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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Water repellency as conditioned by particle size and drying in hydrophobized sand
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Water repellency as conditioned by particle size and drying in hydrophobized sand

机译:疏水性取决于粒径和在疏水性砂中干燥的条件

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The effects of particle size and soil moisture on water repellency (WR) from hydrophobized sand are studied in this research. Quartz sand samples were separated into three sieve fractions: 0.5-2 mm (coarse sand, CS), 0.25-0.5 mm (medium sand, MS), and 0.05-0.25 mm (fine sand, FS). WR of sand was induced using different concentrations of stearic acid (SA; 0.5, 1, 5, 10, 20 and 30 g kg(-1)). Moist samples have been exposed to two types of drying: air-drying at standard laboratory conditions and oven-drying at 50 degrees C. Change in moisture content, and water repellency has been monitored every 24 h for 10 days. After 1 day of drying, SA concentrations >= 10 g kg(-1) caused extreme WR in oven-dry samples, independently of sieve fraction. In air-dried samples, time of drying and decreasing soil moisture content increased WR, but an erratic behaviour was observed in MS and FS samples. All air- and oven-dried samples became extremely water repellent after 7 days of treatment. At all SA concentrations and drying temperatures, WR was extreme in the CS fraction after one day. Superhydrophobicity of CS samples is suggested as a possible explanation of this response. In MS and FS samples, water repellency showed an erratic behaviour at lower SA contents, which may be due to contact of water droplets with a high proportion of areas not covered by hydrophobic coatings. The higher severity of WR observed in CS is in agreement with the idea of hydrophobicity associated with coarser particles. Coarse-textured soils have a lower specific surface than fine-textured soils, and a limited amount of organic matter may cause higher WR than in finely textured soils.
机译:本研究研究了粒径和土壤水分对疏水性砂的憎水性(WR)的影响。石英砂样品分为三个筛分:0.5-2 mm(粗砂,CS),0.25-0.5 mm(中砂,MS)和0.05-0.25 mm(细砂,FS)。使用不同浓度的硬脂酸(SA; 0.5、1、5、10、20和30 g kg(-1))诱导砂的WR。潮湿的样品已经历了两种干燥:在标准实验室条件下进行风干和在50摄氏度下进行烘箱干燥。水分含量的变化以及每24小时监测一次防水性,持续10天。干燥1天后,SA浓度> = 10 g kg(-1)导致烘干样品中极度的WR,与筛分无关。在风干样品中,干燥时间和降低土壤水分含量会增加WR,但在MS和FS样品中观察到不稳定的行为。处理7天后,所有风干和烤箱干燥的样品都具有极高的防水性。在所有的SA浓度和干燥温度下,一天后WR的CS含量都极高。建议使用CS样品的超疏水性来解释这种反应。在MS和FS样品中,疏水性在较低的SA含量下表现出不稳定的行为,这可能是由于水滴与疏水涂层未覆盖的大部分区域接触所致。在CS中观察到的WR的更高严重性与与较粗颗粒相关的疏水性的想法一致。粗纹理的土壤比细纹理的土壤具有更低的比表面积,与细纹理的土壤相比,有限的有机物含量可能会导致更高的WR。

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