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  • 1
    In: (2000)
    In: year:2000
    Materialart: Online-Ressource
    Seiten: Ill., graph. Darst
    Sprache: Unbestimmte Sprache
    Anmerkung: Chemical geology
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    ISSN: 1573-3025
    Schlagwort(e): Algae ; Sandstone ; Biodeterioration ; Trentepohlia ; Aerobiology
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Biologie
    Notizen: Abstract The occurrence of a sub-aerial microbial community dominated by a species ofTrentepohlia, a red-orange pigmented filamentous green alga, growing on a 13th century sandstone building in the Scottish borders appears to be associated with unusual stone decay. Decay, in the form of extensive surface spalling and grain dissagregation over large areas of external stonework, are coincident with the distribution of the algal community on the north facade of the building. Comparison of S.E.M. images taken of fresh intact stone and spalled stone from decayed zones suggests that the mechanisms of decay may, in part, be a physical process which results in quartz crystals becoming separated. The investigations carried out revealed little evidence of chemical processes which may be involved in the decay. Large filaments ofTrentepohlia are clearly visible growing vertically between separate grains of stone and the amount of highly absorbent mucilage present makes the friable dry spall become soft and gelatinous on wetting. It is possible that the observed decay may have been created through the mechanical action of wet-dry cycling of mucilage and expansive stress from the growth of algal filaments.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Digitale Medien
    Digitale Medien
    Springer
    Water, air & soil pollution 98 (1997), S. 79-104 
    ISSN: 1573-2932
    Schlagwort(e): acid rain ; mineral weathering ; model assessment ; PROFILE ; soil
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Energietechnik
    Notizen: Abstract The PROFILE model is used extensively in the European Critical Loads programme as an aid to international negotiations on SO2 emission abatement. PROFILE calculates the rates of cation release by mineral weathering and it then uses these data to calculate soil solution and runoff chemistry. No independent assessment of the underlying assumptions and data in the model has been published and this paper reports such an assessment. The rate equations, which are the key to the PROFILE model require rate coefficients and constants. These have been derived from the literature but more work is required to produce a consistent set of constants. Manipulation of these rates to take into account the exposed reactive surface area of the minerals is fraught with problems. Calculation of exposed mineral surface area from soil textural data results in under-estimates and the requirement to determine the surface area fraction of the different minerals in the soil to be known is extremely difficult if not impossible. Further uncertainty is introduced by adjustment of the rates to take into account temperature differences and by the use of a default mineralogy which is compositionally unrealistic. Despite its flaws PROFILE usually predicts similar weathering rates to other methods of calculation. It is argued that the unrealistic constraints imposed by the use of the surface area equation may be responsible for limiting calculated weathering rate to a fixed range which coincides with characteristically determined values for weathering rates.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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