Carbon Sequestration

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Carbon Sequestration

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Title: Carbon Sequestration


1
Carbon Sequestration
  • Darmawan Prasodjo

2
Introduction Background
  • Under Kyoto Protocol industrialized countries
    have pledged to reduce their carbon emissions to
    below 1990 emission levels over period 2008-2012.
  • A number of AF practices are known to stimulate
    the absorption of atmospheric carbon or reduce
    GHG emission at relatively modest cost. (McCarl,
    Schneider, Murray 2001)
  • Proposal the inclusion of three broad land
    management activities forest, cropland and
    grazing land management (Feng et al 2000).

3
Introduction Sequestration
  • Sequestration reducing atmospheric carbon stock
    by removing carbon from the atmosphere and
    storing it in soil or biomass.

4
Sequestration Forestry Ag activities
(McCarl presentation, Purdue University, April
2003)
5
Why Sequestration ?
  • Society is searching for low cost options.
  • Forest and Ag costs estimated near 100 per ton
    carbon for Kyoto implementation. Non ag costs are
    bigger
  • (McCarl presentation, Purdue University, April
    2003)
  • The climate benefit of one ton of sequestered
    carbon and one ton of non emitted carbon are
    roughly equivalent

6
Sequestration Potential
  • Carbon sequestration potential of US cropland
    through improvement management is 75 208
    MMTC/year (Lal et al).
  • Soil sinks and forest sinks could potentially be
    used by US to meet half of its emission reduction
    commitment.

7
Bridge To The Future
  • Costs of sequestration are significantly lower
    than GHGs emissions abatement costs in the energy
    system.
  • Carbon sequestration can serve as the bridge to
    the future.

8
Permanence Issue
  • Saturation storage reservoirs fill up due to
    physical or biological capacity
  • Volatility carbon released through land use
    change, tillage change, harvesting, fires, or
    other natural disturbance

9
Permanence Issue Saturation
Gitz et al 2004
  • Sequestration accumulates carbon until absorptive
    capacity is used up
  • West and Post find a 10-15 year period for
    tillage changes.
  • Birdsey shows a longer period 30-70 years for
    forest carbon.
  • Majority of gains occur in the first couple of
    decades.

10
Permanence issues Volatility
Gitz et al 2004
  • When practice is discontinued, reverting from
    reduced back to conventional tillage, most of the
    carbon is released quickly.
  • If one is to permanently retain then the program
    must be designed to both encourage and maintain a
    change in land management
  • May also lead to discounts ala McCarl and Murray.

11
Economics Drive Abatement
  • How efficient is carbon saving technology.
  • Rate and speed of abatement

12
Economics Drive Sequestration
  • Cost of sequestration (McCarl, April 2003)
  • Afforestation land cost opportunity. (Gitz et
    al 2004)

13
Economics Drive Land Opportunity Cost
  • Costs of sequestration are indeed affected by the
    opportunity costs of lands diverted from other
    uses to sequester carbon.
  • Average net revenue of agricultural land in 1997
    to evaluate the marginal opportunity cost of
    using land for sequestration purposes.

14
Economic Drive Cost of Carbon(already discussed
in the class)
  • Carbon will cost money to produce, sell, and
    measure.

DISC (1-ADD)(1-LEAK)(1-UNCER)(1-PERM)
(McCarl, April 2003)
15
Timing Of Sequestration
  • Sequestration potential should start immediately
    as a brake slowing down both the rate of growth
    of concentration and the rate of abatement in the
    energy sector (Gitz et al 2004)
  • Carbon sinks should be utilized as early
    possible, and carbon flow into sinks should last
    until the atmospheric carbon concentration is
    stabilized. (Feng, Kling 2002)

16
Optimal Control Model Setup
  • Motion for C(t)
  • (1)
  • Motion for A(t)
  • (2)
  • Social planners net payoff function
  • (3)

Maximizing (3) subject to (1) and (2) yields the
optimal carbon sequestration and emission level
over time.
17
Optimal Control Optimal Paths of Sequestration
  • Current value of Hamiltonian
  • (4)
  • (5)
  • (6)

