Lect4-Habitat_Processes

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Physical Stream Habitat

What is “Habitat”?

Broad Definition (EPA):

“The spatial structure of the environment which allows species to live, reproduce, feed and move”

In Relation to Streams (USGS):

“The physical and chemical characteristics of a stream that determine suitability for habitation and reproduction of stream organisms”

What is “Physical Habitat”?

“The template of water depth, water velocity, substrate, cover and temperature that supports the stream ecosystem” – USGS

Hydrologic

Conditions

Land Use

Geology

Topography

Vegetation

Stream Morphology

Physical Habitat

Chemical Habitat

Aquatic Community

Interspecies

Interactions

Measurable Characteristics of

Physical Habitat

• Channel morphology / type

• Flow regime

• Sediment texture / mobility

• Bank structural features / stability

• Riparian condition and connectivity

• Physiochemical – temperature, DO, metals, nutrients, turbidity, etc.

Mill Creek

Salmon and trout habitat requirements include:

• adequate but not excessive stream flows

• cool well-oxygenated unpolluted water

• streambed gravels that are relatively free of finesediments

• adequate food supply

• instream structural diversity (interposed pools, riffles, hiding and resting cover)

Washington State Dept of Fish Wildlife

Physical stream characteristics affect stream organisms by defining:

• Habitat volume

• Habitat quality

• Disturbance magnitude

• Disturbance frequency

Habitat varies over spatial & temporal scales

Stream Corridor

Restoration, 199x

Large

Scale

Fine

Scale

Heirarchical Classification System

Scalar Unit Definition

Role in Habitat

Characterization

Watershed

Basin

Segment

Area defined by topography that contributes water and sediment to the stream network

Physiographically defined unit, based on relief, morphology and landscape position

Reach Type Length of channel with uniform constraints resulting in a specific assemblage of geomorphic units

Geomorphic

Unit

Fluvial channel forms representing distinct form-process associations

Habitat Type Patches of relatively uniform flow and substrate characteristics

Determines boundary conditions within which river operates

Determines boundary conditions within which river operates

Describes channel planform and geometry

Determines channel character and behavior

Describes ecologically relevant hydraulic and substrate conditions

Watershed

10 3 m

Segment

10 2 m

Reach Type

10 1 m

Geomorphic

Unit

10 0 m

Microhabitat

Type

10 -1 m

How is each scale important to the species of interest?

Salmon

Macroinverts

Temporal Variability incorporates

‘predictable’ and ‘unpredictable’ cycles

Physical habitat a function of processes operating at multiple spatial and temporal scales

How do we objectively assess it?

Define Stream Habitat Types

(Classification)

• Bisson et al, 1982

• McCain et al, 1990 (USFS)

• Hawkins et al, 1993 (USFS)

• Thomson et al, 2001 (UK, AUS)

Fish -

Centric

McCain et al, 1990

McCain et al, 1990

Bisson et al, 1982

Hawkins et al, 1993

Hawkins et al, 1993

McCain et al, 1990

Hydraulic Habitat

Flow types can be distinguished by velocity and depth using

Froude Number

F = v gd

Panfil & Jacobson, 2000

Thomson et al, 2001

Stream Habitat types are created and maintained by erosion and deposition of sediments.

Hjulstrom’s Diagram

Mechanics of Habitat Formation

• Shear Stress/Velocity Reversal

Hypothesis

• Helical Flow

• Contraction/Expansion of Flow

t = rghs v ~ f(Rs)

Knighton, 1998

Helical flow in meander bends

Knighton, 1998

Flow contraction and expansion

Wohl, 1998

McBain & Trush, 2004

Increased roughness reduces shear, promoting deposition of finer material

What promotes Habitat Diversity?

Diversity is a function of fluctuations in erosion and deposition processes over varying scales

Disturbance

Natural stream systems are subject to the full spectrum of spatial & temporal disturbances

• Natural flow regime

• Varying sediment inputs

Episodic Sediment Transport

• Structural diversity - LWD

Natural Flow Regime

• 5 characteristics :

 Frequency

 Magnitude

 Duration

 Timing

 Rate of Change

• Key factor = extremes included

Disturbance acts to ‘reset’ processes

Mount, 1995

Large Woody Debris

• Increases local scour and deposition

• Provides structural habitat

• Transient nature (moves, breaks, clumps, decays)

All add to habitat diversity and complexity

Plane Bed

Wood-poor

Pool-riffle

Buffington & Montgomery 1999

Wood-rich

Pool-riffle

Buffington & Montgomery 1999

Stream habitat diversity maintained over time

Species adapt

• Salmon – spawning and run timing

• Foothill Yellow-legged Frog – oviposition timing

• Cottonwood regeneration – accidental forest

Spawning habitat with incubation of eggs

Movement to

Spawn

Refugia from harsh environmental conditions (e.g., extreme temperatures or flows) with unfavorable growth conditions

Movement to Spawn

Movement to Feed

Movement to Refuge

Movement to Feed

Mosaic of feeding habitat(s) with favorable growth conditions

Habitat

1

Habitat

3

Habitat

2

Diversity in Trout Habitat Redrawn by Bledsoe from

Schlosser (1995)

Alterations to flow regime & sediment supply alter habitat diversity & biodiversity

Stream

Corridor

Restoration,

1998

Alterations to Stream Systems

• Flow extraction

– diversions

– groundwater withdrawal

• Flow augmentation

– ag runoff

– hydropower

• Sedimentation

– development

– logging

– mining

• Sediment Loss

– dams

– mining

Degradation

• Channel Bed Coarsening

• Loss of Fines/Gravels

• Vegetation Encroachment

• Low bed mobility

Aggradation

• Channel Bed Fining

• Excess Fines/Gravels

• Lack of vegetation

• High bed mobility

Effect of Dams

• Block Sediment

• “Flatline”

Hydrograph

• Disrupt

Connectivity

• Channel Degradation bed coarsening, loss of fines/gravels

• Loss of extreme flows

(loss of disturbance) – low bed mobility, vegetation encroachment, low habitat diversity

• Block habitat access, alter water chemistry, shift from lentic to lotic system

What can we do to improve spawning habitat conditions downstream of dams?

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