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Total phosphorus inference models and indices for coastal plain streams based on benthic diatom assemblages from artificial substrates.

机译:基于人工基质底栖硅藻组合的沿海平原河流总磷推断模型和指标。

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We investigated the potential for using diatoms to monitor and assess nutrient enrichment in coastal plain streams using weighted-averaging inference models and diatom trophic indices. Samples were collected from low-gradient, clay- to sand-bottom streams in New Jersey (NJ), USA, using artificial substrates (diatometers). Multivariate analysis showed that conductivity was overall the most important explanatory variable. Total phosphorus (TP) explained a significant proportion of the variation in diatom species composition. There was statistical justification for development of inference models for TP but not for total nitrogen (TN). We developed and tested models for inferring TP using weighted-averaging (WA) and weighted-averaging partial least squares (WA-PLS) regression and calibration techniques. We also created a diatom TP index by rescaling the inferred TP values. WA-PLS provided the best model (n=38), which showed moderate predictive ability (r2boot=0.43; RMSEPboot=0.30 log10 .g l-1 TP); it performed best at lower TP concentrations and tended to underestimate values above 100 .g l-1. The TP index performed well; it assigned the majority of the index scores to the correct nutrient category. TP models and indices developed for the Coastal Plain had lower predictive ability than those developed for northern NJ and streams in other comparable geographic regions of the US. This lower performance can be attributed primarily to a data gap in the TP gradient in the calibration dataset (lack of sites with TP concentrations between 240 and 560 .g l-1), and a smaller number of samples. We conclude that diatom-based TP inference models and artificial substrate sampling are useful for assessing and monitoring nutrient enrichment in coastal plain streams. Given the worldwide distribution of streams similar to those in this study, these tools should be widely applicable.
机译:我们研究了使用硅藻通过加权平均推断模型和硅藻营养指数来监测和评估沿海平原溪流中营养物富集的潜力。使用人造基质(直径计)从美国新泽西州(新泽西州)的低梯度,粘土到砂底流采集样品。多变量分析表明,电导率总体上是最重要的解释变量。总磷(TP)解释了硅藻物种组成变化的很大一部分。对于TP的推理模型的开发有统计学依据,但对于总氮(TN)的推理模型则没有。我们开发并测试了使用加权平均(WA)和加权平均偏最小二乘(WA-PLS)回归和校准技术推断TP的模型。我们还通过重新缩放推断的TP值来创建硅藻TP索引。 WA-PLS提供了最佳模型( n = 38),该模型具有中等预测能力( r 2 boot = 0.43; RMSEP boot = 0.30 log 10 .gl -1 TP);它在较低的TP浓度下表现最佳,并且倾向于低估100 .g l -1 以上的值。 TP指数表现良好;它把大多数指数得分分配给了正确的营养类别。为沿海平原开发的TP模型和指数的预测能力低于为新泽西北部和美国其他可比较地理区域的河流开发的TP模型和指数。这种较低的性能主要归因于校准数据集中TP梯度中的数据缺口(缺乏TP浓度在240至560 .g l -1 之间的位点)和较少的样本量。我们得出的结论是,基于硅藻的TP推断模型和人工底物采样可用于评估和监测沿海平原流域的营养富集。鉴于与本研究类似的流在世界范围内的分布,这些工具应广泛适用。

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