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351.
Several homologous monoalkylated benzenes were photo-oxidized as surface films on and dissolved in pure water and purified natural seawater by solar and equivalent artificial UV irradiation in the presence of anthraquinone as photo-sensitizer. The main reaction products were the 1-phenylalkanones, the corresponding secondary alcohols, benzaldehyde and, when the side chain contained four or more carbon atoms, the products of what appears to be a Norrish type II photo-degradation. The detection among the reaction products of an aldehyde with one carbon atom less than the olefin produced by the Norrish type II photo-degradation suggests a photolytic decomposition of 1-alkenes, resulting in the formation of highly reactive compounds capable of abiotic reactions in the electronic ground state with a variety of organic compounds occurring in seawater. 相似文献
352.
353.
Earthquakes in Switzerland and surrounding regions during 2004 总被引:1,自引:0,他引:1
Manfred Baer Nicolas Deichmann Jochen Braunmiller Stephan Husen Donat F?h Domenico Giardini Philipp K?stli Urs KRadolfer Stefan Wiemer 《Eclogae Geologicae Helvetiae》2005,98(3):407-418
This report of the Swiss Seismological Service summarizes the seismic activity in Switzerland and surrounding regions during
2004. During this period, 677 earthquakes and 96 quarry blasts were detected and located in the region under consideration.
With 22 events with ML≥2.5, the seismic activity in the year 2004 was close to the average over the last 30 years. As in previous years, most of
the activity was concentrated in the Valais and in Graubünden. In addition, several moderate earthquakes occurred in the lower
crust below the northern Alpine foreland. Unusual was that five earthquakes were sufficiently strong to cause ground shaking
of intensity IV over large portions of the territory. Two were located in Switzerland (Liestal, ML 3.8, and Brugg, ML 4.0). The epicenters of the other three strong events were located outside Switzerland (Besan?on in the French Jura, ML 4.8, Waldkirch in southern Germany, ML 5.1, and Lago di Garda in northern Italy, ML 5.3). 相似文献
354.
Yangrong Ling Manfred Ehlers E. Lynn Usery Marguerite Madden 《ISPRS Journal of Photogrammetry and Remote Sensing》2007,61(6):381-392
Existing image fusion techniques such as the intensity–hue–saturation (IHS) transform and principal components analysis (PCA) methods may not be optimal for fusing the new generation commercial high-resolution satellite images such as Ikonos and QuickBird. One problem is color distortion in the fused image, which causes visual changes as well as spectral differences between the original and fused images. In this paper, a fast Fourier transform (FFT)-enhanced IHS method is developed for fusing new generation high-resolution satellite images. This method combines a standard IHS transform with FFT filtering of both the panchromatic image and the intensity component of the original multispectral image. Ikonos and QuickBird data are used to assess the FFT-enhanced IHS transform method. Experimental results indicate that the FFT-enhanced IHS transform method may improve upon the standard IHS transform and the PCA methods in preserving spectral and spatial information. 相似文献
355.
