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Re-Meandering Of Lowland Streams:  Will Disobeying the Laws Re-Meandering Of Lowland Streams:  Will Disobeying the Laws

Re-Meandering Of Lowland Streams: Will Disobeying the Laws - PowerPoint Presentation

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Uploaded On 2016-03-21

Re-Meandering Of Lowland Streams: Will Disobeying the Laws - PPT Presentation

Pedersen Kristensen Friberg 2014 PlosOne Volume 9 110 Katie Halvorson Introduction to area Methods and ideas on project Results from project S ummary Overview Catchment areas of Jutland Denmark ID: 264670

streams natural channelized stream natural streams stream channelized results restoration pebble differed jutland areas cont physical reach ideas water

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Slide1

Re-Meandering Of Lowland Streams: Will Disobeying the Laws of Geomorphology Have Ecological Consequences?Pedersen, Kristensen, Friberg, 2014, PlosOne, Volume 9, 1-10

Katie HalvorsonSlide2

Introduction to areaMethods and ideas on projectResults from project

S

ummary

OverviewSlide3

Catchment areas of Jutland, DenmarkWhere the study was doneSlide4

Jutland areas based on last glaciation

Western: ice-free

Eastern: sub-glacial loamy moraineSlide5

Determine how natural streams and rivers are structured Physical habitat

Flow

Sediment regime

Improve ecological status of bodies of wate

r

in Europe

Key Ideas:Slide6

“All restoration measures were aimed at creating a more heterogeneous and natural stream reach.”The goal:Slide7

Catchment–scale controlsHydrology, geology

Differences

in channel

pattern

at reach scale

local

slope, geology

Variations in structure and composition

bank

material, flow, and turbulent structure

Morphology of river depends

on:Slide8

18 reaches selected6 natural meandering streams with little alterations

6 channelized

6 formally channelized

Field work done over 40days in April and May 2002

The study:Slide9

Water chemistryPhysical habitatsMacroinvertebrates

Looked at:Slide10

Results:Composition of stream bed varied significantly among stream types.

Cobble and pebble

dominant in restored streams

Sand in natural and channelized

streamsSlide11

Natural streams width variation was significantly higher than in channelized streams.Macroinvertebrate communities differed in species by stream type.

Results cont.Slide12

Huge change in physical habitats of the restored streams (pebble and gravel) compared to natural and channelized streams (sand).Stream bed slope differed between the threeHigh slopes = restored

Lowest = channelized

Results cont.Slide13

Natural functioning of the geomorphological process is affected by both channelization and restoration and that restoration DOES NOT re-establish the natural functioning at a 3+ year time-scale.In summary: