page.
Chapter 2 Structure of the Water Molecule and the Nature of the Hydrogen Bond in Water
p10 Sketches of electron density
p11 Bjerrum tetrahedral model of water molecule. Van der Waals diameter 0.282nm, same as neon which has the same number of electrons. He says "isoelectronic". Neon is 1s22s22p. Interesting comments on the usefulness of this model.
p12 Rather technical discussion of modeling the water dimer, uses "coordination number" n which is not defined. But n=4->4.4 upon melting says that water contracts relative to ice. But n=12->11 upon melting says that argon expands, the more typical situation.
p13-14 More of a technical discussion of IR frequencies and modes of vibration for water molecule.
Chapter 3 Physical Properties of Liquid Water
p16-17 PVT diagrams
p17 The fact that the water-ice phase change energy (~80cal/gm) is only 15% of the water-steam phase change energy (540 cal/gm) "suggests that liquid water retains much of the order of the solid state and that this order is only destroyed at the boiling point." Look at this page carefully to make sure I have covered all this in hph.
p18 Table of liquid properties
p19 Isotopic composition
p20 Thermodynamic properties. Different temperature for the maxima of different properties.
p22 3.98°C for maximum density at 1 atmosphere.
p23 Graph of volume as a function of temperature
p25 Raman spectra of water vibrations
p26-29 Detailed measurement of properties.
p29-31 Bulk transport properties.
p31 Graph of viscosity. Near freezing point there is a minimum of viscosity vs pressure. Curious. Related to changing slipperiness of wet ice?
Chapter 4 Crystalline Water
p32 Antarctica contains 99.997% of the fresh water on the planet.
p33 Fig 4.1 Growth habits of ice crystals
p34 Fig 4.2 Conditions favoring snow
p35 Fig 4.3 Diagram of ice structure. Ice at 80°C and higher under high pressure.
p35-37 Ice forms
p39 Cathrates - balllike structures
Chapter 5 The Structure of Liquid Water
p41 Diffraction studies
p45 Pair correlation data
p46 Water molecule geometry from neutron diffraction.
p50 Discussion of some of the mysteries
p51-52 More about progress and remaining uncertainties
Chapter 6 Aqueous Solutions of 'Simple' Molecules
p53-55 Framework of solute-solute and solute-solvent contributions.
p60 Hydrophobic hydration
Chapter 7 Aqueous Solutions of Electrolytes
Chapter 8 Aqueous Solutions of Polar Molecules
p88 Polyhydroxyl compounds (PHCs) - biological applications
p105 Hydrophobic/Hydrophilic competition
Chapter 9 Chemical Reactions in Aqueous Solutions
p108 Solvent
p109 Self-ionization
p112 Ionization reactions
Chapter 10 Hydration and the Molecules of Life
p118 Brief introduction to water's role with the molecules of life
p119 Points main emphasis toward proteins
p120 List of questions
p132-133 Diagrams of water-DNA interactions
Chapter 11 Water in the Chemistry and Physics of Life
p142 Most of the history of life is in water. Life on land only 400My, and still will start life in an aqueous environment.
p142 Notes that the transition to land required major changes to maintain a correct water balance. Water management is a major issue for all of life.
p143 Brief discussion of water's role in photosynthesis and its path to ATP.
p144 The citric acid cycle, mitochondria and ATP. He fusses at educators for being sloppy about making clear the role of water in the reactions. The bottom paragraph on water balance for the body is interesting.Water turnover 2.5kg daily, 300 gm produced as product of metabolism,
p145 Details of a simplified glucose oxidation reaction to produce ATP and water. Then points to real in vivo process which involves many more water molecules.
p146 The reactions above are so finely balanced that substitution of D for H disrupts it! "Heavy water is thus toxic to all higher forms of life." Remarkable!
p146 Paragraph 2. Details of O2 required for making 300 gm of water. Diagram 11.1. Review carefully for hph. Quantitative overview of production of the 300 gm of water. Make diagram for hph with body outline.
p147 Numbers for plant conversion of CO2 into carbohydrates. Review carefully. Splitting of water in photosynthesis. Fine balance of N and CO2.
p147 List of the properties of water that have influenced the development of life.
p148 Two density anomalies for water:
- Non-monotonic temperature dependence, maximum density at 4°C.
