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Changes in net ecosystem productivity and greenhouse gas exchange with fertilization of Douglas fir: Mathematical modeling in ecosys Grant, R.F.; Black, T. Andrew; Jassal, Rachhpal S.; Bruemmer, Christian
Abstract
The application of nitrogen fertilizers to Douglas fir forests is known to raise net ecosystem productivity (NEP), but also N2O emissions, the CO2 equivalent of which may offset gains in NEP when accounting for net greenhouse gas (GHG) exchange. However, total changes in NEP and N2O emissions caused by fertilizer between times of application and harvest, while needed for national GHG inventories, are difficult to quantify except through modeling. In this study, integrated hypotheses for soil and plant N processes within the ecosystem model ecosys were tested against changes in CO2 and N2O fluxes recorded with eddy covariance (EC) and surface flux chambers for 1 year after applying 20 g N m−2 of urea to a mature Douglas fir stand in British Columbia. Parameters from annual regressions of hourly modeled versus measured CO2 fluxes conducted before and after fertilization were unchanged (b = 1.0, R2 = 0.8, RMSD = 3.4 mmol m−2 s−1), indicating that model hypotheses for soil and plant N processes did not introduce bias into CO2 fluxes modeled after fertilization. These model hypotheses were then used to project changes in NEP and GHG exchange attributed to the fertilizer during the following 10 years until likely harvest of the Douglas fir stand. Increased CO2 uptake caused modeled and EC‐derived annual NEP to rise from 443 and 386 g C m−2 in the year before fertilization to 591 and 547 g C m−2 in the year after. These gains contributed to a sustained rise in modeled wood C production with fertilization, which was partly offset by a decline in soil C attributed in the model to reduced root C productivity and litterfall. Gains in net CO2 uptake were further offset in the model by a rise of 0.74 g N m−2 yr−1 in N2O emissions during the first year after fertilization, which was consistent with one of 1.05 g N m−2 yr−1 estimated from surface flux chamber measurements. Further N2O emissions were neither modeled nor measured after the first year. At the end of the 11 year model projection, a total C sequestration of 1045 g C m−2 was attributed to the 20 g N m−2 of fertilizer. However, only 119 g C m−2 of this was sequestered in stocks that would remain on site after harvest (foliage, root, litter, soil). The remainder was sequestered as harvested wood, the duration of which would depend on use of the wood product. The direct and indirect CO2‐equivalent costs of this application, including N2O emission, were estimated to offset almost all non‐harvested C sequestration attributed to the fertilizer. An edited version of this paper was published by AGU. Copyright 2010 American Geophysical Union.
Item Metadata
Title |
Changes in net ecosystem productivity and greenhouse gas exchange with fertilization of Douglas fir: Mathematical modeling in ecosys
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Creator | |
Publisher |
American Geophysical Union
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Date Issued |
2010-10
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Description |
The application of nitrogen fertilizers to Douglas fir forests is known to raise net
ecosystem productivity (NEP), but also N2O emissions, the CO2 equivalent of which may
offset gains in NEP when accounting for net greenhouse gas (GHG) exchange. However,
total changes in NEP and N2O emissions caused by fertilizer between times of
application and harvest, while needed for national GHG inventories, are difficult to
quantify except through modeling. In this study, integrated hypotheses for soil and plant
N processes within the ecosystem model ecosys were tested against changes in CO2 and
N2O fluxes recorded with eddy covariance (EC) and surface flux chambers for 1 year
after applying 20 g N m−2 of urea to a mature Douglas fir stand in British Columbia.
Parameters from annual regressions of hourly modeled versus measured CO2 fluxes
conducted before and after fertilization were unchanged (b = 1.0, R2 = 0.8, RMSD =
3.4 mmol m−2 s−1), indicating that model hypotheses for soil and plant N processes did
not introduce bias into CO2 fluxes modeled after fertilization. These model hypotheses
were then used to project changes in NEP and GHG exchange attributed to the fertilizer
during the following 10 years until likely harvest of the Douglas fir stand. Increased CO2
uptake caused modeled and EC‐derived annual NEP to rise from 443 and 386 g C m−2 in
the year before fertilization to 591 and 547 g C m−2 in the year after. These gains
contributed to a sustained rise in modeled wood C production with fertilization, which
was partly offset by a decline in soil C attributed in the model to reduced root C
productivity and litterfall. Gains in net CO2 uptake were further offset in the model by a
rise of 0.74 g N m−2 yr−1 in N2O emissions during the first year after fertilization, which
was consistent with one of 1.05 g N m−2 yr−1 estimated from surface flux chamber
measurements. Further N2O emissions were neither modeled nor measured after the first
year. At the end of the 11 year model projection, a total C sequestration of 1045 g C m−2
was attributed to the 20 g N m−2 of fertilizer. However, only 119 g C m−2 of this was
sequestered in stocks that would remain on site after harvest (foliage, root, litter, soil). The
remainder was sequestered as harvested wood, the duration of which would depend on use
of the wood product. The direct and indirect CO2‐equivalent costs of this application,
including N2O emission, were estimated to offset almost all non‐harvested C sequestration
attributed to the fertilizer. An edited version of this paper was published by AGU. Copyright 2010 American Geophysical Union.
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Genre | |
Type | |
Language |
eng
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Date Available |
2011-05-25
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Provider |
Vancouver : University of British Columbia Library
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Rights |
Attribution-NonCommercial-NoDerivatives 4.0 International
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DOI |
10.14288/1.0041931
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URI | |
Affiliation | |
Citation |
Grant, Robert F.; Black, T. Andrew; Jassal, Rachhpal S.; Bruemmer, Christian. 2010. Changes in net ecosystem productivity and greenhouse gas exchange with fertilization of Douglas fir: Mathematical modeling in ecosys. Journal of Geophysical Research Biogeosciences 115 G04009
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Publisher DOI |
10.1029/2009JG001094
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Peer Review Status |
Reviewed
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Scholarly Level |
Faculty
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Copyright Holder |
Black, T. Andrew
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Rights URI | |
Aggregated Source Repository |
DSpace
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Rights
Attribution-NonCommercial-NoDerivatives 4.0 International