chapter 5: the nonliving environment

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Chapter 5: The Nonliving Environment

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Chapter 5: The Nonliving Environment. Section 1: Abiotic Factors. Abiotic Factors: “not” biotic factors, nonliving Name 4 from the pic . Air Soil Rocks Water Sunlight Temperature Climate. Atmosphere. Air contains: 78% Nitrogen 21% Oxygen .03% Carbon Dioxide - PowerPoint PPT Presentation

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Page 1: Chapter 5:  The Nonliving Environment

Chapter 5: The Nonliving Environment

Page 2: Chapter 5:  The Nonliving Environment

Section 1: Abiotic FactorsAbiotic Factors: “not” biotic factors, nonliving

Name 4 from the pic. Air Soil Rocks Water Sunlight Temperature Climate

Page 3: Chapter 5:  The Nonliving Environment

AtmosphereAir contains:

78% Nitrogen21% Oxygen.03% Carbon Dioxide

Needed for Photosynthesis. The process that supports all life.

Page 4: Chapter 5:  The Nonliving Environment

WaterEssential for life on earth.

Living organisms are 50-95% water.Water covers over 70% of earth’s surface,

however: Over 97% of it is saltwater in the oceans. Only 3% of the earth’s water is freshwater.

68% of this water is locked in glaciers. 30% is found in the ground Less than 0.3% of the freshwater on earth is in

lakes, rivers, swamps, and the atmosphere. AKA, usable water.

Page 5: Chapter 5:  The Nonliving Environment
Page 6: Chapter 5:  The Nonliving Environment

SoilMixture of minerals, rock particles,

decaying organisms, water, and air.Abiotic because it is mostly rocks and

minerals.Contains many biotic factors as well:

BacteriaFungusInsectsWorms

Page 7: Chapter 5:  The Nonliving Environment

Sunlight and TemperatureSunlight is the original source of energy for earth.Used in photosynthesis. Eventually supports all life.

Temperature of a region is controlled by the sunlight.Latitude:

The closer to the equator, the more direct sunlight a region gets for more days per year.

ElevationLower temperature at higher elevations. Why?Air is thinner, therefore less molecules. Heat is the amount of energy that molecules have……..

Page 8: Chapter 5:  The Nonliving Environment

Climate and WindAn area’s average weather conditionsTemperature and Precipitation: 2 key

componentsInfluence the type of life that inhabits any

ecosystem.

WindAlso a result of the sun.Wind is caused when molecules in an area of

the atmosphere are heated.

Page 9: Chapter 5:  The Nonliving Environment

Abiotic Factors influencing Biotic Factors.

Abiotic

Biotic

Biotic

Biotic

Biotic Biotic

Biotic

Page 10: Chapter 5:  The Nonliving Environment

Section 2: Cycles in NatureThe Water Cycle

Page 11: Chapter 5:  The Nonliving Environment

Nitrogen Cycle: What is Nitrogen?Important ingredient in proteins of life.Essential part of our DNA chain.The most plentiful gas in the atmosphere.

(78%)Very few organisms can use N from the air.Nitrogen fixing bacteria in the soil form N

compounds that plants can use. These bacteria are found in the nodules (roots) of

soybeans, peas, and clover.Lightning also releases Atmospheric Nitrogen

to the rain and eventually soil to be used by plants. (5-8% )

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The Nitrogen Cycle.

Page 13: Chapter 5:  The Nonliving Environment

The Carbon CycleA cycle of carbon atoms between the living

and non-living parts of the ecosystems.

Page 14: Chapter 5:  The Nonliving Environment

Section 3: Energy FlowPhotosynthesis vs. Chemosynthesis

Photo: the use of light by plants to produce energy rich molecules

Chemo: the use of chemicals by bacteria to produce energy rich molecules Deep sea ocean vents. No sunlight. Food webs begin with bacteria, not plants. Sulfur emitted by the volcanic vents is synthesized

by the bacteria into energy.

Page 15: Chapter 5:  The Nonliving Environment

Energy Pyramid