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3.1 – Population Dynamics IB Topics 3.1.1-3.1.4 Topic 3 – Human Population, Carrying Capacity, and Resource Use

3.1 – Population Dynamics

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Topic 3 – Human Population, Carrying Capacity, and Resource Use. 3.1 – Population Dynamics. IB Topics 3.1.1-3.1.4. Current Human Population. There are about 7 billion people living on Earth For about 200,000 years, there were between 1-15 million people on Earth. Milestones. - PowerPoint PPT Presentation

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Page 1: 3.1 – Population Dynamics

3.1 – Population DynamicsIB Topics 3.1.1-3.1.4

Topic 3 – Human Population, Carrying Capacity, and Resource Use

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Current Human Population There are about 7

billion people living on Earth

For about 200,000 years, there were between 1-15 million people on Earth

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Milestones 1 Billion: 1804 2 Billion: 1927 3 Billion: 1960 4 Billion: 1974 5 Billion: 1987 6 Billion: 1999 7 Billion: 2012

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Demographics If you reduce the worlds population to a

village of 100 people…

http://www.toby-ng.com/graphic-design/the-world-of-100

/

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Predicted Growth Some predict

a stabilization of human population, while others predict a continued increase

Global Population Forecast

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Calculating Rates Crude Birth Rate

(CBR) The number of

live births per 1000 people

Equation:

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Calculating Rates Crude Death Rate

(CDR) The number of deaths

per 1000 people Equation:

Natural Increase Rate (NIR) CBR-CDR

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Calculating Rates Fertility

The average number of births per women of child-bearing age

Equation:

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Calculating Rates Doubling Time

The amount of time it takes for a population to double

Equation:

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Population Pyramids

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Population Pyramids

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Population Pyramids

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Population Pyramids

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Demographic Transition Model

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3.2 – Resources – Natural CapitalIB Topics 3.2.1-3.2.7

Topic 3 – Human Population, Carrying Capacity, and Resource Use

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Natural CapitalNatural

resources/natural assets

Can become natural incomeGoods or

services

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Resources Non-renewable

Cannot be replenished at the same rate they are used

Renewable Living resources that

can be replenished at the rate they are used via human processes

Replenishable Non-living resources

that can be replenished via natural processes

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Nature of a ResourceThe value of a

resource changes with human technology/culture

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Sustainability Using resources at a

rate that allows natural regeneration

Living within the means of nature

Development that meets the needs of the present without compromising the ability of future generations to meet their own needs

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Sustainable development

Development that meets the needs of the present without compromising the ability of future generations to meet their own needs.

Ex: fishing, hunting, energy

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3.3 – Energy SourcesIB Topics 3.3.1-3.3.3

Topic 3 – Human Population, Carrying Capacity, and Resource Use

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Making Energy Electricity is

delivered to homes and businesses via alternating current (AC)

AC power is generated when electromagnets are spun using a turbine

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Energy Sources Worldwide85% of the

worlds energy comes from fossil fuels.

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Energy Production in Wisconsin

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Pollution from Energy in Wisconsin

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Renewable Energy in Wisconsin

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Energy Production Examples: WI:

Pleasant Prairie Coal Plant 1190 MW Oak Creek Coal Plant 1135 MW Point Beach Nuclear Plant 1033 MW

Other Examples: Three Gorges Dam 22,500 MW Hoover Dam 2080 MW Nellis Solar Power Plant 14MW (70,000 panels) Big Wind Turbine 1.6 MW Typical Geothermal Plant 40 MW

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Energy Source

Description Pros Cons

Fossil Fuels

Nuclear

Wind

Hydro

Solar

Geothermal

Biofuels

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Fossil Fuels

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Nuclear Power

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Wind Power

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Hydropower

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Solar Power

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Geothermal Power

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Biofuels

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Oil Palms

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Future Solutions Hydrogen Nuclear Fusion Carbon

Sequestration

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3.4 – Soil SystemsIB Topics 3.4.1 – 3.4.5

Topic 3 – Human Population, Carrying Capacity, and Resource Use

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SoilSoil is eroded

rock, nutrients, decaying organic matter, and water

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Soil Formation

Soil is produced by: Weathering of rock Deposition of

sediments by erosion

Decomposition of organic matter in dead organisms

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Soil Horizons Soils generally have distinct horizons: A horizon

Humus (decaying organic matter with mineral particles) E horizon

Not always present, pale layer where minerals have been leached B horizon

Organic matter and mineral deposits C horizon

Weathered rock/bedrock

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Soil TextureSoil type depends on the particle size

Sand = BiggestSilt = MediumClay = Smallest

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Soil Texture

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Soil TypesPotential to hold organic matter

Drainage

Water holding capacity

Air Spaces

Plants and animals

Primary Productivity

Sandy Soil

Clay Soil

Loam Soil

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Soil TypesPotential to hold organic matter

Drainage

Water holding capacity

Air Spaces

Plants and animals

Primary Productivity

Sandy Soil

Low Very Good

Low Large Few Low

Clay Soil Low Poor Very High Small Few Very Low

Loam Soil Medium Good Medium Medium Many High

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Nutrients Macronutrients

Nitrogen (needed for chlorophyll)

Phosphorous (needed for photosynthesis)

Potassium (needed for fruiting and growth)

Calcium Magnesium Sulfur

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NutrientsMicronutrients

BoronCopperChloride IronManganeseZinc

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Nitrogen cycle Atmospheric Nitrogen has to be ‘fixed’ (usually

by bacteria) for plants to use it.

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Soil DegradationWater erosionWind erosionAcidificationGroundwater usePollutionDesertificationClimate changeOvergrazingDeforestationRoads

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Soil Degradation

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Soil Degradation

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Soil ConservationMechanical/

physical barriersOrganic farmingAfforestationContour plowingTerracingCrop rotationSoil conditioners

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