Class 13b: Soils (pedology). What is soil? Not just dirt.

Slides:



Advertisements
Similar presentations
Soil formation begins with weathering of bedrock
Advertisements

Soil Orders Here we go!.
Weathering and Soil Formation
GES 175, The Science of Soils Lecture 1, Introduction.
LECTURE 17 Soil Classification. Recap from yesterday… Soil classification: “The ordering of soils into a hierarchy of classes. The product is an arrangement.
Soil It’s not just DIRT.
Agriscience and Technology I Introduction to Soil Science
Soil Profiles and Soil Classification What processes result in the formation of soil horizons? What are the typical characteristics of O, E, A, B, C and.
Sedimentation & Stratigraphy (89.352)
Chapter 18 The Geography of Soils
GES 175: Science of Soils Laboratory Week 1.
Review and soil formation:
Soils.
The Nature of the Soil Soil is the natural surface layer that contains both inorganic weathered debris and living matter. Soils are developed over a long.
Chapter Five Weathering: The Breakdown of Rocks. CHAPTER 5: WEATHERING: THE BREAKDOWN OF ROCKS A) WEATHERING: PROCESS BY WHICH ROCKS AND MINERALS BREAK.
Soil Composition 1/13/12. What determines characteristics of soil? Physical (such as water) Parent material (chemical make-up) Life (biological activity)
The Nature and Properties of Soil
Chapter 14 Final Review Weathering and Erosion By: Britni Surprenant period 4.
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.
Unit 2 Topic 2 soil. What is soil and why do we care about it?  complex mixture:  weathered mineral materials from rocks  partially decomposed organic.
Earth’s Surface is Constantly Changing
Environmental Sciences: Towards a Sustainable Future Chapter 8 Soil and the Soil Ecosystem.
Soils.
Igneous Sedimentary Metamorphic Rock Very slowly weathered minerals (e.g., quartz, muscovite) Slowly weathered minerals (e.g., feldspars, biotite) Easily.
Topic 5 Part 1 soil.
The Twelve USDA Soil Orders
 Plants and Soil  Soil Degradation  Addressing Soil Degradation.
SOIL GENESIS, PHYSICAL, CHEMICAL AND COLLOIDAL PROPERTIES OF SOIL
10-1 Environmental Geology James Reichard Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
Soil and the Soil Ecosystem. Soil Characteristics Profiles Profiles Texture Texture Classes Classes.
Soil Profile, Classification and Physical Properties Soils & Fertilizers for Master Gardeners In-service Training June 9, 2008 Amy Shober UF/IFAS Gulf.
Earth Science Unit 1.4: Weathering and Soils. The Rock Cycle.
Soil is made of loose, weathered rock and organic material.
Where does soil come from?
Getting Dirty with SOILS. Older than dirt????!!!!
Soil. Mechanical and chemical weathering of rocks form soil. Soil covers much of the land on Earth. It is made up of minerals, air, water, and organic.
Understanding Soil.
Soils and Regolith.
Chapter 8: Soil. Goals Understand how the soil quality determines what can grow Understand how soil quality can determine the survival of societies.
SOIL: A RENEWABLE RESOURCE Soil is a slowly renewed resource that provides most of the nutrients needed for plant growth and also helps purify water. Soil.
Soil Taxonomy- Properties of Soil
Chapters 14 & 21 Super Seven: Soil Sciences Section; Selected, Stylized, Shrunk and Shown by Stephen Mauney and Holly Roberts.
Why is a study of soil important? 90% of the world’s food comes from land- based agriculture. Maintenance of soil is the cornerstone of sustainable civilizations.
© 2015 John Wiley & Sons, Inc. All rights reserved. BIO 112 June 22, 2015  The Soil System (part of ch. 14)  Soil Properties and Major Soil Types  California.
Origins- parent material; mixtures of eroded rock, mineral nutrients, decaying organic matter, and billons of living organisms (mostly decomposers)
Soil: One of Our Natural Resources
Soil: One of Our Natural Resources
Chapter 12 Soils.
Exam III Wednesday in Class
Soil Formation Soil is an important natural resource
Getting Dirty with SOILS
The Twelve USDA Soil Orders
Foundation for Land Ecosystems
Weathering and Soils.
Soil Formation.
Soils.
Soil An interface in the Earth system, a boundary between different systems (biosphere, lithosphere, atmosphere). Soil is a combination of mineral matter,
Soil Regolith – layer of rock and mineral fragments produced by weathering Soil – part of regolith that supports plant growth.
PRT 2008 Lecture 7.
SOIL.
5.2: Soil regolith: layer of rock and mineral fragments created from weathering soil: part of regolith that can support plant life.
Module 25 Weathering and Soil Science
The Twelve USDA Soil Orders
GES166/266, Soil Chemistry Lecture 1, Introduction.
GES 175, The Science of Soils
Food, Soil, and Pest Management
Chapter Five Weathering: The Breakdown of Rocks
Weathering.
The Formation of Soil Earth Science Mr. Cloud.
Presentation transcript:

Class 13b: Soils (pedology)

What is soil? Not just dirt

Soil components Parent material: Temperature and moisture

Soil formation Bedrock breaks apart into regolith

Classifying soils: color Color tells you about chemistry

Classifying soils: texture Size, organization of particles

Classifying soils: texture

Classifying soils: structure Arrangement of soil particles

Classifying soils: structure Porosity: Permeability:

Soil moisture

Soil-water balance Warmer temperatures: higher ET Higher precipitation: higher percolation

Soil profiles

Soil classification More complicated than climate

Entisols Relativey new: most recent soils

Oxisols Old soils; minerals except oxides leached out

Aridisols Found in arid environments

Mollisols Most productive soil

Alfisols Significant aluminum (Al) and iron (Fe)

Spodosols Most acidic soil; minerals leached to lower horizon

Soil degradation Forms in 500 years, but can disappear in one

Soil degradation

Salinization: salty soil