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NEW ANALYTICAL METHOD FOR ORGANIC MATTER DETERMINATION

机译:有机物测定的新分析方法

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The determination of organic matter is applied mostly to soils analysis. Literature evidences two volumetric methods for determination, both of them consisting in samples oxidation with dichromate in excess and back titration of the excess with the Mohr salt solution. In addition, two spectrophotometrical analysis are used: one is based on the determination of chromium(III) within the reducing reaction, while the other uses a calibration curve for a sample with an already known organic matter content. The purpose of this study is the elaboration of a new spectrophotometric method, which is more specific, using standard humic acid sodium salt (from Aldrich). Standard solutions of humic acid sodium salt oxidised with dichromate in acidic medium are spectrophoto-metrically analysed. The spectral profile has a maximum at 425 nm and a shoulder at 500-650 ran. When overlaying the spectra of the standard solution of dichromate and humic acid sodium salt, differences between them are being displayed, thus proving the specificity of the method. Moreover, the dichromate excess does not interfere with the oxidated humic acid, due to its different spectral profile. The calibration curve at λ = 645 nm is linear in the range 0.2-2 mg/ml humic acid sodium salt oxidated. The calibration equation, having a very good correlation coefficient (r>0.99), is used for organic matter determination expressed in humic acid sodium salt for mud samples. The mud from the Techirghiol lake -18 km south of Constanta, Romania, traditionally used in therapy of rheumatic diseases, after water extraction and filtration, has been analysed under the same spectrophotometric conditions. Calibration equation at X. = 645 nm was applied for organic matter determination of the mud samples expressed in humic acid sodium salt. The results for most of the samples showed a content of C = 0.5-0.7 (g humic acid Na salt)/(100 g mud). The method for organic matter determination using humic acid sodium salt is specific, reproducible and accurate.
机译:有机物的测定主要用于土壤分析。文献证明了两种体积测定方法,这两种方法都包括用重铬酸盐过量氧化样品和用摩尔盐溶液反滴定过量样品。另外,使用了两种分光光度分析:一种是基于还原反应中铬(III)的测定,另一种是使用具有已知有机物含量的样品的校准曲线。这项研究的目的是使用标准腐殖酸钠盐(来自Aldrich),拟定一种更具体的新分光光度法。用分光光度法分析了在酸性介质中被重铬酸盐氧化的腐植酸钠盐的标准溶液。光谱轮廓在425 nm处有最大值,在500-650 nm处有肩峰。当覆盖重铬酸盐和腐植酸钠盐标准溶液的光谱时,显示出它们之间的差异,从而证明了该方法的特异性。此外,由于重铬酸盐的光谱分布不同,因此过量的重铬酸盐不会干扰氧化的腐殖酸。 λ= 645 nm处的校准曲线在0.2-2 mg / ml氧化的腐植酸钠盐范围内呈线性。具有非常好的相关系数(r> 0.99)的校准方程用于以腐植酸钠盐表示的泥浆样品中的有机物测定。在相同的分光光度法条件下,对罗马尼亚康斯坦萨以南-18公里处Techirghiol湖中的泥浆进行了萃取和过滤后,将其用于风湿性疾病的治疗,该泥浆过去通常用于风湿性疾病的治疗。将X. = 645 nm的校准方程用于以腐植酸钠盐表示的泥浆样品的有机物测定。大多数样品的结果表明,其含量为C = 0.5-0.7(腐殖酸钠盐)/(100 g泥浆)。使用腐植酸钠盐测定有机物的方法具有特异性,可重复性和准确性。

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