TEST REVIEW ON WEATHERING, SOIL AND WATER

Slides:



Advertisements
Similar presentations
The Water Cycle.
Advertisements

Soil and Water Cycle Review
mechanical weathering
Weathering and Soil.
Weathering, Erosion, Deposition, and Soil
The Nature Of Soil Ms. Scerra
Weathering & Soil.
Ch 14 Weathering and Erosion
Rocks, Weathering, and Soil Information
Chapter 7: Weathering & Soil
Weathering and Erosion
1 2 pt 3 pt 4 pt 5pt 1 pt 2 pt 3 pt 4 pt 5 pt 1 pt 2pt 3 pt 4pt 5 pt 1pt 2pt 3 pt 4 pt 5 pt 1 pt 2 pt 3 pt 4pt 5 pt 1pt Soil My name is not Dirt My name.
Weathering, Soil, and Erosion
Soil and Soil Conservation
Chapter 14 Weathering and Erosion
By: Kelsey Bowman and Tiffany Gee
200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt.
Weathering and Soil Erosion
Earth’s Surface: Chapter 4 Section 3 Human Activities Affect Soil
Weathering and Soil Formation
Chapter 23 – Sections 1, 2, and 3 Earth’s Surface.
Weathering and Soil Formation
Weathering and Soil Formation
< BackNext >PreviewMain Weathering and Soil Formation Section 1 WeatheringWeathering Section 2 Rates of WeatheringRates of Weathering Section 3 From Bedrock.
The Flow of Fresh Water Chapter 11.
Big Idea: Natural forces break rocks apart and form soil, which supports life.Big Idea: Natural forces break rocks apart and form soil, which supports.
From Bedrock to Soil.
Weathering and Soil Formation
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.
Weathering and Soil Formation Notes. Weathering Two types – Mechanical Weathering Ice Abrasion Wind, Water, Gravity Plants Animals Chemical Weathering.
Processes that Shape the Earth
The Flow of Fresh Water Chapter 11. Rivers: Agents of Erosion Many years ago there was a vast plain in the southwestern U.S. Many years ago there was.
The Water Cycle 01/20/ a pgs  IN: Where does our water come from and where does it go?
Weathering and Erosion
Are these examples of weathering, erosion, or both?  1. Ice breaking rock  2. Wind breaking away and moving rock  3. A river moving sediment  4. Tree.
Weathering  It is surface processes that break down rock  Breaks rocks into smaller and smaller pieces  Ex.) Sand, silt, clay  The formation of soil.
Weathering.
Rates of Weathering Ch. 10 Section 2 Ch. 10 Section 2.
Unit 1 Lesson 2 Weathering
Weathering, Erosion, and Rivers Chapters 7 and 9
Section 4.1 Notes: Mechanical & Chemical Forces Break Down Rocks
Weathering Rates of Weathering Soil & Soil Conservation Fresh Water
Weathering and Soil Formation
Weathering & Soil Erosion
23.1 Fresh Water 71% of Earth is covered with water, 3% is fresh
Weathering, Erosion, and Soil Notes
Chapter 7 Earth Science Weathering and Soil.
Weathering.
Chapter 2: Weathering and Soil Lesson 1: Rocks and Weathering
Chapter 10 Table of Contents Section 1 Weathering
Weathering: Processes of Change
Physical Weathering How does physical weathering affect rocks?
Water in Earth’s Processes Study Guide
Rocks, Weathering, and Soil Information
Rocks, Weathering, and Soil Information
The Truth about Soil and Soil Conservation
The Water Cycle.
Rocks, Weathering, and Soil Information
Weathering: Chemical Weathering: the breakdown of rock into sediments
Weathering and Erosion
Unit 1 Lesson 2 Weathering
Rocks, Weathering, and Soil Information
Rocks, Weathering, and Soil Information
9.1 Weathering.
Unit 1 Lesson 2 Weathering
The Water or Hydrological Cycle
Rocks, Weathering, and Soil Information
Unit 1 Lesson 2 Weathering
Weathering and Erosion
Rocks, Weathering, and Soil Information
Presentation transcript:

TEST REVIEW ON WEATHERING, SOIL AND WATER

WEATHERING Mechanical Weathering Is the breakdown of material into smaller pieces by physical means Types of Mechanical Weathering Ice: Freezing and thawing of soil and rock is Frost action or Ice wedging Abrasion: The grinding and wearing away of rock surfaces by Wind, Water, and Gravity. Plants: Tree roots are strong enough to slowly break soil and rock. Animals: When animals burrow in the ground, they break up soil and loosen rocks to be exposed to further weathering.

