Water repellency as conditioned by particle size and drying in hydrophobized sand

被引:43
|
作者
Gonzalez-Penaloza, Felix A. [1 ,2 ]
Zavala, Lorena M. [2 ]
Jordan, Antonio [2 ]
Bellinfante, Nicolas [2 ]
Barcenas-Moreno, Gema [2 ]
Mataix-Solera, Jorge [2 ,3 ]
Granged, Arturo J. P. [2 ,4 ]
Granja-Martins, Fernando M. [2 ,5 ]
Neto-Paixao, Helena M. [2 ,5 ]
机构
[1] Univ Valencia, Dept Geog, SEDER Res Grp, Valencia, Spain
[2] Univ Seville, Fac Quim, Dept Cristalog Mineral & Quim Agricola, MED Soil Res Grp, E-41012 Seville, Spain
[3] Univ Miguel Hernandez, Dept Agroquim & Medio Ambiente, GEA, Environm Soil Sci Grp, Alicante, Spain
[4] Univ Seville, Escuela Tecn Super Ingn Tecni Agricola, Dept Fis Aplicada, Seville, Spain
[5] Univ Algarve, Inst Super Engn Faro, Dept Civil Engn, Faro, Portugal
关键词
Contact angle; Hydrophobized sand; Sieve fraction; Soil water repellency; Super-hydrophobicity; SOIL HYDROLOGICAL RESPONSE; DROP PENETRATION TIME; LAND-USE TYPES; ROCK FRAGMENT COVER; CONTACT-ANGLE; ORGANIC-MATTER; SW SPAIN; AGGREGATE STABILITY; SPLASH EROSION; FIRE;
D O I
10.1016/j.geoderma.2013.05.022
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
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. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:31 / 40
页数:10
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