OOS 61-4
Effects of soil biota disturbance on inorganic carbon dynamics in renewable energy developments

Thursday, August 13, 2015: 9:00 AM
316, Baltimore Convention Center
Amanda Swanson, University of California, Riverside
Edith Allen, Botany and Plant Sciences and Center for Conservation Biology, University of California, Riverside, Riverside, CA
Michael F. Allen, Biology, University of California Riverside, Riverside, CA

Renewable energy developments are projected to be deployed over desert wildland areas with deep soil inorganic carbon (SIC) deposits which often involves elimination of deep-rooted vegetation. Vegetation removal may systemically alter SIC pools because respired CO2 is the carbon source during SIC formation. We sought to understand how removal of creosote bush scrub affects soil carbon (C) pools. We hypothesized that vegetation plays a significant role in maintaining both SIC and soil organic C pools and that disturbance to the vegetation and soil biota will change CO2 flux, increasing C loss from SIC sources. Soils were collected from sites that had intact creosote bush scrub habitat adjacent to disturbed, bare areas where the native vegetation had been previously removed. Samples were taken from beneath shrub canopies and interspaces in intact areas, and from random points in the disturbed area. Two sets of points were sampled in the disturbed area, one set that will remain bare and the other prior to planting creosote bush seedlings. An incubation experiment was conducted to determine potential flux from disturbed and undisturbed soils and potential C sources contributing to C loss. Each soil underwent two treatments, control (unwatered) and water addition at 25°C with three replicates per soil. Flux and isotopic composition (δ13C) of CO2were measured continuously for each replicate.


There was no significant CO2 flux from any control (unwatered) replicates. CO2 flux from water-treated soils was higher beneath shrub canopy (18.57µmol g soil-1 day-1±1.86) than the interspace soils (0.86 µmol g soil-1 day-1±0.17). Soils collected from bare areas (bare and pre-seedling) had an intermediate flux (5.41 µmol g soil-1 day-1±2.68 and 3.68 µmol g soil-1 day-1±0.85, respectively) lying between shrub canopy and interspace soils. There was no significant difference between the δ13C values of CO2 from intact soils (shrub canopy and interspace), both of which had a very low δ13C values (-22.60‰±0.64 and -23.88‰±0.89, respectively), resembling that of organic C. However, the isotopic values of CO2 from disturbed soils (bare and pre-seedling) were significantly higher (-16.68‰±1.36 and -15.22‰±2.12, respectively) suggesting that these soils effluxed a greater proportion of CO2 from an inorganic source than intact soils. The vegetation and soil biota play important roles in desert carbon balance. Disturbances, such as vegetation removal to accommodate renewable energy developments, may negatively impact the soil biota, potentially leading to unintended increased soil C losses from the SIC pool.