Abstract
Rain event samples have been collected in Haifa, Israel, for nine hydrological years 1981 to 1990. Precipitation amount, pH, SO4 =, NO3 −, Cl−, NH4 +, Na+, K+, Ca++, Mg++ and alkalinity of rainwater samples were recorded. The sampling and analysis program was based on WMO recommendations for background networks. The sampling was performed manually, and the analysis was based on wet chemistry for ions and atomic absorptions for metals. Data of 187 rain samples showed that the average pH was 5.3±1.1∶ 26% of the rain events were below pH of 5.6 and 23% above pH of 7.0. Some simple chemical mass-balance considerations indicate that natural sources, sea salt and soil carbonates are the main contributors to rain chemistry. However, the presence of low pH events observed over the years suggests that the impact of anthropogenic emissions may overwhelm the buffering capacity of the alkaline aerosol.
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Mamane, Y., Gottlieb, J. Ten years of precipitation chemistry in Haifa, Israel. Water Air Soil Pollut 82, 549–558 (1995). https://doi.org/10.1007/BF00479411
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DOI: https://doi.org/10.1007/BF00479411