Chemical components (Na
+, NH
4+, K
+, Mg
2+, Ca
2+, F
−, Cl
−, NO
2−, Br
−, NO
3−, PO
43−, SO
42−) of fresh rime and snow collected on the summit of
Mt. Kajigamori (ALT. 1400 m), Kochi, Shikoku Island in West Japan, where there is a watershed protection forest of Riv. Yoshinogawa during winter season of 2008–2014 y. was obtained with [Pb] and [Cd]. In both the rime and snow precipitated under similar back trajectories in a one day meteorological event, there was a strong positive correlation (
r2 = 0.9665, [Pb]/[Cd] = 35±1.9) in [Pb]
vs. [Cd] plots, indicating the same origin. The ratio was in agreement with the ratio of 37 for the emission in Shandong, China (37). In the case of these metals
vs. [nss-SO
42−] plots although there was a good positive correlation in snow, there was an incorrect correlation in the rime. In some rimes, an excess [nss-SO
42−] could be found more than [nss-SO
42−] calculated based on the proportionality in the snow at its [Pb], indicating the existence of different types of origin of nss-SO
42− species in the south Liaoning, China. In rime (2014–2012 y.) and snow (2014–2013 y), it was found that a good positive correlation (
r2 = 0.9038, 32±3) and (
r2 = 0.9173, 38±3) in [Pb]
vs. [Cd] plots, respectively, when back trajectories passed through around Liaoning-south Jilin area and around Bohai. In the case of these metals
vs. [nss-SO
42−] plots, there were two individual good positive correlations in only the rime. In order to treat the same manner as the one-day sampling, the excess [nss-SO
42−] estimated in rime was attributed to urban aerosol around northeast China. It was considered that the excess [nss-SO
42−]. When the back trajectories passed through around Korea, the ratio of [Pb]/[Cd] = 15±2 (
r2 = 0.9355) corresponded to that of 14 for the ratio collected in winter season at rural area of near Seoul, Korea.
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