首页> 外文OA文献 >Estimation of the molecular hydrogen soil uptake and traffic emissions at a suburban site near Paris through hydrogen, carbon monoxide, and radon-222 semicontinuous measurements.
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Estimation of the molecular hydrogen soil uptake and traffic emissions at a suburban site near Paris through hydrogen, carbon monoxide, and radon-222 semicontinuous measurements.

机译:通过氢,一氧化碳和radon-222半连续测量,估算巴黎附近郊区的分子氢土壤吸收和交通排放。

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摘要

Since June 2006, simultaneous semicontinuous measurements of tropospheric molecular hydrogen (H2), carbon monoxide (CO), and radon-222 (222Rn) have been performed at Gif-sur-Yvette (Paris region), a suburban atmospheric measurement site in France. Molecular hydrogen mixing ratios range from 500 to 1000 ppb, CO mixing ratios vary from 100 to 1400 ppb, and 222Rn concentrations fluctuate from 0 to 20 Bq m−3. The H2 seasonal cycle shows the expected pattern for the Northern Hemisphere with a maximum in spring and a minimum in autumn. We inferred a mean baseline value of 533 ppb with a peak-to-peak amplitude of 30 ppb. Carbon monoxide exhibits a seasonal cycle with a maximum in winter and a minimum in summer. The mean baseline value reaches 132 ppb with a peak-to-peak amplitude of 40 ppb. Radon-222 presents weak seasonal variations with a maximum in autumn/winter and a minimum in spring/summer. The diurnal cycles of H2 and CO are dominated by emissions from nearby traffic with two peaks during morning and evening rush hours. The typical H2/CO emission ratio from traffic is found to be 0.47 ± 0.08 on a molar basis (ppb/ppb). The radon tracer method is applied to nighttime H2 observations to estimate the H2 soil uptake of the nocturnal catchment area of our sampling site. The influences from nocturnal local anthropogenic combustion sources are estimated by parallel measurements of CO at 0.14 × 10−5 g(H2) m−2 h−1. The mean inferred dry deposition velocity is 0.024 ± 0.013 cm s−1 with a seasonal amplitude of 40% at Gif-sur-Yvette. © 2009, American Geophysical Union
机译:自2006年6月以来,在法国郊区的伊夫特河畔吉夫(Gif-sur-Yvette)(巴黎地区)进行了对流层分子氢(H2),一氧化碳(CO)和ra 222(222Rn)的同步半连续测量。分子氢的混合比为500至1000 ppb,CO的混合比为100至1400 ppb,222Rn的浓度在0至20 Bq m-3之间波动。 H2季节周期显示北半球的预期模式,春季最大,秋季最小。我们推断平均基线值为533 ppb,峰峰幅度为30 ppb。一氧化碳表现出季节性循环,冬季最大,夏季最小。平均基线值达到132 ppb,峰峰值幅度为40 ppb。 Radon-222的季节变化较弱,秋季/冬季最大,春季/夏季最小。 H2和CO的昼夜周期主要由附近交通的排放量决定,早上和晚上高峰时间有两个峰值。发现交通产生的典型H2 / CO排放比为0.47±0.08(摩尔)(ppb / ppb)。 night示踪法应用于夜间H2观测,以估算我们采样地点夜间集水区对H2土壤的吸收。夜间局部人为燃烧源的影响是通过在0.14×10-5 g(H2)m-2 h-1处平行测量CO来估算的。在伊夫特河畔吉夫,平均推断干沉降速度为0.024±0.013 cm s-1,季节性幅度为40%。 ©2009,美国地球物理联合会

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