Understanding Matter and Energy in Environmental Science

School
Western University**We aren't endorsed by this school
Course
GEOGRAPH 1022B
Subject
Biology
Date
Dec 12, 2024
Pages
6
Uploaded by MagistrateDugong6372
ESCI 1100 Lecture 4Introduction to Environmental Science September 19, 2023 Our Physical Environment Understanding how the environment works requires knowing:1.How matter (any material that has a mass and occupies space) and energy enter and cycle through the natural world2.How human activities affect these natural processesMatter and Energy Knowledge required to understand environmental processes/functions Physical, geological, chemical and biological Required basic concepts Atoms, isotopes (stable and radioactive), ions, molecules, compounds, solutions, bonding, pH, organic, inorganic Conservation of matter and energy Thermodynamic1st Law: conservation of Matter‘Energy can’t be created of destroyed, only transformed from one form to another’Ex. photosynthesis = solar changed to chemical energy 2nd Law: thermodynamics ‘Amount of energy available to do work in the universe is decreasing with time’Conversion of energy to not work is not 100% efficient Energy loss = heat = not ‘usable’ energyComposition (matter) of Environmental ‘Spheres’Elements are substances with specific properties that cannot be broken down into substances with other propertiesThe most abundant elements in the Earth are oxygen, hydrogen,silicon, nitrogen, and carbon3 to 8 major elementsProportions differAtoms and Elements are Chemical Building Blocks Atoms are the smallest units that still have all of the element’s chemical propertiesAtoms of each of the elements are made up of three particles:Protons, which are positively-charged and determine the element’s atomic number
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Neutrons, which have no chargeElectrons, which are negatively-chargedProtons and neutrons are found within the dense center of the atom called its NucleusThe element’s mass number is determined by its number of protons and neutronsElectrons orbit the nucleusAtoms of the same element always have the same number of protonsThe number of electrons can change, creating ionsWithin an element, the number of neutrons may also vary, creating atoms with different masses called isotopesIsotopes have special notations indicating their atomic mass.Some isotopes are radioactive, meaning they “decay” and change their identity by emitting subatomic particles and high-energy radiationIsotopes with this property are called radioisotopesRadioisotopes do the most damage when they enter the bodies of living organisms through eating or breathingAfter Fukushima, scientists began regularly testing food and water for radioisotopesAtoms Bond to Form Molecules and CompoundsMolecules are combinations of two or more atoms chemically bonded together, such as O2If the molecule is made of two or more different elements, it is classified as a compound, such as water (H2O) and carbon dioxide (CO2.Atoms form bonds due to the attraction they have for each other’s electronsAtoms and Elements are Chemical Building Blocks Covalent bonds form when electrons are shared between atomsIn some covalent compounds, such as water, one part of the molecule attracts electrons more strongly, creating oppositely-charged polesThe charged ends of water molecules attract each other, forming a weak interaction called hydrogen bondsIf the strength of attraction within a molecule is sufficiently unequal, an electron will be transferred from one atom to anotherThis creates oppositely charged ions, which attract each other, forming an ionic bondAtoms and molecules can also come together in mixtures, where they don’t react with each otherEvenly distributed mixtures are called solutions.Matter Is Composed of Organic and Inorganic CompoundsOrganic compounds are made of carbon atoms joined together with covalent bondsOne important class of organic compounds is the hydrocarbons, which only contain hydrogen and carbonFossil fuels and petroleum products like plastic are mostly made of hydrocarbons
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Macromolecules Are the Building Blocks of LifeOrganic compounds also include polymers, long chains of repeated moleculesPolymers and lipids are referred to as macromolecules, because they are so large.Proteins are polymers made of amino acids.They are found in skin, hair, muscles; as part of the immune system; and as enzymes that catalyze chemical reactionsNucleic acids, including deoxyribonucleic acid (DNA) and ribonucleic acid (RNA), carry the hereditary information for organismsContain the blueprints for producing all of the proteins in living organisms Nucleic acids are polymers made of molecules called nucleotidesRegions of D N A that encode for specific proteins are called genesCarbohydrates include simple and complex sugars, such as:Glucose, or blood sugarCellulose, a complex carbohydrate found in leaves, bark, stems, and rootsChitin, which is found in insect exoskeletonsLipids include a diverse group of molecules that do not dissolve in water:Fats and oils, which store energyWaxes, which are structuralSteroids, which are part of hormonesHydrogen Ions Determine AcidityIn any aqueous solution, a small number of water molecules split apart into hydrogen ions (H+) and hydroxide ions (OH)Pure water contains equal concentrations of these two ions and is considered neutralAcidic solutions have higher concentrations of hydrogen ionsBasic or alkaline solutions have higher concentrations of hydroxide ionsThe pH scale quantifies the acidity or alkalinity of a solutionPure water has a H+concentration of 10-7 and a pH of 7Acids have a pH of below 7Bases have a pH above 7The pH scale is logarithmic, meaning each step in the scale represents a 10- fold change in H+concentrationEnergy: An IntroductionEnergy is the capacity to change the position, composition, or temperature of matterWhen energy causes an object to move, it is a force that can accomplish workPotential energy is the energy of position or compositionFor example, river water held behind a dam contains potential energyKinetic energy is the energy of motionRiver water rushing through a dam and downstream contains kinetic energyEnergy is able to be converted back and forth between these two forms.Energy Comes in Different Forms Converting molecules with high-energy bonds (such as glucose) to molecules with low-energy bonds (such as carbon dioxide) releases kinetic energy.
