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Technical note: a constant-volume artificial stream for reducing variation in aquatic process measurements.

机译:技术说明:恒定体积的人造流,用于减少水生过程测量值的变化。

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This paper describes the construction, operation, and assessment of a constant-volume artificial stream designed to control water quality and reduce variation to improve aquatic process measurements. The system was used to investigate suspended clay influence on phosphorus acquisition (load buffering) by lotic periphyton. Spatial and temporal heterogeneity represent the greatest sources of variation in the distribution and activity of aquatic biota in natural systems. Imposing experimental treatments simultaneously addresses temporal variation. Spatial variability is managed by controlling physical and chemical variables such as temperature, light, substrate, flow, and water quality. Controlling environmental conditions leads to reduced variation in biotic state, which improves the measurement of biotic processes. This artificial stream design minimizes water volume fluctuation, which facilitates solution manipulation and measurement and reduces environmental variation. A unique reservoir and valve arrangement compensates for evaporative water loss, allowing the operating water volume of individual stream units to be maintained (<+or-1%) over long periods. In pre-experiment assessments, mean total dissolved salts were maintained to within 3% of their initial concentration over a one-week period, and suspended clay turbidity was within 4.3% after some initial settling. During experimental use, artificial stream variation in periphyton biomass and phosphorus uptake was less than that reported from several natural streams.
机译:本文介绍了用于控制水质并减少变化以改善水产养殖过程测量结果的恒定体积人工流的构造,运行和评估。该系统用于研究悬浮黏土对乐透水生植物磷吸收(负载缓冲)的影响。时空异质性是自然系统中水生生物群落分布和活动变化的最大来源。施加实验处理可同时解决时间变化。通过控制物理和化学变量(例如温度,光,底物,流量和水质)来管理空间变异性。控制环境条件可减少生物状态的变化,从而改善生物过程的度量。这种人造水流设计最大程度地减少了水量波动,从而有利于溶液处理和测量,并减少了环境变化。独特的储水器和阀门装置可补偿蒸发水的损失,从而可长期保持各个物流单元的工作水量(<+或-1%)。在实验前的评估中,平均溶解盐在一周内保持在其初始浓度的3%以内,并且在一些初始沉降后,悬浮粘土的浊度在4.3%以内。在实验使用期间,浮游生物量和磷吸收量的人工流变化小于几种天然流的人工流变化。

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