Microbial activity and bacterial composition of H2-treated soils with net CO2 fixation

The effects of H₂ gas treatment of an agricultural soil cultivated previously with a mixture of clover (Trifolium pratense) and alfalfa (Medicago sativa) on CO₂ dynamics and microbial activity and composition were analyzed. The H₂ emission rate of 250 nmol H₂ g⁻¹ soil h⁻¹ was similar to the upper limit of estimated H₂ amounts emitted from N₂ fixing nodules into the surrounding soil ([Dong, Z., Layzell, D.B., 2001. H₂ oxidation, O₂ uptake and CO₂ fixation in hydrogen treated soil. Plant and Soil 229, 1-12.]). After 1 week of H₂ supply to soil samples simultaneously with H₂ uptake net CO₂ production declined continuously and this finally led to a net CO₂ fixation rate in the H₂-treated soil of 8 nmol CO₂ g⁻¹ soil h⁻¹. The time course of H₂ uptake and CO₂ fixation in the soils corresponded with an increase in microbial activity and biomass of the H₂-treated soil determined by microcalorimetric measurements, fluorescence in situ hybridization analysis (FISH) and DNA staining (DAPI). Shifts in the bacterial community structure caused by the supply of H₂ were recorded. While the H₂ treatment stimulated β-and γ-subclasses of Proteobacteria, it had no significant effect on α-Proteobacteria. In addition, FISH-detectable bacteria of the Cytophaga-Flavobacterium-Bacteroides phylum increased in numbers.     

Acidic deposition and its effects in southwestern China

The emissions of SO₂ in China correspond at present to 8–10 TgSyr^?1. The rapid industrialization has caused a dramatic increase in the emissions in recent years and this increase is likely to continue. This paper describes studies of concentrations and effects of acidifying substances in parts of the Guizhou and the Sichuan provinces where the S-emissions are large. A small catchment about 10 km from Guiyang centre was equipped with instruments for studies of soils, soil water and streamwater chemistry. The molar ratio Al/(Ca+Mg) is > 0.8 in soil water in some places. Two small streams have median pH-values about 4.6 and 5.1. Laboratory studies with selected Chinese soils showed that the anion adsorption was low. These studies gave also important information on soil sensitivity. The studies confirm that acid deposition may affect soils in parts of south-western China, but the sensitivity varies dramatically and there is a strong need for more information.     

Die Rolle der mikrobiellen Biomasse und des mineralisch fixierten Ammoniums bei den Stickstoff-Transformationen in niedersächsischen Löß-Ackerböden unter Winter-Weizen. I. Poolgrößenveränderungen

Significance of microbial biomass and non-exchangeable ammonium with respect to the nitrogen transformations in loess soils of Niedersachsen during the growing season of winter wheat. I. Change of pool sizes Nitrogen transformations in loess soils have been examined by laboratory and field experiments. After straw application (· 8 t · ha^?1), N in microbial biomass (N_mic) increased by about 20 mg · kg^?1 soil (· 90 kg N · ha^?1 · 30 cm^?1) after 9 days of incubation (20 °C). Another laboratory experiment yielded an increase of about 400 mg of NH₄+-N · kg^?1 fixed by minerals within 1 h after addition of 1 M NH₄+-acetate. Defixation of the recently fixed NH₄+ after addition of 1 M KCl amounted to only 60 mg · kg^?1 within 50 days. In a field experiment with winter wheat 1991, an increase in N_mic of about 80 kg N · ha^?1 · 30 cm^?1 was observed from March to June. After July, growth of the microbes was limited by decreased soluble carbon concentrations in the rhizosphere. Different levels of mineral N-fertilizer (0, 177 and 213 kg N · ha^?1) did not affect significantly the microbial biomass. The same field experiment yielded a decrease of non-exchangeable ammonium on the “zero”-fertilized plot in spring by 200 kg N · ha^?1 · 30 cm^?1. The pool of fixed ammonium increased significantly after harvest. After conventional mineral N-fertilizer application (213 kg N · ha^?1). NH₄+-defixation was only about 120 kg N · ha^?1 · 30 cm^?1 until July.     

Effektivität sowie Stabilität des interspezifischen Chromosomen- und Gentransfers beim hexaploiden Weizen,Triticum aestivum L.

