Stacy et al., 2015

Paper/Book

Soil carbon and nitrogen erosion in forested catchments: implications for erosion-induced terrestrial carbon sequestration.

Stacy, E., Hart, S.C., Hunsaker, C.T., Johnson, D.W., Berhe, A.A. (2015)
Biogeosciences, 12, 4861-4874  

Plain English Summary

Stacy et al. explore patterns in the erosion, transport, and deposition of soil organic matter, carbon, and nitrogen in forest ecosystems. This study utilizes seven years of data from eight different stream catchments throughout the southern Sierra Nevada of California.

Abstract

Enrichment ratios for carbon (ERC) and nitrogen (ERN) in material (<2mm) collected from sediment basins at the outlet of each catchment over the water years 2005–2011.

Enrichment ratios for carbon (ERC) and nitrogen (ERN) in material (<2mm) collected from sediment basins at the outlet of each catchment over the water years 2005–2011.

Lateral movement of organic matter (OM) due to erosion is now considered an important flux term in terrestrial carbon (C) and nitrogen (N) budgets, yet most published studies on the role of erosion focus on agricultural or grassland ecosystems. To date, little information is available on the rate and nature of OM eroded from forest ecosystems. We present annual sediment composition and yield, for water years 2005–2011, from eight catchments in the southern part of the Sierra Nevada, California. Sediment was compared to soil at three different landform positions from the source slopes to determine if there is selective transport of organic matter or different mineral particle size classes. Sediment export varied from 0.4 to 177 kg ha−1, while export of C in sediment was between 0.025 and 4.2 kg C ha−1 and export of N in sediment was between 0.001 and 0.04 kg N ha−1. Sediment yield and composition showed high interannual variation. In our study catchments, erosion laterally mobilized OM-rich litter material and topsoil, some of which enters streams owing to the catchment topography where steep slopes border stream channels. Annual lateral sediment export was positively and strongly correlated with stream discharge, while C and N concentrations were both negatively correlated with stream discharge; hence, C : N ratios were not strongly correlated to sediment yield. Our results suggest that stream discharge, more than sediment source, is a primary factor controlling the magnitude of C and N export from upland forest catchments. The OM-rich nature of eroded sediment raises important questions about the fate of the eroded OM. If a large fraction of the soil organic matter (SOM) eroded from forest ecosystems is lost during transport or after deposition, the contribution of forest ecosystems to the erosion-induced C sink is likely to be small (compared to croplands and grasslands).

Citation

Stacy, E., Hart, S.C., Hunsaker, C.T., Johnson, D.W., Berhe, A.A. (2015): Soil carbon and nitrogen erosion in forested catchments: implications for erosion-induced terrestrial carbon sequestration. Biogeosciences, 12, 4861-4874 . DOI: 10.5194/bg-12-4861-2015

This Paper/Book acknowledges NSF CZO grant support.