Features and assessment of decolorization of chernozems of Ukraine

IF 1.4 Q4 SOIL SCIENCE
Yaroslav Vitvitskyi, V. Haskevych, S. Pozniak, I. Kasiianyk
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引用次数: 0

Abstract

The article presents the results of colorimetry and practical study of the processes of decolorization of chernozems by using a scanner as one of the effective and available methods for assessing soil color at the macromorphological level. The infl uence of moisture on the objectivity of the color parameters of typical chernozem samples in the color space of the CIE L*a*b* system is experimentally analyzed. Based on the parameters of brightness (L*), red (a*) and yellow (b*) color components, the color differences of typical chernozems of arable land and adjacent forest belts were established, and the horizontal color heterogeneity of the arable horizon of plain and slope areas was determined. The results of the study indicate that chernozems undergo an intense change in the natural color on slopes with a steepness of ≥ 4%. In soil samples, an increase in the range of the chromatic index b* indicates a low humus content and an increase in the role of loess loams in the pigmentation of the arable horizon. Compared to arable land, soil samples of typical chernozem taken under forest belts are characterized by low brightness (L*) and high levels of humus. The obtained results show the possibility of using this approach to assess the quality state of chernozems. In addition, a direct study of the color of chernozems will allow obtaining data regardless of weather conditions, the presence of vegetation, and soil cultivation technology. The minimized infl uence of the external environment on the process of fi xing the color parameters of the soil will contribute to the objectivity of information, which can later be used as an addition to the results of remote sensing. The formation of a digital database of color data will allow localizing areas of manifestation of decolorization of chernozems and assessing the risks associated with the soil management system.
乌克兰黑钙土的脱色特征及评价
本文介绍了比色法的研究结果,并对黑钙土的脱色过程进行了实际研究,认为扫描仪是在宏观形态水平上评价土壤颜色的有效和可行的方法之一。实验分析了水分对典型黑钙土样品在CIE L*a*b*色空间中颜色参数客观性的影响。基于亮度(L*)、红色(a*)和黄色(b*)三个颜色分量参数,建立了耕地和邻近林带典型黑钙土的颜色差异,确定了平原区和坡坡区耕地地平的水平颜色异质性。研究结果表明,当坡度≥4%时,黑钙土的自然颜色发生强烈变化。在土壤样品中,色指数b*范围的增加表明腐殖质含量较低,黄土壤土在耕地层色素沉着中的作用增加。与耕地相比,森林带下典型黑钙土的土壤样品具有亮度低(L*)和腐殖质含量高的特点。结果表明,用该方法评价黑钙土的质量状态是可行的。此外,对黑钙土颜色的直接研究将允许在不考虑天气条件、有无植被和土壤耕作技术的情况下获得数据。将外部环境对土壤颜色参数确定过程的影响降到最低,将有助于信息的客观性,以后可以作为遥感结果的补充。颜色数据数字数据库的形成将有助于确定黑钙土脱色现象的局部区域,并评估与土壤管理系统有关的风险。
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来源期刊
Soil Science Annual
Soil Science Annual SOIL SCIENCE-
CiteScore
2.50
自引率
6.70%
发文量
0
审稿时长
29 weeks
期刊介绍: Soil Science Annual journal is a continuation of the “Roczniki Gleboznawcze” – the journal of the Polish Society of Soil Science first published in 1950. Soil Science Annual is a quarterly devoted to a broad spectrum of issues relating to the soil environment. From 2012, the journal is published in the open access system by the Sciendo (De Gruyter).
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