Isabelle Coutand † Barbara Carrapa† Anke Deeken‡ Axel K. Schmitt§ Edward R. Sobel† Manfred R. Strecker† 《Basin Research》2006,18(1):1-26
The arid Puna plateau of the southern Central Andes is characterized by Cenozoic distributed shortening forming intramontane basins that are disconnected from the humid foreland because of the defeat of orogen‐traversing channels. Thick Tertiary and Quaternary sedimentary fills in Puna basins have reduced topographic contrasts between the compressional basins and ranges, leading to a typical low‐relief plateau morphology. Structurally identical basins that are still externally drained straddle the eastern border of the Puna and document the eastward propagation of orographic barriers and ensuing aridification. One of them, the Angastaco basin, is transitional between the highly compartmentalized Puna highlands and the undeformed Andean foreland. Sandstone petrography, structural and stratigraphic analysis, combined with detrital apatite fission‐track thermochronology from a ~6200‐m‐thick Miocene to Pliocene stratigraphic section in the Angastaco basin, document the late Eocene to late Pliocene exhumation history of source regions along the eastern border of the Puna (Eastern Cordillera (EC)) as well as the construction of orographic barriers along the southeastern flank of the Central Andes. Onset of exhumation of a source in the EC in late Eocene time as well as a rapid exhumation of the Sierra de Luracatao (in the EC) at about 20 Ma are recorded in the detrital sediments of the Angastaco basin. Sediment accumulation in the basin began ~15 Ma, a time at which the EC had already built sufficient topography to prevent Puna sourced detritus from reaching the basin. After ~13 Ma, shortening shifted eastward, exhuming ranges that preserve an apatite fission‐track partial annealing zone recording cooling during the late Cretaceous rifting event. Facies changes and fossil content suggest that after 9 Ma, the EC constituted an effective orographic barrier that prevented moisture penetration into the plateau. Between 3.4 and 2.4 Ma, another orographic barrier was uplifted to the east, leading to further aridification and pronounced precipitation gradients along the mountain front. This study emphasizes the important role of tectonics in the evolution of climate in this part of the Andes. 相似文献
356.
357.
Mineral supply is controlled by a feedback mechanism. When there is a shortage of a commodity in a market economy, prices will rise, triggering this mechanism. The expectation of high financial returns will encourage inventiveness and creativity in the quest for new solutions. On the supply side, for primary resources, the appropriate response is to cut losses in the mining process, to lower the cut-off grade, to improve recoveries in the beneficiation and smelting processes, to expand existing production facilities, and to discover and bring into production new deposits. For secondary resources, the key to increasing the supply lies in improving recycling rates by better technology, reprocessing lower-grade scrap which becomes economic because of increased prices, and reducing downgrading to optimize the usefulness of secondary materials. On the demand side, implementation of new and more efficient processes, development of substitution technologies, material savings, and the invention of entirely new technologies that fulfill the same function without the need of using the scarce and suddenly more expensive material are effective reactions to a price rise. The effectiveness of this self-regulating mechanism can be shown by examples of historical price peaks of metals, such as Mo, Co, and Ta, and the current rare earth elements peak. Concerning supply from secondary resources, a model is developed in order to determine how far the supply from this resource domain can be achieved and how the recycling rate is influenced by growth rate and lifetime. The feedback control cycle of mineral supply is influenced on the demand side by ever shorter life cycles, by products getting more complex with ever more elements involved in their production, and by an increase in element dispersion. All these factors have an immediate effect on the feasibility of sourcing raw materials from the technosphere. The supply side of primary materials is influenced by increasing lead times for new production and by relatively low flexibility in responding to changing demand. 相似文献
358.
359.
Fischer Manfred M. Paez Antonio Staufer-Steinnocher Petra 《Journal of Geographical Systems》2022,24(1):1-4
Journal of Geographical Systems - 相似文献
360.
Poverty tourism: theoretical reflections and empirical findings regarding an extraordinary form of tourism 总被引:1,自引:0,他引:1
Manfred Rolfes 《GeoJournal》2010,75(5):421-442
During the mid-1990s, a new form of tourism was established in metropolises of several developing countries or emerging nations. This type of tourism consists in visits to the most disadvantaged parts of the respective city. Poverty tours or slum tours
are offered on a relatively large scale in the South African cities of Johannesburg and Cape Town, Rio de Janeiro in Brazil,
as well as in Indian metropolises, to name some important examples. The target group of these tours consists primarily of
international tourists. It is estimated that 40,000 such tourists visit favelas in Rio de Janeiro each year, around 300,000
the townships in Cape Town. This contribution refers to and comments on these developments and insights regarding poverty
tourism or slumming, based on empirical research and experiences in South Africa, Brazil, and India. It will be shed light
on the phenomenon from an observational-theoretical perspective. It is aimed to open a discussion on the ways poverty tours
or slumming observes and simultaneously programmatically charges poverty. And, it will be considered in which way poverty
tourism is observed. 相似文献