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  1. en.wikipedia.org › wiki › IndiaIndia - Wikipedia

    19 hours ago · India, officially the Republic of India ( ISO: Bhārat Gaṇarājya ), [21] is a country in South Asia. It is the seventh-largest country by area; the most populous country as of June 2023; [22] [23] and from the time of its independence in 1947, the world's most populous democracy.

  2. en.wikipedia.org › wiki › RenaissanceRenaissance - Wikipedia

    2 days ago · The architectural perspective and new systems of banking and accounting were introduced during the time. The Renaissance ( UK: / rəˈneɪsəns / rən-AY-sənss, US: / ˈrɛnəsɑːns / ⓘ REN-ə-sahnss) [1] [2] [a] is a period of history and a European cultural movement covering the 15th and 16th centuries. It marked the transition from the ...

  3. 5 days ago · This phenomenon of adding a catalyst and altering the rate of a reaction is known as catalysis. These catalysts remain unchanged chemically and in quantity that means that they are not used up quantitatively in the reaction and at the end of the reaction the same amount of catalyst is obtained as it was added. Let us consider an example

  4. 5 days ago · Innovation starts with insight and seeing challenges in a new way. Our breadth, depth, and scale, combined with our passion for business innovation, create powerful opportunities to help our clients stay ahead of change, deliver impact that matters, and transform disruption into lasting value.

  5. 4 days ago · Enzymes are. Organic catalysts, and decrease activation energy. This enzyme part contains the enzyme active site. apoenzyme. this molecule has a shape complementary to an enzyme's active site. substrate. this is a metallic ion that adjusts the shape of the active site. cofactor.

  6. en.wikipedia.org › wiki › OzoneOzone - Wikipedia

    3 days ago · Ozone ( / ˈoʊzoʊn /) (or trioxygen) is an inorganic molecule with the chemical formula O. 3. It is a pale blue gas with a distinctively pungent smell. It is an allotrope of oxygen that is much less stable than the diatomic allotrope O. 2, breaking down in the lower atmosphere to O.