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Stream Order
Dr. Surjya Kumar Saikia
Department of Zoology
Visva-Bharati
Physical Methods
• Stream order is a measure of the
relative size of streams.
• Range from smallest, first-order,
to the largest, the twelfth-
order(Amazon)
• Over 80% of total length of
Earth’s rivers and Streams are
headwater streams(first and
second order)
• As water travels from
source to mouth, the
streams tend to increase
in width, depth, and
discharge.
First order streams
• Perennial: carry water
all year
• Smallest streams
• Have no permanently
flowing tributaries
Second Order Streams
• Two first order
streams come together
to form one second
order streams.
• However, if a first
order stream joins a
second order, it is still
a second order
Third Order Stream
• When two second
order streams come
together, it forms a
third order stream.
• How has the width of
the stream changed
since it was 2nd order?
How about since 1st
order?
Fourth Order Stream
• When 2 third order
streams come
together,it forms a
fourth order stream
• How has the width and
canopy changed since
1st, 2nd, and 3rd order
stream?
Stream order
• Two of the same order
streams must come
together before that
stream goes up one
level.
Stream Ordering
Headwater (1-3)
Mid reach
(4-6)
Lower reach (>6)
4 - 6
1 - 3
> 6
STREAM ORDER
Headwaters
Midreach
Lower
Reaches
Types of organic matter
• Particulate organic matter
–CPOM-Coarse particulate organic matter
• Woody material & leaves (> 1 mm)
–FPOM-Fine particulate organic matter
• Leaf fragments, invertebrate feces, and
organic precipitates (50um – 1 mm)
– Ultrafine (UPOM)
• Even smaller fragments (0.5 – 50um)
Types of organic matter
• DOM- Dissolved organic matter
– Soluble organic compounds (<0.5 um) that leach
from leaves, roots, decaying organisms, and other
terrestrial sources
– Microbial sources: algal exudates, senescent
bacteria
– 50% is humic material- HDOM
– Largest pool of organic matter in streams
Dynamic Equilibrium
• Stream forms equilibrium between physical
parameters (width, depth, velocity, and sediment load, both means
and extremes) and biological factors
– SEASONAL: Uniform energy processing over
time; different species exploit different available
organic substrates as efficiently as possible
– SPATIAL: Energy loss from upstream = energy
gain/income for downstream
Energy Sources- Headwaters
• Shading: Riparian vegetation, limits
light to stream, low autotrophic
production
• Photosynthesis/Respiration (P/R) ratio
will be less than 1 (heterotrophic
stream)
• Lots of CPOM: allochthonous
carbon/energy sources (leaves from
watershed)
• Low temperture
Energy Sources- Midreach
• Stream broadening, more light
• P/R > 1, autotrophic production
(phytoplankton, periphyton, macrophytes)
• More FPOM, b/c CPOM
processed upstream
• Energy source is autochthonous.
• High temp variation
Energy Sources- Lower Reaches
• Increasing turbidity, even
wider stream, increased
macrophytes
• P/R < 1, net heterotrophic
• Mostly FPOM (vs. CPOM
in the headwaters)
• High phytoplankton, not
enough to cause the river
to become autotrophic
• Large volume, low temp
Connections from
upstream to downstream
habitats control flow of
energy and carbon in
fluvial ecosystems, as
well as the species of
aquatic organisms
River Continuum Concept: Vannote et al. 1980
Theme: importance of
light availability in
controlling in situ
production (e.g. P/R)
4 - 6
1 - 3
> 6
STREAM ORDER
River Continuum Concept- BENTHIC INVERTEBRATES
CPOM
CPOM
CPOM
FPOM
FPOM
FPOM
Collectors
Shredders
Scrapers/Grazers
Collectors
Collectors
TESTABLE HYPOTHESIS- Taxonomy is the tool to measure this
RCC and Fish Communities
• Headwaters: cool water species (e.g., trout)
• Lower reaches: warm water species (e.g., carp)
• Most headwater fishes feed on invertebrates
• Mid to lower reaches, piscivorous species are also
abundant
• Lower reaches, planktivorous species may be present
Construction of a dam
changes the means and
extremes to which the stream
biota are adapted
Construction of a dam can
correspond to a “resetting” of
the river continuum, by
trapping material and making
sunlight more available to
support autotrophic growth.
