Effectiveness of carbon isotopic signature for estimating soil erosion and deposition rates in Sicilian vineyards
| Autor: | Novara Agata, Dazzi Carmelo, Gristina Luciano, Cerdà Artemi, Lo Papa Giuseppe, Santoro Antonino |
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| Přispěvatelé: | Novara, A., Cerdà, A., Dazzi, C., Lo Papa, G., Santoro, A., Gristina, L. |
| Jazyk: | angličtina |
| Rok vydání: | 2015 |
| Předmět: |
Stable isotope ratio
Mediterranean environment Sediment Method Soil Science Soil science Soil carbon Spatial distribution Vineyard Deposition (geology) Settore AGR/02 - Agronomia E Coltivazioni Erbacee Isotopic signature Settore AGR/14 - Pedologia Erosion Soil erosion Carbon isotopic signature Transect Agronomy and Crop Science Geology Earth-Surface Processes |
| Popis: | Traditional methods for measurement of soil erosion provide information on erosion rates and mechanisms but fail to determine the spatial distribution of sediment redistribution. Recent studies have used carbon (C) stable isotopes to trace sediment and to monitor soil organic carbon (SOC) redistribution. The difference in δ 13 C values in a slope-transect or in a watershed provides information about the source of suspended organic matter and sediment removal and deposition, but miss enough information to quantify sediment loss. The objective of this research was to develop a method to estimate soil erosion using the natural discrimination of δ 13 C-SOC with soil depth, comparing δ 13 C variation in different profiles sampled along a slope. The method was developed in a Sicilian vineyard, where soil losses were previously measured by means of Gerlach collectors and by pole methods. δ 13 C was measured in different soil profiles in the top, middle and bottom of the slope. The variation of δ 13 C with soil depth in the profiles along the slope was compared to the δ 13 C values of the near flat area, in order to reconstruct the original topography of slope transect. δ 13 C increased with depth and decreased from the top to the bottom of the slope in all pedons. The soil δ 13 C signature ranged from −26.7‰ to −25.7‰, from −26.2‰ to −25.3‰, and from −27.0‰ to −24.8‰ in the profiles at the top, middle, and bottom of the slope, respectively. The rates of δ 13 C enrichment along the slope could be explained as different rates of detachment and deposition. The erosion value estimated with δ 13 C method was 77 Mg ha −1 y −1 . The comparison of different methods (102 Mg ha −1 y −1 with the pole method and 89.6 Mg ha −1 y −1 with the Gerlach method) indicate that carbon isotopic signature is a reliable indicator of short- and long-term soil erosion processes. |
| Databáze: | OpenAIRE |
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