Carbon redistribution by erosion processes in an intensively disturbed catchment

• Published in: Catena (Giessen) 2017-02, Vol.149, p.799-809
• Main Authors: Boix-Fayos, Carolina, Martínez-Mena, María, Cutillas, Pedro Pérez, de Vente, Joris, Barberá, Gonzalo G., Mosch, Wouter, Navarro Cano, Jose Antonio, Gaspar, Leticia, Navas, Ana
• Format: Article
• Language: English
• Subjects: 137Cs; Erosion; Organic carbon pools; Sediment dynamics, check-dam, reforestation, catchment scale, connectivity; Soil organic carbon
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2016.08.003

Understanding how organic carbon (OC) moves with sediments along the fluvial system is crucial to determining catchment scale carbon budgets and helps the proper management of fragile ecosystems. Especially challenging is the analysis of OC dynamics during fluvial transport in heterogeneous, fragile, and disturbed environments with ephemeral and intense hydrological pulses, typical of Mediterranean conditions. This paper explores the catchment scale OC redistribution by lateral flows in extreme Mediterranean environmental conditions, from a geomorphological perspective. The study area is a catchment (Cárcavo) in SE Spain with a semiarid climate, erodible lithologies, and shallow soils, which is highly disturbed by agricultural terraces, land levelling, reforestation, and construction of check-dams. To increase our understanding of catchment scale OC redistribution induced by erosion, we studied in detail the subcatchments of eight check-dams distributed along the catchments main channel. We determined 137Cs, physicochemical characteristics, and the OC pools of the catchment soils and sediments deposited behind each check-dam, performed spatial analysis of catchment properties and buffer areas around the check-dams, and carried out geomorphological analysis of the slope-channel connections. The soils showed very low total organic carbon (TOC) values, oscillating between 15.2 and 4.4gkg−1 for forest and agricultural soils, respectively. Sediments mobilized by erosion were poor in TOC (6.6±0.7gkg–1) compared to the eroded (forest) soils, and the redistribution of OC through the catchment, especially of the mineral associated organic carbon (MAC) pool, showed the same pattern as clay particles and 137Cs. The TOC erosion rates estimated for the Cárcavo watershed are relatively low (0.031±0.03Mgha−1y−1) but similar to those reported for subhumid Mediterranean catchments that are less fragile and more conducive to plant growth. The TOC erosion/total erosion ratio was lower (0.06%) than other estimates, although the average OC concentration of the sediments was higher than that of the agricultural soils of the catchment, underlining the problem of maintaining sustainable soil OC contents. The OC in deposited sediments came not only from surface erosion processes, but also from deeper soil or sediment layers mobilized by concentrated erosion processes. Sediment richer in OC came from the surface soil of vegetated (reforested) areas close and well connected to the c