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Title: Partitioning sources of soil-respired CO2 and their seasonal variation using a unique radiocarbon tracer

Abstract

Soil respiration is derived from heterotrophic (decomposition of soil organic matter) and autotrophic (root/rhizosphere respiration) sources, but there is considerable uncertainty about what factors control variations in their relative contributions in space and time. We took advantage of a unique whole-ecosystem radiocarbon label in a temperate forest to partition soil respiration into three sources: (1) recently photosynthesized carbon (C), which dominates root and rhizosphere respiration; (2) leaf litter decomposition and (3) decomposition of root litter and soil organic matter 41-2 years old. Heterotrophic sources and specifically leaf litter decomposition were large contributors to total soil respiration during the growing season. Relative contributions from leaf litter decomposition ranged from a low of 1 3% of total soil respiration (63 mgCm 2 h 1) when leaf litter was extremely dry, to a high of 42 16% (96 38mgCm 2 h 1). Total soil respiration fluxes varied with the strength of the leaf litter decomposition source, indicating that moisture-dependent changes in litter decomposition drive variability in total soil respiration fluxes. In the surface mineral soil layer, decomposition of C fixed in the original labeling event (3-5 years earlier) dominated the isotopic signature of heterotrophic respiration. Root/rhizosphere respiration accounted for 16 10% to 64more » 22% of total soil respiration, with highest relative contributions coinciding with low overall soil respiration fluxes. In contrast to leaf litter decomposition, root respiration fluxes did not exhibit marked temporal variation ranging from 34 14 to 40 16mgCm 2 h 1 at different times in the growing season with a single exception (88 35 mgCm 2 h 1). Radiocarbon signatures of root respired CO2 changed markedly between early and late spring (March vs. May), suggesting a switch from stored nonstructural carbohydrate sources to more recent photosynthetic products.« less

Authors:
 [1];  [1];  [2]
  1. University of California, Irvine
  2. ORNL
Publication Date:
Research Org.:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Oak Ridge National Environmental Research Park
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
930811
DOE Contract Number:  
DE-AC05-00OR22725
Resource Type:
Journal Article
Journal Name:
Global Change Biology
Additional Journal Information:
Journal Volume: 12; Journal ID: ISSN 1354-1013
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; CARBOHYDRATES; CARBON DIOXIDE; FORESTS; ORGANIC MATTER; RESPIRATION; SEASONAL VARIATIONS; SEASONS; SOILS

Citation Formats

Cisneros-Dozal, Luz Maria, Trumbore, Susan E., and Hanson, Paul J. Partitioning sources of soil-respired CO2 and their seasonal variation using a unique radiocarbon tracer. United States: N. p., 2006. Web. doi:10.1111/j.1365-2486.2005.001061.x.
Cisneros-Dozal, Luz Maria, Trumbore, Susan E., & Hanson, Paul J. Partitioning sources of soil-respired CO2 and their seasonal variation using a unique radiocarbon tracer. United States. https://doi.org/10.1111/j.1365-2486.2005.001061.x
Cisneros-Dozal, Luz Maria, Trumbore, Susan E., and Hanson, Paul J. 2006. "Partitioning sources of soil-respired CO2 and their seasonal variation using a unique radiocarbon tracer". United States. https://doi.org/10.1111/j.1365-2486.2005.001061.x.
@article{osti_930811,
title = {Partitioning sources of soil-respired CO2 and their seasonal variation using a unique radiocarbon tracer},
author = {Cisneros-Dozal, Luz Maria and Trumbore, Susan E. and Hanson, Paul J},
abstractNote = {Soil respiration is derived from heterotrophic (decomposition of soil organic matter) and autotrophic (root/rhizosphere respiration) sources, but there is considerable uncertainty about what factors control variations in their relative contributions in space and time. We took advantage of a unique whole-ecosystem radiocarbon label in a temperate forest to partition soil respiration into three sources: (1) recently photosynthesized carbon (C), which dominates root and rhizosphere respiration; (2) leaf litter decomposition and (3) decomposition of root litter and soil organic matter 41-2 years old. Heterotrophic sources and specifically leaf litter decomposition were large contributors to total soil respiration during the growing season. Relative contributions from leaf litter decomposition ranged from a low of 1 3% of total soil respiration (63 mgCm 2 h 1) when leaf litter was extremely dry, to a high of 42 16% (96 38mgCm 2 h 1). Total soil respiration fluxes varied with the strength of the leaf litter decomposition source, indicating that moisture-dependent changes in litter decomposition drive variability in total soil respiration fluxes. In the surface mineral soil layer, decomposition of C fixed in the original labeling event (3-5 years earlier) dominated the isotopic signature of heterotrophic respiration. Root/rhizosphere respiration accounted for 16 10% to 64 22% of total soil respiration, with highest relative contributions coinciding with low overall soil respiration fluxes. In contrast to leaf litter decomposition, root respiration fluxes did not exhibit marked temporal variation ranging from 34 14 to 40 16mgCm 2 h 1 at different times in the growing season with a single exception (88 35 mgCm 2 h 1). Radiocarbon signatures of root respired CO2 changed markedly between early and late spring (March vs. May), suggesting a switch from stored nonstructural carbohydrate sources to more recent photosynthetic products.},
doi = {10.1111/j.1365-2486.2005.001061.x},
url = {https://www.osti.gov/biblio/930811}, journal = {Global Change Biology},
issn = {1354-1013},
number = ,
volume = 12,
place = {United States},
year = {2006},
month = {1}
}