Environmental Controls on Soil Co2 Flux Following Fire in Black Spruce, White Spruce, and Aspen Stands of Interior Alaska

By K. O''Neill, E. Kasischke, D. Richter. 2002

118 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Climate change feedbacks to microbial decomposition in boreal soils (2011, unknown): “Similarly, O’Neill et al. (2003) found that soil respiration was 40e50 % lower in recently burned black spruce forests in Alaska, but suggested that decomposition rates had increased by >3-fold based on a C balance model and prior lab incubation results (Richter et al. 2000; O’Neill et al. 2006).”
A global relationship between the heterotrophic and autotrophic components of soil respiration? (2004, background): “After disturbance, forest ecosystems will have lower RC, due to a drop in RA and environmental changes – for example, rising temperature and soil moisture (O’Neill et al., 2002) – in the soil substrate that raise RH.”
Relationships among fires, fungi, and soil dynamics in Alaskan Boreal Forests (2004, methodology): “Antibody concentrations were determined by using a microplate reader (EL800, Bio-tek instruments, Winooski, Vermont, USA) equipped with a 405-nm filter, and then comparing values to those of a glomalin standard extracted from fresh AM hyphae.”