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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Variation in hopanoid composition and abundnce in forest soild during litter decomposition and humification
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Variation in hopanoid composition and abundnce in forest soild during litter decomposition and humification

机译:凋落物分解和腐殖化过程中土壤土壤中类胡萝卜素组成和丰度的变化

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The structures and concentrations of hopanoids, a family of pentacyclic triterpenoids, were analysed to determine their contribution to the alkyl carbon with increasing soil depth of a Haplic Podzol (from the Oi to the Bs horizon). After the isoltion of solvent-extractable hopanoids, the soil samples were subjected to sequential chemical degradtion comprising the cleavage of ester and ther bonds and the oxidative cleavage of aliphatic-aromatic carbon linkages between hopanoids and the macromolecular organic matrix. Identification and quantification of the substances investigatd were carried out by GC-MS. On the basis of the different analytical steps hopanoids were released as hydro-carbons, alcohols, and acids, with 31 up to 35 carbon aotms. No hopanoids were found in the Oi horizon; the concentrations rose markedly from the Oe to the Oa and E1 horizon (up to 565 #mu#g g~(-1) total organic carbon) showing a minimum in the E2 horizon and a second maximum in the Bs horizon. The behaviour of these substances with increasing depth can be explained by varying activity of hopanoid-producing microorganisms and/or translocation processes due to podzolization. Because of ht elow concentrations, hopanoids and other triterpenoids do not play an important role in the enrichment of alkyl-carbon compounds during litter decomposition and humification in the forest soil under study.
机译:分析了七环类化合物(五环三萜类化合物)的结构和浓度,以确定它们在Haplic Podzol(从Oi到Bs层)的土壤深度增加时对烷基碳的贡献。分离可萃取溶剂的类胡萝卜素后,对土壤样品进行顺序化学降解,包括酯和ther键的裂解以及类胡萝卜素与大分子有机基质之间脂族-芳族碳键的氧化裂解。通过GC-MS对被调查物质进行鉴定和定量。根据不同的分析步骤,类胡萝卜素以碳氢化合物,醇和酸的形式释放,碳原子数为31至35。在Oi地平线上未发现类胡桃碱;从Oe到Oa和E1层浓度(最高565#mu#g g〜(-1)总有机碳)浓度显着上升,在E2层最小,在Bs层第二高。这些物质随着深度的增加而发生的行为可以通过产生足突类生物的微生物的活度变化和/或由于足爪动物化引起的易位过程来解释。由于ht的浓度低,在所研究的森林土壤中,凋落物分解和腐殖化过程中,类胡萝卜素和其他三萜类化合物在烷基碳化合物的富集中不发挥重要作用。

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