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“Hydrological Cycle and Residence Time”




Muhammad Fahad Ansari 12IEEM14
Water never leaves the Earth. It is constantly
being cycled through the atmosphere, ocean,
and land. This process, known as the water
cycle, is driven by energy from the sun. The
water cycle is crucial to the existence of life on
our planet.
The process of evaporation from plants is
called transpiration. (In other words, it’s like
plants sweating.)
   = Average length of time a
    substance spends


    (remains dissolved) in seawater
    Residence Time = Amount of element in the ocean .
   The rate at which the element is added to
   or removed from the ocean



   • Long r.t. = Unreactive
   ∀ Higher concentration in seawater



   • Short r.t. = Reactive
   ∀ Smaller concentration in seawater





    *  Residence time of water = Average length of time a water molecule

    remains in a particular reservoir -- e.g., ocean, atmosphere, etc.
   • Conservative constituents
   – Long residence times
   – Concentrations change slowly through time
   – Occur in constant proportions
   – Are the most abundant dissolved materials
   (major ions) in the ocean
   • Nonconservative constituents
   – Short residence times
   – Concentrations change quickly through time
   – Usually seasonal, biological, or short geological
   or chemical cycles
   – Gases in seawater

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Water cycle by Muhammad Fahad Ansari 12IEEM14

  • 1.
  • 2. “Hydrological Cycle and Residence Time” Muhammad Fahad Ansari 12IEEM14
  • 3. Water never leaves the Earth. It is constantly being cycled through the atmosphere, ocean, and land. This process, known as the water cycle, is driven by energy from the sun. The water cycle is crucial to the existence of life on our planet.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8. The process of evaporation from plants is called transpiration. (In other words, it’s like plants sweating.)
  • 9.
  • 10.
  • 11.
  • 12.
  • 13.
  • 14.
  • 15.
  • 16. = Average length of time a substance spends   (remains dissolved) in seawater Residence Time = Amount of element in the ocean .  The rate at which the element is added to  or removed from the ocean  • Long r.t. = Unreactive  ∀ Higher concentration in seawater  • Short r.t. = Reactive  ∀ Smaller concentration in seawater   * Residence time of water = Average length of time a water molecule remains in a particular reservoir -- e.g., ocean, atmosphere, etc.
  • 17.
  • 18. • Conservative constituents  – Long residence times  – Concentrations change slowly through time  – Occur in constant proportions  – Are the most abundant dissolved materials  (major ions) in the ocean  • Nonconservative constituents  – Short residence times  – Concentrations change quickly through time  – Usually seasonal, biological, or short geological  or chemical cycles  – Gases in seawater