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Ecological investigations at four streams in Saxony‐Anhalt have shown that there are considerable differences between the self‐purification power of upland and lowland streams. This result is reflected in chemistry and in microbiology. The structure of the bottom substrate mainly influences the degree of self‐purification in connection with rate of flow and flow velocity. The results and differences are demonstrated using the example of Katzsohlbach in the landscape unit “Mittel‐ and Unterharz” and the stream Olbe in the landscape unit “Magdeburger Börde”. 相似文献
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Azad Sağlam Selçuk M. Korhan Erturaç Serkan Üner Erman Özsayın Edwige Pons-Branchu 《Geodinamica Acta》2017,29(1):1-19
Fissure-ridge travertines (FRTs) are of great importance for the determination and comparison of tectonic deformation in a region. The coeval development of these travertines with active fault zones supplies significant information about regional dynamics in terms of deformation pattern and evolution. In this paper, the characteristics of FRTs of the Ba?kale basin (eastern Turkey) and responsible regional tectonism are discussed for the first time. The Ba?kale basin is located between the Ba?kale Fault Zone (BFZ) characterised by Çaml?k fault and I??kl?–Zirani? fault. It is located between dextral Yüksekova Fault Zone and southern end of dextral Guilato–Siahcheshmeh–Khoy Fault system (Iran). Various morphological features indicating recent activity are exposed along the BFZ, including offsetting rivers, fissure-ridge travertine and fault scarps. The Çaml?k fissure-ridge travertine composing of three different depositions is observed along the eastern edge of the BFZ with approximately parallel orientations. The Çaml?k fissure-ridge travertine has been formed and developed on fault zone related to strike-slip or oblique movements. We explain how kinematic changes of faults can influence the fissure-ridge development. 相似文献
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Z. Lagn 《洁净——土壤、空气、水》1999,27(1):19-26
The species composition of clostridial communities of the sediment in a polluted area of the Danube (South of Budapest, Háros‐Bay, Hungary) was investigated. The spore counts exceeded 700...800 CFU per gram (wet weight). 23 clostridial strains were identified by using API 20A anaerobe identification kits, another 20 physiological, biochemical, and ecological tests were also carried out. Results of numerical analysis showed that the clostridial community in the sediment of the Danube is composed of at least 4 different species. Members of C. perfringens, indicating to fecal contamination, C. subterminale and related bacteria were dominant in the examined area. All strains showed wide pH (5...9) and temperature (3...45°C) tolerance. They were able to grow on media containing significant amounts of lead (Pb2+), mercury (Hg2+), copper (Cu2+), and zinc (Zn2+). Strains of C. perfringens showed a wide range of degradative capacities (acid production from many different carbohydrates, gelatinase, lecithinase, lipase production, etc.). 相似文献
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