首页> 外文期刊>Journal of Biotechnology >Evaluation of pre-treatment procedures for improved interpretation of mid infrared spectra of soil organic matter
【24h】

Evaluation of pre-treatment procedures for improved interpretation of mid infrared spectra of soil organic matter

机译:改善土壤有机质中红外光谱解释预处理程序的评价

获取原文
获取原文并翻译 | 示例
           

摘要

This study evaluated the effectiveness of dry ashing of soils and subsequent spectral subtraction procedure in comparison with alternative chemical methods in accentuating organics for diffuse reflectance infrared Fourier transform (DRIFT) spectroscopic analysis of soil organic matter composition. Chemical oxidation of soil with sodium hypochlorite (NaOC1) and demineralisation by hydrofluoric acid (HF) treatment were assessed as possible alternatives to the dry ashing method. Surface samples (0-10 cm) of four contrasting soils i.e., Ferralsol, Luvisol, Vertisol and Solonetz were used in the study. We observed the spectral changes before and after pre-treatments using DRIFT spectroscopy of bulk soils and their respective four separated density fractions (1.8,1.8-2.2, 2.2-2.6, and >2.6 g cm(-3)). Dry ashing of soils altered the absorption bands of gibbsite and goethite in the Ferralsol; however, phyllosilicate bands in the Luvisol, Vertisol and Solonetz remained largely unaffected. The organic bands were incompletely removed by the dry ashing method and shifts in some major organic bands were also noticed. Thus the accuracy of the dry ashed spectral subtraction was limited due to the mineral and organic bands alteration. The Na0C1 treatment oxidised labile organic carbon (OC) (e.g., aliphatics) without any mineral alteration, but the rest of the OC fractions remained largely unaffected. Therefore, the result of spectral subtraction of the Na0C1 treated samples from original spectra was ambiguous. The HF treatment removed minerals efficiently from both bulk soils and density fractions, which noticeably highlighted the organic bands with little or no mineral interferences in the spectra of the treated samples. HF treatment also removed a small portion of the total OC that was associated with minerals. We conclude that HF treatment was more effective than dry ashing and Na0C1 oxidation to accentuate organics in the soil DRIFT spectra, since it provided mineral interference free spectra with in general least affected organic bands. Thus, HF treatment of soil offers a potential pretreatment method for improved spectroscopic characterisation of soil.organic matter. (C) 2016 Elsevier B.V. All rights reserved.
机译:该研究评估了土壤干灰化的有效性及随后的光谱减法过程与弥漫性反射率红外傅里叶变换(漂移)光谱分析的替代化学方法相比,土壤有机物质组合物的促进有机物。用氢氟酸钠(NaOC1)和氢氟酸(HF)处理的土壤化学氧化,作为干灰化法的可能替代品。在研究中使用了四个对比度土壤的表面样品(0-10cm),即,二甲酚,Luvisol,Vertisol和Solonetz。我们观察了使用散装土壤的漂移光谱和它们各自的四个分离密度级分(<1.8,1.8-2.2,2.2-2.6和> 2.6g cm(-3))前后处理前后处理前后的光谱改变。土壤的干灰化改变了花翅膀和甲磺酸盐的吸收带;然而,Luvisol,Vertisol和Solonetz中的字节硅酸盐条仍然很大程度上不受影响。通过干灰化方法不完全除去有机条带,并注意到一些主要有机带中的换档。因此,由于矿物和有机带改变,干灰光谱减法的精度受到限制。 Na0C1处理在没有任何矿物质的情况下氧化不稳定的有机碳(OC)(例如,aliphatics),但其余的OC馏分在很大程度上不受影响。因此,来自原始光谱的Na0C1处理样品的光谱减法的结果含糊不清。 HF处理从散装土壤和密度分数中有效地除去矿物质,这明显突出显示了处理样品的光谱中的矿物干扰的有机带。 HF治疗还除去与矿物质相关的总OC的一小部分。我们得出结论,HF处理比干灰化和Na0C1氧化更有效,以强调土壤漂移光谱中的有机物,因为它提供了矿物干扰的自由光谱与一般最小影响的有机带。因此,土壤的HF处理提供了一种潜在的预处理方法,可改善土壤的光谱性表征。有机物质。 (c)2016年Elsevier B.v.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号