Tree Physiology · 1997 · 93 citations · 36 references
Life SciencesPlant BiologyPlant SciencesPhysiological EcologyPlant EcophysiologyPlant PhysiologyCarbon CyclePlant RespirationRespiration PhysiologyRoot EcologyRoot PhysiologySoil RespirationAboveground RespirationBelowground RespirationForest Ecosystem RespirationPlant Tissue SamplingRespiration In Root SystemsRespiration Rate MeasurementRespiration RatesSoil Respiration Measurement
Accurate estimates of root respiration are crucial to predicting belowground C cycling in forest ecosystems. Inhibition of respiration has been reported as a short-term response of plant tissue to elevated measurement [CO(2)]. We sought to determine if measurement [CO(2)] affected root respiration in samples from mature sugar maple (Acer saccharum Marsh.) forests and to assess possible errors associated with root respiration measurements made at [CO(2)]s lower than that typical of the soil atmosphere. Root respiration was measured as both CO(2) production and O(2) consumption on excised fine roots (</= 1.0 mm) at [CO(2)]s ranging from 350 to > 20,000 micro l l(-1). Root respiration was significantly affected by the [CO(2)] at which measurements were made for both CO(2) production and O(2) consumption. Root respiration was most sensitive to [CO(2)] near and below normal soil concentrations (< 1500 micro l l(-1)). Respiration rates changed little at [CO(2)]s above 3000 micro l l(-1) and were essentially constant above 6000 micro l l(-1) CO(2). These findings call into question estimates of root respiration made at or near atmospheric [CO(2)], suggesting that they overestimate actual rates in the soil. Our results indicate that sugar maple root respiration at atmospheric [CO(2)] (350 micro l l(-1)) is about 139% of that at soil [CO(2)]. Although the causal mechanism remains unknown, the increase in root respiration at low measurement [CO(2)] is significant and should be accounted for when estimating or modeling root respiration. Until the direct effect of [CO(2)] on root respiration is fully understood, we recommend making measurements at a [CO(2)] representative of, or higher than, soil [CO(2)]. In all cases, the [CO(2)] at which measurements are made and the [CO(2)] typical of the soil atmosphere should be reported.
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Intracellular pH and its Regulation
F. Andrew Smith, John A. Raven · Annual Review of Plant Physiology · 1979 · 612 citations
Richard D. Bowden, Knute J. Nadelhoffer, Richard D. Boone et al. · Canadian Journal of Forest Research · 1993 · 449 citations
Agriculture, Ecology, Soil Sciences +17