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Disturbance and recovery of soil C following infrequent activities

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Title: Disturbance and recovery of soil C following infrequent activities


1
Disturbance and recovery of soil C following
infrequent activities
  • Rich Conant, Keith Paustian,
  • Mark Easter, Amy Swan
  • Natural Resource Ecology Laboratory
  • Colorado State University

Supported by CASMGS-USDA/CSREES
2
Background
3
Background
4
Background
  • Periodic use of plow or chisel can increase
    yields
  • In IL (58) and IN (77), most (corn/soybean)
    fields are in NT
  • But, most (57 and 59) of those fields are under
    NT less than two years and the average time under
    continuous NT is less than 2.5 years.
  • For MN, NT is less common (21 of all fields) and
    less than 10 have had continuous NT for more
    than one year

Source Hill, PM. 2001. Use of continuous no-till
and rotational tillage systems in the central and
northern corn belt. J of Soil Water Cons. 56
286-290
  • How does soil C content for fields that are
    tilled occasionally from fields that are not
    tilled?
  • How does inclusion of non-disruptive, high input
    crops impact soil C stocks?

5
Literature data - tillage
Pierce et al. East Lansing, MI Continuous corn.
Decline in SOC stocks, but all treatments
mysteriously lost SOC. Declines greater for
tilled soils than for NT.
VandenBygaart et al. S. Ontario Cash-cropping.
Soil C distributed throughout the profile. No
measurable decline in SOC stocks.
Stockfish et al. S. Saxony NT SOC stocks
declined to match CT stocks after moldboard
plowing to 30cm.
6
Literature data meadow/hay
7
Observations
  • From the published literature
  • All results are solid published in the
    peer-reviewed literature
  • Methods vary some (i.e., sampling depth, methods,
    etc.)
  • We have every reason to believe the results
  • But
  • There are only a few published studies
  • Results for those studies vary substantially from
    place to place
  • This makes it difficult to draw conclusions about
    what might happen elsewhere
  • Furthermore
  • Infrequent activities and their impact on soil C
    stocks are not the focus for most agricultural
    field stations
  • Incorporating variable tillage frequency or
    meadow duration into experimental design would be
    a challenge
  • Integrating this type of experiment with other
    ongoing experiments is impractical

8
Methods model, tillage impacts
  • Century model
  • Cultivation modeled as
  • Transfer of organic matter from surface into
    soils (CULTRA)
  • Multiplicative effect on organic matter
    decomposition (CULTEFF)
  • Parameters vary from 1 to 6
  • Values depend on degree of soil stirring and
    disruption

metabolic C
Lignin content
CO2
Structural C
Active C
CO2
CO2
CO2
CO2
Slow C
CO2
Passive C
CO2
9
Methods model performance
Morrow Plots
10
Methods model performance
Hoytville
11
Methods sites, model runs
Sites E. Lansing, MI cool, mesic, 46 silt plus
clay, corn Hoytville, OH warm, mesic, 79 silt
plus clay, corn-soybean corn-oats-meadow Manhat
tan, KS warm, mesic, 92 silt plus clay,
wheat Sidney, NE warm, semiarid, 60 silt plus
clay, wheat-fallow (unique) Lethbridge, SK
cool, semiarid, 54 silt plus clay
fallow-wheat-wheat-hay
Model experiments NT, CT, NT2, NT4, NT6, NT8,
NT10 COM, COMM, COMMM, etc.
12
Results tillage frequency
13
Results tillage frequency
14
Results tillage frequency
15
Results tillage frequency
16
Results meadow frequency
17
Results hay frequency
18
Results tillage frequency
19
Results meadow duration
20
Conclusions
  • Tillage leads to decreased soil C stocks
  • True at all sites, rotations
  • Increased tillage frequency leads to greater
    declines in soil C stocks
  • Responses vary from site to site
  • Largest responses observed at E. Lansing, MI and
    Manhattan, KS
  • Average NT2 was 90 of NT after 20 years and
    slightly greater for decreased tillage frequency
  • Meadow/Hay in rotation can increase soil C
    stocks, but may not
  • Inputs drive net soil C response (in model)
  • This makes it difficult to draw conclusions about
    what might happen elsewhere
  • Summary
  • Infrequent activities can have a significant
    impact on soil C stocks
  • Modeled responses are a result of disturbance and
    C inputs
  • Improved yield assessments could improve results
  • Tools exist with which to assess impacts of
    infrequent activities, but their accuracy needs
    to be evaluated
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