Topsoil status of cohesive soils as related to trafficability

Adapting soil engaging operations to the soil moisture status may limit damage of the soil structure or degradation processes. This requires the quantification of soil trafficability in dependence on soil hydrological conditions. The aim was to test the relevance of topsoil parameters in relation to trafficability and to study their temporal variability during a springtime period.

On different sites located in the holocene regions east of Berlin, soil moisture, density and strength parameters were analysed and related to the actual score of trafficability. The results show that those parameters being most suitable to characterise the trafficability in the field such as consistence and density, are easy and reliable to estimate on the basis on framework guidelines. Vehicle mobility and the risk of topsoil and subsoil structural damage are mainly influenced by the topsoil status of the upper 10 cm, in particular of the soil surface of cohesive soils. Trafficability state may be derived at least from two or more relevant consistency and density parameters.

Trafficability states are autocorrelated in the time domain. One‐step‐ahead forecasting of trafficability is possible using autocorrelations and weather data.     

Einfluss von klima und textur auf die biologische aktivität beim umsatz der organischen bodensubstanz

Der Umsatz organischer Bodensubstanzen läßt sich durch Kinetiken 1. Ordnung beschreiben. Die Reaktionskoeffizienten sind von der Bodentemperatur und ‐feuchte sowie den Aerationsverhältnissen im Boden abhängig. Unter Verwendung des Quasistationaritätsprinzips können die Umsatzprozesse in einer biologischen Zeitbasis, der wirksamen Mineralisierungszeit (WMZ), auf einfache und überschaubare Art und Weise beschrieben werden. Die standortspezifischen Werte der WMZ müssen in der Regel durch zeitaufwendige Simulationsrechnungen über verschiedene Fruchtfolgen ermittelt werden. Zur Vereinfachung wurde eine Regressionsgleichung entwickelt, mit deren Hilfe eine Abschätzung der standorttypischen Jahressumme der WMZ bei Kenntnis des Jahresmittels der Lufttemperatur, des Niederschlags sowie des Feinanteilgehaltes im Boden möglich ist.     

Cross-border molecular tracing of brucellosis in Europe

To assess the general impact of endemic countries on the re-emergence of brucellosis in non-endemic regions of the European Union, the genetic fingerprints of Brucella melitensis strains imported to Germany were compared to ovine strains from Turkey in a molecular epidemiological study. Genotyping of 66 Brucella strains (based on Multiple Locus of Variable number of tandem repeats Analysis) isolated from German travellers and Turkish immigrants living in Germany revealed epidemiological concordance with 20 sheep isolates originating from Eastern Anatolia, Turkey. In summary, cross-border molecular tracing confirmed brucellosis being a zoonosis of concern for European public health.     

Organic carbon in soils of Germany: Status quo and the need for new data to evaluate potentials and trends of soil carbon sequestration

Uncertainties in estimates of soil carbon (C) stocks and sequestration result from major gaps in knowledge of C storage in soils, land‐use history, the variability of field measurements, and different analytical approaches applied. In addition, there is a lack of long‐term datasets from relevant land‐use systems. As in many European countries, a national database on soil organic carbon (SOC) including all relevant information for the determination of soil C stocks is likewise missing in Germany. In this paper, we summarize and evaluate the present state of knowledge on organic‐C contents/pools in soils of Germany and discuss the need for the acquisition and access to new data on soil organic carbon. Despite the number of agricultural sites under permanent soil monitoring, regional surveys on SOC, comprehensive ecosystem studies, and long‐term field experiments, there is a striking lack of data in Germany particularly with regard to agricultural soils. Apart from a missing standardization of methods and homogeneous baseline values, the implementation of a periodic, nation‐wide soil inventory on agricultural soils is required in order to simultaneously record information on land use, land‐use change, and agricultural practice. In contrast, the existing national inventory of forest soils provides information on C‐stock changes in forest soils, although there is some concern with regard to the representativeness of the sampling design to adequately address the problem of spatial heterogeneity and temporal variability. It is concluded that the lack of comprehensiveness, completeness, actuality, data harmonization, and standardized sampling procedures will further prevent the establishment of a SOC database in Germany with regard to the monitoring of trends in soil C pools and fluxes and the assessment of long‐term C‐sequestration potentials of soils under different land use. A future soil inventory should represent the heterogeneity of organic matter through functionally different SOC pools, topsoil characteristics as well as content, pool, and flux data for the deeper mineral‐soil compartments.     

