The Activity of Deep Roots in Bedrock Fractures at the Susquehanna Shale Hills Critical Zone Observatory, USA

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Elizabeth Ann Hasenmueller1, Xin Gu2, Julie N Weitzman2, Thomas S Adams2, Gary E Stinchcomb3, David M Eissenstat2, Susan L Brantley2 and Jason P Kaye2, (1)Saint Louis University, Earth and Atmospheric Sciences, Saint Louis, MO, United States, (2)Pennsylvania State University Main Campus, University Park, PA, United States, (3)Murray State University, Murray, KY, United States
Many areas in the world are characterized by shallow soils underlain by weathered bedrock, but root-rock interactions and their implications for regolith weathering are poorly understood. To test the role of tree roots in weathering bedrock, we excavated four pits along a catena in a shale-hosted catchment near the Susquehanna Shale Hills Critical Zone Observatory, USA. We measured a variety of physical and chemical properties including: (1) root density, distribution, and respiration rates, (2) soil gas, and (3) soil, rock, and rock fracture sediment elemental compositions, mineralogy, and morphology. As expected, root density declined rapidly with depth; nevertheless, roots were present in rock fractures even in the deepest, least weathered shale sampled (~ 1.8 m). Root density in the shale fractures was highest at the ridge for all depths and decreased 23-fold downslope as soils thickened and in spite of increasing rock fracture density. Root respiration rates (per gram of root) in fractures were comparable to those in augerable soil, with the highest respiration rates for all depths observed at the ridge. We only observed roots in larger shale fractures (> 50 μm) that were coated with sediment. These sediments were mineralogically and geochemically similar to overlying B and C soil horizons with respect to clay composition, total C and N, and potentially mineralizable C. Such similarities indicate that the sediment coatings are likely the result of translocation of soil particles downward into the fractures. However, concentrations of extractable inorganic N were higher in fracture sediments than in surface soils. Shale in contact with deep roots resembled unweathered parent material geochemically. In the bulk soil, depletion profiles (K, Mg, Si, Fe, and Al) relative to unweathered shale reflected characteristic weathering of illite and chlorite to kaolinite. Approximately 50% of soil K and Mg was lost as eroding particles, supporting the idea that fracture sediments are the result of downward transport of soil particles rather than in situ rock weathering. Overall, our data suggest that roots and sediments present in shale fractures down to ~ 1.8 m are qualitatively similar to those in surface soil horizons, with the main difference being that there are simply fewer roots and less sediment in the bedrock fractures.