Effect of in-situ aged and fresh biochar on soil hydraulic conditions and microbial C use under drought conditions

Biochar (BC) amendments may be suitable to increase the ecosystems resistance to drought due to their positive effects on soil water retention and availability. We investigated the effect of BC in situ ageing on water availability and microbial parameters of a grassland soil. We used soil containing 13C labeled BC and determined its water holding capacity, microbial biomass and activity during a 3 months incubation under optimum and drought conditions. Our incubation experiment comprised three treatments: soil without BC (Control), soil containing aged BC (BCaged) and soil containing fresh BC (BCfresh), under optimum soil water (pF 1.8) and drought conditions (pF 3.5). Under optimum water as well as drought conditions, soils containing BC showed higher soil organic carbon (SOC) mineralization as compared to control soil. Moreover, BC effects on the soil water regime increase upon in situ aging. Native SOC mineralization increased most for soils containing BCaged. The BCaged led to improved C use under drought as compared to the other treatments. We conclude that BC addition to soils can ameliorate their water regime, especially under drought conditions. This beneficial effect of BC increases upon its aging, which also improved native substrate availability

Sustainable and resource efficient intensivation of crop production – Perspectives of agro-ecosystem researchPolicy paper of the DFG Senate Commission on Agroecosystem Research

Mit dem vorliegenden Grundsatzpapier zeigt die Senatskommission für Agrarökosystemforschung Perspektiven für die Grundlagenforschung zur nachhaltigen Erhöhung der Kulturpflanzenproduktion auf.Agrarsysteme stehen im Spannungsfeld zwischen steigendem Bedarf an landwirtschaftlichen Produkten, der Verknappung der Ressourcen, dem Verlust der Biodiversität und dem Klimawandel. Die für das Jahr 2050 prognostizierte notwendige Ertragssteigerung zur Sicherstellung des Bedarfs an Nahrungsmitteln kann, ohne die Belastbarkeitsgrenzen ökologischer Systeme zu überschreiten, nur durch wissenschaftlichen Fortschritt bewältigt werden (Abb. 1), der eine nachhaltige und ressourcen­effiziente Steigerung der Agrarproduktion ermöglicht (FAO, 2011; Dobermann und Nelson, 2013). Die nachhaltige Intensivierung stellt die Agrarwissenschaften vor neue Aufgaben, die weit über ihre klassischen Grenzen hinausgehen.Die Senatskommission plädiert daher für eine Erweiterung der agrarwissenschaftlichen Perspektive. Die meist auf einzelne Feldfrüchte bezogene Bewertung der Rela­tion zwischen Input und Ertrag muss ergänzt werden um die Optionen, die sich aus der räumlichen und zeitlichen Diversifikation der Produktionssysteme unter Einbeziehung der standörtlichen Eigenschaften, des Landschaftskontextes sowie des Klimawandels ergeben. Um Ökosystemleistungen einzubeziehen, müssen Produktionsstrategien entwickelt werden, die sich auf ganze Landschaften und Regionen richten und auch entsprechende sozio­öko­no­mische und agrarpolitische Rahmenbedingungen berücksichtigen.Vor diesem Hintergrund schlägt die Senatskommission drei interdisziplinäre Forschungsschwerpunkte zur ressourceneffizienten Erhöhung der Flächenproduktivität vor:(1) Ausnutzung des Potentials von Kulturpflanzen zur umweltschonenden Ertragssteigerung im Kontext öko­systemarer Bedingungen.(2) Nachhaltige Steigerung der Pflanzenproduktion im Landschaftskontext.(3) Ökonomische, gesellschaftliche und politische Dimensionen der Ertragssteigerung von Kulturpflanzen. DOI: 10.5073/JfK.2014.07.01, https://doi.org/10.5073/JfK.2014.07.01With its policy paper the Senate Commission on Agro-ecosystem Research of the Deutsche Forschungsgemeinschaft (DFG) summarizes potential benefits of basic research for the sustainable intensification of crop production. Agro-ecosystems critically contribute to fulfilling the need for increasing food and fiber production, diminishing resource depletion as well as counteracting biodiversity loss and climate change. Yield demands that are needed to ensure the food supply predicted for the year 2050 can only be achieved by scientific progress that allows the intensive yet environmentally friendly production of plant biomass (Figure 1), (FAO, 2011; Dobermann und Nelson, 2013; Ray et al., 2013). Sustainable intensification requires a scientific realignment that allows for broadening the scope of agricultural research. The productivity of farming systems should be evaluated with regard to their efficiency (input-output relation). In addition, the spatial and temporal variability of these systems must be considered by addressing local conditions, the landscape context and climate change. With respect to ecosystem services, new production strategies must be developed that take all aspects of landscape and regional complexity as well as socio-economic conditions and agricultural policy into account.Against this background, the Senate Commission on Agro-ecosystem Research proposes three priority areas of interdisciplinary research on resource efficient intensification of crop production:(1) Exploiting the biological potential of the individual crop plants for an environmentally friendly intensification in an ecosystem approach(2) Exploring sustainable intensification of crop production within a landscape context(3) Taking full account of the economic, social and political dimensions of sustainable intensification of crop production DOI: 10.5073/JfK.2014.07.01, https://doi.org/10.5073/JfK.2014.07.0

