Abstract
Submarine subsurface fluid flow is ubiquituous with rates varying enormously with space and time. Therefore, fluid flow most probably is of paramount importance for the transport of matter and heat as well as to control fluxes between the subsurface and the ocean. However, rates to date still are only very poorly understood. In this study we therefore first identify major fluid flow systems including fault transport at active and passive margins, gas hydrate affected flow systems, or submarine groundwater discharge. Then, we describe geophysical and geochemical methods which are capable to better and quantitatively understand interacting submarine fluid flow systems and lastly, propose strategies for future research.
Keywords
- Fluid Flow
- Continental Margin
- Accretionary Prism
- Submarine Groundwater Discharge
- Remotely Operate Vehicle
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
References
Bolton A, Maltman A (1998) Fluid-flow pathways in actively deforming sediments: The role ofpore fluid pressures and volume change. Mar Petrol Geol 15: 281–297
Dia AN, Castrec-Rouelle M, Boulègue J, Comeau P (1999) Trinidad mud volcanoes: Where do the expelled fluids come from? Geochim Cosmochim Acta 63 :1023–1038
Haese RR (2002) Macrobentic Activity and its Effects on Biogeochemical Reactions and Fluxes. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 219–234
Hinkelmann R, Helmig R (2002) Numerical Modelling of Transport Processes in the Subsurface. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 269–294
Mann D, Kukowski N (1999) Numerical modelling of focussed fluid transport in the Cascadia accretionary prism. J Geodynamics 27:359–372
Mienert J, Berndt C, Laberg JS, Vorren TO (2002) Slope Instability of Continental Margins. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 179–193
Moore JC, Vrolijk P (1992) Fluids in accretionary prisms. Rev Geophys 30:113–135
Schlüter M (2002) Fluid Flow in Continental Margin Sediments. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 205–217
Sibuet M, Olu-Le Roy K (2002) Biological Indicators for Seeps. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 235–251
Soetaert K, Middelburg J, Wijsman J, Herman P, Heip C (2002) Ocean Margin Early Diagenetic Processes and Models. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 157–177
Suess E, Bohrmann G, von Huene R, Linke P, Wallmann K, Lammers S, Sahlig H, Winckler G, Lutz RA, Orange D(1998) Fluid venting in the Aleutian subduction zone. J Geophys Res 103:2597–2614
Zabel M, Hensen C (2002) The Importance of Mineralisation Processes in Surface Sediments at Continental Margins. In: Wefer et al. (eds) Ocean Margin Systems. Springer, Berlin pp 253–267
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2002 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Kukowski, N. et al. (2002). Subsurface Fluid Flow and Material Transport. In: Wefer, G., Billett, D., Hebbeln, D., Jørgensen, B.B., Schlüter, M., van Weering, T.C.E. (eds) Ocean Margin Systems. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-05127-6_18
Download citation
DOI: https://doi.org/10.1007/978-3-662-05127-6_18
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-07872-9
Online ISBN: 978-3-662-05127-6
eBook Packages: Springer Book Archive