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Total content of macroelements and trace elements in Holocene calcareous gyttja from the post-bog area of North-western Poland

机译:波兰西北部沼泽地区全新世钙质Gyttja中宏观重组和微量元素的总含量

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摘要

The study covered 6 sites located in the Vistula glaciation area in north-western Poland, where the Holocene calcareous (gyttja) deposits occur. Three types of such calcareous deposits were isolated: manly (groundwater calcretes) (CaCO3 80%, loss of ignition 20%, non-carbonate fractions 20%), calcareous gyttja (CaCO3 50-80%, loss of ignition 40%, non-carbonate fractions 40%), and clay calcareous gyttja (CaCO3 20-50%, loss of ignition 30%, non-carbonate fractions 60%). The content of major and trace elements was determined in different horizons. Several parameters of Holocene calcareous deposits were determined, namely carbonate status, total organic carbon, non-carbonate mineral fractions and several major and minor components. Close correlations between CaCO3 and Ca, Mg contents, between non-carbonate fraction and K, Zn and Cu contents, as well as between ignition loss and Zn and Cu contents were observed in the sediments. The sediments exhibit vertical variability which relates to the genesis of sediments and soils. The highest content of macroelements was recorded in the uppermost layers for Ca, Mg, Na, and Mn and for microelements (trace elements) in bottom layers for S, P, K, Fe, Zn, Cu, Pb, and Ni.
机译:该研究涵盖了位于波兰西北波兰维斯杜的冰川地区的6位点,其中发生全新世钙(Gyttja)沉积物。孤立三种类型的这种钙质沉积物:男子气概(地下水囊)(CaCo3& 80%,点火丧失<20%,非碳酸酯馏分20%),钙质Gyttja(CaCO 3 50-80%,丧失点火& 40%,非碳酸馏分馏分40%)和粘土钙质Gyttja(CaCO 3 20-50%,点火损失<40-50%,损失叶片30%,非碳酸盐馏分60%)。主要和微量元素的含量在不同的视野中确定。确定全新世钙质沉积物的几个参数,即碳酸盐状态,总有机碳,非碳酸矿物级分和几种主要和次要成分。在沉积物中观察到CaCO 3和Ca,Mg含量,非碳酸酯馏分和K,Zn和Cu含量之间的相关性,以及点火损失和Zn和Zn和Cu含量之间的相关性。沉积物表现出垂直变异性,涉及沉积物和土壤的成因。宏观重组的最高含量被记录在Ca,Mg,Na和Mn的最上层中,以及S,P,K,Fe,Zn,Cu,Pb和Ni的底层中的微量元素(痕量元素)。

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