Zusammenfassung Basierend auf experimentellen Ergebnissen wird demonstriert, daß chromosomale Manipulationen effektiv zur gezielten Übertragung von Fremdgenen in den hexaploiden Weizen genutzt werden können und zu züchterisch bzw. agronomisch verwertbaren Produkten führten. Die Stabilität der Integration von Chromosomen oder Chromosomensegmenten und die Expression der übertragenen Gene hängt von einer Vielzahl von cytologischen und genetischen Faktoren ab. Homöologe Austauschereignisse erweisen sich als besonders geeignet, obwohl auch nichthomöologe Substitutionen und Translokationen toleriert sowie beständig vererbt werden können. Die Vorteile unterschiedlicher Transferverfahren und die dabei auftretenden Probleme werden diskutiert.

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The efficiency and stability of interspecific chromosome and gene transfer in hexaploid wheat,Triticum aestivum L.

Summary The transfer of alien chromosomes and genes into wheat can be efficiently achieved by cytogenetic manipulations. They contributed to several substitution and translocation lines with improved resistance against diseases and abiotic stress, which are utilized in breeding programs. The stability of the insertion of alien chromosomes/segments and the expression of the alien genes is depending on numerous cytological and genetical factors. When an alien segment is transferred, the natural organisation of the genes is usually maintained intact. The genes not only can compensate for most of the replaced wheat genes, but they also interact well with their neighbouring recipient genes. Although nonhomoeologous recombinations occured, the homoeologous exchanges are the most dominating. If dosage effects are desired, the target segment can be introduced to additional homoeologous chromosomes. The advantages of different procedures of transfer and their limitations are discussed.

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,Triticum aestivum L.

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Studies of Soils, Soil Water and Stream Water at a Small Catchment near Guiyang, China

Acid deposition is considered to be a major environmental problem in China, but information about effects on soils and waters is scarce. To contribute to increased knowledge about the problem a small catchment (about 7 ha) in the outskirts of Guiyang, the provincial capital of Guizhou in south-western China, was instrumented for collection of precipitation, throughfall, soil water and stream water. In addition soil samples have been collected and analyzed for key properties. Median pH in the precipitation is 4.40 (quartiles: 4.19 and 4.77) and the median sulfate concentration 228 µeq/L (quartiles: 147 and 334 µeq/L). The dry deposition of both SO₂ and alkaline dust is considerable. The sum of wet deposition of sulfate and dry deposition of SO₂ has been estimated to about 8.5 gSm^-2yr^-1. The total S-deposition may be somewhat higher due to dry deposition of sulfate and occult deposition. In soil water, SO₄ ^2- is the major anion, generally ranging from 300 to 2500 µeq/L in the different plots. Calcium is an important cation, but there is also a considerable contribution of aluminum from the soil. In some of the plots the concentrations of inorganic monomeric aluminum (Ali) are typically between 200 and 400 µm. Potential harmful levels of aluminum and/or high Ali/(Ca²⁺ + Mg²⁺) molar ratios occur in the catchment, but damages to vegetation have not yet been reported. In most cases exchangeable aluminum accounts for between 75 and 95% of the total effective cation exchange capacity (CEC_E) in the mineral soils. The aluminum chemistry cannot easily be explained by conventional models as the Gaines-Thomas ion-exchange equation or equilibrium with an Al(OH)₃ mineral phase. The stream water is generally less acidic and has considerably lower concentrations of aluminum than the soil water, even though quite acid events have been observed (pH < 4.4). The median pH values are 4.9 and 5.0 in the two first order streams and 6.3 in the dam at the lower boarder of the catchment.     

Die Bestimmung des hydraulischen Gradienten an der Befeuchtungsfront und seine Bedeutung für die Tonablösung im Boden

The determination of the hydraulic gradient of the wetting front and its relevance for clay detachment in soil As a result of some observations and experiments it must be supposed that clay migration does not only depend on the physico-chemical conditions but also on the water regime. Mechanical displacement of clay particles from its carrier can be the result of only rarely occuring high pore water velocities or of intensive changes of moisture suction at the wetting front, which can be quantified with the hydraulic gradient. A method how to determine the hydraulic gradient of the wetting front will be described. The determination and its importance for clay displacement will be explained by results of laboratory-experiments with sandy material packed into columns.     

Release and perception of ethyl butanoate during and after consumption of whey protein gels: relation between textural and physiological parameters

The influence of gel texture on parameters such as positioning of food material in the oral cavity during mastication, and salivation, and their influence on aroma release in vivo was studied. Retronasal perception was followed by means of time-resolved sensory evaluation, while volatile release patterns were observed by means of PTR-MS. A clear correlation was found between individual-specific consumption patterns and the respective sensory perception. Also, gel texture could be clearly correlated with respective physicochemical release patterns in vivo and to the corresponding retronasal aroma perception.     

