Whitall David, Hendrickson Brad, Paerl Hans
Department of Civil and Environmental Engineering, Syracuse University, 220 Hinds Hall, 13244, Syracuse, NY, USA.
Environ Int. 2003 Jun;29(2-3):393-9. doi: 10.1016/S0160-4120(02)00175-7.
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.
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。