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Chapter 5 Topics Systems concepts Ecosystems Matter and energy Spatial patterns Services Biogeochemical cycles Water Carbon Nitrogen Phosphorus Human impacts
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Why “systems”? Our planet consists of innumerable parts connected by myriad processes into a vast number of complex networks Systems approaches allow us to investigate and understand these parts, processes, and networks in both focused and comprehensive ways
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Systems fundamentals System = a network of relationships among parts, elements, or components that interact with and influence one another and exchange energy, matter, or information When studying systems, scientists identify an arbitrary “boundary” that defines what’s “inside” the system and what’s “outside” the system Because no system is truly isolated from its surroundings, we must therefore consider “inputs to” and “outputs from” the system being studied
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Feedback loops Feedback loop = a circular process in which a system’s output serves as input to that same system Depending on the system response, the feedback loop is called either “positive” or “negative” Positive and negative feedback loops do not mean “good” and “bad”
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Positive feedback loop Positive feedback loop = the system response is amplified (unidirectional), driving the system toward an extreme condition Rare in nature, but common in systems altered by human actions
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Negative feedback loop Negative feedback loop = the system response is dampened (bidirectional), driving the system toward a more-or-less stable condition Most systems in nature operate in this way
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Other systems concepts Dynamic equilibrium = system processes move in opposing directions balancing their effects Homeostasis = systems seek to maintain constant (stable) internal conditions Emergent properties = system characteristics that are not evident in the components alone
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Earth’s systems – a reminder The framework of Earth’s four systems helps make complexity comprehensible Lithosphere = rock Atmosphere = air Hydrosphere = water Biosphere = life The boundaries overlap, so the systems interact
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Tools for studying systems - models A scientific model = a simplified representation of a complex natural process that helps us understand the process and make predictions Researchers gather data Form a hypothesis about relationships The model predict how the system will behave New data refine and increase the model’s accuracy
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Other tools Remote sensing allows a whole-landscape perspective – especially important for studying climate systems Geographic information system (GIS) = used to analyze the spatial arrangement of landscape elements
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Applying systems concepts Solving environmental problems requires considering all of the parts and processes in the system of interest The Gulf of Mexico’s “dead zone”, a region of water so depleted of oxygen (hypoxia) that marine organisms are killed or driven away
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Eutrophication – excess nutrients Nutrients (nitrogen and phosphorous) are added to the Mississippi River from Fertilizers and manure from Midwestern farms Sewage treatment plants, run-off, and emissions Nutrient over-enrichment causes Phytoplankton to grow rapidly and die, then… Bacteria eat dead phytoplankton and other wastes Explosions of bacteria deplete oxygen, causing… Fish and other aquatic organisms to suffocate
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Eutrophication yields hypoxia
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Ecosystems Ecosystem = all organisms and nonliving conditions that exist and interact at a given place and time Parts and processes… Living organisms (biotic factors) are tightly intertwined with chemical and physical conditions (abiotic factors) Through interactions and feedback loops Inputs and outputs… Energy flows through ecosystems, arriving as solar radiation and leaving as heat Matter is recycled within ecosystem, through food-web relationships and decomposition
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Energy and matter
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Energy becomes biomass Productivity = rate at which biomass is generated Primary production = conversion of solar energy to chemical energy in sugars by autotrophs Gross primary production (GPP) = the total amount of energy assimilated by autotrophs Net primary production (NPP) = the energy converted by autotrophs into biomass (available for consumption by heterotrophs) Secondary production = biomass generated by heterotrophs from consuming autotrophs
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NPP by ecosystem
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Global distribution of NPP
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Ecosystems interact spatially The term “ecosystem” is most often applied to self- contained systems of moderate geographic extent Adjacent ecosystems, such as prairies and forests, may share components and interact along their boundaries These transitional zones between ecosystems are called ecotones
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Landscape ecology Landscape ecology = studies how landscape structure affects the abundance, distribution, and interaction of organisms The landscape is divided into patches whose size depends on the relationships being studied Patches can take on complex patterns, called mosaics, leading to the development of metapopulations, subpopulations in which most members remain within a patch but others move among patches Widely spaced patches can lead to speciation or endanger an organism’s survival
