MétaCan
Menu
Back to cohort

Soil carbon sequestration in a pine forest after 9 years of atmospheric CO<sub>2</sub> enrichment

2008· article· en· W2158584557 on OpenAlexaff
John Lichter, Sharon Billings, Susan E. Ziegler, Deeya Gaindh, Rebecca Ryals, Adrien C. Finzi, Robert B. Jackson, Elizabeth A. Stemmler, William H. Schlesinger

Bibliographic record

VenueGlobal Change Biology · 2008
Typearticle
Languageen
FieldAgricultural and Biological Sciences
TopicSoil Carbon and Nitrogen Dynamics
Canadian institutionsMemorial University of Newfoundland
FundersU.S. Department of EnergyOffice of ScienceNational Science Foundation
KeywordsForest floorEnvironmental scienceCarbon sequestrationEcosystemSoil waterOrganic matterLitterLeaching (pedology)Soil organic matterForest ecologyCarbon sinkPlant litterTerrestrial ecosystemEnvironmental chemistrySoil carbonCyclingCarbon dioxideEcologySoil scienceChemistryForestryBiology

Abstract

fetched live from OpenAlex

Abstract The impact of anthropogenic CO 2 emissions on climate change may be mitigated in part by C sequestration in terrestrial ecosystems as rising atmospheric CO 2 concentrations stimulate primary productivity and ecosystem C storage. Carbon will be sequestered in forest soils if organic matter inputs to soil profiles increase without a matching increase in decomposition or leaching losses from the soil profile, or if the rate of decomposition decreases because of increased production of resistant humic substances or greater physical protection of organic matter in soil aggregates. To examine the response of a forest ecosystem to elevated atmospheric CO 2 concentrations, the Duke Forest Free‐Air CO 2 Enrichment (FACE) experiment in North Carolina, USA, has maintained atmospheric CO 2 concentrations 200 μL L −1 above ambient in an aggrading loblolly pine ( Pinus taeda ) plantation over a 9‐year period (1996–2005). During the first 6 years of the experiment, forest‐floor C and N pools increased linearly under both elevated and ambient CO 2 conditions, with significantly greater accumulations under the elevated CO 2 treatment. Between the sixth and ninth year, forest‐floor organic matter accumulation stabilized and C and N pools appeared to reach their respective steady states. An additional C sink of ∼30 g C m −2 yr −1 was sequestered in the forest floor of the elevated CO 2 treatment plots relative to the control plots maintained at ambient CO 2 owing to increased litterfall and root turnover during the first 9 years of the study. Because we did not detect any significant elevated CO 2 effects on the rate of decomposition or on the chemical composition of forest‐floor organic matter, this additional C sink was likely related to enhanced litterfall C inputs. We also failed to detect any statistically significant treatment effects on the C and N pools of surface and deep mineral soil horizons. However, a significant widening of the C : N ratio of soil organic matter (SOM) in the upper mineral soil under both elevated and ambient CO 2 suggests that N is being transferred from soil to plants in this aggrading forest. A significant treatment × time interaction indicates that N is being transferred at a higher rate under elevated CO 2 ( P =0.037), suggesting that enhanced rates of SOM decomposition are increasing mineralization and uptake to provide the extra N required to support the observed increase in primary productivity under elevated CO 2 .

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.040
Threshold uncertainty score0.536

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.023
GPT teacher head0.232
Teacher spread0.209 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations96
Published2008
Admission routes1
Has abstractyes

Explore more

Same venueGlobal Change BiologySame topicSoil Carbon and Nitrogen DynamicsFrench-language works237,207