- Decrease in density with freezing.
Seawater temperature for maximum density is below the freezing point, so the coldest seawater is the deepest.
p148 Data on stability of plants in terms of Young's modulus. Buoyancy of marine animals. Swim bladder operation.
p149 Discussion of blood pressure. Discussion of osmotic pressure's role in getting water to treetops.
p150 Discussion of pressure in xylem of plants - check this out more carefully. Makes some claims I can't justify.
p150 Plants up to about 74cm high can supply themselves with water by capillary action.
p150 Says 5nm effective tube size which would give maximum capillary height of 3.4km, but cohesive strength of water limits to about 280m, whichis still twice the height of any tree.
p150-151 Sea creatures must drink sea water and excrete salt to maintain correct osmotic pressure - special cells in gills.
p151 Points to the major problem of salinization and the need for study of salt tolerant plants - but not as thorough as Ball's treatment.
Chapter 12 'Unstable' Water
p152 Liquid water can exist from -41°C to about 280°C, and all the way down to 0K if vitrified.
p153 (Lowest temperature with undercooling)/(Equilibrium freezing point) ~0.80+/-0.05
p153 Diagram 12.1 Molar heat capacity vs temperature
p154-155 Gets beyond me, but some new ideas to consider. "Ice and undercooled water have dramatically different physical properties." Even more dramatic for ions such as H and Li+ in water vs ice. Table 12.1
p155 Free energy discussion
p156 Critical clusters in undercooled water. Table 12.2
p156-158 More detail on undercooled water - more than I can take in.
p159 Nucleation of ice by particulate matter.
p159 Most interesting example is that of the Lobelia telekii plant which grows on Mount Kenya where its temperature cycles daily between 10°C and -10°C . Something about its surface catalyzes the formation of ice crystals, which in forming help suppress the excessive undercooling of the plant's critical internal fluids. The catalyst, a kind of polysaccharide, has been isolated in vitro. Fig 12.4 shows data for this.
The discussions in the chapter relate to some interesting ideas, like the critical nature of drop formation in upper atmosphere, comparison to nucleation by particles which might relate to seeding clouds, nucleation points for crystal formation in undercooled water, but I couldn't get my head around all of it.
p161 Glassy water is possible, but if cooling is rapid, ice crystals will usually form. Discusses fast cooling experiments such as spraying aerosol water on cold copper plates.
p Discusses amorphous solid water
p Superheated water as pure droplets in immiscible oil to 552.7K - eventual boiling is explosive.
Chapter 13 Supersaturated and Solid Aqueous Solutions
p163 You can mix H and O gases and get a stable mixture, but if you add MnO2 they react explosively to form water.
p164-5 NaCl solutions increase concentration with cooling Fig 13.1, 13.2
p166-7 Sucrose-water solutions, Fig 13.3
p168-176 too detailed and specific for me to follow
p177-179 Implications for drying processes - the science of drying
p179- 186 Natural freezing and drought resistance and other implications for plants
Chapter 14 Water Availability, Usage and Quality
p187 Water availability. Says that earth's water resources are recycled 37 times annually. All precip would cover globe to 0.5m if uniform.
p188 70% of rainfall evaporates, 30% runoff - total amount recycled is only 0.003% of total freshwater
p188 Oceans eventually receive 90% of total runoff. Less than 3% of world's available freshwater is in streams and lakes.
p189 Underground water flow 33-40% of total runoff.
p189 80% of present supplies are drawn from surface sources, but 5 states including Arkansas get over half from groundwater.Eight others 25-50%.
p189 Semi-arid agricultural countries such as India (>90%) get majority of water from groundwater.
p189-190 India discussion
p191-193 Water management programs
p193-196 Water enhancement by climate modification
p196-202 Water quality and pollutants
p204-206 Pure water in medicine and industry
Chapter 15 Economics and Politics
p207-209 Economics of water consumption and list of measures for ensuring adequate supply.
p211 Future outlook
Chapter 16 Summary and Prognosis
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