Structural changes of microbial transglutaminase during thermal and high-pressure treatment

The activity of microbial transglutaminase (MTG) and the corresponding secondary structure, measured by circular dichroism (CD), was analyzed before and after treatment at different temperatures (40 and 80 degrees C) and pressures (0.1, 200, 400, 600 MPa). Irreversible enzyme inactivation was achieved after 2 min at 80 degrees C and 0.1 MPa. Enzyme inactivation at 0.1, 200, 400, and 600 MPa and 40 degrees C followed first-order kinetics. The enzyme showed residual activity of 50% after 12 min at 600 MPa and 40 degrees C. Mobility of aromatic side chains of the enzyme molecule was observed in all temperature- and/or pressure-treated samples; however, high-pressure treatment at 600 MPa induced a loss of tertiary structure and a significant decrease in the alpha-helix content. The relative content of beta-strand substructures was significantly increased after 30 min at 600 MPa and 40 degrees C or 2 min at 0.1 MPa and 80 degrees C. We conclude that the active center of MTG, which is located in an expanded beta-strand domain, is resistant to high hydrostatic pressure and pressure-induced inactivation is caused by destruction of alpha-helix elements with a corresponding influence on the enzyme stability in solution.     

Determination of 12 type A and B trichothecenes in cereals by liquid chromatography-electrospray ionization tandem mass spectrometry

A new sensitive method for the simultaneous determination of 12 trichothecenes (deoxynivalenol, nivalenol, 3-acetyldeoxynivalenol, 15-acetyldeoxynivalenol, fusarenon X, T-2 toxin, HT-2 toxin, neosolaniol, monoacetoxyscirpenol, diacetoxyscirpenol, T-2 triol, and T-2 tetraol) by liquid chromatography-electrospray ionization tandem mass spectrometry (LC-ESI-MS/MS) is presented. The development of the method and investigations on the matrix influence on the MS signal are described in particular. The matrix effect was thereby minimized by using an internal standard, a special mobile phase, and specific fragmentation parameters. The sample was extracted with acetonitrile/water (84:16, v/v), and the extract was cleaned up with a MycoSep 227 column. Quantification was based on the internal standard de-epoxy-deoxynivalenol. Calibration curves were linear between 16 and 1600 ng/g, and the limits of detection ranged from 0.18 to 5.0 ng/g. The developed method was applied for the determination of trichothecenes in 120 naturally contaminated wheat and oat samples.     

The temperature dependence of organic-matter decomposition—still a topic of debate

The temperature dependence of organic matter decomposition is of considerable ecosphysiological importance, especially in the context of possible climate-change feedback effects. It effectively controls whether, or how much, carbon will be released with global warming, and to what extent that release of carbon constitutes a dangerous positive feedback effect that leads to further warming.The present paper is an invited contribution in a series of Citation Classics based on a review paper of the temperature dependence of organic matter decomposition that was published in 1995. It discusses the context and main findings of the 1995 study, the progress has been made since then and what issues still remain unresolved.Despite the continuation of much further experimental work and repeated publication of summary articles, there is still no scientific consensus on the temperature dependence of organic matter decomposition. It is likely that this lack of consensus is largely due to different studies referring to different experimental conditions where confounding factors play a greater or lesser role.Substrate availability is particularly important. If it changes during the course of measurements, it can greatly confound the derived apparent temperature dependence. This confounding effect is illustrated through simulations and examples of experimental work drawn from the literature. The paper speculates that much of the current disagreement between studies might disappear if different studies would ensure that they are all studying the same system attributes, and if confounding factors were always considered and, if possible, eliminated.