4.7 Article

Soil and microbial respiration in a loblolly pine plantation in response to seven years of irrigation and fertilization

Journal

FOREST ECOLOGY AND MANAGEMENT
Volume 258, Issue 11, Pages 2431-2438

Publisher

ELSEVIER
DOI: 10.1016/j.foreco.2009.08.020

Keywords

Pinus taeda; Microbial respiration; Microbial biomass; Soil CO2 efflux; Intensive forest management

Categories

Funding

  1. USDA Forest Service
  2. Alabama Agricultural Experiment Station
  3. US Department of Energy Savannah River Operations office through the USDA Forest Service Savannah River and the Forest Service Southern Research Station [DE-IA09-00SR22188]

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Because Soil CO2 efflux or soil respiration (R-S) is the major component of forest carbon fluxes, the effects of forest management on R-S and microbial biomass carbon (C), microbial respiration (R-H), microbial activity and fine root biomass were studied over two years in a loblolly pine (Pinus taeda L.) plantation located near Aiken, SC. Stands were six-years-old at the beginning of the study and were subjected to irrigation (no irrigation versus irrigation) and fertilization (no fertilization versus fertilization) treatments since planting. Soil respiration ranged from 2 to 6 mu mol m(-2) s(-1) and was strongly and linearly related to soil temperature. Soil moisture and C inputs to the soil (coarse woody debris and litter mass) which may influence R-H were significantly but only weakly related to R-S. No interaction effects between irrigation and fertilization were observed for R-S and microbial variables. Irrigation increased R-S, fine root mass and microbial biomass C. In contrast, fertilization increased R-H, microbial biomass C and microbial activity but reduced fine root biomass and had no influence on R-S. Predicted annual soil C efflux ranged from 8.8 to 10.7 Mg C ha(-1) year(-1) and was lower than net primary productivity (NPP) in all stands except the non-fertilized treatment. The influence of forest management on R-S was small or insignificant relative to biomass accumulation suggesting that NPP controls the transition between a carbon source and sink in rapidly growing pine systems. (C) 2009 Elsevier B.V. All rights reserved.

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