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Carbon Dioxide, Alkalinity and pH
3 Equations for CO 2 Speciation The equilibrium of gaseous and aqueous CO 2: CO 2(g) ↔ CO 2(aq) Subsequent hydration and dissociation reactions: CO 2(aq) + H 2O ↔ H 2CO 3 ↔ HCO 3-+ H+HCO 3-↔ CO3-2 + H+ Hint: when pH is between 7.5 and 8.5:
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THE GODDESS PELE - SOEST
www.soest.hawaii.eduTHE GODDESS PELE 173 'Thehousehold of Pele and her company, Those who bail, those who work the paddles, On the canoe were Ku and Lono.' It came to land, rested there, The island rose before them, Hi'iaka stepped ashore seeking
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Lecture 6: Weathering
www.soest.hawaii.edu1. Read Chapter 7! 2. Complete homework assignment #6! 1. What you should know from today:" 2. 1. Compare/contrast 3 types of weathering" 3. 2. Describe types of physical weathering" 4. 3. Describe the role of water in chemical weathering" 5. 4. List and define typical soil layers" 6. 5. Describe ways by which sediments are eroded"
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www.soest.hawaii.edu5 Mass Movement Can be either slow (creep) or fast (landslides, debris flows, etc.) As terrain becomes more mountainous, the hazard increases In developed nations impacts of mass-wasting or landslides can result in millions of dollars of damage with some deaths In less developed nations damage is more extensive because of population density, lack of stringent zoning laws, …
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