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Ecotones, patches, and mosaics
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Ecosystems provide vital services Humans depend on healthy, functioning ecosystems They provide goods & services we need to survive Ecosystem services = economically beneficial services provided by the planet’s natural systems Soil formation, water and air purification, pollination Breakdown of some pollutants and waste Quality of life issues (inspiration, spiritual renewal) Nutrient cycling
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Ecosystem goods and services
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Nutrients Nutrients = elements and compounds required for survival that are consumed by organisms Macronutrients = required in larger amounts Micronutrients = nutrients needed in smaller amounts Nitrogen and phosphorus are the primary nutrients needed for plant and algal growth Phosphorous in a “limiting nutrient” for freshwater Nitrogen and iron are the “limiting nutrients” for saltwater
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Nutrient cycles Because of the their importance for plant growth, the cycling of carbon, nitrogen, and phosphorous are of special interest for ecosystems These are known as biogeochemical cycles and are characterized by their Pools (reservoirs) where nutrients reside for varying amounts of time (the residence time) Flux = the rate at which materials move between pools which can change over time
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Nutrient sources and sinks Pools function as sources and sinks for nutrients depending on relative rates of in-flux and out-flux, yielding different residence times
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The hydrologic (water) cycle Process (flux) terms Evaporation Condensation Precipitation Run-off Infiltration Uptake Transpiration Extraction Groundwater terms Groundwater = water contained in soil/rock Aquifer = a soil/rock layer that transmits and produces water easily Water table = the upper surface of groundwater in unconfined aquifers Discharge = the release of groundwater to surface water bodies
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Hydrologic cycle diagram
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Human impacts to hydrologic cycle Removing forests and vegetation increases runoff and erosion, reduces transpiration and lowers water tables Irrigating agricultural fields depletes rivers, lakes and streams and increases evaporation Damming rivers increases evaporation and infiltration Emitting pollutants changes the nature of precipitation The most threatening impact: overdrawing groundwater for drinking, irrigation, and industrial use Water shortages create worldwide conflicts
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The carbon cycle Carbon cycle = describes the route of carbon atoms through the environment Photosynthesis by plants, algae and cyanobacteria removes carbon dioxide from air and water Respiration returns carbon to the air and oceans Sedimentary rocks are the primary long-term sink for carbon The oceans, atmosphere, plants, and soil are also important pools
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Carbon cycle diagram
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Human impacts to carbon cycle Burning fossil fuels moves carbon from geologic pools into the atmosphere Cutting forests and burning fields moves carbon from vegetation into the atmosphere Today’s atmospheric carbon dioxide reservoir is the largest in the past 800,000 years Elevated atmospheric carbon dioxide is the driving force behind climate change Ocean acidification results when carbon moves from the atmosphere into the ocean
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The nitrogen cycle Nitrogen cycle = describes the routes that nitrogen atoms take through the environment Nitrogen gas comprises 78% of our atmosphere but cannot be used by organisms Nitrogen fixation = lightning or nitrogen-fixing bacteria combine (fix) nitrogen with hydrogen to form ammonium (NH 4 + )
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Nitrogen cycle processes Nitrification = bacteria convert ammonium ions first into nitrite and nitrate ions which plants can take up Animals obtain nitrogen by eating plants (animals) Decomposers release NH 4 + to nitrifying bacteria Denitrifying bacteria = convert nitrates in soil or water to gaseous nitrogen releasing it back to the atmosphere
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Nitrogen cycle diagram
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Human impacts to nitrogen cycle Haber-Bosch process = production of fertilizers by combining nitrogen and hydrogen to synthesize ammonia Fixing atmospheric nitrogen with fertilizers Increases emissions of greenhouse gases and smog Washes calcium and potassium out of soil Acidifies water and soils Moves nitrogen into terrestrial systems and oceans Reduces diversity of plants adapted to low-N soils Changes estuaries and coastal ecosystems and fisheries
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The phosphorus cycle Phosphorus cycle = describes the routes that phosphorus atoms take through the environment Sediments and sedimentary rocks are the primary pool There is no significant atmospheric component With naturally low environmental concentrations phosphorus is a limiting factor for plant growth
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The phosphorus cycle
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Humans impacts to phosphorus cycle Mining rocks for fertilizer moves phosphorus from the soil to water systems Wastewater discharges also release phosphorus Runoff containing phosphorus causes eutrophication of aquatic systems
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