首页> 美国卫生研究院文献>other >Imidacloprid transport and sorption nonequilibrium in single and multilayered columns of Immokalee fine sand
【2h】

Imidacloprid transport and sorption nonequilibrium in single and multilayered columns of Immokalee fine sand

机译:Immokalee细砂单层和多层柱中吡虫啉的运移和吸附非平衡

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Imidacloprid (IMD) is a neonicotinoid pesticide soil-drenched to many crops to control piercing-sucking insects such as the Asian citrus psyllid (ACP). Neonicotinoids are persistent in the environment and transport analyses are helpful estimate leaching potential from soils that could result in groundwater pollution. The objective of this study was to analyze IMD breakthrough under saturated water flow in soil columns packed with three horizons (A, E, Bh) of Immokalee Fine Sand (IFS). Also, we used the dimensionless form of the convective-dispersive model (CD-Model) to compare the optimized transport parameters from each column experiment (retardation factor, R; fraction of instantaneous-to-total retardation, β; and mass transfer coefficient, ω) with the parameters obtained from sorption batch equilibria and sorption kinetics. The tracer (Cl-) breakthrough curves (BTCs) were symmetrical and properly described by the CD-Model. IMD BTCs from A, Bh, and multilayered [A+E+Bh] soil columns showed steep fronts and tailing that were well described by the one-site nonequilibrium (OSNE) model, which was an evidence of non-ideal transport due to IMD mass transfer into the soil organic matter. In general, IMD was weakly-sorbed in the A and Bh horizons (R values of 3.72 ± 0.04 and 3.08 ± 0.07, respectively), and almost no retardation was observed in the E horizon (R = 1.20 ± 0.02) due to its low organic matter content (0.3%). Using the HYDRUS-1D package, optimized parameters (R, β, ω) from the individual columns successfully simulated IMD transport in a multilayered column mimicking an IFS soil profile. These column studies and corresponding simulations agreed with previous findings from batch sorption equilibria and kinetics experiments, where IMD showed one-site kinetic mass transfer between soil surfaces and soil solution. Ideally, sandy soils should be maintained unsaturated by crop irrigation systems and rainfall monitoring during and after soil-drench application. The unsaturated soil will increase IMD retardation factors and residence time for plant uptake, lowering leaching potential from soil layers with low sorption capacity, such as the E horizon.
机译:吡虫啉(IMD)是一种新烟碱农药,可在多种农作物上灌溉,以控制刺穿吸食性昆虫,例如亚洲柑橘木虱(ACP)。新烟碱类物质在环境中持续存在,运输分析有助于估计土壤中的淋溶潜能,可能导致地下水污染。这项研究的目的是分析在Immokalee细砂(IFS)的三个层(A,E,Bh)填充的土壤柱中,在饱和水流下的IMD突破。此外,我们使用对流扩散模型(CD-Model)的无量纲形式来比较每个色谱柱实验的优化传输参数(延迟因子R;瞬时总延迟量β)和传质系数, ω)具有从吸附批平衡和吸附动力学获得的参数。示踪剂(Cl -)穿透曲线(BTC)是对称的,并由CD模型正确描述。来自A,Bh和多层[A + E + Bh]土柱的IMD BTC表现出陡峭的前部和尾部,一站式非平衡(OSNE)模型很好地描述了这一点,这证明了IMD导致的非理想运输大量转移到土壤中的有机物。通常,IMD在A和Bh层中被弱吸收(R值分别为3.72±0.04和3.08±0.07),并且由于E层较低,在E层中几乎没有观察到延迟(R = 1.20±0.02)。有机物含量(0.3%)。使用HYDRUS-1D软件包,来自各个色谱柱的优化参数(R,β,ω)成功模拟了模拟IFS土壤剖面的多层色谱柱中的IMD运移。这些色谱柱研究和相应的模拟与批吸附吸附平衡和动力学实验的先前发现一致,IMD显示了土壤表面和土壤溶液之间的单点动力学传质。理想情况下,应在施肥过程中和施肥后通过作物灌溉系统和降雨监测使沙质土壤保持不饱和状态。非饱和土壤将增加IMD延迟因子和植物吸收的停留时间,从而降低低吸附能力土壤层(例如E层)的浸出潜力。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号