منابع مشابه
The Determination of Total Carbon Dioxide in Water
Compared with oxygen the estimation of carbon dioxide in water presents much greater difficulties, and the methods published until now do not approach in sensitivity the Winkler method for dissolved oxygen by which the latter can be measured to 0-02 mg./l. in unpolluted and 0-2 mg./l. in polluted natural waters (Wheatland & Smith, 1955, Beadle, 1958). This is partly due to the high solubility a...
متن کاملCarbon dioxide sequestration in deep-sea basalt.
Developing a method for secure sequestration of anthropogenic carbon dioxide in geological formations is one of our most pressing global scientific problems. Injection into deep-sea basalt formations provides unique and significant advantages over other potential geological storage options, including (i) vast reservoir capacities sufficient to accommodate centuries-long U.S. production of fossi...
متن کاملQuality control of measurements of pH, carbon dioxide tension, and total carbon dioxide in plasma.
We have measured total carbon dioxide in plasma with a new carbon dioxide analyzer, and compared the results with total carbon dioxide data derived from measurements of carbon dioxide tension and pH. The results agree sufficiently well to demonstrate that the new instrument provides a simple, efficient procedure for monitoring the precision and accuracy of pH, carbon dioxide tension, or total c...
متن کاملModeling Caspian Sea water level oscillations under different scenarios of increasing atmospheric carbon dioxide concentrations
The rapid rise of Caspian Sea water level (about 2.25 meters since 1978) has caused much concern to all five surrounding countries, primarily because flooding has destroyed or damaged buildings and other engineering structures, roads, beaches and farm lands in the coastal zone. Given that climate, and more specifically climate change, is a primary factor influencing oscillations in Caspian Sea ...
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ژورنال
عنوان ژورنال: Journal of the Oceanographical Society of Japan
سال: 1965
ISSN: 0029-8131,2186-3113
DOI: 10.5928/kaiyou1942.21.54