Aerosol and precipitation chemistry measurements in a remote site in Central Amazonia: the role of biogenic contribution

Abstract

Abstract. In this analysis a 3.5 years data set of aerosol and precipitation chemistry, obtained in a remote site in Central Amazonia (Balbina, (1 • 55 S, 59 • 29 W, 174 m a.s.l.), about 200 km north of Manaus) is discussed. Aerosols were sampled using stacked filter units (SFU), which separate fine (d < 2.5 µm) and coarse mode (2.5 µm < d < 10.0 µm) aerosol particles. Filters were analyzed for particulate mass (PM), Equivalent Black Carbon (BC E ) and elemental composition by Particle Induced X-Ray Emission (PIXE). Rainwater samples were collected using a wet-only sampler and samples were analyzed for pH and ionic composition, which was determined using ionic chromatography (IC). Natural sources dominated the aerosol mass during the wet season, when it was predominantly of natural biogenic origin mostly in the coarse mode, which comprised up to 81 % of PM 10 . Biogenic aerosol from both primary emissions and secondary organic aerosol dominates the fine mode in the wet season, with very low concentrations (average 2.2 µg m −3 ). Soil dust was responsible for a minor fraction of the aerosol mass (less than 17 %). Sudden increases in the concentration of elements as Al, Ti and Fe were also observed, both in fine and coarse mode (mostly during the April-may months), which we attribute to episodes of Saharan dust transport. During the dry periods, a significant contribution to the fine aerosols loading was observed, due to the large-scale transport of smoke from biomass burning in other portions of the Amazon basin. This contribution is associated with the enhancement of the concentration of S, K, Zn and BC E . Chlorine, which is commonly associated to sea salt and also to biomass burning emissions, presented higher concentration not only during the dry season but also for the April-June months, due to the establishment of more favorable meteorological conditions to the transport of Atlantic air masses to Central Amazonia. The chemical composition of rainwater was similar to those ones observed in other remote sites in tropical forests. The volume-weighted mean (VWM) pH was 4.90. The most important contribution to acidity was from weak organic acids. The organic acidity was predominantly associated with the presence of acetic acid instead of formic acid, which is more often observed in pristine tropical areas. Wet deposition rates for major species did not differ significantly between dry and wet season, except for NH + 4 , citrate and acetate, which had smaller deposition rates during dry season. While biomass burning emissions were clearly identified in the aerosol component, it did not present a clear signature in rainwater. The biogenic component and the long-range transport of sea salt were observed both in aerosols and rainwater composition. The results shown here indicate that in Central Amazonia it is still possible to observe quite pristine atmospheric conditions, relatively free of anthropogenic influences.

Soluble iron nutrients in Saharan dust over the central Amazon rainforest

“…Potassium in submicron aerosols also has a source from vegetation fires and is frequently used as a tracer for biomass burning aerosols (Andreae et al, 1983;Martin et al, 2010;Zhang et al, 2015). Soil-dust-related elements are typically present at the highest concentrations during the early wet-to-dry season transition (May), as has been shown in previous studies (Pauliquevis et al, 2012;Andreae et al, 2015). This is mainly driven by large-scale atmospheric circulation patterns that favor the transport of dust plumes in a trans-Atlantic airflow from the Sahara and Sahel regions and towards the Amazon Basin (Artaxo and Maenhaut, 1990;Artaxo et al, 1994;Formenti et al, 2001;Graham et al, 2003;Martin et al, 2010;Baars et al, 2011;Ben-Ami et al, 2010).…”

“…Andreae et al (1990), and later Pauliquevis et al (2012), observed a positive correlation between Na and Cl in rainwater in the Manaus region, a strong indication of sea salt reaching central Amazonia. Pauliquevis et al (2012) also observed increases in the concentration of total Fe with values reaching 60 ng m −3 in the fine mode mostly during February to April in the Amazon Basin, with a seasonal average of 36 ng m −3 . They attributed this to episodes of Saharan dust transport.…”

Diel and seasonal changes of biogenic volatile organic compounds within and above an Amazonian rainforest

“…During the wet season, it reaches values of 350 mm month −1 where solar radiation is lower due to higher cloud cover (Araujo et al, 2002;Pauliquevis et al, 2012). We measured during two different campaigns, which represent the two extremes of seasonality (see information about seasonality analysis in Sect. )…”

Natural or anthropogenic? On the origin of atmospheric sulfate deposition in the Andes of southeastern Ecuador

“…The opposite was found by Eklund et al (1997) and Gordon et al (1994) in Costa Rica and Puerto Rico, respectively, where no significant pollution footprints where found in the samples of the two studied tropical mountain forests. The same was noticed by Pauliquevis et al (2012) in the central Amazon of Brazil, where high sulfate loads in rainwater likely stem from the oxidation of sulfur compounds from the Atlantic Ocean.…”