首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Source and depth translocation of combustion residues in Chinese agroecosystems determined from parallel polycyclic aromatic hydrocarbon (PAH) and black carbon (BC) analysis
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Source and depth translocation of combustion residues in Chinese agroecosystems determined from parallel polycyclic aromatic hydrocarbon (PAH) and black carbon (BC) analysis

机译:通过平行多环芳烃(PAH)和黑碳(BC)分析确定中国农业生态系统中燃烧残留物的来源和深度易位

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Rice straw burning in agroecosystems delivers BC (black carbon) to soil/sediment but its contribution relative to other BC sources is unspecified. We have differentiated for the first time combustion residues (CRs) derived from autochthonous and pyrogenic agricultural vs. allochthonous and biogenic riverine input by way of complementary analysis of BC and PAH (polycyclic aromatic hydrocarbon) abundance and composition. Both CR markers in four upland and six periodically flooded paddy soils having different cultivation times were analyzed. BC was the quantitatively dominant CR fraction at 16-512 mg/g SOC (soil organic carbon), whereas PAHs yielded trace amounts of eleven EPA-PAHs at 1.5-47.0 mu/g SOC. CR concentrations in paddy soils exceeded those in upland topsoil. The lowest BC and PAH concentration occurred in subsoil <= 700 yr old, independent of paddy or upland use, but BC content increased in paddy subsoil >= 700 yr old. Exceptional BC enrichment and composition of benzene polycarboxylic acid (BPCA) products revealed dark buried horizons (700 and 1000 yr sites) as former topsoil. Relative distributions of 5-ring PAHs differentiated CRs from biogenic residues in substrate, topsoil and subsoil. Perylene was enriched in tidal wetland substrate, indicating allochthonous input from soil/sediment erosion in the Yangtze River catchment. An identical pattern was observed in subsoil. Present and former topsoil yielded a distinctive distribution of rice ash PAHs. Although PAHs occurred in traces, their wider compositional variation improved source discrimination power exceeding that of BPCAs. The former are recommended for source identification and the latter for quantifying CR input to soil/sediment. Parallel application of both methodological approaches is advocated for investigating combustion processes in ecosystems. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在农业生态系统中燃烧稻草可将BC(黑碳)传递到土壤/沉积物中,但相对于其他BC来源的贡献尚未确定。通过对BC和PAH(多环芳烃)的丰度和组成进行互补分析,我们首次区分了来自土生和热生农业与异源和生物源河流输入的燃烧残留物(CR)。分析了在四个旱地和六个周期性淹水的稻田中具有不同耕种时间的CR标记。 BC是在16-512 mg / g SOC(土壤有机碳)下定量占主导地位的CR分数,而PAHs在1.5-47.0 mu / g SOC下产生痕量的11种EPA-PAH。稻田土壤中的CR含量超过了表层土壤中的CR。最低的BC和PAH浓度发生在<= 700岁的底土中,与稻田或旱地的使用无关,但是BC含量在> = 700岁的稻田底土中增加。出色的BC富集和苯多元羧酸(BPCA)产品的成分显示,前表层土壤为深色的隐蔽地层(700和1000年位点)。 5环多环芳烃的相对分布使CRs与底物,表土和底土中的生物残留物区分开。 ylene在潮汐湿地基质中富集,表明长江流域土壤/沉积物侵蚀的异源输入。在下层土壤中观察到相同的模式。现在和以前的表土产生了独特的稻灰PAHs分布。尽管PAHs出现在痕迹中,但其更广泛的成分变化改善了源识别能力,超过了BPCA。建议前者用于来源识别,后者用于量化土壤/沉积物中的CR输入。提倡同时使用两种方法来研究生态系统中的燃烧过程。 (C)2016 Elsevier Ltd.保留所有权利。

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