ЕКОЛОГІЧНІ АСПЕКТИ СТАНУ УРБАНОЗЕМІВ

Ольга Олександрівна Мислюк, Олена Хоменко, Оксана В’ячеславівна Єгорова, Вікторія Ігорівна Пидоренко
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Abstract

Physical and chemical transformation is typical for urban soils, that considerably aggravate their agroecological functions. The purpose of this work consists in ecological assessment of the current state of urban soils of Cherkasy. The city soils have a significant man-made load and contain many chemical xenobiotics. Diagnostics of the indicators of urban soils, which are crucial for assessing their ecological status and their agroecological functions, will provide an opportunity to determine the optimal and critical values for the sustainable functioning of urban landscapes and to propose the most effective and timely measures to be implemented. The urban soils analysis has shown that the humus content varies within the range of 0.03- 3.01 %, with an average value of 0.84 %, a standard deviation of 0.67, a dispersion of 0.41, a variation coefficient of 76 %. 6.25 % of the studied soil samples have insufficient supply of humus (2-4 %), 25 % have poor supply (1-2 %) and 69 % have extremely poor supply (less than 1 %). The active acidity (pH) varies from 6.45 to 10.90 with an average value of 7.20, a standard deviation of 0.83, a dispersion of 0.69, a variation coefficient of 11 %. The soils mostly have a weakly alkaline and neutral environment. The oxidation-reducing potential varies from 252 to 287 mV, with an average value of 262 mV (standard deviation of 7.3, a dispersion of 52.6, a variation coefficient of 3 %). The ratio of Ca2+ and Mg2+cations in soil adsorption complex is not optimal. The content of Ca2+ ranges from 3.80 to 10.12 mg-eq./100 g of soil with an average value of 6.60, a standard deviation of 1.66, a dispersion of 2.77, a variation coefficient of 25 %. The content of Mg2+ varies from 0.0 to 10.40 mg-eq./100 g of soil with an average value of 3.14 (standard deviation of 2.50, a dispersion of 6.26, a variation coefficient of 80 %). The content of K+ ranges from 0.12 to 6.20 with an average value of 0.59 mg-eq./100 g of soil, a standard deviation of 0.67, a dispersion of 1.39, a variation coefficient of 95 %. The soils have a significant deviation from optimal values and that characterizes them as anthropogenically and technogenically urbanized. There is a need in soil gypsuming, organic fertilizers, moisture supply and reduction of moisture evaporation, improvement of aeration conditions.
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城市土壤发生了典型的物理和化学转化,大大加重了其农业生态功能。本研究的目的在于对切尔卡西地区城市土壤现状进行生态评价。城市土壤具有显著的人为负荷,并含有许多化学异种。城市土壤指标对评估其生态状况及其农业生态功能至关重要,对这些指标的诊断将提供一个机会,确定城市景观可持续运作的最佳和临界值,并提出要执行的最有效和及时的措施。城市土壤腐殖质含量变化范围为0.03 ~ 3.01%,平均值为0.84%,标准差为0.67,离散度为0.41,变异系数为76%。6.25%的土壤腐殖质供应不足(2 ~ 4%),25%的土壤腐殖质供应不足(1 ~ 2%),69%的土壤腐殖质供应极差(不足1%)。活性酸度(pH)变化范围为6.45 ~ 10.90,平均值为7.20,标准差为0.83,离散度为0.69,变异系数为11%。土壤多为弱碱性和中性环境。氧化还原电位变化范围为252 ~ 287 mV,平均值为262 mV(标准差为7.3,离散度为52.6,变异系数为3%)。土壤吸附复合物中Ca2+和Mg2+阳离子的比例并不理想。Ca2+含量在3.80 ~ 10.12 mg-eq之间。平均值为6.60,标准差为1.66,离散度为2.77,变异系数为25%。Mg2+的含量在0.0 ~ 10.40 mg-eq之间。平均值为3.14(标准差为2.50,离散度为6.26,变异系数为80%)。K+含量为0.12 ~ 6.20,平均值为0.59 mg-eq。/100 g土壤,标准差为0.67,离散度为1.39,变异系数为95%。土壤与最佳值有显著偏差,这表明它们是人为和技术城市化的。需要对土壤进行石膏处理、施用有机肥、补水和减少水分蒸发、改善通气条件。
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