What we have learnt………
• How to name and count river order
• The river continuum concept (RCC) and its
features
• Change in biota and physical features across
the stream orders

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Stream order

  • 1. Stream Order Dr. Surjya Kumar Saikia Department of Zoology Visva-Bharati
  • 2. Physical Methods • Stream order is a measure of the relative size of streams. • Range from smallest, first-order, to the largest, the twelfth- order(Amazon) • Over 80% of total length of Earth’s rivers and Streams are headwater streams(first and second order)
  • 3. • As water travels from source to mouth, the streams tend to increase in width, depth, and discharge.
  • 4. First order streams • Perennial: carry water all year • Smallest streams • Have no permanently flowing tributaries
  • 5. Second Order Streams • Two first order streams come together to form one second order streams. • However, if a first order stream joins a second order, it is still a second order
  • 6. Third Order Stream • When two second order streams come together, it forms a third order stream. • How has the width of the stream changed since it was 2nd order? How about since 1st order?
  • 7. Fourth Order Stream • When 2 third order streams come together,it forms a fourth order stream • How has the width and canopy changed since 1st, 2nd, and 3rd order stream?
  • 8. Stream order • Two of the same order streams must come together before that stream goes up one level.
  • 9. Stream Ordering Headwater (1-3) Mid reach (4-6) Lower reach (>6)
  • 10. 4 - 6 1 - 3 > 6 STREAM ORDER Headwaters Midreach Lower Reaches
  • 11. Types of organic matter • Particulate organic matter –CPOM-Coarse particulate organic matter • Woody material & leaves (> 1 mm) –FPOM-Fine particulate organic matter • Leaf fragments, invertebrate feces, and organic precipitates (50um – 1 mm) – Ultrafine (UPOM) • Even smaller fragments (0.5 – 50um)
  • 12. Types of organic matter • DOM- Dissolved organic matter – Soluble organic compounds (<0.5 um) that leach from leaves, roots, decaying organisms, and other terrestrial sources – Microbial sources: algal exudates, senescent bacteria – 50% is humic material- HDOM – Largest pool of organic matter in streams
  • 13. Dynamic Equilibrium • Stream forms equilibrium between physical parameters (width, depth, velocity, and sediment load, both means and extremes) and biological factors – SEASONAL: Uniform energy processing over time; different species exploit different available organic substrates as efficiently as possible – SPATIAL: Energy loss from upstream = energy gain/income for downstream
  • 14. Energy Sources- Headwaters • Shading: Riparian vegetation, limits light to stream, low autotrophic production • Photosynthesis/Respiration (P/R) ratio will be less than 1 (heterotrophic stream) • Lots of CPOM: allochthonous carbon/energy sources (leaves from watershed) • Low temperture
  • 15. Energy Sources- Midreach • Stream broadening, more light • P/R > 1, autotrophic production (phytoplankton, periphyton, macrophytes) • More FPOM, b/c CPOM processed upstream • Energy source is autochthonous. • High temp variation
  • 16. Energy Sources- Lower Reaches • Increasing turbidity, even wider stream, increased macrophytes • P/R < 1, net heterotrophic • Mostly FPOM (vs. CPOM in the headwaters) • High phytoplankton, not enough to cause the river to become autotrophic • Large volume, low temp
  • 17.
  • 18. Connections from upstream to downstream habitats control flow of energy and carbon in fluvial ecosystems, as well as the species of aquatic organisms River Continuum Concept: Vannote et al. 1980 Theme: importance of light availability in controlling in situ production (e.g. P/R)
  • 19. 4 - 6 1 - 3 > 6 STREAM ORDER River Continuum Concept- BENTHIC INVERTEBRATES CPOM CPOM CPOM FPOM FPOM FPOM Collectors Shredders Scrapers/Grazers Collectors Collectors TESTABLE HYPOTHESIS- Taxonomy is the tool to measure this
  • 20.
  • 21. RCC and Fish Communities • Headwaters: cool water species (e.g., trout) • Lower reaches: warm water species (e.g., carp) • Most headwater fishes feed on invertebrates • Mid to lower reaches, piscivorous species are also abundant • Lower reaches, planktivorous species may be present
  • 22.
  • 23.
  • 24. Construction of a dam changes the means and extremes to which the stream biota are adapted Construction of a dam can correspond to a “resetting” of the river continuum, by trapping material and making sunlight more available to support autotrophic growth.
  • 25. What we have learnt……… • How to name and count river order • The river continuum concept (RCC) and its features • Change in biota and physical features across the stream orders