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Chesapeake Bay Dissolved Oxygen Criterion Attainment Deficit: Three Decades of Temporal and Spatial Patterns

机译:切萨皮克湾的溶解氧判据缺乏:三个时空格局

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摘要

Low dissolved oxygen (DO) conditions are a recurring issue in waters of Chesapeake Bay, with detrimental effects on aquatic living resources. The Chesapeake Bay Program partnership has developed criteria guidance supporting the definition of state water quality standards and associated assessment procedures for DO and other parameters, which provides a binary classification of attainment or impairment. Evaluating time series of these two outcomes alone, however, provides limited information on water quality change over time or space. Here we introduce an extension of the existing Chesapeake Bay water quality criterion assessment framework to quantify the amount of impairment shown by space-time exceedance of DO criterion (“attainment deficit”) for a specific tidal management unit (i.e., segment). We demonstrate the usefulness of this extended framework by applying it to Bay segments for each 3-year assessment period between 1985 and 2016. In general, the attainment deficit for the most recent period assessed (i.e., 2014–2016) is considerably worse for deep channel (DC; n = 10) segments than open water (OW; n = 92) and deep water (DW; n = 18) segments. Most subgroups - classified by designated uses, salinity zones, or tidal systems - show better (or similar) attainment status in 2014–2016 than their initial status (1985–1987). Some significant temporal trends (p < 0.1) were detected, presenting evidence on the recovery for portions of Chesapeake Bay with respect to DO criterion attainment. Significant, improving trends were observed in seven OW segments, four DW segments, and one DC segment over the 30 3-year assessment periods (1985–2016). Likewise, significant, improving trends were observed in 15 OW, five DW, and four DC segments over the recent 15 assessment periods (2000–2016). Subgroups showed mixed trends, with the Patuxent, Nanticoke, and Choptank Rivers experiencing significant, improving short-term (2000–2016) trends while Elizabeth experiencing a significant, degrading short-term trend. The general lack of significantly improving trends across the Bay suggests that further actions will be necessary to achieve full attainment of DO criterion. Insights revealed in this work are critical for understanding the dynamics of the Bay ecosystem and for further assessing the effectiveness of management initiatives aimed toward Bay restoration.
机译:低溶解氧(DO)条件是切萨皮克湾水域中反复出现的问题,对水生生物资源有不利影响。切萨皮克湾计划的合作伙伴关系已制定了标准指南,以支持州水质标准的定义以及溶解氧和其他参数的相关评估程序,从而提供了达到或损害的二进制分类。但是,仅对这两个结果的时间序列进行评估只能提供有限的水质随时间或空间变化的信息。在这里,我们介绍了现有切萨皮克湾水质标准评估框架的扩展,以量化特定潮汐管理单元(即分段)的时空超出DO准则(“成就赤字”)时空所显示的损害量。我们通过在1985年至2016年之间的每个3年评估期将其应用于海湾地区,证明了此扩展框架的有用性。总的来说,最近评估的时期(即2014-2016年)的成就赤字对于深层评估而言更为严重渠道(DC; n = 10)段比开水(OW; n = 92)和深水(DW; n = 18)段要大。大多数亚类(按指定用途,盐分带或潮汐系统分类)在2014-2016年的状况比其初始状况(1985-1987年)更好(或类似)。检测到一些显着的时间趋势(p <0.1),为切萨皮克湾部分地区的溶解氧达到标准提供了证据。在30个为期3年的评估期(1985-2016年)中,七个OW区段,四个DW区段和一个DC区段观察到了显着的改善趋势。同样,在最近的15个评估期(2000-2016年)中,在15个OW,五个DW和四个DC区域中观察到了显着的改善趋势。亚组显示出不同的趋势,其中Patuxent,Nanticoke和Choptank河的短期(2000-2016)趋势显着改善,而伊丽莎白的短期趋势则显着下降。整个海湾地区普遍缺乏明显改善的趋势,这表明必须采取进一步的行动才能完全达到溶解氧标准。这项工作中揭示的见解对于理解海湾生态系统的动态以及进一步评估旨在恢复海湾的管理计划的有效性至关重要。

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