Tuesday, November 6, 2007 - 1:30 PM
207-1

Microbial Biomass and Soil Organic Carbon Fractions of the Reclaimed Age-Chronosequence minesoils under Pasture in Eastern Ohio.

David Ussiri, School of Natural Resources, Ohio State University - Columbus, Ohio State University, 2021 Coffey Rd, Columbus, OH 43210 and Rattan Lal, 2021 Coffey Road, Ohio State University - Columbus, Ohio State University, Carbon Management & Sequestration Center, Columbus, OH 43210.

Abstract

Surface coal mining of coal causes drastic landscape disturbances and severe soil degradation. Reclamation could restore soil quality and ecosystem productivity. A study was conducted to evaluate the effects of age since reclamation on different biological and chemical fractions of soil organic C and N. Microbial biomass C was determined by chloroform fumigation, followed by incubation for 10 days. Head-space gas samples were collected and analyzed at 3, 6 and 10 days for the fumigated non-fumigated samples. After 10 days, non fumigated samples were further incubated for 60 days with weekly gas sampling. Gas samples were analyzed by GC for CO2, CH4 and N2O. In addition, samples were treated by sodium thiosulphate, sodium hypochlorite, and hydrogen peroxide. Microbial biomass and microbial mineralizable C in the top 0-10 cm depth ranged from 0.17 to 0.320 and 0.42 to 1.35 mg g-1 of soil respectively, and increased with increasing age since reclamation. Biological OC fraction was generally correlated with oxidation fraction. Results indicate that microbial biomass C could be used as an indicator of ecosystem restoration.