ms. peterson

34
Ms. Peterson

Upload: others

Post on 27-May-2022

1 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Ms. Peterson

Ms. Peterson

Page 2: Ms. Peterson

What is soil??

Is it dirt?

Is it mud?

Page 3: Ms. Peterson

Soil is the top few inches of earth’s crust and the stuff that plant roots grow in.

Page 4: Ms. Peterson

There are four major soil ingredients

Minerals

Organic Matter

Water

Air

Page 5: Ms. Peterson

Minerals and organic matter are the solid particles in the soil

Water and air fill the spaces between the particles

Soil also contains living organisms-some large, some small

Page 6: Ms. Peterson

Inorganic elements are compounds that naturally occur.

Minerals in soil comes from rocks and other materials that have weathered

Page 7: Ms. Peterson

Sand

Silt

Clay

Other Minerals

Page 8: Ms. Peterson

Sand is the largest-size mineral particle in soil

Page 9: Ms. Peterson

Sand does not hold water well

Soils that are high in sand are not fertile because water moves through it quickly and washes the nutrients away

Page 10: Ms. Peterson

Silt particles are smaller than sand

Page 11: Ms. Peterson

Silt particles fill spaces between sand particles

Sometimes deposited by water when land is flooded or washed into the oceans where streams empty

Page 12: Ms. Peterson

The Mississippi River Delta is an example of a land mass that was developed by silt settling from the flood water of the Mississippi River.

Can you think of another famous river delta?

Page 13: Ms. Peterson

Clay is the smallest particle in soil

Page 14: Ms. Peterson

Clay fills the spaces between sand and silt particles

It gives soil the ability to hold water

Soils that are high in clay are slow to dry out after a rainfall

Page 15: Ms. Peterson

Clay holds minerals that plants need for growth

Page 16: Ms. Peterson

Other minerals in soil are important in plant growth

They are often added in fertilizer to give plants more nutrients.

Page 17: Ms. Peterson

The major minerals are:

Calcium

Phosphorus

Nitrogen

Potassium

Page 18: Ms. Peterson

When reading the label

on a bag of fertilizer,

the 3 numbers on the

bottom stand for

Nitrogen

Phosphorus

Potassium

Page 19: Ms. Peterson

Organic matter is plant and animal remains in various stages of decay.

The decaying organic matter releases nutrients

These soils are dark brown or black, are high in nutrients, and hold a lot of water

Page 20: Ms. Peterson

Soils with high organic matter are more productive

The soil is more easily tilled and made into a seedbed for planting

Page 21: Ms. Peterson

Minimum and no-till farming is a practice where soil is left alone between crops. It increases the amount of water and organic matter in the soil and decreases erosion

Page 22: Ms. Peterson

Water is an important nutrient for plant growth.

It is held between soil particles and sticks to their surfaces

Soil that is too wet or too dry will not support the growth of most crops and ornamental plants

Page 23: Ms. Peterson

Air also fills spaces between soil particles

Plant roots need air to live and grow

Some plants adapt to different environments

Page 24: Ms. Peterson

For example:

Cypress trees grow in wet places. For these trees to have hair, the roots grow structures known as “knees”. The knees rise a few feet above the water level.

Page 25: Ms. Peterson

A way of looking at a cross section of soil

Soil has layers known as horizons

O Layer: Organic Material

A Layer: Topsoil

B Layer: Subsoil

C Layer/Bedrock

Page 26: Ms. Peterson

Color of soil comes from minerals and organic matter

Indicates the quality of the soil

Dark brown or black=High in organic matter The darker the soil, the higher the amount of organic

material

Red or yellow=High in iron

Gray=Poor drainage

White=Low nutrient levels

Spotted appearance=“Mottling”…due to variability of moisture in the soil

Page 27: Ms. Peterson

3 groups:

Organic Elements: Carbon

Hydrogen

Oxygen

Major Elements: Nitrogen

Phosphorus

Potassium

Minor Elements: Other elements required in small amounts for plant growth

Page 28: Ms. Peterson

pH=Acidity or Basicity

pH is based on a scale from 1 to 14

1=Most acidic

14=Most basic

7=Neutral

Most soils are between 4-9

Most plants do well in an acidic soil-6.6 being the best

Page 29: Ms. Peterson

What is soil erosion? Soil erosion is the removal of soil by water and wind.

What causes soil erosion? slope

water splash, runoff

wind drying and blowing soil

accelerated erosion caused by farming and construction

Page 30: Ms. Peterson

Sheet Erosion: The gradual and fairly uniform removal of surface soil

Caused by splash erosion and slow runoff

Page 31: Ms. Peterson

Rill erosion is small streamlets that are cut into the soil surface by running water.

Caused by runoff

Page 32: Ms. Peterson

Gully erosion is rills that have become extremely large.

Caused by uncontrolled runoff for an extended period of time.

Page 33: Ms. Peterson

Sandblows are the result of wind picking up soil particles and carrying them away.

Caused by the removal of vegetative cover, which allows the soil to become dry and loose.

Page 34: Ms. Peterson

Plant Trees

Terraces

No/Minimal Till Farming

Contour Plowing

Crop rotation

Soil pH

Water in the Soil

Salinity Management

Soil Organisms

Indigenous Crops

10 Ways to Conserve Soil