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3-1 ATB

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3-1 ATB. What is desertification? Today: Discuss the presentations you will create over the next three days. Soil Peds. How sand, silt and clay are arranged Forms soil structure. 3-2 ATB. What is weathering? Today: Research! - PowerPoint PPT Presentation
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3-1 ATB • What is desertification? • Today: – Discuss the presentations you will create over the next three days.
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Page 1: 3-1 ATB

3-1 ATB

• What is desertification?

• Today:– Discuss the presentations you will create over

the next three days.

Page 2: 3-1 ATB

Soil Peds

• How sand, silt and clay are arranged

• Forms soil structure

Page 3: 3-1 ATB

3-2 ATB

• What is weathering?

• Today:– Research!– Is your worksheet done for the class??? (I

need them tomorrow, at the latest)

Page 4: 3-1 ATB

3-3 ATB

• What was the dust bowl?

• Today:– Last day of research

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3-4 ATB

• Is your presentation finished?

• Today:– Finish presentations– Give me your worksheet / note outline

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3-7 – 2 hr delay --- No ATB

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3-8 ATB

• What is IPM?

• Today:– Start presenting– I’ll need your rubric for grading your presentation

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3-9 ATB

• What are the positive benefits of no-till farming? What could be a negative?

• Today:– Continue the presentations

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3-10 ATB

• Where do some carnivores begin eating large prey animals?

• Today:– Continue with presentations

Page 10: 3-1 ATB

3-14 ATB

• Which is the worst type of erosion? Splash, Rill or Sheet erosion?

• Today:– Finish soil conserv and degradation– Start Tarek / Elliot presentation– Planet Earth…

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3-15 ATB

• What is the most effective irrigation method?

• Today:– Continue with presentations

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3-16 ATB

• What is salinization? How does it occur?

• Today:– Sir-Oly and J. Mutch present

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3-17 ATB

• What was one benefit and one problem with the green revolution?

• Today:– Continue with presentations

• Quiz Monday on the first 3 presentations

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3-18 ATB

• How long ago do we believe agriculture began?• Today:

– Get Soil Samples– Lab Quiz Monday– Ch 9 Quiz Monday (Tarek & Elliot – presentation

posted?)

Page 15: 3-1 ATB

Soil Lab– HOMEWORK: – Soil Samples

• Find an area at your house that indicative of normal soil (IE, do not dig the soil out of a compost heap)

• Dig at least 6 inches down (no more then 10 inches)• Get a a sandwich bag full of soil (write you name on

the bag)

– Read background on Soil Formation & Properties• Quiz on the reading Monday (so yes, two quizzes on

Monday)

Page 16: 3-1 ATB

3-22 ATB

• What was the green revolution?

• Today:– Ch 9 quiz– Lab background quiz– Tomorrow – start soil lab

Page 17: 3-1 ATB

3-24 ATB - none • Soil Lab Today:

– Get out your lab procedure– Get a piece of paper to make observations

• 5 observations from mechanical weathering• 2 observations from the chemical weathering• Make the applicable observations for the Soil Texture

and Soil Consistence activities

– Do not spray each other with the spray bottles– Make sure everything is cleaned up before you

leave

Page 18: 3-1 ATB

3-25 ATB

• What is shaking the rock samples supposed to be simulating?

• Today:– Finish the mechanical weathering section of the

lab– Set up the chemical weathering portion of the lab

Page 19: 3-1 ATB

3-28 ATB

• What is a monoculture?

• Today:– Finish the chemical weather part of the lab

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3-29 ATB

• What were the three things that make up soil?

• Today:– Testing soil types

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3-30 ATB

• What are some examples of problems caused by overgrazing?

• Today:– Finish the last two presentations– Thursday – Finish soil lab

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3-31

• What is aquaculture? What is one pro and one con?

• Today:– Lab:

• Finish “Determining Soil Consistence”• Set up the “Soil Organization”, but do not add the food

coloring

– Test – next week

Page 23: 3-1 ATB

4-1 ATB• Before agriculture, what was our primary

means of obtaining food?

• Today:– Test / study guide -- Wednesday – Finish your lab from yesterday.– Read the Article, “Fighting Over Food”

• Create 5 questions that can be answered from the article

• Create 2 “thinking” questions dealing with the article. (due before you leave)

– People on Ffaablaah trip:• Get a review sheet – due when you get back. • Finish your lab questions – skip pages 15 & 16.

Page 24: 3-1 ATB

4-6 ATB• Even if no one cared about the dolphins being

killed, what is dangerous about this?

• Today:– Finish “The Cove”– Paragraph or two on your feelings / questions

about the movie. (Ie: Is this okay? What about the mercury? Etc)

– Work on your review sheet – Test Friday

Page 25: 3-1 ATB

4-7 ATB

• What is bioaccumulation?

• Today:– Labs due, article Q’s due, “The Cove” paragraph due– Review – any questions about the test?– Test / Study Guide - Tomorrow– Discuss GM foods in the “Viewpoints” packet

Page 26: 3-1 ATB

4-7 Assignment

• Pg 259– #2– #8

• Pg 291– #1– #8

Page 27: 3-1 ATB

• Article, “Fighting Over Food”– Create 6 questions that can be answered from

the article – Answer:

• Pg 24-25 in Viewpoints packet – Read– Which article do you find yourself siding with?

Explain

Page 28: 3-1 ATB

Worksheet example• Page # you’re presenting• Term:• Term:• Term:• Term:• Term:

• Extra Info:

Page 30: 3-1 ATB

Questions…

Get a slice of paper and answer the following…• What is no till farming?• What are soil horizons? List them• What is desertification?• What is weathering?• Name two factors that lead to the Dust Bowl.• What is IPM?

