Pa. Tanner et Ays. Wong, ATMOSPHERIC GASES, PARTICULATES AND RAINFALL CONCENTRATIONS DURING SUMMER RAIN EVENTS, International journal of environmental analytical chemistry, 67(1-4), 1997, pp. 185-202
Concentrations of the predominant ions and of hydrogen peroxide in rai
nwater were measured during two rain events in Hong Kong in August 199
5. The ambient nitrogen oxides, sulphur dioxide and ozone concentratio
ns, as well as respirable suspended particulates, were monitored throu
ghout the month, and the concentration and composition of total suspen
ded particulates were also measured before and after the events. Event
1 heralded the commencement of a typhoon. The concentrations of all a
nalytes, with the exception of hydrogen ion, decreased during event 1,
due to exhaustive washout of alkaline particulate matter. The pH reac
hed 3.8 at the end of the event, compared with 5.1 at the start. The s
horter, more intense event 2 followed a sharp build-up of atmospheric
pollutants and rainwater pH varied in a narrower range, between 3.4-3.
7. The concentrations of H+, SO42- and NO3- in rainwater were much hig
her than in event 1, and all analyte concentrations exhibited minima a
t maximum rainfall intensity. Contributions from in-cloud scavenging a
nd below-cloud gas scavenging to rainwater acidity were both identifie
d, and neutralization by suspended particulate matter also played an i
mportant role. The rainwater acidity is attributed to mainly local sou
rces in both events. Both events were characterized by tropical cyclon
es in the China Seas, which when approaching Hong Kong, lead to a stag
nation of local air pollutants. Strengthening winds at the time of eve
nt 1 provided more ventilation. Hydrogen peroxide concentrations in ra
inwater decreased rapidly during both events, and were higher in event
1 than in event 2 because SO2, and NOx levels were lower. Elevated co
ncentrations of nitrogen (II) oxide were found to occur during periods
of thunderstorm activity, in conjunction with low levels of ozone.