Soil organic matter plays a key role in determining soil physical and chemical properties, porosity, availability of nutrients and cation exchange capacity (Bellanger et al., 2004; Lal, 1999). The basic sources of organic carbon include decomposing dead plant and animal matter in the soil, root exudate from plants and, importantly, fertilizers, including manure (Mahmoodabadi & Heydarpour, 2014). Losses are in turn associated with the mineralization of organic carbon and its transformation into carbon dioxide gas (CO 2). According to Van Oost et al. (2007), 26% of organic carbon transported during erosion-related processes escapes from the soil into the atmosphere. Another very important element related to the extraction of carbon and the degradation of soil is the process of water erosion. The transport of organic carbon with eroded materials poses a serious problem, particularly for arable land, which becomes more susceptible to runoff and soil losses after being subjected to intensive cultivation. In addition, the loss of organic carbon in dissolved or particulate forms may have severe consequences not only on the soils from which it is exported but also on the water