Soho Observations of the Connection Between Line Profile Parameters in Active and Quiet Regions and the Net Red Shift in Euv Emission Lines

We present high spatial and spectral resolution observations of one active and one quiet-Sun region, obtained with CDS and SUMER on SOHO. The connections between the line profile parameters are studied and a systematic wavelength shift towards the red with increasing peak line intensity (line broadening) is detected. The large scatter in the data calls for another approach. We apply conditional probability analysis to a series of EUV emission lines and find significant correlations between line profile parameters. For a given interval in wavelength shift we find that: (1) line profiles with large intensities (line widths) and red shifts above the average constitute an increasing fraction of the profiles as the relative wavelength shift increases, (2) line profiles with large intensities (line widths) and blue shifts compared to the average, on the other hand, constitute a decreasing fraction of the profiles as the relative wavelength shift increases. These results extend the findings of an earlier quiet-Sun study from one to several emission lines and expand the validity to include the active region. Interestingly, the active region observations show correlations between peak line intensity and wavelength shift in the coronal lines.The tendency for red-shifted profiles to be more intense than blue-shifted profiles will shift line profiles derived by integrating along the slit towards the red. From the present observations we are not able to determine the fraction of the net red shift that emerges from this correlation. We suggest that the same mechanism is responsible both for the correlation between the line profile parameters and for the differential red shift between the transition region and chromospheric emission lines.     

Transport von Feldspäten und Quarz im Temperaturgefälle

In the attempt to study the composition and behaviour of metasomatically active solutions we have examined the kind of gaseous solutions which are formed by water in contact with the minerals of a granite under a pressure of 2000 bars at 600° C, and how these solutions behave within a temperature gradient at the same pressure. The temperature ranged from 620° to 180° C. The following minerals were considered: quartz, K-feldspar (adularia), plagioclase (andesine) and mixtures of quartz with adularia, quartz with andesine, quartz with adularia and andesine, quartz mixed with mierokline-perthite, oligoelase and biotite.All these minerals are completely dissolved by water under these physical conditions. The solutions always contain more silica than the minerals, if quartz is present. The dissolved components are transported within the temperature gradient. In the solutions, Ca derived from the anorthite-component of the plagioclase and Mg from the biotite form associations together with silica, which travel tohigher temperatures. There they crystallize in form of wollastonite and/or diopside. On the other hand, Na and K, AI and the Fe from the biotite and the largest part of the silica, travel from the 600° C-region tolower temperatures. There they crystallize in form of quartz, K-feldspar, albite, some muscovite and Mg-free biotite rich in Fe. In experiments of only short duration, metastable analcime instead of albite has been formed. In long lasting experiments of 10 weeks, a separation of Na and K was evident: Albite was formed in the temperature range 470° to 420° C, whereas K-feldspar (with some albite component) and Mg-free biotite crystallize together with quartz in a larger temperature range below 420° C; see figure 6.The different minerals from a mixture influence each other's solubility in such a way that the amount of both feldspars and quartz dissolved and transported within a unit of time is decreased. Compared with the amount obtained when quartz alone constitutes the solid phase, only 40 % of that amount is dissolved and transported when the quartz had been mixed with adularia; the value amounts to only 30% when it was mixed with andesine. When both feldspars. are present together with quartz, the amount of dissolved and transported quartz is decreased to about 20 % of the original amount; see table 7. However, in all cases the amount of dissolved quartz is larger than the sum of the dissolved feldspar substances. Thus, the solution formed from a mixture of quartz and feldspars which is transported to lower temperatures always contains more silica than the mineral mixture. The amount of adularia dissolved and transported is reduced by the presence of quartz to 1/6 of that amount furnished at 6000 C by adularia alone. Under the same conditions the amount of andesine is reduced to one half. — The amount of adularia transported per unit of time is nearly equal to the amount of plagioclase components if quartz is present. However, if no quartz is present, the proportion of dissolved and transported adularia to plagioclase-components is noticeably shifted in favour of adularia. This would be the case with syenite as the source for the solutions.In the attempt to produce skarns in a way closely related to nature, silica-rich solutions from a granite have been brought into contact with dolomite. The contact was situated at 600°, 570° and 500° C. With equal duration of the experiments, the results were similar. With different durations the following effect was observed: at the beginning, the silica-rich solution reacts with the dolomite under formation of forsterite, calcite and C0₂. When more materialis transported into the contact,region diopside (the mineral containing more silica) is formed from calcite, forsterite and additional silica. When the same metasomatically active solution meets a marble, (contact at 600° C) wollastonite is formed. In these metasomatic processes the partial pressure of C0₂ in the gasphase remained low under our experimental conditions.     

