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OCCURRENCE OF THE RARE EARTH ELEMENTS IN COAL DERIVED HUMIC SUBSTANCES

机译:煤衍生腐殖质中稀土元素的发生

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Humic acids are ubiquitously occurring in the bio/geosphere(Stevenson 1994).Due to their polyfunctionality they can interact with metals and can fixate them in soils and sediments in a permanent manner via complexation(Tipping 2002).On coal samples high amounts of HA-heavy metal species were found(Cezikova 2001).There,the amount of humic substances depends on provenance and weathering of the coal(Martinez 1995).Aside other heavy metals also rare earth elements(REE)are bound on humic substances.Rare earth elements are widely utilized as tracers of geochemical and geological processes(Bechtel 2001).So total amounts of REE are used to indicate variations in redox conditions.Focus of this work is to evaluate the REE loads of humic substances and to obtain information on typical REE patterns useful for paleo-environmental investigations.
机译:在生物/地理学(Stevenson 1994)中,腐殖酸普遍存在于它们的多官能和它们可以与金属相互作用,并且可以通过络合(TIPPING 2002),以永久的方式将它们固定在土壤和沉积物中(TIPPET 2002)。煤样品大量HA找到了炼金石(Cezikova 2001)。腐殖质的物质量取决于煤炭的出处和风化(Martinez 1995).Aside其他重金属也稀有地球元素(REE)在腐殖质中束缚.Rare地球元素被广泛利用作为地球化学和地质过程的示踪剂(Bechtel 2001)。所以REE的总量用于表示氧化还原条件的变化。这项工作的焦点是评估腐殖质物质的重量载荷,并获取有关典型REE的信息可用于古环境调查的模式。

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