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Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

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https://foothillsri.ca/sites/default/files/null/HLP_2009_12_Prsnttn_InfoSession_SpatialandTemporalDynamicsofLWDinStreamsofABFoothills_Daniels.pdf
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Spatial and Temporal Dynamics of Large Woody Debris in Streams of the Alberta Foothills Lori D. Daniels, Geography, UBC
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Page 1: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Spatial and Temporal Dynamics of Large Woody Debris

in Streams of the Alberta Foothills

Lori D. Daniels, Geography, UBC

Page 2: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

What is LARGE woody debris (LWD) and why is it important?

Accumulated dead wood in streams

Page 3: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

What is LARGE woody debris (LWD) and why is it important?

Creates structure

Page 4: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

What is LARGE woody debris (LWD) and why is it important?

Dissipates stream energy

Page 5: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

What is LARGE woody debris (LWD) and why is it important?

Bank stability and sediment storage

Page 6: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Why are spatial and temporal variation in LWD important for streams?

LWD function depends on position relative to stream channel

LWD function changes over time

Page 7: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Research Questions• How much LWD is in foothills streams?• As LWD decays, how does function change?• What dynamic processes affect LWD?• How does disturbance affect LWD dynamics?• How does terrestrial coarsewood differ from

in-stream LWD?

Page 8: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Methods

• Surveys of stream reaches for abundance and function of in-stream LWD

• Surveys of riparian and upland forests for abundance of snags and logs

• Tree-ring reconstructions of forest dynamics and years of tree death

• Integration of tree-ring outcomes with HWP long-term permanent plot data

Page 9: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

• 21 headwater streams

• width <3.5m, no transport

• mature riparian forests

Page 10: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

BridgeBridge

PartialPartialBridgeBridge

LooseLoose

Large Woody DebrisPosition Classes:

BridgePartial BridgeLooseBuried

Photo: Rich McCleary

Page 11: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Large Woody DebrisPosition Classes:

BridgePartial BridgeLooseBuried

Photos: Rich McCleary

Page 12: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Other LWD attributes

• Decay classes: – I to V

• Orientation classes:– perpendicular, diagonal, parallel

• Function classes:– stabilizing banks, retaining sediment, forming

pools and riffles, creating log jamsLARGE WOODY DEBRISDecay classesOrientation classesFunction classes

Photo: Sonya Powell

Page 13: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Photos: Trevor Jones

Page 14: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Freq

uenc

y (#

50m

-1)

0

10

20

30

40

50

60

Alberta foothills MountainBoreal Mixed broadleafCoastal

Channel width at bankfull (m)0 1 2 3 4 5

In-s

tream

vol

ume

(m3 h

a-1)

0

200

400

600

800

1000

1200

Mean frequency:32±1.7 LWD 50 m-1

Mean volume:202±21 m3 ha-1

Page 15: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels
Page 16: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Bridge PartialBridge

Loose Buried

I

II

III

II

IV

III

IV

III

IV

III

IV

d o w n –

s t r e a m t r a n s p o r t

d o w n –

s t r e a m t r a n s p o r t

d o w n –

s t r e a m t r a n s p o r t

TreesSnags (III)

Snags(IV-V)

Snags(VI-IX)

Page 17: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

Acknowledgements:Acknowledgements:Funding Agencies and Collaborators:

Your financial and in-kind support has supported research by…

Page 18: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

3 Post Docs3 MSc Students2 BSc Theses8 Lab Assistants10 Field Assistants

Page 19: Hlp 2009 12 prsnttn infosession spatialandtemporaldynamicsoflwdinstreamsofabfoothills daniels

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