Morphological development of Perkpolder tidal basin

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Since the termination of the ferry service between Perkpolder (Zeeuws Vlaanderen) and Kruiningen in 2003 the area needed a new destination. In close cooperation with stakeholders a new plan was developed which combines, housing, recreation and the development of a salt march (www.perkpolder.nl). For the development of this salt march a freshwater agricultural area is now connected to the Western Scheldt, since July 2015.
   
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The salt water from the Western Scheldt will flow through an opening in the dyke. The morphological dynamics of this inlet (or breach in the dyke) will depend on the flow velocity, size of the salt march area, tidal range and the present type of material (sand and clay). In this study you will monitor the development of the inlet, which will give Rijkswaterstaat important information concerning the stability of the dyke. Furthermore you will investigate the morphological development (height levels) of the Perkpolder basin, based on field measurements of sediment thickness, and sediment concentrations in the water column.
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'''Research type:''' field research, deskwork (GIS, Excel) Research 
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'''level:''' bachelor internship, minor research
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'''Prerequisite:''' interest in morphology and geology or fluid dynamics
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'''Partners:''' Rijkswaterstaat Zee en Delta, Deltares
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'''Client:''' Joao Salvador de Paiva
 
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{{Project
  
{{Project
 
|Supercontext=Building with Nature
  
|Supercontext=Building with Nature
 
|Project type=Standaard
  
|Project type=Standaard
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|Name=MORPHOLOGICAL DEVELOPMENT OF PERKPOLDER TIDAL BASIN
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|Name=Morphological development of Perkpolder tidal basin
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|Start date=2016/08/01
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|Start date=2018/09/01
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|End date=2017/02/01
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|End date=2019/02/01
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|Summary=Since the termination of the ferry service between Perkpolder (Zeeuws Vlaanderen) and Kruiningen in 2003 the area needed a new destination. In close cooperation with stakeholders a new plan was developed which combines, housing, recreation and the development of a salt march (www.perkpolder.nl). For the development of this salt march a freshwater agricultural area is now connected to the Western Scheldt, since July 2015.
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|Summary=Morphological development of Perkpolder tidal basin
   
 
Research type: field research, deskwork (GIS, Excel) Research  
  
Research type: field research, deskwork (GIS, Excel) Research  
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level: bachelor internship, minor research
  
level: bachelor internship, minor research
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Prerequisite: interest in morphology and geology or fluid dynamics
  
Prerequisite: interest in morphology and geology or fluid dynamics
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Partners: Rijkswaterstaat Zee en Delta, Deltares
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|Show summary=Ja
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Client: Matthijs Boersema
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The salt water from the Western Scheldt will flow through an opening in the dyke. The morphological dynamics of this inlet (or breach in the dyke) will depend on the flow velocity, size of the salt march area, tidal range and the present type of material (sand and clay). In this study you will monitor the development of the inlet, which will give Rijkswaterstaat important information concerning the stability of the dyke. Furthermore you will investigate the morphological development (height levels) of the Perkpolder basin, based on field measurements of sediment thickness, and sediment concentrations in the water column.
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|Show sub projects=Ja
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|Show participants=Ja
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Huidige versie van 23 aug 2018 om 11:21

Since the termination of the ferry service between Perkpolder (Zeeuws Vlaanderen) and Kruiningen in 2003 the area needed a new destination. In close cooperation with stakeholders a new plan was developed which combines, housing, recreation and the development of a salt march (www.perkpolder.nl). For the development of this salt march a freshwater agricultural area is now connected to the Western Scheldt, since July 2015.

The salt water from the Western Scheldt will flow through an opening in the dyke. The morphological dynamics of this inlet (or breach in the dyke) will depend on the flow velocity, size of the salt march area, tidal range and the present type of material (sand and clay). In this study you will monitor the development of the inlet, which will give Rijkswaterstaat important information concerning the stability of the dyke. Furthermore you will investigate the morphological development (height levels) of the Perkpolder basin, based on field measurements of sediment thickness, and sediment concentrations in the water column.


Research type: field research, deskwork (GIS, Excel) Research 

level: bachelor internship, minor research

Prerequisite: interest in morphology and geology or fluid dynamics

Partners: Rijkswaterstaat Zee en Delta, Deltares

Client: Joao Salvador de Paiva















Project summary

Morphological development of Perkpolder tidal basin

Research type: field research, deskwork (GIS, Excel) Research

level: bachelor internship, minor research

Prerequisite: interest in morphology and geology or fluid dynamics

Start date: september 1, 2018
End date: februari 1, 2019



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