Intercropping, defined as two or more crops grown on the same land area at the same time, is a sustainable alternative to sole crops. Intercropping has been associated with multiple benefits, such as increased nutrient and soil organic carbon (SOC) cycling, decreased soil erosion and increased carbon (C) sequestration. A common intercropping practice is to integrate cereal and legume crops such as maize (Zea mays L.), and soybean (Glycine max (L.) Merr.). Most studies on intercropping have focused on yield, weed control, and land use efficiency in the tropics. Few studies have researched C and nitrogen (N) dynamics in temperate intercrops, with respect to soybean and maize residue stabilization. Soil from Balcarce, Argentina, was incubated for 140 days with soybean, maize, or no residue. Throughout the incubation, results illustrated the effect of residue application upon the soil, specifically through significantly higher amounts of light fraction (LF) C and LFN concentrations, soil microbial biomass (SMB) C and SMBN concentrations, higher microbial diversity, lower N2O production rates, in addition to distinct isotopic values in soil fractions and CO2 (p<0.05). Furthermore, it was observed from δ15N-TN and δ15N-LF that treatments with soybean residues included had higher N cycling (p<0.05), emphasizing the importance of including N-fixing legumes in complex agroecosystems. Significant changes over time in SMB and SMCS characteristics, and isotope values (p<0.05) indicated the preferential utilization of relatively young and easily accessible litter. Furthermore, the loss of labile material over the incubation resulted in more recalcitrant forms (such as older C and lignin) to be utilized. Slightly higher SOC, TN, LFC and LFN concentrations, as well as lower CO2 production rates suggested 2:3 (rows of maize:rows of soybean) as a more desirable intercrop design for C sequestration. The 1:2 intercrop design was observed to be more beneficial for microbial community structure, furthering the idea that intercropping is a beneficial alternative to sole cropping. This study improves knowledge in residue stabilization and C sequestration in complex agroecosystems, providing encouragement for the implementation of more sustainable management practices.

Intercropping, defined as two or more crops grown on the same land area at the same time, is a sustainable alternative to sole crops. Intercropping has been associated with multiple benefits, such as increased nutrient and soil organic carbon (SOC) cycling, decreased soil erosion and increased carbon (C) sequestration. A common intercropping practice is to integrate cereal and legume crops such as maize (Zea mays L.), and soybean (Glycine max (L.) Merr.). Most studies on intercropping have focused on yield, weed control, and land use efficiency in the tropics. Few studies have researched C and nitrogen (N) dynamics in temperate intercrops, with respect to soybean and maize residue stabilization. Soil from Balcarce, Argentina, was incubated for 140 days with soybean, maize, or no residue. Throughout the incubation, results illustrated the effect of residue application upon the soil, specifically through significantly higher amounts of light fraction (LF) C and LFN concentrations, soil microbial biomass (SMB) C and SMBN concentrations, higher microbial diversity, lower N2O production rates, in addition to distinct isotopic values in soil fractions and CO2 (p<0.05). Furthermore, it was observed from δ15N-TN and δ15N-LF that treatments with soybean residues included had higher N cycling (p<0.05), emphasizing the importance of including N-fixing legumes in complex agroecosystems. Significant changes over time in SMB and SMCS characteristics, and isotope values (p<0.05) indicated the preferential utilization of relatively young and easily accessible litter. Furthermore, the loss of labile material over the incubation resulted in more recalcitrant forms (such as older C and lignin) to be utilized. Slightly higher SOC, TN, LFC and LFN concentrations, as well as lower CO2 production rates suggested 2:3 (rows of maize:rows of soybean) as a more desirable intercrop design for C sequestration. The 1:2 intercrop design was observed to be more beneficial for microbial community structure, furthering the idea that intercropping is a beneficial alternative to sole cropping. This study improves knowledge in residue stabilization and C sequestration in complex agroecosystems, providing encouragement for the implementation of more sustainable management practices.

