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A dynamic method to determine the O2‐partial pressure distribution within soil aggregates

机译:确定土壤团聚体内O2分压分布的动态方法

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AbstractDuring amperometric measurements of oxygen concentration an electrode itself consumes oxygen. To make sure that oxygen concentration at a soil microsite is not lowered by the measurement itself, but determines thein situsituation, the sensitive tip of the electrode should not be in a static position for a longer time than is necessary to reach equilibrium. If the electrode is moved stepwise through the soil aggregate and is allowed to reach equilibrium at every position, it is possible to measure profiles of oxygen partial pressure distribution from the surface to the center of single soil aggregates. We used a small electromotor attached to a micromanipulator to push the pO2‐sensitive microelectrode at a constant speed through the soil aggregate. As an advantage this ‘dynamic’ method needs no man power and gives continuous profiles of oxygen concentration from the surface to the center of the aggr
机译:摘要在氧浓度的电化学测量过程中,电极本身会消耗氧气。为确保土壤微点的氧气浓度不会因测量本身而降低,而是确定原位情况,电极的敏感尖端处于静止位置的时间不应超过达到平衡所需的时间。如果电极在土壤团聚体中逐步移动,并允许在每个位置达到平衡,则可以测量从单个土壤团聚体表面到中心的氧分压分布曲线。我们使用连接到显微操纵器的小型电动机,以恒定速度推动对 pO2 敏感的微电极穿过土壤聚集体。其优点是,这种“动态”方法不需要人力,并且可以提供从表面到膨胀中心的连续氧气浓度曲线

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