Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
CHAPTER 3 The Physical Science of the Environment Lecture by David Serrano, Broward College PERIODIC TABLE © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Atoms–basic unit of matter – Made of three particles • Protons – In central nucleus, has positive charge • Neutrons – In central nucleus, electrically neutral • Electrons – Surrounds nucleus, has negative charge © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Elements are made of one type of atom • Number of protons determine Characteristics and name • 92 naturally occurring elements • Represented by a symbol – H, hydrogen – C, carbon – O, oxygen – N, nitrogen © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Isotopes – Same number of protons, different number of neutrons • Carbon has 6 protons, may have 6, 7, or 8 neutrons • Different weights useful in science • Radioactive isotopes • Some unstable, decay at steady rate, emit radiation • Half-life: time it takes for half of the atom to decay © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Ions – Atom gained or lost an electron – Results in overall charge • Gained electron = negative charge • Lost electron = positive charge © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Molecules – Two or more atoms combined • Oxygen (O2), nitrogen (N2) • Compounds – Molecules made from more than one element • Carbon dioxide (CO2), water (H2O) © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Chemical bonds hold molecules together – Ionic bond • Strong bond • Electron transferred between atoms • Termed ionic compounds or salts © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Water–important to life – Polar molecule • Forms dipole bonds with other water molecules – Gives water unique properties, stability • An excellent solvent – Many biological functions use water as solvent. © 2013 Pearson Education, Inc. 3.1 Chemistry of the Environment • Water–important to life – Acids and bases • Water dissociates into H+ and OH– • Chemicals (acid/base) may shift amounts – Shift measured by pH scale • pH of solution affects biological functions © 2013 Pearson Education, Inc. Increasingly basic (lower H+ concentration) 14 1.0 M NaOH Increasingly acidic (greater H+ concentration) Neutral [H+] = [OH–] 13 Ammonia Household ammonia 12 11 Milk of magnesia 10 Baking soda 9 8 Seawater Human blood 7 Pure water Milk 6 5 4 3 2 1 Tomatoes Wine Vinegar, colas Lemon juice Stomach acid 0 pH scale © 2013 Pearson Education, Inc. Neutral [H+] = [OH–] Increasingly acidic (greater H+ concentration) 0 1 pH scale © 2013 Pearson Education, Inc. 2 3 4 5 6 7 Increasingly basic (lower H+ concentration) 8 9 10 11 12 13 14 3.2 The Organic Chemistry of Life • Organic molecules – Carbon atom covalently bonded to hydrogen and other atoms – Primary structural and function component of life – Range in size – Inorganic molecules not made of carbon and hydrogen © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Organic molecules–types – Hydrocarbons • Only made of carbon and hydrogen – Carbohydrates • Made of carbon, hydrogen, oxygen • Sugars, (CH2O)n, with n between 3 and 7 • Glucose (C6H12O6) the basic form of energy for most organisms • Sugars known as saccharides © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Organic molecules–types – Lipids • Long chains of carbon and hydrogen and a shorter region with one to several oxygen molecules – Fats and oils – Nonpolar – Lipids not water soluble – Important energy storage © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Macromolecules – Small organic molecule linked together • Polymers – Linked together in long chains • Polysaccharides – Polymers of simple sugars • Starch • Cellulose © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Macromolecules – Proteins • Polymers of amino acids • 20 amino acids–same base structure – Amino group (–NH2) – Carboxylic acid group (–COOH) • Proteins made of chains of 100 to 1,000+ amino acids © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Macromolecules – Proteins – Fold to particular shapes yielding function – Structural or functional – May act as catalysts • Termed enzymes • Almost all biological reactions use enzymes © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Nucleic acids – Polymers of nucleotides • 5-carbon sugar, phosphate group, and nitrogenous base – Deoxyribonucleic acid (DNA) • Hereditary material • Traits coded in sequence of bases – adenine (A), thymine (T), cytosine (C), and guanine (G) © 2013 Pearson Education, Inc. 3.2 The Organic Chemistry of Life • Nucleic acids – Ribonucleic acid (RNA) • Structure similar to DNA • Protein synthesis – Transcription • DNA code to