18
Optimal Control Optimal Paths of Sequestration
  • (7)
  • Transversality condition
  • (8)

19
Optimal Control Steady State
Assuming that a steady state exists, setting
and using (1), (2), (6) and (7), we can derive
(iv)
(i)
(ii)
(v)
(iii)
20
Optimal Control Long Run Emission
(i)
  • Carbon sequestration activities do not play
    additional role in the long run.
  • Emissions should be in balance with reduction due
    to the natural decay

21
Optimal Control Sequestration in Steady State
From (ii), (iii) and (iv) we can derive
From (iii) we can sign
D(.) gt 0
We can deduce the sign
Q(.) gt 0
22
Optimal Control Sequestration in Steady State
  • This means that
  • The result of using sequestration during the
    transition path toward the steady state (Feng et
    al 2002)
  • Sequestration does affect the process of reaching
    long run targets.

23
Optimal ControlMarginal Cost of Sequestration
(steady state)
From (iv) we can
interpret
  • amount of sequestration depends on the Q(.),
    marginal cost of sequestration
  • Q(.) is lower (sequestration more effective),
    then the amount of sequestration is higher.

24
Marginal Cost of Sequestration(empirical)
Annual offset arising from agricultural soils
(McCarl et al 2001)
Annual offset arising from forest (McCarl et al
2001)
  • The amount of sequestration increases as the
    sequestration technique is becoming more
    effective.
  • Steady state analysis is empirically confirmed.

25
Optimal Control Carbon Marginal Abatement Cost
(MAC)
From (ii), (iii) and (iv) we can derive
B(.) represents the marginal benefit of emission
which is equivalent to Marginal Abatement Cost
(MAC)
Replacing B(.) with MAC
As the marginal abatement cost is increasing,
the amount of carbon sequestration is also
increasing
26
Optimal Control Carbon Marginal Abatement Cost
(MAC)

MAC0
MAC0
Seq market
Seq0
A0
Abatement
L0
Lpolicy
Panel A
as MAC increases, the amount of sequestration
also increases which is in synch with the result
of steady state
27
Payment Scheme PAYG(Pay-As-You-Go)
  • Owners sinks sell and repurchase emission credits
    based simply on the permanent reduction of
    carbon.
  • A farmer who adopts conservation tillage
    practices on 100 acres may earn 200 permanent
    carbon.
  • If in the fifth year, the farmer plows the land,
    he would be required to purchase carbon credits.

(Feng, Zhao, Kling 2000)
28
Payment Scheme VLC (Variable-Length-Contract)
  • VLC system evolves through independent broker
    arrangements.
  • A broker wishes to buy permits from sink sources
    and sell them to emitters
  • The broker must contract with sink sources to
    achieve permanent reduction.
  • Permanent carbon reduction is produced from a
    series of temporary reduction.
  • Broker contacts farmer 1 to sign a contract to
    adopt conservation tillage, say 3 years before
    plowing the land.
  • Broker contacts farmer 2 to plant trees at
    beginning of year 4.

(Feng, Zhao, Kling 2000)
29
Payment Scheme CAA Carbon Annuity Account
  • The generator of a sink is paid the full value of
    the permanent reduction in the GHGs stored in
    the sink.
  • Payment is put directly into the annuity account.
  • Owner can access the earning of the account as
    long as the sink remains in place.
  • The principal is withdrawn when and if the sink
    is removed.
  • If the sink remains permanently, the sink owners
    eventually earns all the interest.

(Feng, Zhao, Kling 2000)
30
Conclusion
  • Agricultural and forest carbon sequestration are
    important components in response to a greenhouse
    gas emission
  • Sequestration should not be treated the same as
    abatement/reduction. Sequestration always has the
    potential to be temporary.
  • Sequestration does affect the path of reaching
    long run targets.

