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NJDEP - NJGS - First Annual Report of the Geological Survey of the ...

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7_(t) (2) _8)Silex, . 49.83 48.50 53.26Alumina_ . . 6.00 7.30 3.85Protoxid <strong>of</strong> iron, oi.53 22.80 24.15. Potash, . 10.12 11.50 5.36Soda, . 1.60Lime, . .50 or less. 1.73_,Iagnesia, . 1.83' . traoe. 1.10Water_ . . 9.80 7.90 10.12Loss, .89I100.00 99,50, 101.17The preceding statements and analytical results Show that<strong>the</strong> subject is by no means u plain one. To me it is one <strong>of</strong>deep interest, and I have taken every pains to inform myselfupon <strong>the</strong> practical agriculture <strong>of</strong> <strong>the</strong> district, and <strong>the</strong> influencewhich marl has exerted in bring'ing it to its present high Con.dition. With this knowledge my chemical examinations hav6been conducted, but <strong>the</strong>y are not yet in suc h a state <strong>of</strong> forwardnessas to be presented complete. Z. f_w approximate •results will be given.In <strong>the</strong>.following table <strong>the</strong> amounts <strong>of</strong> phosphoric acid" and,lime are given, in <strong>the</strong> fim_ and second columns. They areaverages from several analyses <strong>of</strong> specimens from diff&entpits. The third and fourth columns give <strong>the</strong> _nount <strong>of</strong> phosph.3teand carbonate <strong>of</strong> llme. The phosphate is calculatedfrom <strong>the</strong> phosphoric acid, and it probably exists in <strong>the</strong> marlin this form. The'only doubt <strong>of</strong> it arises from <strong>the</strong> fact thatphgsphate <strong>of</strong> iron is a common mineral in this Stratum. Carefulexaminations have not been made to determine <strong>the</strong> amount_<strong>of</strong> potash and soda ; enough, he,rover, has beeh done to showthat <strong>the</strong>y are always present, bud constituting fi'om five to tenper cent. <strong>of</strong> <strong>the</strong> whole.tNEW JERSEY GEOLOGICAL SURVEY

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