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Statistical relationship between selected physicochemical properties of peaty-muck soils and their fraction of humic acids

机译:菜泥土某些理化性质与腐殖酸含量之间的统计关系

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Influence of humic acids on soil environment is still subject of scientific discussions. The aim of above studies was to investigate the relationships between selected physicochemical properties of eleven peaty-muck soils and properties of humic acids isolated from these soils. The following parameters were determined for soils: total and organic carbon, density, ash, humification, and the water absorption index. Humic acids were described by: absorbance at 280 nm, absorbance ratios at 465 and 665 nm, at 260 and 665 nm, elemental composition and atomic ratios: H/C, O/H, O/C, C/N, the degree of internal oxidation, and the content of carboxylic and phenolic groups. Statistical analyses showed that an increase in density, humification, and water absorption indices of soils caused a significant increase in the humic acid parameters: absorbance at 280 nm, the oxygen content, O/H, O/C ratios, internal oxidation degree, and functional groups. Statistically significant negative correlations were found for the same parameters of soils and for the hydrogen and carbon content as well as the H/C ratio of humic acids. The relationships showed that there was a possibility to express the properties of humic acids on the basis of more simple parameters measured for soil and without time-consuming isolation of humic acids.
机译:腐殖酸对土壤环境的影响仍然是科学讨论的主题。上述研究的目的是研究十一种泥炭土的选定理化性质与从这些土中分离出的腐殖酸性质之间的关系。确定了以下土壤参数:总碳和有机碳,密度,灰分,增湿和吸水率。腐殖酸的描述如下:280 nm处的吸光度,465 nm和665 nm处,260 nm和665 nm处的吸光度比,元素组成和原子比:H / C,O / H,O / C,C / N,内部氧化以及羧基和酚基的含量。统计分析表明,土壤密度,腐殖化和吸水率的增加引起了腐殖酸参数的显着增加:腐殖酸参数为280 nm,氧含量,O / H,O / C比,内部氧化度和功能组。对于相同的土壤参数,氢和碳含量以及腐殖酸的H / C比,发现统计学上显着的负相关。这些关系表明,有可能根据针对土壤测量的更简单的参数来表达腐殖酸的性质,而无需耗时地分离腐殖酸。

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