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Energy Is Always Conserved, but It Changes in QualityLight Energy from the Sun Powers our PlanetOrganisms called autotrophs use the sun’s radiation directly to produce their own foodThey use a process called photosynthesis to transform molecules with low-energy bonds (water and carbon dioxide) into sugar molecules with high-energy bonds.Photosynthesis Converts Solar Energy to Chemical EnergyPhotosynthesis occurs within cell organelles called chloroplastsA pigment called chlorophyll uses solar energy to initiate a series of reactions called lightreactionsLight reactions split water molecules into hydrogen ions (H+), oxygen molecules (O2), and small high-energy molecules of ATP and NADPHThe Calvin cycle reactions link together carbon atoms to form sugarsExample: Photosynthesis Stores chemical energySolar energy converts H2O and CO2into carbohydrates and O2Causes increased weight (biomass gain)Example: green plants & algaeWater + carbon dioxide + sunlight glucose (sugar) + oxygen6H2O + 6CO2+ solar energy → C6H12O6+ 6O2Example: Respiration Releases chemical energyO2used to burn carbohydrates to produce energy & do workResults in decreased weight (biomass loss)Example: humansGlucose (sugar) + oxygen → water + carbon dioxide + energyC6H12O6+ 6O26H2O + 6CO2+ energyGeology: The Physical Basis for Environmental ScienceGeology is the study of Earth’s physical features, processes, and historyThese processes shape the landscape, lay the foundation of environmental systems, and provide resources like metals and fossil fuelsAt the Earth’s center is a dense core made of solid iron at the center surrounded by molten ironThe core is surrounded by a thick layer of less dense, elastic rock called the mantleEarth Consists of Layers The asthenosphere is an area of the upper mantle with especially soft rockThe lithosphere contains the uppermost mantle and the crustThe crust is a thin, brittle, low-density layer of rock that covers the entire surface
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Plate Tectonics Shapes Earth’s GeographyHeat from the Earth drives loops of convection currents that cycle material upward and downwardThis creates about 2–15cm of movement of large plates of lithosphere every year, called plate tectonicsThere Are Three Types of Plate Boundaries1.At divergent plate boundaries, plates move apart as magma rises to the surface and cools2.At transform plate boundaries, plates slip and grind alongside each other. This causes earthquakes3.When two plates come together, it is known as a convergent boundaryThe Rock Cycle Produces a Diversity of Rock Types A rock is any solid aggregation of mineralsA mineral is any naturally occurring solid element or inorganic compound with a crystal structure, distinct chemical composition, and physical propertiesOver time, rocks and their minerals are heated, melted, cooled, broken down, and reassembled in a process called the rock cycleMagma is made of liquid rock that has melted at high temperatures. When magma erupts and reaches the surface, it is called Lava Rock that forms when lava or magma cool is called igneous rockThe Rock Cycle Produces a Diversity of Rock TypesAs rock weathers from wind and water, particles called sediment come to rest downwind or downstreamSediment layers accumulate over time and are compacted as they are buriedMinerals may seep through them and cement particles together. This forms sedimentary rock, like sandstoneEarthquakes Result from Movement at Plate Boundaries and FaultsAn earthquake is a sudden release of energy at a tectonic plate boundaryEarthquakes may also occur in the interior of tectonic plates due to stretching and pulling from forces within the Earth.Volcanoes Arise from Rifts, Subduction Zones, or HotspotsA volcano is formed where molten rock, ash, or hot gas erupts through the Earth’s surfaceOften found in subduction zones of convergent plate boundariesJapan is the most volcanically active nation, with 100 active volcanoes or about 10% of the world’s totalLava may also be emitted at hotspots, localized areas where plugs of molten rock from the mantle erupt through the crust.The type of eruption released by volcanoes can be very different
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At Mount Kilauea, lava has been slowly flowing downhill since 1983Mount Saint Helens unleashed a huge amount of cinder and ash in a 1980 eruptionThe Roman city of Pompeii was buried in a pyroclastic flow of gas, ash, and rock that erupted from Mount Vesuvius in A.D.79.There was a 0.4–0.7° Celsius decrease in global temperatures following the eruption of Mount Tambora in 1815Landslides Are a Form of Mass WastingLandslides occur when large amounts of rock or soil collapse and flow downhillThe downward gravitational movement that causes this is called mass wastingMost commonly affects unstable hillsidesTsunamis Can Follow Earthquakes, Volcanoes, or LandslidesEarthquakes, volcanic eruptions, and large coastal landslides can all displace huge volumes of ocean water instantly, triggering a tsunamiThe 2011 tsunami that hit northeastern Japan was triggered by an earthquakeWe Can Worsen or Lessen the Impacts of Natural HazardsEarthquakes, tsunamis, and volcanoes are referred to as “natural hazards,” but our decisions can worsen their impactsLiving in areas prone to hazards, such as floodplainsDamming or diking riversClearcutting forests on slopes, inducing mass wastingHuman-induced climate changeAltering these decisions, as well as implementing better engineering technology, can help to minimize our risk
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