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151.
152.
Morphology and environment of cold-water coral carbonate mounds on the NW European margin 总被引:6,自引:0,他引:6
A. J. Wheeler A. Beyer A. Freiwald H. de Haas V. A. I. Huvenne M. Kozachenko K. Olu-Le Roy J. Opderbecke 《International Journal of Earth Sciences》2007,96(1):37-56
Cold-water coral carbonate mounds, owing their presence mainly to the framework building coral Lophelia pertusa and the activity of associated organisms, are common along the European margin with their spatial distribution allowing them
to be divided into a number of mound provinces. Variation in mound attributes are explored via a series of case studies on
mound provinces that have been the most intensely investigated: Belgica, Hovland, Pelagia, Logachev and Norwegian Mounds.
Morphological variation between mound provinces is discussed under the premise that mound morphology is an expression of the
environmental conditions under which mounds are initiated and grow. Cold-water coral carbonate mounds can be divided into
those exhibiting “inherited” morphologies (where mound morphology reflects the morphology of the colonised features) and “developed”
morphology (where the mounds assume their own gross morphology mainly reflecting dominant hydrodynamic controls). Finer-scale,
surface morphological features mainly reflecting biological growth forms are also discussed. 相似文献
153.
Peter Herzsprung Elke Bozau Olaf Büttner Anja Duffek Kurt Friese Matthias Koschorreck Martin Schultze Wolf v. Tümpling Katrin Wendt‐Potthoff 《洁净——土壤、空气、水》2006,34(6):593-607
Pore water of sediments plays an important role in aquatic systems as mediator and as the reactive zone between the sediment and surface water. Sediment pore waters with high ionic strength from acidified pit lakes were investigated to obtain information about the influence on the lake water quality. The analysis of soluble reactive phosphorus, nitrate, ammonium, silica, dissolved organic carbon, ferrous iron, sulfate, chloride, sodium, potassium, calcium, magnesium, manganese, and total dissolved iron was predetermined as the dataset required for evaluation of water quality. The data collection procedure was optimised by designing a methodology for stabilisation, dilution of pore water samples and adaptation of analytical methods. The developed methodology was evaluated with respect to the effort required in the laboratory under routine conditions. In the first round of analyses, 72% of 638 individual analyses from a random selection of pore water profiles were found to be within the calibration ranges. Remedial actions to handle the remaining 28% of invalid analytical results are exemplified. Differences between comparative analyses of some ions by continuous flow analysis, ion chromatography, and atomic emission spectroscopy were evaluated. The majority of results measured by ion chromatography differed on a highly significant level from results measured by atomic emission spectroscopy. Possible reasons, originating from the extreme sample matrix, are discussed. Finally, the designed methodology and the results of the method comparison are used to recommend the selection of analytical methods under specific conditions. 相似文献
154.
G. Beyer 《Journal of Geodesy》2003,76(9-10):557-568
155.
In international climate policy discussions, one of the centralissues for medium- to long run climate protection strategiesis the uncertainty about the costs and the distributional effectsof specific unilateral or multilateral emission reductions. Thispaper looks at the world-wide effects of climate protection strategieson the allocation of resources, on economic growth in differentregions, and on the regional welfare effects. The analysis isbased on a global recursively dynamic, multi-region, multi-sectorcomputable general equilibrium model parameterized accordingto the ICLIPS (Integrated Assessment of Climate Protection Strategies)integrated assessment model. The simulations show that nationalclimate policies will have important international repercussions.It is therefore important to consider international allocationeffects in the analysis of national climate protection strategies.The welfare costs of greenhouse gas emission reductions risemore than proportionally with lower emission targets. The analysisof the carbon leakage rate indicates that most of the leakagerapidly disappears if emission reduction moves towards an efficientdistribution of emission targets. 相似文献
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In this work, numerical modeling is used to evaluate and interpret a series of detailed and well‐controlled two‐dimensional bench‐scale conservative tracer tank experiments performed to investigate transverse mixing in porous media. The porous medium used consists of a fine matrix and a more permeable lens vertically aligned with the tracer source and the flow direction. A sensitivity analysis shows that the tracer distribution after passing the lens is only slightly sensitive to variations in transverse dispersivity, but strongly sensitive to the contrast of hydraulic conductivities. A unique parameter set could be calibrated to closely fit the experimental observations. On the basis of calibrated and validated model, synthetic experiments with different contrasts in hydraulic conductivity and more complex setups were performed and the efficiency of mixing evaluated. Flux‐related dilution indices derived from these simulations show that the contrasts in hydraulic conductivity between matrix and high‐permeable lenses as well as the spatial configuration of tracer plumes and lenses dominate mixing, rather than the actual pore scale dispersivities. These results indicate that local material distributions, the magnitude of permeability contrasts, and their spatial and scale relation to solute plumes are more important for macro‐scale transverse dispersion than the micro‐scale dispersivities of individual materials. Local material characterization by thorough site investigation hence is of utmost importance for the evaluation of mixing‐influenced or ‐governed problems in groundwater, such as tracer test evaluation or an assessment of contaminant natural attenuation. 相似文献
160.