Gersmehl Diagrams.

Slides:



Advertisements
Similar presentations
Ecology The study of interactions that take place between organisms and their environment.
Advertisements

INTRODUCTION TO SOILS FIELD STUDY
Model of the Mineral Nutrient Cycle developed by P.F. Gersmehl in 1976
A5: Soil Composition Grade 6.
Weathering and Soil Formation
Soil, an Essential Natural Resource
Soil! By: Oksanna Loya.
 an organism that makes its own food  an organism that eats other living things to get energy.
Soil 6 th grade Earth Science Howard Middle School.
BIOGEOCHEMICAL CYCLES Nitrogen Cycle Water Cycle Carbon Cycle.
Nutrient cycles The nitrogen cycle Inputs of nutrients : 1.Precipitation & dry deposition 2.Weathering of bedrock 3.[Artificial supplements]
Soil No soil, No planet Earth. Soil Terminology Vocabulary: Soil Horizon – layers or zones of soil. Soil profile: different zones or layers starting at.
Cycles of Matter Matter moves in Biogeochemical cycles through living systems, the Earth, the atmosphere, and the oceans. These cycles connect biological,
Soil Class Notes. Soil Soil is made of out of rocks, dead plants, and animals. Decomposed plants and animal remains add nutrients to the soil.
HOW SOIL FORMS 6.E.2.3 Explain how the formation of soil is related to the parent rock type and the environment in which it.
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?
Soil Formation and Composition.  I. Soil Formation –A. When bedrock is exposed, it weathers. –B. Particles of rock mix with other material. –C. Soil.
Soil By Shane and Chloe. What is soil. Soil is a mixture of broken rocks and minerals, living organisms, and decaying organic matter called humus. Humus.
Soil in Anchorage, Alaska, is very shallow
Soil.
Factors Affecting Ecosystems
Schimmel Soil Study Guide
SOIL Describe how soil forms. Explain the characteristics of soil.
Chapter 2 Section 2 Pages How Soil Forms Chapter 2 Section 2 Pages
Chapter 7 Earth Science Weathering and Soil.
The Cycling of Matter in Ecosystems
Soil.
What is the composition of soil?
Soil Formation and Composition
Soil Formation How Soil Forms.
Natural Sciences and Technology Grade 5
Soil Vocabulary.
SOIL AND ITS FORMATION.
SOIL.
What is soil?.
Rocks Weathering and Soil Components
The Ground Beneath Our Feet
Soil.
Weathering.
Soil as a System A.S: Topic 7: A – D
Lithosphere & Soil ; ;
Weathering and Soil Information
8th Grade: The Dynamic Earth (Module E)
The Ground Beneath Our Feet
Soil Tests & Profiles.
C.2 Communities and Ecosystems part 1
What is the composition of soil?
Soil Study Guide Soil is loose material that covers much of the Earth’s surface. Soil is made up of bits of rock, minerals, and material that was part.
SOL 3.1 & 3.7.
Soil is A loose mixture of small minerals and rock fragments, organic material, water, and air.
SOIL Don’t Call it Dirt.
Rocks Weathering and Soil Components
Ecology
How can we define soil with what we know?
What is the composition of soil?
Soil Formation and Composition
Rocks Weathering and Soil Components
The Ground Beneath Our Feet
Lithosphere & Soil ; ;
The Ground Beneath Our Feet
What is the composition of soil?
Review.
C.2 Communities and Ecosystems part 1
How Soil Forms Vocab Words
What is the composition of soil?
Soil Formation How Soil Forms
SOL 3.1 & 3.7.
The Ground Beneath Our Feet
What is soil? What is it made of? What’s in it?
HOW SOIL FORMS 6.E.2.3 Explain how the formation of soil is related to the parent rock type and the environment in which it.
Presentation transcript:

Gersmehl Diagrams

The Soil The soil is a mixture of Decomposing organic material (from dead animals and plants, leaf litter, etc. Tiny rock particles being eroded from the earth Water Air spaces

Biomass Biomass is the mass of living organisms. All the species of an ecosystem contribute to its biomass.

Litter At any time there are dead animals or fallen parts of plants being decomposed on the ground. They have not yet become humus in the soil. This makes up the ‘litter’.

Arrows There is a constant transfer of nutrients between each of the three stores, soil, litter and biomass. The arrows show the size of the transfer.

Decomposition Where there is fast decomposition of little there will be a smaller amount of litter. Where decomposition happens slowly there will be more litter on the surface of the soil

Temperature and Precipitation As the temperature rise and the precipitation rises the amount of biomass increase. The uptake of minerals from the soil increases.