Editorial     

Prof. Dr. Dr.habil. Gerd Wegener 《Wood Science and Technology》1997,31(1):1-1

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Prof. Dr. Gerd Wegener, Editor     

Gerd Wegener 《Wood Science and Technology》2005,39(5):327-327

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Studies on milled wood lignin from spruce Part II. Electron microscopic observations on the milled wood     

Dietrich Fengel  Manfred Stoll  Gerd Wegener 《Wood Science and Technology》1978,12(2):141-148

Summary Wood samples that had been ball-milled and extracted with dioxane under various conditions were observed in the scanning electron microscope. Ball milling causes not only a reduction in size of the cells and cell walls but also an internal disruption of the particles. The intensity of milling has a larger influence on the particle size than a prolongation of the milling time. A direct relation was established between particle size and the previously determined yield of purified milled wood lignin.Submitted by Erwin-Riesch-Stiftung zur Förderung der wissenschaftlichen Forschung.  相似文献   

Manuscript submission and processing: the new electronic pathway     

Gerd?WegenerEmail author  Robert?W.?Kennedy 《Wood Science and Technology》2004,38(7):475-476

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Editorial     

Prof. Dr. Gerd Wegener  Editor 《Wood Science and Technology》2005,39(1):1-1

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Influence of slope and exposition on water balance of loess soils   总被引：1，自引：0，他引：1  

Gerd Wessolek  Christian Roth  Ralf Knig  Manfred Renger 《植物养料与土壤学杂志》1994,157(3):165-173

Laboratory and field measurements as well as deterministic simulation models were used to determine the water components of loess derived soils with different expositions and slopes in the hilly region South of Hannover, Germany. Studies were investigated from 1987-1990 on three positions of a loess slope with 8 % inclination, 200 m length and northern exposition. Crop rotation was sugar beet, winter wheat, sugar beet. Results show that the soil water budget is strongly related to slope position, relief and plant available water in the rootzone. It was found that drainage at the bottom of a slope is often higher than on top of the slope. On slopes with northern exposition groundwater recharge increases with inclination whereas actual evapotranspiration decreases. For slopes with southern exposition the opposite reaction can be expected. The thickness of loess deposits and the root depth determine the plant available water; a sensitivity study demonstrates how groundwater recharge decreases with the amount of plant available water. This reaction is independent of the exposition of the slope. Field and simulation studies show that runoff occurs under sugar beet whenever soil is bare or sparsely covered, rainfall intensity is high and topsoil is sealed. Moreover, in loess derived soils interflow may occur on sites with stagnic horizons. Sensitivity analyses show that this process probably takes place whenever saturated hydraulic conductivity of this horizon is less than 10cm/d.  相似文献   

Einfluß von Monoethanolamin auf Ertrag und Wasserausnutzung von Sommergerste     

Hans Bergmann  Hans Eckert  Gerd Meisgeier 《植物养料与土壤学杂志》1990,153(1):21-24

Effect of monoethanolamine on yield and water use efficiency of barley The effect of monoethanolamine (EA) on yield and water use efficiency (WUE) of spring barley plants was tested in pot experiments. The application of EA (8 to 12 mg/pot) increased the grain yield and WUE by about 4 to 15 per cent under stress conditions. In addition, EA improved the utilization of fertilizer nitrogen. The yield-increasing effect of EA was associated with an increase of the number of ear-bearing tillers and an improved root growth. The effects of EA were only significant at α = 0.05.  相似文献   

a new high-pressure squeezing technique for pore fluid extraction from terrestrial soils     

Böttcher  Gerd  Brumsack  Hans-J.  Heinrichs  Hartmut  Pohlmann  Markus 《Water, air, and soil pollution》1997,94(3-4):289-296

A core consisting of minerogenic peat and organic-rich mineral sediments was collected at an altitude of 4275 m in the Ovejuyo valley, 100 km NE of La Paz in Bolivia. Age dating with 210Pb showed that the core represents approximately three centuries of sediment accumulation. None of the peats are ombrotrophic. Despite this, the Cd/Al, Cu/Al, Zn/Al, and Pb/Al ratios are all significantly higher in the surface layers, particularly in the top 6 cm: natural, abiological geochemical processes, therefore, cannot account for these elevated heavy metal/Al ratios. There are two possible explanations for the metal enrichments, relative to Al, in the surface layers: bioaccumulation by living plants, and anthropogenic atmospheric metal deposition. While the living plant layer may be responsible for the Cd, Cu, and Zn enrichments, this is an unlikely explanation for the Pb profile. In contrast to the other metals, the concentration of Pb in the first sample (dating from 1985-1994) is less than that of the second sample (dating from 1970-1985). The Pb/Al profile is consistent with the well documented, rapid increase in atmospheric Pb emissions during the present century (which accelerated following the introduction of leaded gasoline), and the decline in Pb pollution during the past 20 years (as a result of the introduction of unleaded gasoline). Thus, the Ovejuyo Valley mire has provided one of the first records of atmospheric Pb pollution in South America.  相似文献   

Measurement modeling of soil‐water dynamics evapotranspiration of drained peatland soils     

Kai Schwrzel  Jirka &#x;imnek  Martinus&#x;Th. van Genuchten  Gerd Wessolek 《植物养料与土壤学杂志》2006,169(6):762-774

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Rhizospheric influence on soil respiration and decomposition in a temperate Norway spruce stand     

Anna Ekberg  Gerd Gleixner 《Soil biology & biochemistry》2007,39(8):2103-2110

Assessments of terrestrial carbon fluxes require a thorough understanding of links between primary production, soil respiration and carbon loss through drainage. In this study, stem girdling was used to terminate autotrophic soil respiration including rhizosphere respiration and root exudation in a temperate Norway spruce stand. Rates of soil respiration and dissolved organic carbon (DOC) formation were measured in the second year after girdling, comparing an intact plant-rhizosphere continuum with an exclusive decomposer system. The molecular and isotopic composition of DOC in the soil solution was analysed with a coupled Py-GC/MS-C-IRMS system to distinguish between the carbon sources of dissolved carbon. Pyrolysis products were grouped according to their precursor origins: polysaccharides, proteins or of mixed origin (mainly derivates of lignins and proteins). When dead roots became available for decomposition, rates of heterotrophic soil respiration in girdling plots peaked at 6.5 μmol m⁻² s⁻¹, comparable to peak rates of total soil respiration (autotrophic and heterotrophic) in control plots, 6.1 μmol m⁻² s⁻¹. A significant response of soil respiration to temperature was found in control plots only, showing that an unlimiting supply of organic substrates for microbial respiration may mask any temperature effects. The enhanced decomposition in girdled plots was further supported by the isotopic composition of DOC in soil solution; all three precursor groups became isotopically enriched as the growing season progressed (polysaccharides by 2.3‰, proteins by 1.9‰, mixed origin group by 2.2‰). This indicates a trophic level shift due to incorporation of organic substrate into the microbial food chain. In the control plots’ mixed origin fraction, the isotopic composition changed over time from a signature resembling that of lignin (−28.9‰) to one similar of the protein fraction (−25.7‰). Significant temporal changes of structural DOC composition occurred in the girdling plots only. These results suggest that changes in the microbial community and in decomposition rates occurred in both girdled and control plots in the following ways: (i) increased substrate availability (dead roots) gave rise to generally enhanced performance of the decomposer community in girdled plots, (ii) root-derived exudates probably contributed to enhanced decomposition of recalcitrant lignin in the control plots and (iii) the structural composition of DOC seemed to be more a result of decomposition than of plant root exudation in all plots.  相似文献