Soil carbon stocks in different bioenergy cropping systems including subsoil

Abstract

Despite the growing importance of energy cropping systems, little is known about their soil organic carbon (SOC) stocks in topsoils and subsoils. Furthermore, information regarding the impact of N-fertilization on C-sequestration for perennial compared with annual energy cropping systems is scarce. In order to study SOC changes in the soils of different energy cropping systems, a long-term study was established in southwestern Germany with the following cropping systems: energy maize (Zea mays) with reduced tillage, Miscanthus (M. x giganteus), switchgrass (Panicum virgatum) and willow (Salix schwerinii x viminalis), as well as a crop rotation with conventional tillage (CT) and no-till (NT) consisting of oilseed rape (Brassica napus ssp. oleifera), winter triticale (Triticale triticosecale) and winter wheat (Triticum aestivum). The soil is a Haplic Luvisol (Siltic). For each cropping system three N-fertilization regimes adapted to the needs of each crop were applied. With the main hypothesis that perennial energy cropping systems increase SOC stocks compared with conventional annual cropping systems, the SOC stocks were analyzed to a depth of 90cm after 11 years of continuous cropping (2002–2012). Compared with the control (CT) with 76 Mg SOC ha−1, the perennial crops had significantly higher SOC stocks in all N-fertilization regimes, which amounted to 92–95 Mg SOC ha−1 in the N1-fertilization regime. The crop rotation with NT also had higher SOC stocks with 93 Mg SOC ha−1 in the N1-fertilization regime. N-fertilization generally led to higher SOC stocks in all cropping systems, although SOC stocks did not increase any further from reduced to highest crop-specific N-fertilization, with the exception of energy maize. The current findings also stress the importance of subsoil carbon analyses: SOC stocks at a depth from 30 to 90cm made up 44–55% of the total stocks and differed significantly between cropping systems.