帕图森特河口氧气变化和耗竭的控制因素

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Allison Dreiss, Amir Reza Azarnivand, Anna Hildebrand, Seyedeh Fardis Pourreza Ahmadi, Syeda Sadia Ali, Veronica Malabanan Lucchese, Qian Zhang, Laura L. Lapham, Ryan J. Woodland, Lora Harris, Jeremy M. Testa
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引用次数: 0

摘要

主要由于富营养化和气候变暖,全球沿岸水域的缺氧现象日益严重。在切萨皮克湾和波罗的海等大型系统中,对营养盐负荷和气候变化引起的缺氧反应进行了广泛的研究,而对较小、较浅的缺氧区的研究则较少。因此,需要进一步了解富营养化和气候变暖对各种不同河口环境中缺氧扩大(或减少)的相互作用。帕塔森特河口是切萨皮克湾的一个富营养化亚河口,每年都会出现季节性缺氧现象。我们对长期记录(1985-2021 年)中的溶解氧(DO)趋势、时间和几项耗竭指标进行了时空分析。我们发现,尽管流域氮负荷减少,磷负荷保持稳定,但内部产生的缺氧区从河口中部开始,随着夏季的到来向上游和下游扩散,缺氧量日(HVD)在记录中一直在增加(每年 0.11,p = 0.03)。河流流量和温度一直在增加,是导致缺氧天数增加的主要因素,其中河流流量占缺氧天数年际变化的 40%(夏季和秋季温度每年分别增加 0.03 ℃ 和 0.06 ℃)。秋季底层水的表观氧利用率(AOU)在增加,这与水温和分层强度的增加趋势一致。HVD 与河口中部地区底栖无脊椎动物的生物量呈负相关(r2 = 0.34,斜率 = -0.59*HVD),表明底栖生物对较高营养级的觅食将受到持续缺氧的限制。这些结果表明,当前和未来的气候多变性在调节帕塔森特河口的氧气耗竭方面发挥着重要作用,这就更有必要将气候变化因素纳入河口的恢复和管理战略中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Controls on Oxygen Variability and Depletion in the Patuxent River Estuary

Controls on Oxygen Variability and Depletion in the Patuxent River Estuary

Oxygen depletion in coastal waters is increasing globally due primarily to eutrophication and warming. Hypoxia responses to nutrient loading and climate change have been extensively studied in large systems like the Chesapeake Bay and the Baltic Sea, while fewer studies have investigated smaller, shallower hypoxic zones. Thus, an improved understanding of the interactions of eutrophication and warming on hypoxia expansion (or reduction) in the wide variety of different estuarine environments is needed. We examined interannual controls on oxygen depletion in the Patuxent River estuary, a eutrophic sub-estuary of Chesapeake Bay where seasonal hypoxia develops annually. We conducted a spatial and temporal analysis of dissolved oxygen (DO) trends, timing, and several metrics of depletion over a long-term record (1985–2021). We found an internally generated hypoxic zone that initiates in the middle estuary, spreading upstream and downstream as the summer progresses, and that hypoxic volume days (HVD) have been increasing (0.11 per year, p = 0.03) over the record despite reduced watershed nitrogen loads and stable phosphorus loads. River flow and temperature have been increasing and are major drivers of increased HVD, with river flow explaining 40% of the interannual variation in HVD (temperature has increased 0.03 and 0.06 °C per year in summer and fall, respectively). Apparent oxygen utilization (AOU) is increasing in bottom waters in the fall, consistent with increasing trends of both water temperature and stratification strength. HVD was negatively related (r2 = 0.34, slope = −0.59*HVD) to the biomass of benthic invertebrates in the middle region of the estuary, suggesting that benthic forage for higher trophic levels will be limited by sustained hypoxia. These results indicate that current and future climate variability plays an important role in regulating oxygen depletion in the Patuxent River estuary, which reinforces the need to factor climate change into strategies for the restoration and management of estuaries.

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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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