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Soil carbon stocks estimation with reference to the degree of volcanic ash additions in Japanese forest soils

机译:参考日本森林土壤中火山灰的土壤碳储量估算

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The objective of this study is to clarify the influence of volcanic ash addition on the soil carbon stocks and their accumulation process in Japanese forest soils. Volcanic ash additions to the soil were estimated based on the acid ammonium oxalate extractable aluminium (Alox) content, lithic fragment abundance and their vertical distribution patterns. The carbon in soil samples is controlled by Al-humus complex formation which is determined by the free Al generated from accumulated volcanic ash. Thestratigraphical relationship of volcanic ash accumulation horizons affected the vertical distribution of carbon. In addition, successive accumulation of volcanic ash on the soil surface leads to development of the soil surface horizon and to increased soil carbon stock. These influences to soil carbon accumulation due to the degree of volcanic ash addition to soil resulted in variable soil carbon stocks among soil types reflecting the degree of volcanic ash addition. Our results suggest that volcanic ash addition controls the soil carbon stock of these Japanese forest soils.
机译:本研究的目的是阐明日本森林土壤土壤碳储量对土壤碳储量的影响及其积累过程。基于草酸铵可提取的铝(Alox)含量,岩石片段丰度及其垂直分布图来估计土壤的火山灰添加。土壤样品中的碳由Al-Humus复合物形成控制,该组络合物形成由来自积聚的火山灰产生的游离A1确定。火山灰积聚视野的分离性关系影响碳的垂直分布。此外,土壤表面上的火山灰的连续积累导致土壤表面地平线的发展和增加土壤碳储备。由于土壤中的火山灰程度导致土壤碳积累的影响导致土壤类型的可变土壤碳储量,反映了火山灰的增加程度。我们的研究结果表明,火山灰添加控制了这些日本森林土壤的土壤碳储备。

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