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. 2016 Jul 20;6:29958. doi: 10.1038/srep29958

Table 1. Statistical parameters of stable isotopes (δ34Ssulfate and δ18Osulfate) and water-soluble ions in Beijing aerosols (SD represents standard deviation).

Species Spring Summer Autumn Winter
Range Average SD Range Average SD Range Average SD Range Average SD
Na+(μg/m3) 0.4–1.8 1.1 0.5 0.1–1.0 0.5 0.2 0.2–2.1 1.1 0.6 0.7–4.4 2.0 1.1
NH4+(μg/m3) 0.6–38.5 9.9 12.6 0.3–25.3 7.4 7.0 1.8–14.0 7.5 3.7 1.4–23.8 8.8 5.9
K+(μg/m3) 0.4–3.6 1.6 1.1 0.2–2.8 1.0 0.6 0.7–3.8 1.8 0.8 0.4–3.9 1.6 1.0
Mg2+(μg/m3) 0.2–1.9 0.8 0.5 0.1–1.6 0.8 0.4 0.3–1.5 0.9 0.4 0.1–1.2 0.5 0.3
Ca2+(μg/m3) 4.7–24.9 11.3 6.9 3.1–10.7 6.8 2.3 3.4–14.8 9.8 3.7 1.5–13.8 6.2 3.1
F(μg/m3) 0.1–2.1 0.7 0.6 0.0–0.5 0.3 0.2 0.3–1.3 0.6 0.3 0.1–1.0 0.5 0.3
Cl(μg/m3) 0.6–6.6 2.8 1.7 0.2–3.8 1.0 0.8 0.3–11.1 4.3 3.1 1.7–12.4 6.5 3.5
NO3(μg/m3) 2.3–89.8 30.7 32.7 2.5–54.6 19.6 13.9 9.3–43.4 25.7 12.2 2.7–46.3 16.3 12.6
SO42−(μg/m3) 3.7–87.7 25.2 31.3 2.4–85.7 22.1 18.5 4.3–34.7 16.6 8.2 4.0–60.7 17.4 13.5
δ34Ssulfate 4.5–9.2 6.4 1.5 3.4–7.0 5.0 0.9 5.0–9.4 6.8 1.3 7.1–11.3 8.6 0.9
δ18Osulfate 7.2–12.5 10.6 1.7 3.8–12.3 9.3 2.1 8.2–12.6 11.1 1.3 11.3–16.1 13.4 1.4