Genetische Variabilität

Zusammenfassung Für die Pflanzenzüchtung ist die genetische Variabilität eine entscheidende Voraussetzung. Sie basiert auf Genmutationen, Chromosomenmutationen, Introgressionen, Autopolyploidie, Alloplasmie, transponiblen DNA-Elementen und der Kombination. Diese Variabilitätskomponenten werden charakterisiert. Außerdem wird anhand von Beispielen ihr Einfluß auf die Entwicklung der Kulturpflanzen demonstriert.Um effektiv in der Pflanzenzüchtung arbeiten zu können, bedarf es der Analyse von genetischer Variabilität. Dies geschieht mit Hilfe von Kreuzungsexperimenten und Parameterschätzungen. In zunehmendem Maße werden auch Marker bei der Analyse eingesetzt.Einen wichtigen Faktor zur zielgerichteten Beeinflussung der genetischen Variabilität stellt die Selektion dar. Sie führt zur Einschränkung der Kombination. Die Selektion ist für die Entwicklung von Sorten notwendig. Sie hat aber auch eine Verarmung an genetischer Information zur Folge.Für den weiteren Fortschritt in der Pflanzenzüchtung gilt es, eine genügende genetische Variabilität zu gewährleisten. Dazu bedarf es auch Maßnahmen zu ihrer Erhaltung. Genetische Variabilität muß außerdem verstärkt charakterisiert und analysiert werden.

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Genetic variability

Summary Genetic variability is a decisive prerequisite to plant breeding. It is based on gene mutations, chromosome mutations, introgressions, autopolyploidy, alloplasmy, transposible DNA elements and recombinations. These components of the genetic variability are illustrated and examples are given to demonstrate their contributions to the evolution of crop plants.Effective plant breeding requires the analysis of the genetic variation. It is analysed by hereditary studies and parameter estimations. The utilization of markers is continuously increasing in studies of the genetic variation.Selection is an important factor to a purposive influence on the genetic variability and leads to a restriction of the recombinations. Selection is necessary for the development of varieties but results also in an impoverishment of genetic information.For the continuous progress in plant breeding an adequate genetic variability is to secure. That includes also activities to its conservation. Furthermore the characterization and analysis of the genetic variability has to be intensified.

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Pathways and dynamics of NO3 and NH4 applied in a mountain Picea abies forest and in a nearby meadow in central Switzerland

To evaluate the pathways and dynamics of inorganic nitrogen (N) deposition in previously N-limited ecosystems, field additions of ¹⁵N tracers were conducted in two mountain ecosystems, a forest dominated by Norway spruce (Picea abies) and a nearby meadow, at the Alptal research site in central Switzerland. This site is moderately impacted by N from agricultural and combustion sources, with a bulk atmospheric deposition of 12 kg N ha⁻¹ y⁻¹ equally divided between NH₄⁺ and NO₃⁻. Pulses of ¹⁵NH₄⁺ and ¹⁵NO₃⁻ were applied separately as tracers on plots of 2.25 m². Several ecosystem pools were sampled at short to longer-term intervals (from a few hours to 1 year), above and belowground biomass (excluding trees), litter layer, soil LF horizon (approx. 5-0 cm), A horizon (approx. 0-5 cm) and gleyic B horizon (5-20 cm). Furthermore, extractable inorganic N, and microbial N pools were analysed in the LF and A horizons. Tracer recovery patterns were quite similar in both ecosystems, with most of the tracer retained in the soil pool. At the short-term (up to 1 week), up to 16% of both tracers remained extractable or entered the microbial biomass. However, up to 30% of the added ¹⁵NO₃⁻ was immobilised just after 1 h, and probably chemically bound to soil organic matter. 16% of the NH₄⁺ tracer was also immobilised within hours, but it is not clear how much was bound to soil organic matter or fixed between layers of illite-type clay. While the extractable and microbial pools lost ¹⁵N over time, a long-term increase in ¹⁵N was measured in the roots. Otherwise, differences in recovery a few hours after labelling and 1 year later were surprisingly small. Overall, more NO₃⁻ tracer than NH₄⁺ tracer was recovered in the soil. This was due to a strong aboveground uptake of the deposited NH₄⁺ by the ground vegetation, especially by mosses.