森林植被对乌克兰草原带北部变异沟壑区土壤颜色、反射率和腐殖质含量的影响

V. Gorban, M. S. Yakuba, A. Huslystyi
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摘要

独特的天然森林生长在乌克兰草原地带的沟壑条件下。土壤科学家研究沟壑土壤已有60多年的历史。尽管进行了长期的研究,但反映在其光学特性上的特定沟壑土壤的成因方面仍然几乎未被探索。在此基础上,我们的工作目的是建立森林植被对乌克兰草原带北部变异沟壑区土壤颜色和反射率的影响特征,以及与之密切相关的腐殖质含量。在Glybokyy峡谷(在第聂伯罗彼得罗夫斯克州新斯科夫斯克区Andriivka村附近)铺设的剖面的每个遗传层上采集了土壤样本。通过扫描土壤样品并进行图像分析来确定土壤颜色指数。用单色仪测定了土壤的反射率。采用《秋林标准》中有机质湿氧化标准法测定土壤腐殖质含量。研究结果表明,在Glybokyy沟壑区土壤表层,HSB、RGB和Lab系统各指标的还原值存在差异,且随深度的增加而增大。沟壑区土壤上层在480、650和750 nm波段亮度系数和综合亮度系数均呈减小趋势,且随深度的增加而逐渐增大。RGB和Lab系统的颜色指标是诊断和预测峡谷土壤腐殖质含量最成功的方法。沟壑区森林黑钙土和森林草甸土是在天然林植被条件下形成的,与黑钙土相比,其HSB、RGB和Lab系统的颜色指标降低,亮度系数降低,腐殖质含量增加,其成因与此有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Influence of forest vegetation on color, reflectivity and humus content in soils of northern variant ravines of the steppe zone of Ukraine
Unique natural forests grow in the conditions of ravines of the steppe zone of Ukraine. Soil scientists have been researching the soils of ravines for more than 60 years. Despite long-term research, aspects of the genesis of specific ravine soils, which are reflected in their optical properties, are still virtually unexplored. Based on this, the aim of our work is to establish the characteristics of the influence of forest vegetation on color and reflectivity, as well as the closely related content of humus in the soils of the northern variant ravines of the steppe zone of Ukraine. Soil samples were taken from each genetic horizon of sections laid in the Glybokyy ravine (near the village of Andriivka, Novomoskovsk district, Dnipropetrovsk region). Soil color indices were determined by scanning soil samples followed by image analysis. The reflectivity of soils was investigated using a monochromator. The humus content in soils was determined by the standard method of wet oxidation of organic matter according to I. V. Tyurin. As a result of the performed researches it is established that the upper horizons of the soils of the Glybokyy ravine differ in the reduced values ​​of the indicators of the HSB, RGB and Lab systems, with depth their values ​​increase. The upper horizons of the ravine soils are characterized by reduced values ​​of brightness coefficients at wavelengths of 480, 650 and 750 nm, as well as the integrated brightness coefficient, with depth there is a gradual increase in their values. The color indicators of the RGB and Lab systems are the most successful for diagnosing and predicting the humus content in the soils of the ravine. Forest chernozems and forest-meadow soil of the ravine, which were formed under natural forest vegetation, are characterized by reduced values ​​of color indicators of HSB, RGB and Lab systems, reduced values ​​of brightness coefficients and increased humus content compared to chernozems, the genesis of which is related.
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