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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Contribution of charred plant fragments to soil organic carbon in Japanese volcanic ash soils containing black humic acids
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Contribution of charred plant fragments to soil organic carbon in Japanese volcanic ash soils containing black humic acids

机译:含黑色腐殖酸的日本火山灰土壤中烧焦的植物碎片对土壤有机碳的贡献

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摘要

Charred plant fragments were isolated from 24 Japanese volcanic ash soils by specific gravity (s.g.) method, using a sodium polytungstate solution. Microscopic observation indicated that the charred plant fragments, which are black or blackish brown, were the main component in both fractions of less than s.g. 1.6 g cm(-3) isolated before and after HCl-HF treatment of the soil samples. Furthermore, it was suggested that most of the fragments in the < 1.6 fraction isolated before the treatment originated from the xylem of woody plants. While, the fragments in the < 1.6 fraction isolated after the treatment were mainly amorphous. The organic-C content of the former fraction, ranging from 0.34 to 6.1 g per kg whole soil, was much lower than that of the latter fraction, ranging from 0.74 to 42 g per kg whole soil. Total organic-C content of the whole soil was highly correlated with contribution to this carbon from the charred plant fragments. In many soils, the percentage contribution was 9% or more with a maximum value of 33%, suggesting that charred plant fragments should not be overlooked as one of the constituents of organic matter in volcanic ash soils. From the findings in the present and previous studies, it was assumed that charred plant fragments deserve close attention as one of the sources of black humic acids which characterize Japanese volcanic ash soils. (C) 2003 Elsevier Ltd. All rights reserved. [References: 24]
机译:使用聚钨酸钠溶液通过比重(s.g.)方法从24种日本火山灰土壤中分离出烧焦的植物碎片。显微镜观察表明,焦炭的植物碎片为黑色或黑褐色,是小于s.g.的两个部分的主要成分。在HCl-HF处理土壤样品之前和之后分离出1.6 g cm(-3)。此外,建议在处理之前分离的<1.6部分中的大多数片段源自木本植物的木质部。而在处理后分离的<1.6部分中的片段主要是无定形的。前一部分的有机碳含量为每千克全土壤0.34至6.1 g,远低于后部分的每千克全土壤0.74至42 g。整个土壤中总有机碳含量与炭化植物碎片对此碳的贡献高度相关。在许多土壤中,贡献百分比为9%或更高,最大值为33%,这表明烧焦的植物碎片不应被视为火山灰土壤有机质的组成成分之一。根据目前和先前研究的发现,认为烧焦的植物碎片作为黑色腐殖酸的来源之一值得密切关注,而腐殖酸是日本火山灰土壤的特征之一。 (C)2003 Elsevier Ltd.保留所有权利。 [参考:24]

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