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Atmospheric dry deposition of sulfur and nitrogen in the Athabasca Oil Sands Region, Alberta, Canada

机译:加拿大艾伯塔省阿萨巴斯卡油砂地区的大气干法沉积硫和氮

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Due to the potential ecological effects on terrestrial and aquatic ecosystems from atmospheric deposition in the Athabasca Oil Sands Region (AOSR), Alberta, Canada, this study was implemented to estimate atmospheric nitrogen (N) and sulfur (S) inputs. Passive samplers were used to measure ambient concentrations of ammonia (NH_3), nitrogen dioxide (NO_2). nitric aciditrous acid (HNO_3/HONO), and sulfur dioxide (SO_2) in the AOSR. Concentrations of NO_2 and SO_2 in winter were higher than those in summer, while seasonal differences of NH_3 and HNO_3/ HONO showed an opposite trend, with higher values in summer. Concentrations of NH_3, NO_2 and SO_2 were high close to the emission sources (oil sands operations and urban areas). NH_3 concentrations were also elevated in the southern portion of the domain indicating possible agricultural and urban emission sources to the southwest. HNO_3, an oxidation endpoint, showed wider ranges of concentrations and a larger spatial extent Concentrations of NH_3, NO_2, HNO_3/HONO and SO_2 from passive measurements and their monthly deposition velocities calculated by a multi-layer inference model (MLM) were used to calculate dry deposition of N and S. NH_3 contributed the largest fraction of deposited N across the network, ranging between 0.70-1.25 kg N ha~(-1) yr~(-1), HNO_3/HONO deposition ranged between 030-0.90 kg N ha~(-1) yr~(-1) and NO_2 deposition between 0.03-0.70 kg N ha~(-1) yr~(-1). During the modeled period, average dry deposition of the inorganic gaseous N species ranged between 1.03 and 2.85 kg N ha~(-1) yr~(-1) and SO_4-S deposition ranged between 0.26 and 2.04 kg ha~(-1) yr~(-1). Comparisons with co-measured ion exchange resin throughfall data (8.51 kg S ha~(-1) yr~(-1)) indicate that modeled dry deposition combined with measured wet deposition (137 kg S ha~(-1) yr~(-1)) underestimated S deposition. Gas phase NH_3 (71%) and HNO_3 plus NO_2 (79%) dry deposition fluxes dominated the total deposition of NH_4-N and NO_3-N, respectively.
机译:由于加拿大艾伯塔省阿萨巴斯卡油砂地区(AOSR)的大气沉积对陆地和水生生态系统具有潜在的生态影响,因此该研究旨在估算大气中的氮(N)和硫(S)投入。使用被动采样器测量氨气(NH_3),二氧化氮(NO_2)的环境浓度。 AOSR中的硝酸/亚硝酸(HNO_3 / HONO)和二氧化硫(SO_2)。冬季NO_2和SO_2的浓度高于夏季,而NH_3和HNO_3 / HONO的季节差异呈现相反的趋势,夏季则较高。靠近排放源(油砂作业和市区)的NH_3,NO_2和SO_2浓度很高。区域南部的NH_3浓度也升高,表明西南部可能存在农业和城市排放源。 HNO_3是一种氧化终点,它显示出更宽的浓度范围和更大的空间范围被动测量得出的NH_3,NO_2,HNO_3 / HONO和SO_2的浓度以及通过多层推断模型(MLM)计算的每月沉积速度来计算N和S的干沉积.NH_3贡献了整个网络中最大的N沉积部分,介于0.70-1.25 kg N ha〜(-1)yr〜(-1)之间,HNO_3 / HONO沉积范围介于030-0.90 kg N之间ha〜(-1)yr〜(-1)和NO_2沉积在0.03-0.70 kg N ha〜(-1)yr〜(-1)之间。在建模期间,无机气态N物种的平均干沉降范围为1.03至2.85 kg N ha〜(-1)yr〜(-1),SO_4-S沉积范围为0.26至2.04 kg ha〜(-1) yr〜(-1)。与共同测量的离子交换树脂穿透数据(8.51 kg S ha〜(-1)yr〜(-1))的比较表明,模拟干沉降与测得的湿沉降(137 kg S ha〜(-1)yr〜() -1))低估了S的沉积。气相NH_3(71%)和HNO_3加NO_2(79%)的干沉积通量分别控制着NH_4-N和NO_3-N的总沉积。

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