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首页> 外文期刊>Soil & Tillage Research >Soil profile distributions of water and solutes following frequent high water inputs.
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Soil profile distributions of water and solutes following frequent high water inputs.

机译:频繁输入大量水后水和溶质的土壤剖面分布。

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摘要

Investigation of factors affecting leaching patterns under tilled and no-till soils are important for successful modelling of solute leaching. There can be various other factors that may offset an anticipated tillage effect on solute leaching. A study was conducted in a Donnelly silty loam (fine-loamy, mixed frigid Typic Cryoboralf) at Dawson Creek, British Columbia, Canada, to investigate how a reactive chemical (FD&C blue#1 dye) and a conservative tracer (bromide, Br-) would leach in a no-till (NT) soil compared to a tilled (T), when high volume of water are provided discretely, at short time intervals. Three plots of 1.5 m x 1.5 m were prepared in each NT and T soil for flood irrigation. The chemicals were applied by spray using a knapsack sprayer. Soil cores were extracted from a maximum depth of 1.25 m using a truck mounted hydraulic soil sampler at 5, 19, and 55 days (S1, S2, and S3, respectively) after irrigating different amounts of water. These soil cores, sub-sampled at different depths, were analysed for water content, Br- and dye concentrations. The analyses indicated that Br- and dye moved in distinctive patterns in the two tillage systems. After irrigating with a total of 240 mm of ponded water in three applications over a period of 10 days, the centre of mass of the travel depth profiles for Br- was 0.15 m in the NT and 0.26 m in the T plots; for the dye, 0.27 m in the NT and 0.17 m in the T plots. At soil core sampling times S1, S2, and S3, the average mass recovered for Br- was 82%, 39%, and 27% in the NT and 78%, 50%, and 45% in the T plots. For the dye, mass recovery rates of 78%, 58%, and 22% were observed in the NT and 92%, 79% and 25% in the T plots. The increasing mass loss of Br- observed with increasing net water inputs in the two tillage systems was more likely due to a lateral loss with water than due to a leaching below sampling depth. The increasing mass loss of dye over time in the two tillage systems was more likely due to a high rate of degradation than to a loss through a lateral or vertical flow..
机译:对耕作和免耕土壤下影响淋溶模式的因素进行调查对于成功建立溶质淋溶模型非常重要。可能还有其他各种因素可能抵消耕作对溶质浸出的预期影响。在加拿大不列颠哥伦比亚省道森克里克(Dawson Creek)的Donnelly粉质壤土壤土(细质壤土,混合的典型Typic Cryoboralf)中进行了一项研究,以研究活性化学物质(FD&C blue#1染料)和保守示踪剂(溴化物,Br-如果在短时间间隔内不连续提供大量的水,则与耕种(T)相比,)会在免耕(NT)的土壤中浸出。在NT和T土中分别准备了三个1.5 m x 1.5 m的地块用于洪水灌溉。使用背负式喷雾器通过喷雾施用化学品。在灌溉不同量的水后的5、19和55天(分别为S1,S2和S3),使用车载液压土壤采样器从最大深度1.25 m提取土壤核心。对这些土壤核心进行了不同深度的二次采样,分析了它们的水含量,Br-和染料浓度。分析表明,Br-和染料在两种耕作系统中的移动方式不同。在三个应用中,在总共10天的时间内使用总计240 mm的积水灌溉后,在NT区,Br-的行进深度剖面的质心为0.15 m,在T区为0.26 m。对于染料而言,在NT中为0.27 m,在T中为0.17 m。在土壤岩心取样时间S1,S2和S3时,NT中Br-的平均回收率为82%,39%和27%,T曲线中为78%,50%和45%。对于染料,在NT中观察到质量回收率为78%,58%和22%,在T图中观察到为92%,79%和25%。在两个耕作系统中,随着净水输入量的增加,观察到的Br-的质量损失增加的可能性更大,这是由于水分的侧向损失,而不是由于低于采样深度的浸出。在两个耕作系统中,随着时间的流逝,随着时间的流逝,染料的质量损失增加的可能性更大,这是由于降解率高,而不是由于横向或垂直流失造成的。

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