A Chapter in the History of Meteorites
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Traces Sulphur . .. .. .. .. .. .. .. .. .. .. .. . 0-503 Phosphoric acid . .. .. .. .. .. .. .. .. .. .. 0-597 Chlorine . .. .. .. .. .. .. .. .. .. .. .. 0-105 Silicic acid . .. .. .. .. .. .. .. .. .. .. .. . 39-661 Alumina . .. .. .. .. .. .. .. .. .. .. .. . 0-415 Chromium sesquioxide . .. .. .. .. .. .. .. 0-036 Iron protoxide . .. .. .. .. .. .. .. .. .. .. 12-234 Magnesia . .. .. .. .. .. .. .. .. .. .. .. . 14*776 Lime . .. .. .. .. .. .. .. .. .. .. . .. .. . 0-878 Potash and soda . ..... .. .. .. .. .. .. .. . 4-151 99-427 I have arranged according to the method adopted in foregoing analyses, the results which Bertolio obtained by treating a portion of the meteorite with acid and have further assumed that the nickel which he quotes in the form of oxide is however present as a con- stituent of the alloy. The metallic minerals broken up by acid chiefly consist of nickel-iron with perhaps a little troilite and schreibersite, and contain : Iron = 84-659; Nickel = 11-791; Sulphur = 2-058; Phosphorus = 1-063; Chlorine = 0-429 ; Copper, trace = 100-000 And their siliceous portions separated by acid have the following composition : Si0 2 A1 3 3 Cr 2 3 FeO NiO MgO CaO K 2 A.
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To quickly assess the difficulty of the text, read a short excerpt:
Traces Sulphur . .. .. .. .. .. .. .. .. .. .. .. . 0-503 Phosphoric acid . .. .. .. .. .. .. .. .. .. .. 0-597 Chlorine . .. .. .. .. .. .. .. .. .. .. .. 0-105 Silicic acid . .. .. .. .. .. .. .. .. .. .. .. . 39-661 Alumina . .. .. .. .. .. .. .. .. .. .. .. . 0-415 Chromium sesquioxide . .. .. .. .. .. .. .. 0-036 Iron protoxide . .. .. .. .. .. .. .. .. .. .. 12-234 Magnesia . .. .. .. .. .. .. .. .. .. .. .. . 14*776 Lime . .. .. .. .. .. .. .. .. .. .. . .. .. . 0-878 Potash and soda . ..... .. .. .. .. .. .. .. . 4-151 99-427 I have arranged according to the method adopted in foregoing analyses, the results which Bertolio obtained by treating a portion of the meteorite with acid and have further assumed that the nickel which he quotes in the form of oxide is however present as a con- stituent of the alloy. The metallic minerals broken up by acid chiefly consist of nickel-iron with perhaps a little troilite and schreibersite, and contain : Iron = 84-659; Nickel = 11-791; Sulphur = 2-058; Phosphorus = 1-063; Chlorine = 0-429 ; Copper, trace = 100-000 And their siliceous portions separated by acid have the following composition : Si0 2 A1 3 3 Cr 2 3 FeO NiO MgO CaO K 2 A.
What to read after A Chapter in the History of Meteorites?
You can find similar books in the "Read Also" column, or choose other free books by Walter Flight to read onlineMoreLess
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