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Using rainfall simulation, TDR, and tracer anions to determine effects of soil properties on nitrate leaching

机译:使用降雨模拟,TDR和示踪阴离子确定土壤性质对硝酸盐淋失的影响

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摘要

Two experiments were performed to evaluate NO3-N leaching features using tracer anions combined with use of non-destructive time domain reflectometry (TDR) techniques. A laboratory experiment was conducted to study the effects of different soil bulk density (1.10, 1.33, 1.57, and 1.81 g/cm 3) in the zone of N application and antecedent soil moisture by mass (10 and 15%) on NO3-N leaching during rainfall simulation (6.5 cm/h for 70 min to runoff/drainage pans with 7.6 cm soil layer). Surface runoff, subsurface drainage, and soil extract samples were analyzed for NO3-N, Br (added with rainfall), and Cl (added uniformly to soil) concentrations. TDR probes were horizontally installed either beneath the zone of NO 3-N applied in a line sources for determination of resident solute transport from measured soil bulk electrical conductivity (ECb), or just 1 cm below the soil surface to estimate solute concentrations in the \u22mixing zone\u22. It was found that the 15% soil moisture content treatment had a longer time to the beginning of drainage and less drainage volume compared to 10% soil moisture. Greater compaction caused lower concentrations and losses of NO3-N in subsurface drainage. A second experiment was outdoor rainfall simulation (5 cm/h for 60 min to lysimeters), using two tillage practices (no-till and tillage) and two methods of N-fertilizer applications (local soil compaction and no compaction as a line source). The results showed that local compaction in the zone of application reduced NO3-N leaching significantly; however, tillage did not have a significant effect. In both studies, soil ECb and volumetric water content, measured by TDR, beneath the fertilizer line sources provided \u22real-time\u22 information; it was found that NO3-N in top soil has a curvilinear relationship to ECb beneath line sources that had the potential to simultaneously indicate solute leaching and water infiltration/movement in that zone. This study could provide new information for improving N fertilizer applicators.
机译:进行了两个实验,以结合示踪阴离子和非破坏性时域反射仪(TDR)技术评估NO3-N淋溶特征。进行了一项室内实验,研究了施氮区不同土壤容重(1.10、1.33、1.57和1.81 g / cm 3)和前土壤水分质量(10%和15%)对NO3-N的影响。在降雨模拟过程中进行淋洗(6.5厘米/小时,持续70分钟到具有7.6厘米土壤层的径流/排水盘)。分析了地表径流,地下排水和土壤提取物样品中的NO3-N,Br(添加了降雨)和Cl(均匀添加到土壤)浓度。将TDR探针水平安装在线源中施加的NO 3-N区域下方,以便从测得的土壤总体电导率(ECb)确定残留的溶质运移,或者仅在土壤表面以下1 cm处以估算土壤中的溶质浓度。 u22混合区\ u22。结果发现,与10%的土壤水分相比,15%的土壤水分处理开始排水的时间更长,排水量更少。更大的压实导致地下排水中较低的浓度和NO3-N的损失。第二个实验是室外降雨模拟(5 cm / h,持续60分钟至lysimeters),使用两种耕作方法(免耕和耕作)和两种氮肥施用方法(局部土壤压实和不压实作为线源) 。结果表明,在施肥区局部压实可以显着减少NO3-N的浸出。但是,耕作没有明显的作用。在两项研究中,在肥料线源下方通过TDR测量的土壤ECb和体积水含量提供了实时信息。结果发现,表层土壤中的NO3-N与线下ECb呈曲线关系,有可能同时表明该区域的溶质淋溶和水的渗透/运动。这项研究可以为改善氮肥施用量提供新的信息。

著录项

  • 作者

    Zhou, Jian;

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  • 年度 2004
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  • 原文格式 PDF
  • 正文语种 en
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