Terrestrial c sequestration at elevated co2 and temperature: the role of dissolved organic n loss
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Citations
Elevated CO2 stimulates net accumulations of carbon and nitrogen in land ecosystems: a meta-analysis.
Organic C and N stabilization in a forest soil: Evidence from sequential density fractionation
Organic C and N stabilization in a forest soil: Evidence from sequential density fractionation
Explicitly representing soil microbial processes in Earth system models
Adaptation of forests and people to climate change - a global assessment report.
References
Amino Acid Absorption by Arctic Plants: Implications for Plant Nutrition and Nitrogen Cycling
Fine Roots, Net Primary Production, and Soil Nitrogen Availability: A New Hypothesis
Thermodynamic constraints on nitrogen transformations and other biogeochemical processes at soil-stream interfaces
Soil C:N ratio as a predictor of annual riverine DOC flux at local and global scales
Thermodynamic constraints on nitrogentransformations and other biogeochemicalprocesses at soil–stream interfaces
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Frequently Asked Questions (14)
Q2. What are the future works in "Running head: role of don losses in carbon sequestration carbon sequestration in terrestrial ecosystems under elevated co2 and temperature: role of dissolved organic versus inorganic nitrogen loss" ?
The best potential for testing their ideas in a timely manner would be to experimentally manipulate ecosystems where the masking effects of within-ecosystem responses are likely to be small relative to the effects of DON losses to determine if there is a trend toward high C sequestration with low DON losses relative to DIN losses. Thus the manipulations should be on ecosystems where the C: N ratio of vegetation is low ( i. e., close to the C: N ratio of soils so that the redistribution of N has a smaller effect ), where the vegetation is unlikely to increase in woodiness ( i. e., to avoid the masking effects of increasing C: N ratios ), and where the total throughput of DON plus DIN is high ( i. e., a high potential to sequester N ). Their aim in this paper has been to examine how considering the relative magnitudes of DON versus DIN losses might influence assessments of potential C sequestration in terrestrial ecosystems. Their conclusions are that it is vital to quantify these fluxes at least in regards to evaluations of the long-term potential for C sequestration.
Q3. What can be done to help mask the effects of DON losses?
In addition, increases in plant and soil C:N ratios can contribute to the withinecosystem responses and help mask the effects of DON losses.
Q4. What is the effect of carbon sequestration in terrestrial ecosystems?
Terrestrial ecosystems are thought to sequester about 25% of the carbon (C) currentlyemitted through fossil-fuel burning and land-use change (IPCC 2001).
Q5. What is the way to test the effects of DON loss on the ecosystem?
The best potential for testing their ideas in a timely manner would be to experimentally manipulate ecosystems where the masking effects of within-ecosystem responses are likely to be small relative to the effects of DON losses to determine if there is a trend toward high C sequestration with low DON losses relative to DIN losses.
Q6. How long did the gradual-change simulations take to develop?
With high DON losses, N gains and losses were small during the first 100 years of all the simulations, and the dynamics in the gradual-change simulations generally lagged behind those in the instantaneous-change simulations by about two decades.
Q7. What is the effect of the gradual-change simulations on the sequestration of N?
Increases in plant and soil C:N ratios contributed less to C sequestration, but in amounts proportionately equivalent to their contributions in the instantaneous-change simulations.
Q8. What is the potential for accumulating N by limiting N losses in terrestrial ecosystems?
In this paper the authors argue that the amount of C sequestered in terrestrial ecosystems in response to elevated CO2 depends on the fraction of N losses that are in the form of dissolved organic N (DON) versus dissolved inorganic N (DIN); because plants can curtail DIN losses as N demand increases in response to elevated CO2, but plants have little control over DON losses, the potential for accumulating N by limiting N losses should be small if DON losses are high.
Q9. What is the effect of increasing the C:N ratio of soils on the ecosystem?
Because the C:N ratio of soils is about 25 and that of plants is about 143 (initial C:N values), this redistribution of N results in a net increase in the amount of C stored per unit N in the ecosystem.
Q10. What is the standard model of carbon sequestration in terrestrial ecosystems?
Their assessment of C sequestration in relation to DON losses relies upon threemodifications to what has been called "the standard model" of N accumulation in terrestrial ecosystems (Vitousek et al. 1998).
Q11. How much of the C sequestered in the ecosystems with low DON losses?
On average, the ecosystems sequestered only about 1 kg C m-2 between years 60 and 1000 or about 7% of the C sequestered during the first 60 years and 6% of the C sequestered in the ecosystems with low DON losses (Fig. 1).
Q12. How long does the C sequestration continue?
Sequestration of C continues for the duration of all low-DON-loss simulations, although at a rate that is only about 17% of that during the first 60 years (Fig. 1,Table 3).
Q13. Why did the models exhibit higher DOC loss?
Because of the explicit linkages between DOC and DON in the various model structures,simulations with higher DON loss also exhibit higher DOC loss.
Q14. What is the effect of elevated CO2 on the N stored in the ecosystem?
with a combination of elevated CO2 and warming, increases in woody tissues and the consequent increase in plant C:N ratio contributed significantly to an increase the C stored per unit N in the ecosystem (Fig. 2).