Interacting Factors – biotic and abiotic factors

Slides:



Advertisements
Similar presentations
One of Our Natural Resources!
Advertisements

INTRODUCTION TO SOILS FIELD STUDY
THE BIOSPHERE: AN INTRODUCTION TO EARTH’S DIVERSE ENVIRONMENTS.
What is Ecology?.
Soil Chapter 12 Section 1.
SB4. Students will assess the dependence of all organisms on one another and the flow of energy and matter within their ecosystems. c. Relate environmental.
Biosphere Soil. What is soil? n Soil is a mixture of particles of weathered rock, decayed organic matter, water and gases in which living organisms are.
Soil Chapter 8.
Soils CharacteristicsTexture Soil Profile Soil Types Threats to Soil.
Objective: Explain what soil consists of Describe the horizons of soil Essential Question: Why do soil horizons form the way they do? Earth’s Surface Text.
1 Soils Soil is made up of a number of different layers.
Healthy Soil? The Nature of Soil
SOIL HORIZONS Mrs. Wilson 9 th Grade Life Science.
Notes: Biotic & Abiotic Factors. A. Ecology The study of interactions between organisms and their environment.
Soils. Formation of Soils Physical Weathering Rain, wind, abrasion Chemical Composition is not altered Influenced by climate Chemical Weathering Acid.
Unit 7 Vocabulary. biotic Organisms living or that had once lived in the environment (i.e., mouse, clover, dead tree)
Soil Chapter 7, Section 3 & 4. Soil  A loose mixture of rock fragments, organic material, water, and air that can support the growth of vegetation.
How Do Soils Form?. Stop treating your soil like DIRT! Soil is a much more complex living thing than most people realize. All the mineral soil on earth.
Soil is made of loose, weathered rock and organic material.
Soils: One of Our Natural Resources!. Some call it dirt…..But it is Soil !!! Soil is made of loose, weathered rock and organic material.
Soil Formation.
SOIL. What is soil:  Soil: is a complex mixture of inorganic minerals, decaying organic matter, water, air, and living organisms.
Soils: One of Our Natural Resources!. Some call it dirt…..But it is Soil !!! Soil is made of loose, weathered rock and organic material.
SOIL PROFILE A vertical strip of soil stretching from the surface down to the bedrock and including all of the successive soil horizons.
Soil Soil is a mixture of weathered rock, organic matter, water, and air that is capable of supporting plant life.
 Soil Horizon. Horizon  Horizon is a side profile of the layers of soil  Soil is usually divided into 3 main layers, but will also include the layers.
Soil Layers Flipbook. Write down the name of each Horizon on the correct line on the cover of your flipbook.
 Soil is the lose covering of rock particles and decaying organic matter(humus)  Results from both physical and chemical weathering.
SOIL AS AN ECOSYSTEM INTRODUCTION TO SOILS FIELD STUDY What do we know about soil now? What makes up soil? What lives there? Where does soil come from?
Soils: One of Our Natural Resources!. Some call it dirt…..But it is Soil !!! Soil is made of loose, weathered rock and organic material.
Soil Horizon.
Ecology is These interactions are two-way: organisms are affected by their environment, and by their presence and activities, change their environment.
Chapter 2 Section 2 Pages How Soil Forms Chapter 2 Section 2 Pages
Characteristics Texture Soil Profile Soil Types Threats to Soil
Soil Horizon.
Interactions of Life.
Characteristics of Soil
Soil Formation How Soil Forms.
Rocks, Weathering, and Soil Information
O On the outside of the foldable illustrate the different layers using colored pencils or crayons. A B C D.
Soil and Its Uses.
Bell Ringer Copy down daily learning log (Soil K.I.M Chart & Video Responses) Copy down homework (Video Responses- Due Wed)
Rocks Weathering and Soil Components
Soil Profiles.
Learning Objectives Identify the levels of organization that ecologists study Explain how biotic and abiotic factors influence an ecosystem.
Basics of Soil What is soil?
Intro to Terrestrial Investigations
Characteristics Texture Soil Profile Soil Types Threats to Soil
Soil Horizon.
How is Soil Formed? Over many years, weathering and erosion will cause the formation of soil. Soil is the loose, weathered material on the Earth’s surface.
Soil Profiles.
Soil and Vegetation.
Soil Tests & Profiles.
How Soil Forms Types of Soil
Ch 52: Intro to Ecology and the Biosphere
5.2: Soil regolith: layer of rock and mineral fragments created from weathering soil: part of regolith that can support plant life.
16.1 Teacher Notes Interactions of Living Things
Soil Layers Flipbook.
One of Our Natural Resources!
Rocks Weathering and Soil Components
Weathering and Soil Formation
PS U6 L3 Soil Horizons.
Ecology.
One of Our Natural Resources!
Characteristics Texture Soil Profile Soil Types Threats to Soil
Review.
Erosion, Deposition and Soil
Soil Formation How Soil Forms
An environment is made up of all the living and non-living things with which an organism (living thing) may interact.
Presentation transcript:

Ecology --The Interrelationships between Organisms and their Environment

Interacting Factors – biotic and abiotic factors

Habitats –places with particular set of physical factors …..

Aquatic habitats -freshwater Running waters

Aquatic habitats - freshwater Slow moving waters

Aquatic habitats – marine_rocky

Aquatic habitats – marine_sandy

Aquatic habitats – marine_muddy

Terrestrial habitats – grassland

Terrestrial habitats – woodland_tpk

Woodland wildlife-tpk

Agricultural habitats

Microhabitats

Biome

Biosphere

Physical environment-light

Physical environment-photoperiod

Physical environment-light _affecting development of plants

Physical environment-nocturnal animals

Physical environment-wind

Physical environment_temperature _cold blooded vs warm blooded

Physical environment_temperature_warm blooded

Physical environment_temperature

Physical environment_temperature

Physical environment_oxygen _fast flowing stream

Physical environment_slow moving water_oxygen

Physical environment _oxygen_eutrophication_red tide

Physical environment_soil layers I The uppermost is called the organic horizon. It consists of detritus, leaf litter and other organic material lying on the surface of the soil. This layer is dark because of the decomposition that is occurring. This layer is not present in cultivated fields. Below is the A horizon or topsoil. Usually it is darker than lower layers, loose and crumbly with varying amounts of organic matter. In cultivated fields the plowed layer is topsoil. This is generally the most productive layer of the soil. This is the layer that soil conservation efforts are focused.

Physical environment_soil layers II The next layer is the B horizon or subsoil. Subsoils are usually lighter in color, dense and low in organic matter. Most of the materials leached from the A horizon stops in this zone. Still deeper is the C horizon. It is a transition area between soil and parent material. At some point the C horizon will give up to the final horizon, bedrock.

Physical environment_soil ecosystem

Soil ecosystem