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Measurement uncertainty in stream nutrient uptake: Detecting land-use impacts on tropical streams

机译:溪流养分吸收的测量不确定性:检测土地利用对热带溪流的影响

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Stream nutrient uptake is an important ecosystem service, because it supplies human needs such as water purification. Uncertainty in nutrient uptake measurement determines, in combination with effect magnitude, whether effects of land use, stream restoration or climate change can be detected by this method. However, measurement uncertainty for nutrient uptake metrics is rarely reported. Here, we compared whole-stream phosphate and nitrate uptake among three pristine and three agricultural tropical Cerrado streams. We quantified uncertainty in uptake metrics estimated by kinetic nutrient-addition experiments and evaluated their potential to detect land-use effects. Ambient phosphate and nitrate uptake lengths (S-w) ranged from 11 to 106 m and from 29 to 357 m, respectively, in pristine streams and from 41 to 586 m and from 76 to 1372 m in agricultural streams. Moderate measurement uncertainty in S-W allowed for the detection of land-use impacts with this metric. However, derived nutrient uptake metrics, such as ambient uptake rates and uptake velocities, as well as parameters of whole-stream saturation kinetics, were associated with high measurement uncertainties that prevented the detection of potential land-use effects. Sensitivity analyses suggested that avoiding high enrichment levels in kinetic addition experiments and increasing sampling effort for plateau nutrient and tracer concentration at the first and last sampling stations of investigated stream reaches are the most promising strategies to reduce measurement uncertainty. Analyzing nutrient uptake without considering measurement uncertainty might lead to poor interpretation in case studies and meta-analyses, such as incorrect evaluations of human impacts or comparisons among systems.
机译:溪流养分吸收是一项重要的生态系统服务,因为它满足了人类的需求,例如水净化。营养摄入量测量的不确定性与影响程度共同决定了通过这种方法是否可以检测土地利用,河流恢复或气候变化的影响。但是,很少有人报告营养吸收指标的测量不确定性。在这里,我们比较了三个原始河道和三个农业热带塞拉多河溪流中全流磷酸盐和硝酸盐的吸收。我们通过动态营养添加实验估算了摄入量指标的不确定性,并评估了其检测土地利用影响的潜力。原始河流中磷酸盐和硝酸盐的环境吸收长度(S-w)分别为11至106 m和29至357 m,而农业河流中的环境磷酸盐吸收长度(S-w)分别为41至586 m和76至1372 m。 S-W中的测量不确定性允许使用此度量来检测土地使用影响。但是,导出的养分吸收指标,例如环境吸收率和吸收速度,以及全流饱和动力学参数,都与高测量不确定度相关联,无法确定潜在的土地利用影响。敏感性分析表明,在动力学加和实验中避免高浓度富集,增加被调查溪流的第一个和最后一个采样站的高原营养物和示踪剂浓度的采样工作,是减少测量不确定度的最有希望的策略。在不考虑测量不确定性的情况下分析养分吸收可能会导致案例研究和荟萃分析的解释不佳,例如对人类影响的评估不正确或系统之间的比较。

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