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  • 1
    ISSN: 1432-0495
    Schlagwort(e): Key words Heavy metal pollution ; Diagenetic processes ; Runoff pollution
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Notizen: Abstract  Retention ponds have been dug along some of the motorways in France to minimize environmental pollution by keeping pollutants from spreading over the surrounding area. In the current work, eight core samples were collected from the bottom of a retention pond located along the A-71 motorway in Sologne to study the pollution of sediment by heavy metals and their diagenetic behaviour. The vertical concentration profiles of metals (Pb, Zn, Cd, Fe and Mn) in sediment as well as in interstitial water were determined. Especially in the case of the sediment, a sequential extraction method was employed to investigate how the movement of each metal is associated with the other metals and with other solid phases such as organic matter. In addition, to investigate the relative mobility of the metals, the distribution coefficients (KD) were also determined. The concentrations of the metals were always found to be highest in the topmost layer of sediment. This so-called surface enrichment is caused by a substantial increase of the non-detrital fraction of these metals at the sediment surface. For instance, the accumulation of Pb and Zn is associated with the increase in the "fraction II" in the sequential extraction. The accumulation of Cd at the surface (0–2 cm) is partly due to the liberation of Cd from the particles during early diagenesis. However, the major factor contributing to the accumulation of Cd at the sediment surface is attributed to the dissolution of Cd from polluted roadside soil during the periods of rainstorms and its subsequent redeposition on the sediment surface after being carried to the retention pond. KD values for Zn and Cd were found to decrease with depth, while KD values for Pb increased. Based on the KD values, the relative mobilities of the studied metals were determined to be as follows: Mn〉Zn〉Cd〉Pb, for the upper layer, and Mn〉Cd〉Zn〉Pb, for the layers below.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 2
    Digitale Medien
    Digitale Medien
    Springer
    Physics and chemistry of minerals 14 (1987), S. 377-382 
    ISSN: 1432-2021
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Geologie und Paläontologie , Physik
    Notizen: Abstract Hydrotalcite-like solid solutions have been synthesized by coprecipitation in basic solutions with variable SO 4 2− /CO 3 2− ratios. Chemical determination of CO 3 2− in the interlayer was impossible because of the presence of minor hydromagnesite. SO 4 2− was determined both by chemical analysis and X-ray photoelectron spectroscopy (XPS), the two methods giving similar results. A Raman spectrometry gave additional data on the SO 4 2− /CO 3 2− ratio. Then, the stoichiometry of the anionic interlayers, X s , X c , and X OH were determined, and the influence of X s on the c′ parameter (increasing from c′=7.97 Å to c′=8.63 Å between X s =0 and X s =1) was characterized. In addition, a partitioning curve of SO 4 2− and CO 3 2− between aqueous solutions and hydrotalcite-like compounds was established. Its general shape strongly suggests a miscibility gap between a sulfate-rich end and a carbonate-rich solid solution (maximum SO 4 2− /CO 3 2− about 0.2). This result explains why most of the hydrotalcites synthesized during experimental alteration of basaltic glasses by sea-water (a sulfate-rich solution) are CO 3 2− -rich solid solutions.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 3
    ISSN: 1432-1866
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Beschreibung / Inhaltsverzeichnis: Abstract Fluid inclusion studies in end-crystallisation minerals from Chavaniac mine (mainly fluorite and baryte) show that temperature and salinity fell during crystallisation. Crystallisation of fluorite began at around 140°C±10°C, in a solution containing about 20% NaCl. The temperature of formation of baryte never exceeded 40°C and the dilute solutions sometimes contained emulsified hydrocarbons. Relations have been established between paragenetic succession, fracture phases, and the above results.
    Notizen: Résumé L'étude des inclusions fluides des minéraux de fin de cristallisation (principalement fluorite et barytine) du filon de Chavaniac, montre une diminution de la température et de la salinité. La fluorite a commencé à se déposer vers 140°C±10°C dans une solution renfermant 20% en poids en équivalents NaCl. La température de formation de la barytine était de 40°C au plus et les solutions diluées renfermaient parfois en émulsion des hydrocarbures liquides. On a pu établir des relations entre succession paragénétique, phases de fracturation, et les résultats précédents.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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