Influence of erosion and deposition on carbon and nitrogen accumulation in resampled steepland soils under pasture in New Zealand

• Published in: Geoderma 2013-01, Vol.192, p.154-159
• Main Authors: Parfitt, R.L., Baisden, W.T., Ross, C.W., Rosser, B.J., Schipper, L.A., Barry, B.
• Format: Article
• Language: English
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Carbon; Carbon accumulation; carbon sinks; case studies; Deposition; Earth sciences; Earth, ocean, space; Erosion; Erosion mechanisms; Exact sciences and technology; forage legumes; Fundamental and applied biological sciences. Psychology; Gain; hills; Isotope geochemistry; Isotope geochemistry. Geochronology; landscapes; landslides; nitrogen; Pasture production; pastures; regression analysis; Sampling; Sedimentation; soil depth; soil horizons; soil profiles; Soil recovery; Soils; steepland soils; Storm sediment; Surficial geology
• ISSN: 0016-7061; 1872-6259
• DOI: 10.1016/j.geoderma.2012.08.006

Although erosion occurs under pastures in New Zealand North Island hill country, previous work shows that the soils on mid-slopes (>19°) have large and significant average gains of soil carbon (C) and nitrogen (N) over a period of about 30years. Both sheetwash erosion (from patches of bare soil) and soil deposition (from upslope) could have occurred in the intervening 30years, and this could have led to a loss or gain of soil C. The fission-derived radionuclide 137Cs is a unique tracer for studying erosion and sedimentation because it is strongly adsorbed onto soil particles, and its movement in the environment is predominantly due to physical processes. We hypothesized that accumulation and loss of 137Cs and C would be correlated if erosion and deposition processes were responsible for the observed changes in soil C. We therefore measured 137Cs in archived samples, previously used to assess changes in C and N, together with 137Cs in the re-sampled soil horizons, to an average depth of 37cm. The data show that, on average, there has been a small gain in total profile 137Cs over this time, and complex patterns within individual soil profiles over 30years. There was only a weak correlation between 137Cs and C accumulation above 15cm soil depth, but, in contrast, a much stronger relationship was found below 15cm. A possible explanation for the observed pattern is soil thickening due to deposition, but the deposition may occur with variable 137Cs contents. Generally deposition does not account for all of the increase in C, and regression analysis between Cs and C for all layers suggested that erosion/deposition accounted for 20–30% of the total change in C. In a detailed case study, the sampling of erosion scars caused by landslides showed that soil C stocks (0–20cm) can increase from 10 to 80 tonne (Mg) C ha−1 within 70years. Use of the CENTURY model indicated that input of N from legumes in the pasture enabled N and C to accumulate in the surface soil. This suggests that gains in soil C and N under hill country pasture that occur in these facets of the landscape are probably largely due to the ongoing input from C and N in the grass-legume pastures rather than erosion or deposition of soil. ► Measured 137Cs and C in archived and re-sampled soils. ► Strong correlation between 137Cs and C accumulation below 15cm soil depth. ► Regression suggested that erosion/deposition accounted for 25% of the change in C. ► Case study showed soil C stocks can increase from 1