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首页> 外文期刊>Soil Science Society of America Journal >Organic matter in volcanic ash soils under forest and paramo along an Ecuadorian altitudinal transect
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Organic matter in volcanic ash soils under forest and paramo along an Ecuadorian altitudinal transect

机译:厄瓜多尔海拔样带下森林和准自然条件下火山灰土壤中的有机物

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摘要

The volcanic ash soils along an altitudinal transect in Guandera Biological Station in northern Ecuador have been developed under varying vegetation around the upper forest line. Generally, the soils currently covered by forest are composed of Fulvic Andosols (melanic index >1.7) while those under paramo (tropical alpine grasslands) have developed into Melanic Andosols. This vegetation effect on soil formation is believed to be associated with differences in organic matter composition. We examined whether Fulvic Andosols differed from Melanic Andosols in organic matter composition. Using analytical pyrolysis techniques, we found hardly any differences in the organic matter characteristics related to vegetation cover, not even between soils that supposedly have been covered by forest and paramo for millennia. Small differences were found within the lipid compounds, while the polysaccharides and lignin were virtually absent from the (deeper) mineral soil horizons. The low abundance of polysaccharides in soils that have undergone severe organic matter decomposition is not unusual for most soils, but is uncommon in other Andosols studied with the same pyrolysis techniques..
机译:厄瓜多尔北部关德拉生物站沿海拔断面的火山灰土壤是在上林线周围的各种植被下发育的。通常,目前森林所覆盖的土壤是由镰刀菌Andosols(黑色素指数> 1.7)组成的,而paramo(热带高山草原)下的土壤已发展为Melanic Andosols。据信这种对土壤形成的植被效应与有机物组成的差异有关。我们检查了Fulvic Andosols在有机物成分上是否不同于Melanic Andosols。使用分析热解技术,我们几乎没有发现与植被覆盖有关的有机质特征有任何差异,甚至在据称几千年来被森林和准分子覆盖的土壤之间也没有差异。在脂质化合物中发现很小的差异,而(较深的)矿物土壤层实际上不存在多糖和木质素。在大多数土壤中,经历了严重有机物分解的土壤中多糖的低丰度在大多数土壤中并不罕见,但在其他使用相同的热解技术研究的Andosols中并不常见。

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