Chemical composition of precipitation during 1984-2002 at Pune, India [An article from: Atmospheric Environment]
Book Details
PublisherElsevier
ISBN / ASINB000RR1EJM
ISBN-13978B000RR1EJ9
AvailabilityAvailable for download now
MarketplaceUnited States 🇺🇸
Description
This digital document is a journal article from Atmospheric Environment, published by Elsevier in 2004. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
Since 1984, bulk precipitation samples have been collected at Pune, a tropical urban location in India, in the monsoon season. Data from these studies are used to analyze the long-term trends in the major chemical constituents of precipitation. Significantly increasing trends were observed for SO"4 and NO"3 which could be attributed to the rise in industrial and vehicular activities during this period. Also Ca, the chief neutralizing constituent, showed decreasing trend, mainly due to the rapid urbanization that reduced the availability of open land which is the major source for Ca. This has resulted in the overall decrease in trend of pH. However, the average pH value is still in the alkaline range due to the dominance of neutralizing potential of precipitation over the acidic potential.
Description:
Since 1984, bulk precipitation samples have been collected at Pune, a tropical urban location in India, in the monsoon season. Data from these studies are used to analyze the long-term trends in the major chemical constituents of precipitation. Significantly increasing trends were observed for SO"4 and NO"3 which could be attributed to the rise in industrial and vehicular activities during this period. Also Ca, the chief neutralizing constituent, showed decreasing trend, mainly due to the rapid urbanization that reduced the availability of open land which is the major source for Ca. This has resulted in the overall decrease in trend of pH. However, the average pH value is still in the alkaline range due to the dominance of neutralizing potential of precipitation over the acidic potential.
