Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia

The interaction of multiple inflows entering a reservoir (Thomson Reservoir, Australia). is investigated with a field experiment and. three-dimensional numerical model simulations.The focus of the study is the mixing and transport patterns within the reservoir of the inflowing water.Data from the fi...

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Main Authors: Marti, Clelia, Mills, R., Imberger, J.
Format: Journal Article
Published: Elsevier 2011
Online Access:http://hdl.handle.net/20.500.11937/65615
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author Marti, Clelia
Mills, R.
Imberger, J.
author_facet Marti, Clelia
Mills, R.
Imberger, J.
author_sort Marti, Clelia
building Curtin Institutional Repository
collection Online Access
description The interaction of multiple inflows entering a reservoir (Thomson Reservoir, Australia). is investigated with a field experiment and. three-dimensional numerical model simulations.The focus of the study is the mixing and transport patterns within the reservoir of the inflowing water.Data from the field experiment showed the existence of multiple inflows intruding horizontally into the reservoir immediately below the thermocline and selectively propagating into the reservoir at a depth determined by the individual density of each inflow. The results serve to show that inflows slot into a stratified reservoir in an orderly fashion, their depth dependent on the separation of inflow densities and reservoir bed, with minimal mixing between intrusions. Inflows thus do not take their nutrient load into the reservoir as a whole, but rather slot their load into an intrusion layer at an appropriate depth. Nutrients brought in via inflows become accessible only when vertical mixing, either directly at the base of the surface layer, or indirectly via the benthic boundary layer flux, transports the intrusion waters into the surface layer. © 2011 Elsevier Ltd.
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spelling curtin-20.500.11937-656152018-02-19T08:06:41Z Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia Marti, Clelia Mills, R. Imberger, J. The interaction of multiple inflows entering a reservoir (Thomson Reservoir, Australia). is investigated with a field experiment and. three-dimensional numerical model simulations.The focus of the study is the mixing and transport patterns within the reservoir of the inflowing water.Data from the field experiment showed the existence of multiple inflows intruding horizontally into the reservoir immediately below the thermocline and selectively propagating into the reservoir at a depth determined by the individual density of each inflow. The results serve to show that inflows slot into a stratified reservoir in an orderly fashion, their depth dependent on the separation of inflow densities and reservoir bed, with minimal mixing between intrusions. Inflows thus do not take their nutrient load into the reservoir as a whole, but rather slot their load into an intrusion layer at an appropriate depth. Nutrients brought in via inflows become accessible only when vertical mixing, either directly at the base of the surface layer, or indirectly via the benthic boundary layer flux, transports the intrusion waters into the surface layer. © 2011 Elsevier Ltd. 2011 Journal Article http://hdl.handle.net/20.500.11937/65615 10.1016/j.advwatres.2011.01.003 Elsevier restricted
spellingShingle Marti, Clelia
Mills, R.
Imberger, J.
Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title_full Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title_fullStr Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title_full_unstemmed Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title_short Pathways of multiple inflows into a stratified reservoir: Thomson Reservoir, Australia
title_sort pathways of multiple inflows into a stratified reservoir: thomson reservoir, australia
url http://hdl.handle.net/20.500.11937/65615