TY - JOUR
T1 - Fine-root mortality rates in a temperate forest
T2 - Estimates using radiocarbon data and numerical modeling
AU - Riley, W. J.
AU - Gaudinski, J. B.
AU - Torn, M. S.
AU - Joslin, J. D.
AU - Hanson, P. J.
PY - 2009/10
Y1 - 2009/10
N2 - Summary We used an inadvertent whole-ecosystem 14C label at a temperate forest in Oak Ridge, Tennessee, USA to develop a model (Radix1.0) of fine-root dynamics. Radix simulates two live-root pools, two dead-root pools, non-normally distributed root mortality turnover times, a stored carbon (C) pool, and seasonal growth and respiration patterns. We applied Radix to analyze measurements from two root size classes (< 0.5 and 0.5-2.0 mm diameter) and three soil-depth increments (O horizon, 0-15 cm and 30-60 cm). Predicted live-root turnover times were < 1 yr and ∼10 yr for short- and long-lived pools, respectively. Dead-root pools had decomposition turnover times of ∼2 yr and ∼10 yr. Realistic characterization of C flows through fine roots requires a model with two live fine-root populations, two dead fine-root pools, and root respiration. These are the first fine-root turnover time estimates that take into account respiration, storage, seasonal growth patterns, and non-normal turnover time distributions. The presence of a root population with decadal turnover times implies a lower amount of belowground net primary production used to grow fine-root tissue than is currently predicted by models with a single annual turnover pool.
AB - Summary We used an inadvertent whole-ecosystem 14C label at a temperate forest in Oak Ridge, Tennessee, USA to develop a model (Radix1.0) of fine-root dynamics. Radix simulates two live-root pools, two dead-root pools, non-normally distributed root mortality turnover times, a stored carbon (C) pool, and seasonal growth and respiration patterns. We applied Radix to analyze measurements from two root size classes (< 0.5 and 0.5-2.0 mm diameter) and three soil-depth increments (O horizon, 0-15 cm and 30-60 cm). Predicted live-root turnover times were < 1 yr and ∼10 yr for short- and long-lived pools, respectively. Dead-root pools had decomposition turnover times of ∼2 yr and ∼10 yr. Realistic characterization of C flows through fine roots requires a model with two live fine-root populations, two dead fine-root pools, and root respiration. These are the first fine-root turnover time estimates that take into account respiration, storage, seasonal growth patterns, and non-normal turnover time distributions. The presence of a root population with decadal turnover times implies a lower amount of belowground net primary production used to grow fine-root tissue than is currently predicted by models with a single annual turnover pool.
KW - Carbon cycling
KW - Carbon isotope
KW - Fine-root turnover time
KW - Monte Carlo simulations
KW - Numerical model
KW - Radiocarbon
KW - Root model parameterization
KW - Roots
UR - http://www.scopus.com/inward/record.url?scp=70349504567&partnerID=8YFLogxK
U2 - 10.1111/j.1469-8137.2009.02980.x
DO - 10.1111/j.1469-8137.2009.02980.x
M3 - Article
C2 - 19694965
AN - SCOPUS:70349504567
SN - 0028-646X
VL - 184
SP - 387
EP - 398
JO - New Phytologist
JF - New Phytologist
IS - 2
ER -