. The depths of the ocean; a general account of the modern science of oceanography based largely on the scientific researches of the Norwegian steamer Michael Sars in the North Atlantic. Oceanography. 256 three DEPTHS OF THE OCEAN chap. found that the diatoms had consumed Brennecke's figures for oxygen in the Atlantic. c/DS hours it was cubic centi- metres of the oxygen in the dark bottle (the amount of carbonic acid being slightly in- creased), whereas in the uncovered bottle thequantity of oxygen had increased by (the amount of carbonic acid being decreased). Brennecke has co
. The depths of the ocean; a general account of the modern science of oceanography based largely on the scientific researches of the Norwegian steamer Michael Sars in the North Atlantic. Oceanography. 256 three DEPTHS OF THE OCEAN chap. found that the diatoms had consumed Brennecke's figures for oxygen in the Atlantic. c/DS hours it was cubic centi- metres of the oxygen in the dark bottle (the amount of carbonic acid being slightly in- creased), whereas in the uncovered bottle thequantity of oxygen had increased by (the amount of carbonic acid being decreased). Brennecke has compared the results of a num- ber of oxygen-de- terminations from the Atlantic Ocean, and in Figs. 173 and 174 his two sec- tions showing the vertical distribu- tion of oxygen in the Atlantic (from the surface to a depth of 1500 metres) between lat. 6o° N. and 50° S. are reproduced. The first section shows the quan- tity in cubic centi- metres per litre. A little north and south of the equa- tor the value is only 1-2 per litre in the water between 200 metres and 600 or 700 metres ; on the equator,. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Murray, John, Sir, 1841-1914; Hjort, Johan, 1869-. London Macmillan
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Keywords: ., bookcentury1900, bookdecade1910, bookpublisherlondo, bookyear1912
