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Evaluation of sediment profile imagery as a tool for assessing water quality in Greenwich Bay, Rhode Island, USA

机译:泥沙剖面图像评估作为评估美国罗德岛格林威治湾水质的工具

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摘要

The Benthic Habitat Quality (BHQ) index was used to assess habitat visible in sediment profile images (SP1) following hypoxia disturbance in a shallow (<10 m) estuarine embayment in Rhode Island, USA. We tested for associations between the BHQ, SPI features and water quality over several assessment windows (1, 3, 7, 14, and 28 days prior to imaging) and at multiple dissolved oxygen (DO) thresholds (2.0 mg l~(-1), 2.9 mg l~(-1), and 4.8 mg l~(-1)). Using categorical data analysis, we established empirical relationships between hypoxia prevalence and presence/absence of biogenic features visible in SPI. Fecal pellets, tubes, feeding pits, voids, mounds, and BHQ score were good affirmative features, meaning that their presence (or score greater than 5) indicated a high probability of good water quality. However, low sensitivity to hypoxia precluded their usefulness as indicators, and was attributed to rarity in images and to factors acting on time intervals longer than those examined, e.g. long-term organic enrichment or hypoxia. Burrow structures and the apparent redox potential discontinuity (aRPD), or oxidized layer of surface sediment, were good discriminatory features, with high sensitivity and specificity for both hypoxia and normoxia. Both were strong surrogates for water quality over multiple assessment windows and DO thresholds, and had the highest overall predictive values. We conclude that SPI images can be used to widen the spatial extent of water quality monitoring efforts by utilizing the relationships between aRPD, burrows and hypoxia prevalence.
机译:在美国罗得岛的浅河口(<10 m)河口低氧扰动后,使用底栖生境质量(BHQ)指数评估沉积物图像(SP1)中可见的栖息地。我们在多个评估窗口(成像前1、3、7、14和28天)和多个溶解氧(DO)阈值(2.0 mg l〜(-1)下,测试了BHQ,SPI特征与水质之间的关联),2.9 mg l〜(-1)和4.8 mg l〜(-1))。使用分类数据分析,我们建立了低氧患病率与SPI中可见的生物特征存在/不存在之间的经验关系。粪便颗粒,试管,进食坑,空隙,土堆和BHQ得分是良好的肯定特征,这意味着它们的存在(或得分大于5)表明水质良好的可能性很高。然而,对低氧的低敏感性使得它们不能用作指标,并且归因于图像的稀有性以及作用于时间间隔长于所检查的时间间隔的因素,例如血氧饱和度。长期器质性富集或缺氧。洞穴结构和表观沉积物的氧化还原电位不连续性(aRPD)或氧化层是良好的鉴别特征,对缺氧和常氧具有很高的敏感性和特异性。两者都是在多个评估窗口和DO阈值上对水质的强烈替代,并且具有最高的总体预测值。我们得出结论,通过利用aRPD,洞穴和缺氧流行率之间的关系,可以将SPI图像用于扩大水质监测工作的空间范围。

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