31
Conclusion
  • Marginal sequestration cost affects the amount of
    carbon sequestered in the long run.
  • The carbon MAC of the industry also affects the
    amount of sequestered carbon. As the MAC
    increases, the amount of carbon sequestration
    also increases.  
  • On the whole, it does not matter whether the
    reduction is done by sequestration or emission
    abatement as long as there is less carbon in the

32
References
  • Birdsey, R.A 1996. Carbon Storage for Major
    Forest Types and Regions in the Contiguous United
    States. . Chapter 1, Forest and Global
    Change, in Vol. 2 Forest Management
    Opportunities for Mitigating Carbon Emissions,
    edited by R.N Sampson and D. Hair. Washington,
    D.C. American Forest.
  • Feng, H, Zhao, J and Kling C. 2000. Carbon
    Sequestration in Agriculture Value and
    Implementation. Working Paper 00-WP 256, Center
    for Agricultural and Rural Development, Iowa
    States University.
  • Feng, H, Zhao, J and Kling, C. 2002 The Time
    Path and Implementation of Carbon Sequestration,
    AJAE, 84, February 2002134-149.
  • Gitz, V, Hourcade, J,C, Ciais, P. 2004.  Energy
    Implications of Optimal Timing of Biological
    Carbon Sequestration . The Energy Journal, 04
    August 2004.
  • Grubler, A., N.Naicenovik, and W.D. Nordhaus,
    The technological change and the environment,
    RFF Washington-DC and IIASA Laxenbury-Austria,
    2002.
  • Intergovernmental Panel on Climate Change (IPCC).
    May 2000 Summary for Policymakers-Land Use,
    Land-Use Change, and Forestry.
  • Kurkalova, L, Kling, C, Zhao J. 2001.
    Institution and the Value of Nonpoint Source
    Measurement Technology Carbon Sequestration in
    Agricultural Soils. Working Paper 00-WP 338,
    Center for Agricultural and Rural Development,
    Iowa States University. 
  • Kurkalova, L, Kling, C, Zhao, J. 2003. Multiple
    Benefits of Carbon Friendly Agricultural
    Practices Empirical Assessment of Conservation
    Tillage. Working Paper 03-WP 326, Center for
    Agricultural and Rural Development, Iowa States
    University.

33
References
  • McCarl, B.A 2003. Cost of Carbon Ideas and
    Research Direction. Presentation for Climate
    Change Segment of Advance Resources Class.
  • McCarl, B.A, and Schneider, U.A. 2000.
    Agricultures Role in a Greenhouse Gas Emission
    Mitigation World An Economic Perspective.
    Review of Agricultural Economics 22 134 59.
  • McCarl, B.A, Murray, B.C, Schneider, U.A. 2001.
    Influences of Permanence on the Comparative
    Value of Biological Sequestration versus
    Emissions Offsets. Working Paper 01-WP 282,
    Center for Agricultural and Rural Development,
    Iowa States University 
  • Schneider, U.A, McCarl, B.A, Murray, B.C,
    Williams, J.R, Sand, R.D. 2001. Economic
    Potential of Greenhouse Gas Emission Reductions
    Comparative Role for Soil Sequestration in
    Agriculture and Forestry. Working Paper 01-WP
    281, Center for Agricultural and Rural
    Development, Iowa State University. 
  • Schneider, U.A. 2002 "The Cost of Agricultural
    Carbon Saving", Working Paper 02-WP 306, Center
    for Agricultural and Rural Development, Iowa
    State University. 
  • Kooten, V, Grainger A, Ley, A, Marland, G, and
    Solberg, B. 1997. Conceptual Issues Related to
    Carbon Sequestration Uncertainty and Time.
    Critical Rev. Environ. Sci. Technol 
  • Richard, K.R. 1997. The Time Value of Carbon in
    Bottom-up Studies. Critical Rev. Environ.Sci
    Technol. 27 S279-S292.
  • West, T., Post, J.A and Marland, J. 2000. Review
    of Task 2.1 National Carbon Sequestration
    Assessment. Paper presented at Department of
    Energy Center for Research on Enhancing Carbon
    Sequestration in Terrestrial Ecosystem (CSITE)
    Program Review, Oakridge National Laboratories,
    TN, November. 
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