Die Definitionen von Grauwacke,Arkose und Ton

Ohne Zusammenfassung     

Ein geologischer Querschnitt durch den Vogelsberg von Gießen bis Stockhausen bei Lauterbach

Ohne Zusammenfassung     

Die Bildung der Dreikanter

Ohne Zusammenfassung     

Physiological changes in the coastal marine cyanobacterium Synechococcus sp. PCC 7002 exposed to low ferric ion levels

Cyanobacteria are ubiquitous in marine waters. These prokaryotic cells are of particular interest in areas of the ocean where the availability of iron may be limiting for cell growth since these organisms commonly excrete iron-specific organic ligands (siderophores) in response to low levels of iron. It is generally considered that the production of siderophores provides a competitive advantage over the competing microorganisms that do not produce these ligands.In order to ascertain the influence of iron availability on the physiology of picoplanktonic cyanobacteria we performed a series of experiments on the coastal coccoid cyanobacterium, Synechococcus sp. PCC 7002. Physiological responses were examined in cells grown in a continuous cuture system with influx media containing a range of iron concentrations (from 4.2 × 10⁻⁵ to 5.1 × 10⁻⁹ M FeCl₃). Steady-state growth rates, combined with growth data from batch cultures demonstrated a non-linear response between iron availability and cell proliferation: cell yields were considerably higher in the lowest-iron chemostats than predicted based on the yields in the higher-iron chemostats. The higher yields during low-iron growth corresponded with the production of the extracellular siderophores and the induction of the specific iron-siderophore membrane transport proteins. A comparison of iron transport and carbon acquisition rates between the low-iron grown cells and the high-iron grown cells indicates that under low-iron growth conditions, iron and carbon acquisition meets the growth demands of the cells, whereas growth at higher iron levels enabled excessive (luxury) carbon acquisition and storage. We conclude that cyanobacteria are efficiently adapted to grow in low-iron environments (providing sufficient light for photosynthesis is available) and the luxury-uptake of carbon may serve as the source material for the extracellular ligands released by these cells. Since the release of siderophores was at iron levels in excess of the levels that induce the siderophore-mediated transport of iron, cyanobacteria growing in an environment with varying levels of iron may contribute substantial amounts of their stored carbon reserves into the DOC as iron-specific ligands.     

Decoding dispossession: Eviction and urban regeneration in Johannesburg's dark buildings

In January 2012 the residents of an inner‐city tenement building in Doornfontein, Johannesburg, were evicted on a court order. The building was situated in a post‐industrial neighbourhood in which thousands of South Africans and foreign nationals, many blind or disabled, live in unlawfully occupied buildings without access to water, basic sanitation, electricity and waste management services. Such buildings are known in policy discourse as ‘bad buildings’, and informally as ‘dark buildings’, invoking both a sense of developmental failure and spiritual insecurity. In this paper I analyse how urban renewal policies created social divisions and alliances not only among the residents of Chambers, which were channelled along nationalist lines, but also between the able‐bodied and disabled, and produced new social alliances. In particular, I document how a group of blind Zimbabweans experienced threats of violence and accusations of betrayal, as they were offered alternate accommodation by the evicting company because of their disability. I argue here that the pressures of private‐sector housing developments intersected with the insecurities and divisions of inner‐city social spaces and also fostered new alliances. Following the work of Deleuze and Guattari, I invoke the concept of ‘decoding dispossession’, proposing that ongoing evictions and dispossessions are characterized by simultaneous movements of ‘decoding and deterritorialization’ and ‘overcoding‐reterritorialization’.     

Geothermal evolution of the Astrakhan Arch region of the Pricaspian basin

The Astrakhan Arch region contains one of the largest sub-salt structures of the Pricaspian basin, where perspectives for hydrocarbon generation and accumulation in the Devonian to Carboniferous deposits are considered to be high. The paper addresses the problem of structural and geothermal evolution of the region deformed by salt movements. Initially, we developed a model of the regional structural evolution along a geological profile using the volume-balancing and back-stripping methods and geological constraints on the sedimentation, erosion, and paleo-water depths. Then we developed geothermal models (along the study profile) associated with the regional structural evolution. The models were constrained by the temperatures measured in four deep boreholes along the profile. We show that the present temperatures and heat flux are influenced by the presence of salt diapirs. Since the Early Carboniferous and till Middle Permian times, the temperatures predicted by the models vary significantly due to the regional transgression and the presence of seawater. The temperature of Devonian–Carboniferous carbonates increases since the Late Permian (time of post-salt deposition) and attains its maximum values in the SW-part of the profile. If the model assumptions concerning the constant vertical and zero lateral heat fluxes are valid, we can conclude that hydrocarbons are most likely to be generated in the SW-part of the region for the post-Early Permian time.