...
首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Measurements of nitric oxide and ammonia soil fluxes from a wet savanna ecosystem site in West Africa during the DACCIWA field campaign
【24h】

Measurements of nitric oxide and ammonia soil fluxes from a wet savanna ecosystem site in West Africa during the DACCIWA field campaign

机译:在DACCIWA野外活动期间,西非湿大草原生态系统网站测量一氧化氮和氨水量

获取原文
   

获取外文期刊封面封底 >>

       

摘要

Biogenic fluxes from soil at a local and regional scale are crucial to study air pollution and climate. Here we present field measurements of soil fluxes of nitric oxide (NO) and ammonia (NH3) observed over four different land cover types, i.e. bare soil, grassland, maize field, and forest, at an inland rural site in Benin, West Africa, during the DACCIWA field campaign in June and July?2016. At the regional scale, urbanization and a massive growth in population in West Africa have been causing a strong increase in anthropogenic emissions. Anthropogenic pollutants are transported inland and northward from the megacities located on the coast, where the reaction with biogenic emissions may lead to enhanced ozone production outside urban areas, as well as secondary organic aerosol formation, with detrimental effects on humans, animals, natural vegetation, and crops. We observe NO fluxes up to 48.05ngNm?2s?1. NO fluxes averaged over all land cover types are 4.79±5.59ngNm?2s?1, and maximum soil emissions of NO are recorded over bare soil. NH3 is dominated by deposition for all land cover types. NH3 fluxes range between ?6.59 and 4.96ngNm?2s?1. NH3 fluxes averaged over all land cover types are -0.91±1.27ngNm?2s?1, and maximum NH3 deposition is measured over bare soil. The observations show high spatial variability even for the same soil type, same day, and same meteorological conditions. We compare point daytime average measurements of NO emissions recorded during the field campaign with those simulated by GEOS-Chem (Goddard Earth Observing System Chemistry Model) for the same site and find good agreement. In an attempt to quantify NO emissions at the regional and national scale, we also provide a tentative estimate of total NO emissions for the entire country of Benin for the month of July using two distinct methods: upscaling point measurements and using the GEOS-Chem model. The two methods give similar results: 1.17±0.6 and 1.44GgNmonth?1, respectively. Total NH3 deposition estimated by upscaling point measurements for the month of July is 0.21GgNmonth?1.
机译:来自地方和区域规模的土壤的生物助条是研究空气污染和气候的至关重要。在这里,我们存在在四种不同的土地覆盖类型,即裸土壤,草原,玉米领域,西非的内陆农村遗址观察一氧化氮(NO)和氨(NH3)的现场测量。在6月和7月的Dacciwa Field运动期间?2016年。在区域规模,城市化和西非人口大规模增长一直导致人为排放的强劲增加。人为污染物被运输内陆,从位于海岸的巨型活动,与生物发射的反应可能导致城市地区以外的臭氧生产,以及次级有机气溶胶形成,对人类,动物,天然植被的不利影响,和庄稼。我们观察到没有48.05ngnm的势次?2s?1。在所有陆地覆盖类型上平均不均匀的助熔剂为4.79±5.59ng?2s?1,并且在裸土壤中记录否的最大土壤排放。 NH3以所有土地覆盖类型的沉积为主。 NH3助焊剂之间的范围?6.59和4.96ng?2s?1。 NH3在所有陆地覆盖类型上平均的助熔剂为-0.91±1.27ngn?2s?1,并且在裸土壤中测量最大NH3沉积。即使对于相同的土壤类型,同一天和相同的气象条件,观察结果也表现出高空间变异性。我们比较现场活动期间没有记录的排放量的点白天平均测量与同一网站的Geos-Chem(戈达德地球观测系统化学模型)模拟的那些,并找到良好的一致性。试图在区域和全国范围内量化排放,我们还提供了7月份全国贝宁的整个国家排放量的初步估计:使用两种不同的方法:升级点测量和使用Geos-Chem模型。这两种方法提供了类似的结果:分别为1.17±0.6和1.44ggnmonth?1。通过7月份的Umpaling Point测量估计的总NH3沉积估计为0.21ggnmonth?1。
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号