E.L. Thompson ORCID iD

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