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Hydrophysical properties of sandy clay contaminated by petroleum hydrocarbon

机译:石油烃污染的砂土的水性性质

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The aim of the presented research was to assess the changes in hydro-physical properties of sandy clay under the influence of petroleum hydrocarbon contamination. An understanding of these changes is fundamental in the right remedial actions and for further use of soil. Laboratory tests of inherently wettable sandy clay showed that the petroleum hydrocarbon induced potential soil water repellency (SWR) of extremely repellent class at the contamination of 18?g?kg?1. The relationship between soil water potential (pF) and SWR determined by the WDPT test for given hydrocarbon contamination, i.e., 6, 12, 18, 30, 100?g?kg?1, showed that the critical soil moisture value (CSMC) corresponds to the pF?=?1.0 ÷ 1.5. Soil retention characteristic (pF) showed that an increase in hydrocarbon contamination from 0 to 100?g?kg?1 caused a reduction of total available water for plants from about 0.19 to 0.06?cm?cm?3. At the same time, in the pF?=?1.5?÷?2.0 range, intensive soil pore drainage was observed. Statistically, significant effect of hydrocarbon contamination and soil moisture potential on SWR was found. Soil hydrophobicity limits the addition of soil retention, because a significant part of the precipitation can be transformed by surface runoff. The carried out tests showed that at a hydrocarbon contamination of 30?g?kg?1, total rainfall amount 14?mm with an intensity of 2?mm?h?1 was transformed into a surface drain in approx. 40%. The conducted studies demonstrate the adverse impact of hydrocarbon contamination on the soil’s hydro-physical properties. The soil water retention reduction and launching of the surface outflow, as a result of limiting the water penetration process resulting from SWR, change the agrohydrological conditions of the contaminated area. It can result as the imbalance of the flow of energy and matter in the ecosystem. The scenarios of environmental effects, among others, depend on the type of soil, the degree of its pollution, the type of ecosystem, and supporting activities undertaken by man. It should be taken into account that the increasing frequency of drought occurrence associated with climate change is conducive to the phenomenon of SWR regardless of the reasons for its occurrence.
机译:本研究的目的是评估在石油烃污染的影响下沙质粘土的水力 - 物理性质的变化。对这些变化的理解是正确的补救措施和进一步使用土壤的基础。固有湿润的砂质粘土的实验室测试表明,石油烃诱导的潜在土壤防水性(SWR)在18Ω·kg?1的污染下极其驱虫阶级。通过WDPT试验对给定烃污染的WDPT试验确定的土壤水电位(PF)和SWR之间的关系,即6,12,18,30,100Ω·kg≤1,表明临界土壤湿度值(CSMC)对应到pf?=?1.0÷1.5。土壤保留特性(PF)表明,烃污染从0到100μl≤kβ1的增加导致植物的总可用水的减少,从约0.19〜0.06Ω·cm?3。同时,在pf?=?1.5?2.0范围,观察到密集的土壤孔隙排水。统计上,发现了碳氢化合物污染和土壤水分潜力对SWR的显着影响。土壤疏水性限制了土壤保留的添加,因为沉淀的大部分可以通过表面径流转化。进行的试验表明,在30?G?kgα1的烃污染下,截止量为14Ω·mm,强度为2Ω·h = H 2。 40%。进行的研究表明烃污染对土壤水力物理性质的不利影响。由于限制由SWR导致的水渗透过程,土壤保险减少和表面流出的发射,改变了污染区域的农学学条件。它可以作为生态系统中能量流动的不平衡。环境效应的情景,等依赖于土壤的类型,污染程度,生态系统的类型,以及人类所开展的支持活动。应考虑到与气候变化相关的干旱发生频率的增加有利于SWR的现象,而不管其发生的原因。

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