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Systematic geochemical study of the soils, litter, and bedrock of a Permian limestone mountain, Central Japan

机译:对日本中部二叠纪石灰岩山地的土壤,凋落物和基岩的系统地球化学研究

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The paper deals with the results of a systematic geochemical study of soils at Mt Kinshozan in Central Japan, a limestone area known for its well-preserved Permian fossils. Compared with the typical composition of the Japanese upper continental crust, here the soils were found depleted in Si, Ca, Na, Mg, and K and rich in Ti, Al, and Fe. They were enriched with some heavy metals (Cr, Ni, Cu, Pb, and Zn) detected also in the acetic-acid residue of the limestone collected from Mt. Kinshozan. Therefore, the residual materials produced through chemical weathering of the limestone bedrock may have significantly contributed to the soils formation. Concentrations of Ctotal were nearly identical to Corg and the relationship between Ctotal and Element/TiO2 suggested a significant contribution of the litter to Si, Mg, Ca, and P in the soils.
机译:本文涉及对日本中部金山山(Mt Kinshozan)土壤进行系统化地球化学研究的结果,该地区以保存完好的二叠纪化石而闻名。与日本上层地壳的典型成分相比,这里的土壤贫化了硅,钙,钠,镁和钾,富含钛,铝和铁。他们还从从山中收集的石灰石的乙酸残留物中富集了一些重金属(Cr,Ni,Cu,Pb和Zn)。金正山。因此,通过石灰石基岩的化学风化产生的残留物质可能对土壤形成有很大贡献。 C total 的浓度几乎与C org 相同,并暗示了C tal 与Element / TiO 2 之间的关系垃圾对土壤中硅,镁,钙和磷的重要贡献。

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