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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Modification of biomarkers in pyrogenic organic matter during the initial phase of charcoal biodegradation in soils.
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Modification of biomarkers in pyrogenic organic matter during the initial phase of charcoal biodegradation in soils.

机译:在土壤中木炭生物降解初期,热解有机质中生物标志物的修饰。

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摘要

The biochemical stability of typical biomarkers from the free lipid extract of different plant chars during biotic degradation was examined using pyrogenic organic matter (PyOM) derived from rye grass (Lolium perenne; Gr) and pine wood (Pinus sylvestris; P) heated at 350 degrees C for 1 (1M) and 4 min (4M) under oxic conditions. The composition of the n-alkanes and n-fatty acids (FA) as well as the contents of the molecular markers levoglucosan and vanillin were determined and related to charring intensity and stability to microbial reworking. Our results confirmed that charring of plant residues results in typical thermal breakdown processes of n-alkanes and FA. Prolonged charring reduced the average chain length of n-alkanes by up to four carbons and shifted the characteristic odd/even predominance of fresh plants towards a balanced odd/even distribution. The unsaturated FA fraction was more prone to heat degradation than the saturated counterparts. Especially, linoleic acid (C18:2) and alpha -linolenic acid (C18:3) were depleted in the severely charred grass, whereas oleic acid (C18:1) was still present. Levoglucosan was detectable in all PyOMs, but the pine wood charred for 1 min (P1M) contained the largest amount. Progressive heating resulted in a strong depletion of levoglucosan for both plant materials. The pine char showed a relative accumulation of vanillin, supporting that some lignin-derived structures can survive charring. Microbial decomposition of the chars within a soil matrix for seven weeks demonstrates that during initial PyOM biodegradation, n-alkanes and FA series are rapidly modified by microbial reworking and biosynthesis. After the incubation, the pine chars were enriched in octadecane (C18) and homologues in the range from C22 to C26. The n-alkanes and FA of the grass chars were more severely affected than those of the pine chars. Levoglucosan was efficiently decomposed, indicating that care has to be taken if these compounds are used as char tracer in soils, since their instability against biodegradation may hamper the identification of charcoal residues.
机译:使用衍生自黑麦草(Lolium perenne; Gr)和松木(Pinus sylvestris; P)的热解有机物(PyOM),在350度加热下,检查了生物降解过程中来自不同植物炭的游离脂质提取物的典型生物标记物的生物化学稳定性。在有氧条件下保持1(1M)和4分钟(4M)。确定了正构烷烃和正脂肪酸(FA)的组成以及分子标记左旋葡聚糖和香兰素的含量,它们与炭化强度和对微生物返工的稳定性有关。我们的结果证实,植物残渣的炭化会导致正构烷烃和FA发生典型的热分解过程。长时间炭化会使正构烷烃的平均链长减少多达四个碳,并使新鲜植物的特征奇/偶优势占主导地位,向平衡的奇/偶分布转变。与不饱和脂肪酸相比,不饱和脂肪酸馏分更易于热降解。特别是,在严重烧焦的草中,亚油酸(C 18:2 )和α-亚麻酸(C 18:3 )枯竭,而油酸(C > 18:1 )仍然存在。在所有PyOM中均可检测到左旋葡聚糖,但烧焦1分钟(P1M)的松木中含量最高。渐进加热导致两种植物材料中的左葡萄糖葡聚糖大量消耗。松木炭显示出香草醛的相对积累,支持某些木质素衍生的结构可以在炭化后存活。七个星期内,土壤基质中碳的微生物分解表明,在最初的PyOM生物降解过程中,正构烷烃和FA系列会通过微生物返工和生物合成而迅速被修饰。温育后,松木炭富含十八烷(C 18 ),其同源物范围从C 22 到C 26 。草炭的正构烷烃和FA比松木炭受更严重的影响。左旋葡聚糖被有效分解,表明如果将这些化合物用作土壤中的示踪剂,则必须格外小心,因为它们对生物降解的不稳定性可能会妨碍鉴定木炭残留物。

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