RNA – Translation • RNA code to protein • Triplet sequences code for amino acids © 2013 Pearson Education, Inc. DNA Replication Transcription RNA Translation Protein © 2013 Pearson Education, Inc. 3.3 Energy and the Environment • Energy – Capacity to do work • Work – Force applied to an object over a distance – Potential energy • Stored energy – Kinetic energy • Energy in motion © 2013 Pearson Education, Inc. 3.3 Energy and the Environment • Laws of thermodynamics – First law • Energy can be neither created nor destroyed; can be transformed – Second law • Energy transformations increase disorder – Entropy – Energy often lost as heat © 2013 Pearson Education, Inc. 3.3 Energy and the Environment • Forms of energy • Four types important for ecosystems – Electromagnetic radiation • Energy moves as photons in waves • Electromagnetic spectrum–entire range of wavelengths – Gamma rays, X-rays, visible light, radiation, infrared, microwaves, radiowaves © 2013 Pearson Education, Inc. Energy sufficient to increase temperature Energy sufficient to activate electrons Visible Light 100 nm Infrared Rays 10 m © 2013 Pearson Education, Inc. Microwaves 1 mm 10 cm Radio Waves 10 m 1 km 100 km 3.3 Energy and the Environment • Forms of energy • Four types important for ecosystems – Heat • Kinetic energy of molecules • Temperature – Average kinetic energy © 2013 Pearson Education, Inc. 3.3 Energy and the Environment • Forms of energy • Four types important for ecosystems – Heat can move in four ways • • • • Conduction Convection Radiation Latent heat transfer © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.3 Energy and the Environment • Forms of energy – Chemical energy • Potential energy • Breaking and forming of chemical bonds – Photosynthesis assembles carbohydrates – Potential energy in glucose bonds – When needed, energy released by respiration © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.4 The Planet Earth in Context • Formation of solar system • Sun began forming 4.6 billion years ago – The gases and dust not consumed by sun became planets and other objects • Planet-like objects • Asteroids • Comets © 2013 Pearson Education, Inc. Pluto and Charon Neptune © 2013 Pearson Education, Inc. Uranus Saturn Jupiter Mars Earth Venus Mercury Sun 3.5 Earth's Structure • Earth's structure – Core–mixture of nickel and iron • Solid inner core • Liquid outer core • Currents in the liquid core produce magnetic field © 2013 Pearson Education, Inc. 3.5 Earth's Structure • Earth's structure – Mantle • Above core • 70% of Earth's volume • Rich in elements magnesium and silicon © 2013 Pearson Education, Inc. 3.5 Earth's Structure • Earth's structure – Crust • Thin surface layer of relatively light rock • < 1% of Earth's volume • Only part that directly interacts with living systems – Lithosphere • Crust and upper part of mantle that interacts with it © 2013 Pearson Education, Inc. Inner solid core Outer core Lower mantle Upper mantle Oceanic crust Continental crust Core radius: 3,480 km (2,160 mi) Mantle radius: 2,900 km (1,800 mi) Crust depth: 5–100 km (3–60 mi) © 2013 Pearson Education, Inc. 3.5 Earth's Structure – Tectonic plates meet at boundaries • Transform fault boundaries – Plates slide past – Sites of earthquakes – Divergent boundaries • Plates spread apart – Convergent boundaries • Plates come together © 2013 Pearson Education, Inc. Transforming boundary C A Oceanic crust Movement of oceanic plate Rising magma Diverging plate boundary Magma forms Ocean plate is subducted © 2013 Pearson Education, Inc. B 3.6 Earth's Atmosphere • Earth has gravity to hold atmosphere • Earth's unique atmosphere supports life – Composition of gases • • • • 78% nitrogen 21 % oxygen 0.039% carbon dioxide Water vapor © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc. 3.6 Earth's Atmosphere • Layers of atmosphere – Troposphere • Lowest layer • Life located here • Temperature drops with elevation – Stratosphere • 11–48 km • Temperature increases approaching ozone • Ozone layer located here – Protects life from ultraviolet radiation © 2013 Pearson Education, Inc. 3.6 Earth's Atmosphere • Layers of atmosphere – Mesosphere • Above stratosphere • Air temperature drops again (173 ºC) at 90 km – Thermosphere • • • • Extends out to space Above 150 km gas density so low no friction International Space Station orbits here Aurora occurs here © 2013 Pearson Education, Inc. 3.7 Earth's Energy Budget, Weather, and Climate • Weather and climate – Climate • Long-term atmospheric conditions – Temperature, humidity, average rainfall – Weather • Short-term variations local atmospheric conditions – Thunderstorms © 2013 Pearson Education, Inc. © 2013 Pearson Education, Inc.