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  2. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water is the medium of the oceans, the medium which carries all the substances and elements involved in the marine biogeochemical cycles. Water as found in nature almost always includes dissolved substances, so water has been described as the "universal solvent" for its ability to dissolve so many substances.

  3. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. [2] The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the environment. When it condenses, it releases energy and warms the environment.

  4. Gassman indole synthesis - Wikipedia

    en.wikipedia.org/wiki/Gassman_indole_synthesis

    The reaction mechanism of the Gassman indole synthesis is divided among three steps. The first step is the oxidation of the aniline 1 using tert-butyl hypochlorite (tBuOCl) to give the chloramine 2. The second step is the addition of the keto-thioether to give the sulfonium ion 3, and is typically done at low temperatures (−78 °C).

  5. Hydroformylation - Wikipedia

    en.wikipedia.org/wiki/Hydroformylation

    In organic chemistry, hydroformylation, also known as oxo synthesis or oxo process, is an industrial process for the production of aldehydes (R−CH=O) from alkenes (R 2 C=CR 2). [ 1 ] [ 2 ] This chemical reaction entails the net addition of a formyl group ( −CHO ) and a hydrogen atom to a carbon-carbon double bond .

  6. Electrosynthesis - Wikipedia

    en.wikipedia.org/wiki/Electrosynthesis

    It has been reported that formate can be formed by the electrochemical reduction of CO 2 (in the form of bicarbonate) at a lead cathode at pH 8.6: [24] HCO − 3 + H 2 O + 2e − → HCO − 2 + 2OH −. or CO 2 + H 2 O + 2e − → HCO − 2 + OH −. If the feed is CO 2 and oxygen is evolved at the anode, the total reaction is: CO 2 + OH − ...

  7. Deep water cycle - Wikipedia

    en.wikipedia.org/wiki/Deep_water_cycle

    Water carried into the mantle eventually returns to the surface in eruptions at mid-ocean ridges and hotspots. [8] This circulation of water into the mantle and back is known as the deep water cycle or the geologic water cycle. [9] [10] [11] [5] Estimates of the amount of water in the mantle range from 1 ⁄ 4 to 4 times the water in the ocean ...

  8. Beckmann rearrangement - Wikipedia

    en.wikipedia.org/wiki/Beckmann_rearrangement

    In the third step, an isomerization step protonates the nitrogen atom leading to the amide. The Beckmann rearrangement mechanism. The same computation with a hydroxonium ion and 6 molecules of water has the same result, but when the migrating substituent is a phenyl group, the mechanism favors the formation of an intermediate three-membered π ...

  9. Sonogashira coupling - Wikipedia

    en.wikipedia.org/wiki/Sonogashira_coupling

    The coupling of 2-iodoprop-2-en-1-ol with a wide range of acetylenes. [52] The preparation of alk-2-ynylbuta-1,3-dienes from the cross-coupling of a diiodide and phenylacetylene, as shown below. [53] Synthesis of an alk-2-ynylbuta-1,3-diene accomplished by Sonogashira coupling. [53]

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