WEATHERING (Cont.) Chemical Weathering The process by which material breaks down due to chemical reactions Common Agents of Chemical Weathering Water, Weak Acids, and Air: Can slowly or rapidly dissolve the chemical bonds between minerals to eventually produce sediment. Scientist measure acid concentration (or acidity) by using a pH scale from 0 to 14. Solutions that have a pH of less than 7 are acidic. Solution that have a pH of greater than 7 are basic. Acid Precipitation: Is a chemical reaction caused by Rain, Sleet, or Snow that contains a higher than normal acid concentration. Acid precipitation can be caused naturally by Volcanoes or by Fossil Fuels and Air Pollution.

WEATHERING (Cont.) Rates of Weathering Differential Weathering: The process by which softer, less weather resistant rocks wear away and leave harder, more weather resistant rocks behind. Surface Area: The greater the surface area the more weathering can take place. Climate: The more humid the climate the higher the rate of both mechanical and chemical weathering. Elevation: Materials at higher elevations are exposed to more wind, rain, and ice than rocks and materials at lower elevations.

Soil Soil Is a loose mixture of small mineral fragments, organic material, water, and air that can support the growth of vegetation. Parent Rock: The source of mineral fragments, formed from weathering, in the soil. Bedrock: is the layer of rock beneath the soil. Transported Soil: Soil that is blown, washed, or moved away by natural or man-made means. Wind and the movement of glaciers are examples natural means. Construction and mining activities are examples man-made means.

Soil (cont.) Soil Conservation Is the method to maintain the fertility of the soil by protecting the soil from erosion and nutrient loss. Erosion: The process by which wind, water, or gravity transport soil and sediment from one location to another. Land Degradation: Occurs when the soil has been damaged due to overuse, poor farming techniques, or overgrazing to point that vegetation will not grow and the area becomes like a desert. Leaching (page 52): Water dissolves and carries nutrients in the topsoil through the different Soil Horizons. Soil pH: The pH of the soil influences how nutrients dissolve. Certain nutrients dissolve at a high pH (basic) and some at a low pH (acidic) Separate plants may need different nutrients….So the right soil pH is required for certain plants.

Soil (Cont.) Soil Conservation Techniques (page 58): Contour Plowing: Helps prevent erosion. Terracing: Prevents erosion on steep slopes. No-till farming: Prevents erosion and nutrient removal (slows leaching) by providing cover during run-off periods. Cover crop: Restores nutrients to the soil. In Syracuse (flat land), out of the above techniques, what do you think the best soil conservation technique(s) would be?

Water Water Cycle( page 71) Condensation: Water vapor cools and changes into water droplets that form clouds in the atmosphere. Water loses energy during condensation. Precipitation: Rain, snow, sleet or hail that falls from the clouds. Evaporation: Water from the oceans and the Earth’s surface changes into water vapor. Water gains energy during water evaporation. Percolation: is the downward movement of water through pores and other spaces due to gravity. Runoff: The precipitation that flows over land into streams and rivers.

Four states of matter (a look back at phase changes) Remember: Enthalpy is a measure of energy. So water gains or loses energy When in turns from vapor to rain or from water to vapor. This is a change in a phase of matter and energy is therefore lost or gained!

Water (cont.) River Systems Watershed : The area of land that is drained by a water system. Tributary : A stream that flow into a lake or larger stream. Divide : The boundary between drainage areas that have streams that flow in opposite directions. Channel: The path that a stream follows. Types of Rivers (pages 75 and 76): Youthful, Mature, Old, and Rejuvenated. Polar Ice Caps : Where the majority of the world’s fresh water is located.

Water (cont.) Water Health Dissolved Oxygen: The concentration of O2 that is dissolved in the water. If dissolved oxygen is to low, it can cause harm to aquatic life. Nitrates : Naturally occurring compounds of nitrogen and oxygen. If nitrate levels are elevated, it can be harmful to aquatic life. Alkalinity : Water’s ability to neutralize acid. Acids and other acid wastes can harm aquatic life. It is important for water to keep pH levels above 6.0.

Water (cont.) (Waste) Water Treatment Sewage Treatment Plants (page 90) : A water treatment facility that cleans the waste materials found in water that comes from sewers or drains. Septic Tanks (page 91) : is a large underground tank that separates solid waste from liquids for a household. According to the pie chart graph on page 91 what could you and your family do to conserve the most water?