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大气沉降氮对北卡罗来纳州纽斯河河口年度氮预算的重要性。

Importance of atmospherically deposited nitrogen to the annual nitrogen budget of the Neuse River estuary, North Carolina.

作者信息

Whitall David, Hendrickson Brad, Paerl Hans

机构信息

Department of Civil and Environmental Engineering, Syracuse University, 220 Hinds Hall, 13244, Syracuse, NY, USA.

出版信息

Environ Int. 2003 Jun;29(2-3):393-9. doi: 10.1016/S0160-4120(02)00175-7.

Abstract

Wet deposition of nitrogen, as NH(4)(+), NO(3)(-), and organic N, contributes up to 50% of the total externally supplied or 'new' N flux to the Neuse River Estuary (North Carolina). Excessive nitrogen (N) loading to N-sensitive waters such as the Neuse River Estuary has been linked to changes in microbial and algal community composition and function (harmful algal blooms), hypoxia/anoxia, and fish kills. In a 4-year study from July 1996 to July 2000, the weekly wet deposition of NH(4)(+), NO(3)(-), and dissolved organic N was calculated, based on concentration and precipitation measurements, at 11 sites on a northwest-southeast transect in the watershed. Data from this period indicate that the annual mean total wet atmospherically deposited (AD)-N flux was 11 kg ha(-1) year(-1). Deposition was fairly evenly distributed between nitrate, ammonium, and organics (32%, 32%, and 36%, respectively). Seasonally, the summer (June-August) months contained the highest weekly wet total N deposition; this trend was not driven by precipitation amount. Estimates of watershed N retention and in-stream riverine processing revealed that the AD-N flux contributed an estimated 20% (range of 15-51%) of the total 'new' N flux to the estuary, with direct deposition of N to the estuary surface accounting for 6% of the total 'new' N flux. This study did not measure the dry depositional flux, which may double the contribution of AD-N to the estuary. The AD-N is an important source of 'new' N to the Neuse River Estuary as well as other estuarine and coastal ecosystems downwind of major emission sources. As such, AD-N should be included in effective nutrient mitigation and management efforts for these N-sensitive waters.

摘要

以铵离子(NH₄⁺)、硝酸根离子(NO₃⁻)和有机氮形式存在的氮的湿沉降,占流入北卡罗来纳州纽斯河河口的外部供应或“新增”氮通量总量的50%。向对氮敏感的水体(如纽斯河河口)过量输入氮,与微生物和藻类群落组成及功能的变化(有害藻华)、缺氧/无氧状态以及鱼类死亡有关。在1996年7月至2000年7月的一项为期4年的研究中,根据浓度和降水量测量数据,计算了流域内一条西北 - 东南走向断面的11个站点的铵离子(NH₄⁺)、硝酸根离子(NO₃⁻)和溶解有机氮的每周湿沉降量。这一时期的数据表明,年平均大气湿沉降(AD)氮通量为11千克·公顷⁻¹·年⁻¹。沉降在硝酸盐、铵和有机物之间分布较为均匀(分别为32%、32%和36%)。从季节上看,夏季(6 - 8月)的每周湿沉降总氮量最高;这一趋势并非由降水量驱动。对流域氮保留和河流中氮处理的估计表明,AD氮通量占流入河口的“新增”氮通量总量的约20%(范围为15% - 51%),氮直接沉降到河口表面占“新增”氮通量总量的6%。本研究未测量干沉降通量,干沉降通量可能使AD氮对河口的贡献增加一倍。AD氮是纽斯河河口以及主要排放源下风处的其他河口和沿海生态系统“新增”氮的重要来源。因此,在针对这些对氮敏感水体的有效养分减排和管理措施中应纳入AD氮。

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