#smallhours

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Darkened Room, Door Crack, Light Bleed. #electriclight #darkness #light #shadow #smallhours #opendoor #farnham #surrey #lookingdown (at Farnham) https://www.instagram.com/p/Bp4iN_dg1Si/?utm_source=ig_tumblr_share&igshid=1r05yoj85lux9

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Reminder: March 2019 Book Discussions: -Small Hours, by Jennifer Kitses - Wed., March 27, 2019, 10:30 AM -The Girl on the Train, by Paula Hawkins - Thurs., March 28, 2019, 6 PM -Boulevard of Dreams, by Constance Rosenblum - Sat., March 30, 2019, 1 PM

An experiment is a question which science poses to Nature, and a measurement is the recording of Nature's answer. — Max Planck 'The Meaning and Limits of Exact Science', Science (30 Sep 1949), 110, No. 2857, 325. Advance reprinting of a chapter from book Max Planck, Scientific Autobiography (1949),

  Gravitational tidal waves are a fluctuational ellipsis (material) of aetheric levels; particulate that scatters in wavelengths outward from their source at the speed of light. "They were proposed by Henri Poincaré in 1905 and subsequently predicted in 1916; by Albert Einstein on the basis of his general theory of relativity."

| OUTLINE | Hilary Keller | OBSERVING THE NITROGEN CYCLE | KEYWORDS | Nitrogen-fixing, decomposition, nitrification and denitrification.   Iron is most often found in the Fe(II) state. Mainly iron exist in 2 oxidation states; Fe(II) is known as ferrous while Fe(III) is known as ferric. That said, Iron ("Fe2+"=, ferrous ion) is a necessary trace element used by every single living organism.   "Work previously by Garrels and Thompson, who investigated the anaerobic oxidation rate suggested the rate-controlling mechanism corresponds to the absorption of ferric and ferrous iron on the pyrite surface. The rate oxidation-reduction potentiality of the solution that is independent of the total iron concentration is within a range that could be examined. Their conclusions are valid; however, neither conclusion is correct."    Indirect oxidation occurs by oxidation of pyrite by ferric ions, the ferric ions being generated by bacterial oxidation of ferrous ions in solution. The bacteria oxidize iron in solution to 70 or 80% ferric. This finding is significant to the fertilizer/soil ammonia Ph equilibrium.    "Direct oxidation implies the oxidation of pyrite." Fourteen mols of ferric ion. Undetermined consummation of oxygen to oxidize one mole of pyrite. Rates are thereby calculated in terms of micromoles of pyrite oxidization per/hour = (singular) gram of pyrite.