{"title":"Hydrologic Management Convolutes Expected Spatiotemporal Patterns of Dissolved Organic Matter in the Hudson River","authors":"Alex C. Collins, Julia Hubbard, Sasha Wagner","doi":"10.1029/2024JG008131","DOIUrl":null,"url":null,"abstract":"<p>Riverine dissolved organic matter (DOM) is a vector for nutrient cycling and elemental exchange between terrestrial and oceanic reservoirs. The quality and quantity of DOM transported in rivers are determined by a complex interplay of watershed-specific conditions (e.g., land use and discharge). In many temperate rivers, the frequency and intensity of hydrologic events are expected to increase with continued climate change, which would result in an overall increased export of terrestrial DOM. However, the presence of dams and other impoundments increase water residence time and could dampen these effects. Here, we examine DOM biogeochemistry in the Hudson River (New York, USA), which experiences intermittent periods of elevated discharge and receives a seasonally varied series of inputs from urban, agricultural, and forested landscapes. DOM was quantified and characterized using optical spectroscopic techniques, including parallel factor analysis (PARAFAC) modeling of fluorescent DOM components. Our findings indicate that the influence of land cover on DOM composition is secondary to that of hydrologic management. We also found DOM pulse-shunt effects to be more muted in the upper Hudson River watershed, where more water is retained by dams and reservoirs than in the Mohawk River watershed. Regardless of hydrologic management, discharge events consistently enhanced aromatic DOM export in the Hudson River and its subbasins, which suggests climate change and increased rainfall will enhance the delivery of humic-like DOM to the estuary and coastal margins.</p>","PeriodicalId":16003,"journal":{"name":"Journal of Geophysical Research: Biogeosciences","volume":"130 4","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2025-04-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Biogeosciences","FirstCategoryId":"93","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JG008131","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
摘要
河流溶解有机物(DOM)是陆地和海洋水库之间营养循环和元素交换的载体。河流中迁移的 DOM 的质量和数量由流域特定条件(如土地利用和排水量)的复杂相互作用决定。在许多温带河流中,随着气候变化的持续,水文事件的频率和强度预计都会增加,这将导致陆地 DOM 的总体输出量增加。然而,水坝和其他蓄水池的存在增加了水的停留时间,可能会抑制这些影响。在此,我们研究了哈德逊河(美国纽约)的 DOM 生物地球化学,哈德逊河在间歇期会出现高排水量,并接收来自城市、农业和森林景观的一系列季节性输入。利用光学光谱技术,包括荧光 DOM 成分的平行因子分析(PARAFAC)建模,对 DOM 进行了量化和表征。我们的研究结果表明,土地覆盖对 DOM 成分的影响次于水文管理的影响。我们还发现,与莫霍克河流域相比,哈德逊河上游流域的 DOM 脉冲分流效应更弱,因为那里的水坝和水库截留了更多的水。无论水文管理如何,哈德逊河及其子流域的排放事件都持续增强了芳香族 DOM 的输出,这表明气候变化和降雨量的增加将增强向河口和沿岸边缘输送腐殖质类 DOM 的能力。
Hydrologic Management Convolutes Expected Spatiotemporal Patterns of Dissolved Organic Matter in the Hudson River
Riverine dissolved organic matter (DOM) is a vector for nutrient cycling and elemental exchange between terrestrial and oceanic reservoirs. The quality and quantity of DOM transported in rivers are determined by a complex interplay of watershed-specific conditions (e.g., land use and discharge). In many temperate rivers, the frequency and intensity of hydrologic events are expected to increase with continued climate change, which would result in an overall increased export of terrestrial DOM. However, the presence of dams and other impoundments increase water residence time and could dampen these effects. Here, we examine DOM biogeochemistry in the Hudson River (New York, USA), which experiences intermittent periods of elevated discharge and receives a seasonally varied series of inputs from urban, agricultural, and forested landscapes. DOM was quantified and characterized using optical spectroscopic techniques, including parallel factor analysis (PARAFAC) modeling of fluorescent DOM components. Our findings indicate that the influence of land cover on DOM composition is secondary to that of hydrologic management. We also found DOM pulse-shunt effects to be more muted in the upper Hudson River watershed, where more water is retained by dams and reservoirs than in the Mohawk River watershed. Regardless of hydrologic management, discharge events consistently enhanced aromatic DOM export in the Hudson River and its subbasins, which suggests climate change and increased rainfall will enhance the delivery of humic-like DOM to the estuary and coastal margins.
期刊介绍:
JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology