Chemical Oceanography (by Ooki) Index

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• Chemical Oceanography (by Ooki) Index

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• The relationship of this page to SDGs
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    This page is a compilation of "Chemical Oceanography" from Hokkaido university's course. At this point, they are only available in Japanese, but we are opening up all the lecture videos and materials so that anyone in the world can learn. We would like to contribute to the achievement of "Goal 4: QUALITY EDUCATION."

    The United Nations has designated the decade starting in 2021 as the "Decade of Ocean Science," with the aim of contributing to SDGs. We will contribute to achieving SDG Goal 14 by promoting ocean science. In this page (chemical oceanography series), you will learn about the flow of nutrients that support the productivity (abundance) of the ocean, the flow of water that controls the flow of nutrients, and the flow of substances that are changed by biological production in the ocean. Experience the fascination of ocean science. We hope that you will contribute to "Goal 14: LIFE BELOW WATER."

    
    

• Index
  • All pages below are in Japanese.
    

  • - Water flow
    - Ocean salinity
    - Deep circulation and belt conveyor model
    - Antarctic bottom water and North Pacific deep water
    - Intermediate water of the North Pacific
    - Surface mixed layer
    - Spring bloom and surface mixed layer
    - Assignment: is the deep circulation permanent?

    - Organic matter in the ocean
    - Organic matter in the ocean (Introduction)
    - Size classification of organic matter in the ocean
    - Organic matter in particulate and dissolved forms
    - Sinking velocity of particles
    - Sinking of organic particles in the ocean (theory)
    - Marine snow and feeding of eel larvae
    - Sediment trap observations
    - Assignment: calculate the sedimentation rate of particles in the ocean
    - Measurement of organic carbon
    - Global distribution of dissolved organic carbon in the ocean
    - Persistent organic matter
    - Radiocarbon age method
    - 14C age of dissolved organic carbon
    - Composition of organic matter
    - Organic gases in the ocean (overview and supplementary)
    - Organosulfur gases and the CLAW hypothesis
    - The demise of the CLAW hypothesis and SOLAS research
    - Aerosol formation and growth, cloud condensation nuclei (supplementary)
    - Halocarbons in the ocean

    - Inorganic carbonate  in seawater
    - History of global climate change and carbon budget
    - Vertical distribution of carbon dioxide in the ocean
    - Reaction equation for equilibrium state of carbonic acid components and water in seawater
    - Calculate the concentration and composition ratio of carbonic acid components dissolved in water
    - Calculate pH of rainwater
    - Calculate pH of seawater
    - Formation of calcium carbonate particles and the saturation concentration of carbon dioxide
    - Alkalinity of the ocean and dissolution of calcium carbonate particles
    - Saturation depth of calcium carbonate particles in the ocean
    - Vertical cross section of alkalinity and total carbonic acid in the Pacific Ocean
    - XY plot of total carbonic acid and alkalinity

    - Oxygen in the ocean
    - Oxygen of the Earth
    - Oxygen in the ocean (overview)
    - Net oxygen consumption
    - Formula for calculating oxygen saturation concentration in seawater (Excel file)
    - Apparent oxygen utility (AOU) overview
    - Vertical distribution of apparent oxygen utility (AOU)
    - Global distribution of dissolved oxygen
    - Dissolved oxygen measurement (water sampling method for DO)

    - Nutrients in the ocean
    - What are the nutrients in the ocean?
    - Factors limiting the primary production of the ocean (nutrient supply to the surface layer)
    - Silicate consumption and biological production by diatoms
    - Diatom growth and silicic acid depletion (cartoon style explanation)
    - Global distribution of nutrients
    - Global distribution of nutrients (differences in silicic acid)
    - Nutrient components limiting primary production (characteristics by sea area)
    - Nitrate deficiency in the Pacific Arctic Ocean (Chukchi Sea)
    - Si uptake ratio under iron-limited and iron-unlimited conditions (Study Introduction)
    - Transfer of C, N, P, and O by primary production and organic decomposition
    - Calculation model of marine primary production (analysis assignment)
    - The mystery of the nitrogen/phosphorus ratio in the ocean (N/P = 16)
    - Ocean observations
    - XY plot of N and P for the entire ocean
    - XY plot of phosphoric acid (P) versus oxygen consumption (AOU)
    - Download climate data from World Ocean Atlas

    - Ocean sediments
    - Chemistry of ocean sediments (Introduction)
    - Ocean sediments and biological disturbance
    - Chemical reactions in sediments (Overview)
    - Energy balance of chemical reactions
    - Energy balance of respiration
    - Hydrogen sulfide generation by sulfate respiration in marine sediments
    - Half-reaction equation for respiration
    - Redox potential of the half-reaction of respiration
    - Nernst equation and redox potential (fundamentals of physical chemistry)
    - Chemical form of sulfur (S) in seawater (Pourbaix diagram)
    - Chemical form of iron (Fe) in seawater (Pourbaix diagram)
    - Introduction to ocean sediment observation

    - Radionuclides in the ocean
    - Sources of artificial radionuclides (Dr. Hyoe Takada, Fukushima University)

    - Polar ocean and sea ice (in preparation)

    - Book review of oceanography textbooks

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