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Bonanza Creek

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... F.S. III, M. Oswood, K. Van Cleve, L.A. Viereck, and D. ... Dyrness, C.T. and K. Van Cleve. 1993. ... Van Cleve, K. , L.A. Viereck and G.M. Marion. 1993. ... – PowerPoint PPT presentation

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Title: Bonanza Creek


1
Bonanza Creek
Andrews LTER
Kerry Malm Phil Garcia
GEOG 4401/5401 Soils Geography Fall 2007 Univ
of Colorado, Boulder
2
Bonanza CreekLTERAlaska
  • The role of soil and Alnus incana subsp.
    Tenuifolia in landscape succession in the Tanana
    River floodplain

http//www.lter.uaf.edu/bcef/default.cfm
3
Why are the soils salty?
http//www.macalester.edu/biology/images/Tanana.JP
G
4
Is this common Why is this bad?
  • Common in the lowlands of the Tanana River
    floodplain
  • Not in all AK floodplains
  • Toxic concentrations of ions build up
  • Limit soil processes which supply plants with N
    and P

5
http//soilslab.cfr.washington.edu/nwfsc/2001Summe
r/index.html
6
Alder to the Rescue
  • Species Alnus incana subsp. Tenuifolia
  • Thinleaf Alder
  • Important for
  • Soil development
  • Stand development

http//www.kenaiwetlands.net/images/297m1b01.jpg
7
Alders
  • Symbiotic actinorhizal bacteria (root nodes)
  • 60-70 of total N accumulation during 200 yrs of
    floodplain succession
  • Top 2 m had 4x increase in N in 20 yrs
  • SOM
  • 50 of OM comes from leaves
  • Erosion control
  • Extensive root system

8
Results
  • More N in the soil
  • Less erosion
  • Increased terrace height
  • Decrease flooding
  • Increased distance to water
  • table
  • Less salty

http//nrm.salrm.uaf.edu/dverbyla/bnz_synthesis_C
D/chapter3/alluvial_terraces_tanana_river.jpg
9
And in the end . . .
  • New plant establishment (succession)

Shrubs
Conifers
Deciduous Trees
Paper Birch
Trembling Aspen
White Spruce
Black Spruce
Willow
Thinleaf Alder
Climax
Time
10
Andrews LTERThe Pacific Northwest
Alnus rubra and Pseudotsuga manziesiis role in
forest development
11
Red Alder and Douglas FirA unique relationship
over a complex landscape
  • Inceptisols are the dominant soil type
  • Alfisols and Spodosols present also
  • Forests range from young gt25yrs to old growth
    lt400yrs
  • An area with considerable potential for C
    sequestration
  • Major Disturbances flood, windfall and fire

12
Red Alders (Alnus rubra)
  • Often first to succeed following disturbance
  • N-fixing because of symbiotic actinomycete
    frankia
  • Leaf fall is a major source of Nitrogen/humus
  • Erosion Control

13
2 Soil Types Examined
  • Nutrient rich soil
  • Nutrient poor soil

3 Different Relationships
  • Douglas-fir monoculture
  • Douglas-fir and Alder stand
  • Alder monoculture

14
Conifer
Nutrient Rich Soil
Conifer Alder
Alder
  • Largest biomass production
  • Straight competition between the 2 species
  • Alder eventually out-competed
  • Slow steady biomass accumulation

15
Nutrient Poor Soil
Conifer
Conifer Alder
Alder
  • Quick increase in biomass
  • Short lived (50yrs)
  • Largest Biomass production
  • Large fast growth, short lived (70yrs)
  • Overtaken by conifers

16
Red Alder in H.J. Andrews
  • Increase total stand and conifer growth in ¼ of
    the forested land
  • Decrease total stand and conifer growth in ½
  • Most useful on nutrient poor sites
  • Important in Erosion Control

17
Conclusions
  • In the Tanana River floodplain alders act as an
    ecosystem engineer to aid in forest succession
  • In the H.J. Andrews experimental forest alders
    act as ecosystem engineers in nutrient poor soils
  • In both sites alders are important because of
    their symbiotic relationship with nitrogen fixing
    bacteria and extensive root systems

18
Works Cited
  • Chapin, F.S. III, M. Oswood, K. Van Cleve, L.A.
    Viereck, and D. Verbyla. 2006. Alaska's Changing
    Boreal Forest. Oxford University Press. New York.
  • Dyrness, C.T. and K. Van Cleve. 1993. Control of
    surface soil chemistry in early-successional
    floodplain soils along the Tanana River, interior
    Alaska. Canadian Journal of Forest Research
    23979-994.
  • Van Cleve, K. , L.A. Viereck and G.M. Marion.
    1993. Introduction and overview of a study
    dealing with the role of salt-affected soils in
    primary succession on the Tanana River floodplain
    of interior Alaska. Canadian Journal of Forest
    Research 23 879-888.
  • Van Cleve, K., J. Yarie, L.A. Viereck and C.T.
    Dyrness. 1993. Conclusions on the role of
    salt-affected soils in primary succession on the
    Tanana River floodplain, interior Alaska.
    Canadian Journal of Forest Research 231015-1018.
  • Viereck, L.A., C.T. Dyrness and M.J. Foote. 1993.
    An overview of the vegetation and soils of the
    floodplain ecosystems of the Tanana River,
    interior Alaska. Canadian Journal of Forest
    Research 23889-898.
  • Binkley, Dan. 2004. A hypothesis about the
    interaction of tree dominance and stand
    production through stand development. Forest
    Ecology and Management. 190 265-271

19
More Works Cited
  • Griffiths, R. P., Bradshaw, G. A., Marks, B., and
    G. W. Lienkaemper. 1996. Spatial distribution of
    ectomycorrhizal mats in coniferous forests of the
    Pacific Northwest, USA. Plant and Soil
    180147-158
  • Radosevich, S.,Hibbs, D.,Ghersa, C. 2006. Effects
    of species mixtures on growth and stand
    development of Douglas-fir and red alder, Can. J.
    For. Res. 36 768-782
  • Griffiths, R. P., Bradshaw, G. A., Marks, B., and
    G. W. Lienkaemper. 1996. Spatial distribution of
    ectomycorrhizal mats in coniferous forests of the
    Pacific Northwest, USA. Plant and Soil
    180147-158

20
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