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Chemical Relations of the Oil-Field Waters in San Joaquin Valley, California
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Excerpt from Chemical Relations of the Oil-Field Waters in San Joaquin Valley, California: Preliminary Report Introduction; Conclucdons and recommendations; Acknowledgments; Need for more analyses; Location of the oil fields; San Joaquin Valley; Geography and drainage; Geology; Underground water; Occurrence of water in the oil fields; General disttibution; Water sands; Texture; Freedom of circulation; Dry sands; Relation to the oil; Physical characteristics; Head or pressure; Temperature; Geologic conditions that influence the composition of water; General features; Origin of salt water in rocks; Relation of geologic structure to distribution of salt water in the oil fields; General association of salt water and petroleum; Distribution of water in the oil fields; Coalings field; Lost Hills field; Lost Hill field; McKittrick field; Midway-Sunset field; Kern River field; Analysis of water and interpretation of results; Mineral constituents in water; collection of samples; Chemical analysis; Determination of constituents; Statement of analysis; Reacting values; Properties of reaction; Source and statement of analyses in this report; Classification of the oil-field waters; Distribution and significance of the constituents; Alkalies (Sodium and potassium); Alkaline earths (calcium and magnesium); Sulphate; Chloride; Carbonate and bicarbonate; Sulphide; Iron and Aluminum; Silica About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
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