Linking stream-reach nitrogen loads and groundwater “reachsheds” to inform wastewater-nitrogen management actions, Cape Cod, Massachusetts

IF 5 2区 地球科学 Q1 WATER RESOURCES
Timothy D. McCobb , Denis R. LeBlanc , Jeffrey R. Barbaro , Marcel Belaval
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引用次数: 0

Abstract

Study Region

Cape Cod, Massachusetts, U.S.A.

Study Focus

Anthropogenic nitrogen (N) is a key factor in degrading groundwater and surface-water quality, particularly in coastal New England where onsite wastewater systems are prevalent. This study evaluated whether direct N-load measurements in streams on Cape Cod, Massachusetts, coupled with flow-path information from groundwater-flow models, can effectively identify potential land areas where nitrogen mitigation could substantially reduce loads to receiving waters. Nitrogen fluxes were measured along 63 stream reaches during winter and summer and paired with simulated groundwater recharge areas to identify and rank potential areas for reduction of nonpoint-source N inputs.

New Hydrologic Insights for the Region

Reach-scale nitrate-N loads ranged from −39.1–1182 kg-N/yr per 100 m of stream, indicating spatially variable groundwater inputs across seasons. “Reachsheds” — areas contributing groundwater recharge to specific stream reaches — were delineated using a regional groundwater-flow model. Strong correlations were found between observed N loads and land-use characteristics, especially the number of septic systems and total N inputs from the sum of considered sources. Observed N loads were moderately correlated with recharge area size and wastewater flow estimates. Correlating reach-specific groundwater N loads with land use and parcel-scale nitrogen-yield data identified reachsheds with the highest potential for N load reduction. This approach enables targeted implementation of restoration efforts to optimize nutrient management and support regional load reduction.

Abstract Image

连接河流到达的氮负荷和地下水“流域”,为废水氮管理行动提供信息,马萨诸塞州科德角
研究区域:美国马萨诸塞州科德角研究重点:人为氮(N)是地下水和地表水质量退化的关键因素,特别是在现场污水系统普遍存在的新英格兰沿海地区。本研究评估了马萨诸塞州科德角河流的直接氮负荷测量,结合地下水流动模型的流动路径信息,是否可以有效地确定潜在的陆地区域,在这些区域,氮减排可以大幅减少接收水的负荷。在冬季和夏季测量了63条河流河段的氮通量,并与模拟地下水补给区配对,以确定减少非点源氮输入的潜在区域并对其进行排序。区域河段尺度的硝酸盐- n负荷范围为- 39.1-1182 kg-N/年/ 100 米,表明地下水输入在不同季节的空间变化。“流域”——为特定河流提供地下水补给的区域——是用区域地下水流动模型划定的。观察到的氮负荷与土地利用特征之间存在很强的相关性,特别是化粪池系统的数量和考虑来源的总氮输入量。观测到的氮负荷与补给面积大小和废水流量估算呈正相关。将特定河段的地下水氮负荷与土地利用和包尺度的氮产量数据相关联,确定了氮负荷减少潜力最大的河段。这种方法能够有针对性地实施恢复工作,以优化养分管理并支持区域负荷减少。
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来源期刊
Journal of Hydrology-Regional Studies
Journal of Hydrology-Regional Studies Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
6.70
自引率
8.50%
发文量
284
审稿时长
60 days
期刊介绍: Journal of Hydrology: Regional Studies publishes original research papers enhancing the science of hydrology and aiming at region-specific problems, past and future conditions, analysis, review and solutions. The journal particularly welcomes research papers that deliver new insights into region-specific hydrological processes and responses to changing conditions, as well as contributions that incorporate interdisciplinarity and translational science.
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