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The magnitude of the snow-sourced reactive nitrogen flux to the boundary layer in the Uintah Basin, Utah, USA

机译:UINTAH盆地边界层的冰雪源反应性氮气通量的大小,USA

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Reactive nitrogen (Nr??=??NO, NO2, HONO) and volatile organic carbon emissions from oil and gas extraction activities play a major role in wintertime ground-level ozone exceedance events of up to 140?ppb in the Uintah Basin in eastern Utah. Such events occur only when the ground is snow covered, due to the impacts of snow on the stability and depth of the boundary layer and ultraviolet actinic flux at the surface. Recycling of reactive nitrogen from the photolysis of snow nitrate has been observed in polar and mid-latitude snow, but snow-sourced reactive nitrogen fluxes in mid-latitude regions have not yet been quantified in the field. Here we present vertical profiles of snow nitrate concentration and nitrogen isotopes (δ15N) collected during the Uintah Basin Winter Ozone Study?2014 (UBWOS 2014), along with observations of insoluble light-absorbing impurities, radiation equivalent mean ice grain radii, and snow density that determine snow optical properties. We use the snow optical properties and nitrate concentrations to calculate ultraviolet actinic flux in snow and the production of Nr from the photolysis of snow nitrate. The observed δ15N(NO3?) is used to constrain modeled fractional loss of snow nitrate in a snow chemistry column model, and thus the source of Nr to the overlying boundary layer. Snow-surface δ15N(NO3?) measurements range from ?5 to 10?‰ and suggest that the local nitrate burden in the Uintah Basin is dominated by primary emissions from anthropogenic sources, except during fresh snowfall events, where remote NOx sources from beyond the basin are dominant. Modeled daily averaged snow-sourced Nr fluxes range from 5.6 to 71??×??107?molec?cm?2?s?1 over the course of the field campaign, with a maximum noontime value of 3.1??×??109?molec?cm?2?s?1. The top-down emission estimate of primary, anthropogenic NOx in Uintah and Duchesne counties is at least 300 times higher than the estimated snow NOx emissions presented in this study. Our results suggest that snow-sourced reactive nitrogen fluxes are minor contributors to the Nr boundary layer budget in the highly polluted Uintah Basin boundary layer during winter?2014.
机译:来自石油和天然气提取活动的反应性氮(NRα= -On'On,NO 2,HONO)和挥发性有机碳排放在冬季地面臭氧的主要作用中起主要作用高达140?PPB在东部的UINTAH盆地犹他州。由于积雪对地面上的稳定性和深度的影响和表面的紫外线通量的稳定性和深度的影响,因此才会发生这种事件。在极地和中纬度的雪中观察到从硝酸的光解的反应性氮的再循环,但中纬度地区的雪源反应性氮气通量尚未在该领域量化。在这里,我们在Uintah盆地冬季臭氧研究期间呈现垂直的雪硝酸盐浓度和氮同位素(Δ15n)(Ubwos 2014),以及不溶性光吸收杂质的观察,辐射当量平均冰颗粒半径,以及雪密度确定雪光学性质。我们使用雪光学性质和硝酸盐浓度来计算雪中的紫外线助焊剂,从硝酸滴光的光解中产生Nr的生产。观察到的Δ15N(NO 3?)用于在雪化学柱模型中限制雪硝酸盐的建模分数损失,从而使NR到覆盖边界层的源极。雪表面Δ15n(no3?)测量范围从?5到10?‰并表明UINTAH盆地的局部硝酸盐负担由人为来源的主要排放主导,除了在新鲜的降雪活动中,远离偏远的NOx来源盆地是占主导地位的。日常平均的雪源NR助焊剂范围从5.6到71 ??×107?分子?2?2?s?1在现场运动过程中,最大的时间值为3.1 ??×109 ?分子?cm?2?s?1。 Uintah和Duchesne县中初级,人为NOx的自上而下排放估计比本研究中展示的估计雪NOx排放量高至少300倍。我们的研究结果表明,冬季冬季污染的UINTAH盆地边界层NR边界层预算的小贡献者是2014年高度污染的UINTAH盆地边界层的小贡献。
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