Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.

Estuarine wetlands of south eastern Australia, typically display a vegetation zonation with a sequence mudflats - mangrove forest - saltmarsh plains from the seaward margin and up the topographic gradient. Estuarine wetlands are among the most productive ecosystems in the world, providing unique...

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Autores principales: Trivisonno, Franco N., Rodriguez, Jose F., Riccardi, Gerardo A., Saco, Patricia M., Stenta, Hernan R.
Formato: conferenceObject documento de conferencia publishedVersion
Lenguaje:Inglés
Publicado: European Geophysical Union 2020
Materias:
Acceso en línea:http://hdl.handle.net/2133/17641
http://hdl.handle.net/2133/17641
Aporte de:
id I15-R121-2133-17641
record_format dspace
institution Universidad Nacional de Rosario
institution_str I-15
repository_str R-121
collection Repositorio Hipermedial de la Universidad Nacional de Rosario (UNR)
language Inglés
orig_language_str_mv eng
topic Estuarine wetlands
Coevolution hydraulic soil and vegetation
Hunter estuary
spellingShingle Estuarine wetlands
Coevolution hydraulic soil and vegetation
Hunter estuary
Trivisonno, Franco N.
Rodriguez, Jose F.
Riccardi, Gerardo A.
Saco, Patricia M.
Stenta, Hernan R.
Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
topic_facet Estuarine wetlands
Coevolution hydraulic soil and vegetation
Hunter estuary
description Estuarine wetlands of south eastern Australia, typically display a vegetation zonation with a sequence mudflats - mangrove forest - saltmarsh plains from the seaward margin and up the topographic gradient. Estuarine wetlands are among the most productive ecosystems in the world, providing unique habitats for fish and many terrestrial species. They also have a carbon sequestration capacity that surpasess terrestrial forest. Estuarine wetlands respond to sea-level rise by vertical accretion and horizontal landward migration, in order to maintain their position in the tidal frame. In situations in which buffer areas for landward migration are not available, saltmarsh can be lost due to mangrove encroachment. As a result of mangrove invasion associated in part with raising estuary water levels and urbanisation, coastal saltmarsh in parts of south-eastern Australia has been declared an endangered ecological community. Predicting estuarine wetlands response to sea-level rise requires modelling the coevolving dynamics of water flow, soil and vegetation. This paper presents preliminary results of our recently developed numerical model for wetland dynamics in wetlands of the Hunter estuary of NSW. The model simulates continuous tidal inflow into the wetland, and accounts for the effect of varying vegetation types on flow resistance. Coevolution effects appear as vegetation types are updated based on their preference to prevailing hydrodynamic conditions. The model also considers that accretion values vary with vegetation type. Simulations are driven using local information collected over several years, which includes estuary water levels, accretion rates, soil carbon content, flow resistance and vegetation preference to hydraulic conditions. Model results predict further saltmarsh loss under current conditions of moderate increase of estuary water levels.
format conferenceObject
documento de conferencia
publishedVersion
author Trivisonno, Franco N.
Rodriguez, Jose F.
Riccardi, Gerardo A.
Saco, Patricia M.
Stenta, Hernan R.
author_facet Trivisonno, Franco N.
Rodriguez, Jose F.
Riccardi, Gerardo A.
Saco, Patricia M.
Stenta, Hernan R.
author_sort Trivisonno, Franco N.
title Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
title_short Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
title_full Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
title_fullStr Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
title_full_unstemmed Coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
title_sort coevolution of hydraulic, soil and vegetation processes in estuarine wetlands.
publisher European Geophysical Union
publishDate 2020
url http://hdl.handle.net/2133/17641
http://hdl.handle.net/2133/17641
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