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首页> 外文期刊>Hydrological Processes >Temporal fluctuations of water repellency in forest soils of Galicia, NW Spain. Do soil samples dried at laboratory reflect the potential soil water repellency? (pages 1179–1187)
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Temporal fluctuations of water repellency in forest soils of Galicia, NW Spain. Do soil samples dried at laboratory reflect the potential soil water repellency? (pages 1179–1187)

机译:西班牙西北加利西亚森林土壤中憎水性的时间波动。实验室干燥的土壤样品是否反映出潜在的土壤疏水性? (第1179–1187页)

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摘要

Water repellency is a widespread property of Pinus pinaster and Eucalyptus globulus forest soils in NW Spain and is particularlynsevere during the summer dry conditions. The aim of this work was to compare actual water repellency at field-moist samplesnwith potential water repellency after drying at 25 and 105 °C in samples collected at different times of year under four forestnsoils. Also, we investigated whether drying at 25 or 105 °C led to repellency values comparable to the highest levels reachednunder field conditions in the summer with a view to developing an appropriate sampling protocol towards estimating thenmaximum possible water repellency of a given soil as a key to establishing its environmental effects. The actual and potentialnwater repellency was determined by using the water drop penetration time (WDPT) and molarity of an ethanol drop (MED)ntests.nClear seasonal patterns of water repellency were observed from the results for the four forest soils, peaking in the dry periodnand disappearing after prolonged wet periods. Water repellency lasts longer in sandy loam soils than in more finely texturednsoils, and also under eucalyptus than under pine forests. Drying soil samples at 25 or 105 °C increased water repellency, asnmeasured with the WDPT method, in the four soils, but especially in the non-repellent samples collected during the wet period.nThe increase was more marked in the sandy loam soils than in the more finely textured soils, and also after drying at 105 °Cnthan at 25 °C. MED measurements exposed a common trait in the four soils; thus, the water repellency values obtained undernfield conditions in summer invariably exceeded those obtained after drying at 25 or 105 °C. In addition, the repellency valuesnfor dried samples collected in the wet period were never comparable to the maximum levels observed under field conditionsnin the summer. Copyright  2011 John Wiley & Sons, Ltd.
机译:拒水性是西班牙西北部的松树松和桉树森林土壤的普遍特性,在夏季干燥条件下尤为严重。这项工作的目的是比较田间潮湿的样品的实际防水性与在四种森林土壤下在每年不同时间收集的样品在25和105°C下干燥后的潜在防水性。此外,我们研究了在25或105°C下干燥是否能产生与夏季夏季田间条件下达到的最高水平相当的驱避性值,以期开发出适当的采样方案来估算给定土壤的最大防水性,这是达到该水平的关键确定其环境影响。通过使用水滴渗透时间(WDPT)和乙醇滴度摩尔浓度(MED)n测试确定实际和潜在的疏水性。n从四种森林土壤的结果中观察到清晰的疏水性季节性模式,在干旱时期达到峰值。长时间潮湿后消失。沙质壤土的疏水性比质地更细的土壤长,并且在桉树下的疏水性比在松树林下的疏水性更长。用WDPT方法测得,在25或105°C下干燥土壤样品可提高四种土壤的憎水性,但尤其是在湿润时期收集的非憎水性样品中.n与沙壤土相比,这种增加更为明显质地更细的土壤,以及在105°C干燥后比25°C干燥的土壤。 MED测量揭示了四种土壤的共同特征。因此,夏季在野外条件下获得的疏水性值始终超过在25或105°C下干燥后得到的值。此外,在湿润时期收集的干燥样品的拒斥性值n不能与夏天在田间条件下观察到的最大水平相比。版权所有©2011 John Wiley&Sons,Ltd.

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