In dieser Studie wurden stabile Isotopenverhältnisse genutzt um die Mechanismen der aquatisch-terrestrischen C – und N-Dynamiken über verschiedene Skalenebenen hinweg in der Moränenlandschaft von Nordostdeutschland zu identifizieren; einer Landschaft, die stark landwirtschaftlich genutzt wird und in der es eine Vielzahl von kleinen Wasserkörpern (Sölle) gibt. Auf der regionalen Landschaftsskala spiegeln d13C-Isotopenkarten des org. Materials in Oberböden und von Pflanzenblättern eines 38.2 km2 großen Gebietes den Eintrag von org. Material von C3-Pflanzen, deren Wassernutzungseffizienz im org. Material des Bodens eingeprägt wurde, sowie den Eintrag von Mais (C4-Pflanze), wider. Die d15N-Isotopenkarte des org. Materials in Böden weist verschiedene Düngepraktiken hin. Auf der regionalen Sollskala deuten die d13C- und d15N-Isotopenwerte von Oberflächensedimenten von 51 Söllen auf kürzliche Einträge des org. Materials und Bewirtschaftungseffekte im Einzugsgebiet hin. Tiefere Sedimente sind durch die Ablagerung org. Materials von terrestrischen Pflanzen sowie dessen Umsetzungsgrad geprägt in Abhängigkeit von der Wasserführung. Auf der Transekt-Skala, d.h. entlang von Transekten von Erosions- zu Depositionsgebieten im Einzugsgebiet eines Solls, beeinflussen Erosion, Pflanzenproduktion, mikrobielle Umsetzung und Gülledüngung verschiedene Fraktionen des org. Materials. Auf der Aggregat-Skalenebene sind die Art und der Anteil spezifischer organo-mineral Assoziationen entlang des Transekts variabel. Bodenpartikel vom Feld und hereinwachsende Makrophyten sind die Quellen des org. Materials in Sedimenten. Diese Studie hat erfolgreich stabile Isotopenverhältnisse zur Identifikation von Mechanismen der C- und N-Dynamik auf individuellen Skalenebenen angewendet. Kleine Inlandwasserkörper sind Schlüsselelemente für die C- und N-Dynamik in landwirtschaftlich genutzten Moränenlandschaften. / In moraine landscapes, carbon (C) and nitrogen (N) dynamics can vary greatly across landscape structures and soil types especially when small water bodies are interspersed in the landscape. This study used stable isotope ratios to identify the mechanisms regulating the aquatic-terrestrial C and N dynamics across different scales in the young moraine landscape of NE Germany – a landscape intensively used for agriculture and interspersed with countless of small water bodies, the so-called kettle holes. At the regional landscape scale, d13C isoscapes of topsoil bulk soil organic matter (SOM) and plant leaves collected from a 38.2 km2 area revealed long-term inputs OM from C3 crops, which imprinted their water use efficiency status onto the soil, as well as short-term inputs from corn. The d15N SOM isoscape identified fertilization-induced impacts on the N dynamics of agricultural fields and grasslands. At the regional kettle hole scale, d13C and d15N of surface sediments of 51 kettle holes reflected recent OM inputs and management practices in the catchment. Deeper sediments recorded the degree to which the OM has been processed within the kettle hole depending on the water-logging period. At the transect scale, erosion, plant productivity, microbial decomposition and slurry fertilization affected OM fractions in topsoil along transects spanning erosional to depositional areas in the catchment of one arable kettle hole. At the aggregate scale, the pathway and magnitude of OM-mineral associations changed along the transect. OM in sediments was derived from clay- and silt-sized particles from the field, together with emergent macrophyte contributions. By means of stable isotopes techniques, different mechanisms were identified at the individual scales. Consideration of the spatial heterogeneity of all scales is essential to understand landscape C and N dynamics. Small inland water bodies are key constituents of C and N dynamics in moraine agricultural landscapes.