An indicator for organic matter dynamics in temperate agricultural soils

The heterogeneity of soil organic matter (SOM) and the small changes in soil organic carbon (SOC) compared to large total SOC stocks hinder a robust estimation of SOC turnover, in particular for more stable SOC. We developed a simple fractionation protocol for agricultural topsoils and tested it extensively on a range of soils in southern Belgium, including farmed soils, soils from long-term field trials, and paired sites after recent conversion to conservation farming. Our simple fractionation involves shaking the soil, wet sieving over 20 μm and analysing the SOC concentration in the soil as well as in the fine fraction (<20 μm). Eight biological indicators measured in an earlier study across the same monitoring network for the 0–10 cm topsoil were analysed in a conditional inference forest model in order to investigate the factors influencing the SOC fractions. Soil microbial biomass N explained the largest proportion of variation in both fractions. The fine fraction was also associated with factors explaining the regional trend in SOC distribution such as farmyard manure input, precipitation, land use and flow length. The variation in SOC content between treatments both in long-term trials and in farmers’ fields converted to conservation management was mainly attributed to changes within the coarse fraction. Thus, this fraction proves to be sensitive to management changes, although care should be taken to sample deep enough to represent the former plough layer inherited from the conventional tillage practice. Furthermore, the ratio between the coarse and the fine fraction showed a linear relationship (r² = 0.66) with the relative changes in SOC concentration over the last ten years. These fractions derived from a simple analytical approach are thus useful as an indicator for changes in SOC concentration. In analogy to biological indicators such as the soil microbial biomass C, the relationship between the fractions and relative changes in SOC concentration are likely to depend on climate conditions. Our methodology provides an indicator for use in routine analysis of agricultural topsoils, which is capable of predicting the effects of management practices on SOC concentrations in the short to mid-term (5–10 years)

Soil organic carbon storage as a key function of soils - A review of drivers and indicators at various scales

The capacity of soils to store organic carbon represents a key function of soils that is not only decisive for climate regulation but also affects other soil functions. Recent efforts to assess the impact of land management on soil functionality proposed that an indicator- or proxy-based approach is a promising alternative to quantify soil functions compared to time- and cost-intensive measurements, particularly when larger regions are targeted. The objective of this review is to identify measurable biotic or abiotic properties that control soil organic carbon (SOC) storage at different spatial scales and could serve as indicators for an efficient quantification of SOC. These indicators should enable both an estimation of actual SOC storage as well as a prediction of the SOC storage potential, which is an important aspect in land use and management planning. There are many environmental conditions that affect SOC storage at different spatial scales. We provide a thorough overview of factors from micro-scales (particles to pedons) to the global scale and discuss their suitability as indicators for SOC storage: clay mineralogy, specific surface area, metal oxides, Ca and Mg cations, microorganisms, soil fauna, aggregation, texture, soil type, natural vegetation, land use and management, topography, parent material and climate. As a result, we propose a set of indicators that allow for time- and cost-efficient estimates of actual and potential SOC storage from the local to the regional and subcontinental scale. As a key element, the fine mineral fraction was identified to determine SOC stabilization in most soils. The quantification of SOC can be further refined by including climatic proxies, particularly elevation, as well as information on land use, soil management and vegetation characteristics. To enhance its indicative power towards land management effects, further “functional soil characteristics”, particularly soil structural properties and changes in the soil microbial biomass pool should be included in this indicator system. The proposed system offers the potential to efficiently estimate the SOC storage capacity by means of simplified measures, such as soil fractionation procedures or infrared spectroscopic approaches