Atmospheric Solid Fallouts as a Source of Hydrophobicity of Urban Soils and Material for Their Formation

IF 1.4 4区 农林科学 Q4 SOIL SCIENCE Eurasian Soil Science Pub Date : 2024-07-22 DOI:10.1134/s106422932460074x
N. V. Goncharov, T. V. Prokof’eva, D. I. Potapov, G. N. Fedotov
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Abstract

In urban conditions, the soil is exposed to a number of adverse factors that have a great impact on its hydrophobic and hydrophilic properties. The water-repellent properties of urban dust and soils were determined with the water drop penetration time (WDPT) test. Hydrophobization of Albic Retisols in the conditions of a megalopolis was modeled, and its rate was estimated. Three dust samples with different values of the WDPT test from 420 to 850 seconds were studied. According to the results of the model experiment, with an increase of solid atmospheric fallout in the Retisols, the level of their hydrophobicity also increases. The rate of the increase depends on the water-repellent properties of the dust. During pollution with the most hydrophobic dust, the maximum hydrophobization of the humus-accumulative soil horizon is achieved upon a 70-year-long impact. For other dust samples, an increase in the time of absorption of a drop was observed up to the maximum period of aerial soil contamination within the model experiment (200 years). Values of the WDPT test for the studied soil horizons ranged from 2.4 s to 1493.5 s for background soil and urban soil forming near a major highway for 90 years, respectively. In the soil of forty-year-old residential area, the value was 237.1 s. The correspondence of the levels of hydrophobicity, the degree of anthropogenic load and the residence time in the urban environment in the model experiment and in the samples of real urban soils indicates that solid atmospheric fallouts are a component of humus-accumulative horizons of urban soils and have a significant impact on their water-repellent properties.

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作为城市土壤疏水性来源的大气固体降尘及其形成材料
摘要 在城市环境中,土壤会受到许多不利因素的影响,对其疏水和亲水特性产生很大的影响。通过水滴渗透时间(WDPT)测试确定了城市灰尘和土壤的憎水性。模拟了大城市条件下阿尔卑斯网状土壤的疏水性,并估算了疏水性的速率。研究了 WDPT 测试值从 420 秒到 850 秒不同的三种粉尘样本。根据模型实验的结果,随着 Retisols 中固体大气沉降物的增加,其疏水程度也随之增加。增加的速度取决于灰尘的憎水性。在受到疏水性最强的粉尘污染时,腐殖质累积土壤层的疏水性在受到 70 年的影响后达到最大值。对于其他粉尘样本,在模型实验中观察到吸收一滴粉尘的时间延长到空中土壤污染的最长时间(200 年)。在研究的土壤层中,背景土壤和在主要高速公路附近形成 90 年的城市土壤的 WDPT 测试值分别从 2.4 秒到 1493.5 秒不等。在模型实验和实际城市土壤样本中,疏水性水平、人为负荷程度和在城市环境中的停留时间的对应关系表明,固体大气沉降物是城市土壤腐殖质累积层的组成部分,对其憎水特性有重大影响。
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来源期刊
Eurasian Soil Science
Eurasian Soil Science 农林科学-土壤科学
CiteScore
2.70
自引率
35.70%
发文量
137
审稿时长
12-24 weeks
期刊介绍: Eurasian Soil Science publishes original research papers on global and regional studies discussing both theoretical and experimental problems of genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. Special sections are devoted to current news in the life of the International and Russian soil science societies and to the history of soil sciences. Since 2000, the journal Agricultural Chemistry, the English version of the journal of the Russian Academy of Sciences Agrokhimiya, has been merged into the journal Eurasian Soil Science and is no longer published as a separate title.
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