Abstract :
From March to June 1996, eight rain events were sampled sequentially on time and volume basis in Uji, Kyoto, Japan. pH was measured by a pH meter. The concentrations (μmol l−1) of chloride ion (Cl−), nitrate ion (NO3−), sulfate ion (SO42−), sodium ion (Na+), ammonium ion (NH4+), potassium ion (K+), calcium ion (Ca2+) and magnesium ion (Mg2+) were measured by ion chromatography. It is found that Cl−, NO3−, SO42−, Na+, NH4+, K+, Ca2+ and Mg2+ concentrations in sequential cumulative rainwater decreased with rain duration. However, hydrogen ion (H+) concentration (derived from pH value) showed approximately an increasing trend with rain duration. The factors influencing H+ concentration as well as the H+ concentration varying pattern for sequential cumulative rainwater were discussed.
Keywords :
Acid factors , Alkali factors , Rainwater chemistry , Ionic balance , Weak acids