Publication | Closed Access
Belowground Carbon Allocation in Forest Ecosystems: Global Trends
804
Citations
44
References
1989
Year
BiogeochemistryCarbon SequestrationSoil RespirationSitu Soil RespirationEngineeringSoil Carbon CycleForestryForest CarbonForest SoilCarbon AllocationDeforestationForest BiomassBelowground Carbon Allocation
Carbon allocation to roots in forest ecosystems is estimated from published data on soil respiration and litterfall. The study aims to predict total soil respiration and root carbon allocation from litterfall measurements and to determine live‑root respiration rates to constrain root production estimates. The authors use the positive correlation between soil respiration and litterfall to predict total soil respiration and root carbon allocation from litterfall data. On a global scale, soil respiration and aboveground litter production are highly positively correlated, and across a litterfall gradient of 70–500 g m⁻² yr⁻¹ belowground carbon allocation increases from 260 to 1100 g m⁻² yr⁻¹ while the allocation‑to‑litterfall ratio declines from 3.8 to 2.5 at lower litterfall and stabilizes near 2.2 at higher litterfall, enabling simple carbon budgets to set upper limits on fine root production.
Carbon allocation to roots in forest ecosystems is estimated from published data on soil respiration and litterfall. On a global scale, rates of in situ soil respiration and aboveground litter production are highly and positively correlated, suggesting that above— and belowground production are controlled by the same factors. This relationship also allows us to predict rates of total soil respiration and total carbon allocation to roots in forest ecosystems from litterfall measurements. Over a gradient of litterfall carbon ranging from 70 to 500 g°m — 2 °yr — 1 , total belowground carbon allocation increases from 260 to 1100 g°m — 2 °yr — 1 . The ratio of belowground carbon allocation to litterfall decreases from 3.8 to 2.5 as litterfall carbon increases from 70 to 200 g°m — 2 °yr — 1 , but changes little (2.5 to 2.2) as litterfall carbon increases from 200 to 500 g°m — 2 °yr — 1 . Use of this relationship permits the construction of simple carbon budgets that can be used to place upper limits on estimates of fine root production in forest ecosystems. Determining live—root respiration rates in forest ecosystems will further constrain the range of possible root production rates.
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