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This lecture will help you understand:• The relationship between

soils and agriculture• Major agricultural

developments • The fundamentals of soil

science• Causes and

consequences of soil erosion and degradation

• Principles of soil conservation

Page 33: 3-1 ATB

No-till agriculture in Southern Brazil• Southern Brazil’s climate

and soils make for bountiful harvests

• Repeated planting has diminished the productivity of the soil

• Leaving crop residues on their fields after harvesting and planting “cover crops” reduced erosion, increased yields and cut costs

• These no-till techniques have benefited everyone

Page 34: 3-1 ATB

Soil: the foundation for agriculture• Land devoted to agriculture covers 38% of Earth’s land

surface • Agriculture = practice of raising crops and livestock

for human use and consumption • Cropland = land used to raise plants for human use • Rangeland or pasture = land used for grazing

livestock • Soil = a complex plant-supporting system consisting of

disintegrated rock, organic matter, water, gases, nutrients, and microorganism – It is a renewable resource

Page 35: 3-1 ATB

Population and consumption degrades soil

• Feeding the world’s rising human population requires changing our diet or increasing agricultural production

• Land suitable for farming is running out • We must find ways to improve the efficiency of food

production• Mismanaged agriculture turns grasslands into

deserts; removes forests; diminishes biodiversity; and pollutes soil, air, and water – Fertile soil is blown and washed away

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Millions of acres of cropland are lost each year

We lose 5-7 million ha (12-17 million acres) of productive cropland annually

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Soil degradation has many causes

• Soil degradation results from deforestation, agriculture and overgrazing

• Over the past 50 years, soil degradation has reduced global grain production by 13%

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Agriculture arose 10,000 years ago• Agriculture was invented independently by different cultures

• The earliest plant and animal domestication is from the “Fertile Crescent” of the Middle East– Wheat, barley, rye, peas, lentils, onions, goats, sheep

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Traditional agriculture• Traditional agriculture = biologically powered

agriculture, using human and animal muscle power– Subsistence agriculture = families produce only enough

food for themselves

– Intensive agriculture = produces excess food to sell

– Uses animals, irrigation and fertilizer, but not fossil fuels

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Industrialized agriculture is a recent phenomenon

• Industrialized agriculture = using large-scale mechanization and fossil fuels to boost yields– Also uses pesticides, irrigation and fertilizers– Monocultures = uniform planting of a single crop

• Green revolution = the use of new technology, crop varieties and farming practices introduced to developing countries– Increased yields– Created new problems and worsened old ones

Page 42: 3-1 ATB

Soil as a system• Soil consists of

mineral matter, organic matter, air, and water– Dead and living

microorganisms, and decaying material

– Bacteria, algae, earthworms, insects, mammals, amphibians, and reptiles

Since soil is composed of living and non-living matter, it is considered an ecosystem

Page 43: 3-1 ATB

Soil formation is slow and complex

• Parent material = the base geologic material of soil– Lava, volcanic ash, rock, dunes

– Bedrock = the continuous mass of solid rock comprising the Earth’s crust

• Weathering = the physical, chemical, or biological processes that break down rocks to form soil– Physical (mechanical) = wind and rain, no chemical

changes in the parent material

– Chemical = substances chemically interact with parent material

– Biological = organisms break down parent material

Page 44: 3-1 ATB

Weathering produces soil

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Other processes affect soil formation

• Erosion = the dislodging and movement of soil by wind or water– Occurs when vegetation is absent

• Biological activity includes deposition, decomposition, and accumulation of organic matter– Humus = a dark, spongy, crumbly mass of material

formed by partial decomposition

Page 46: 3-1 ATB

A soil profile consists of horizons• Horizon = each layer of soil

• Soil profile = the cross-section of soil as a whole

• Up to six major horizons may occur in a soil profile– Topsoil = inorganic and

organic material most nutritive for plants

– Leaching = dissolved particles move down through horizons

Page 47: 3-1 ATB

Soils are characterized in many ways• Soils are classified based on color, texture,

structure, and pH

• Soil color = indicates its composition and fertility– Black or dark brown = rich in organic matter– Pale gray or white = indicates leaching

• Soil texture = determined by the size of particles– From smallest to largest = clay, silt, sand– Loam = soil with an even mixture of the three– Influences how easy it is to cultivate and let air and

water travel through the soil

Page 48: 3-1 ATB

Soil texture classification

Silty soils with medium-size pores, or loamy soils with mixtures of pore sizes are best for plant growth and crop agriculture

Page 49: 3-1 ATB

Soil structure and pH• Soil structure = a measure of soil’s “clumpiness”

– Large clumps can discourage plant roots– Repeated tilling compacts soil, decreasing its water-

absorbing capabilities– Plowpan = a hard layer resulting from repeated

plowing that resists water infiltration and root penetration

• Soil pH = influences a soil’s ability to support plant growth– Soils that are too acidic or basic can kill plants

Page 50: 3-1 ATB

Cation exchange is vital for plant growth

• Cation exchange = process that allows plants to gain nutrients– Negatively charged soils hold cations (positively

charged ions) of calcium, magnesium, and potassium

• Cation exchange capacity = a soil’s ability to hold cations, preventing them from leaching, thereby increasing their availability to plants

• A useful measure of soil fertility• Greatest in fine soils

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Regional differences in soils affect agriculture

• Rainforests have high primary productivity, but the nutrients are in plants, not the soil– Rain leaches minerals and

nutrients deeper into the soil, reducing their accessibility to roots

– Swidden agriculture = cultivation of a plot for a few years and then letting it regrow into forest

• Temperate grasslands have lower rainfall and less nutrient leaching

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Erosion degrades ecosystems and agriculture

• Deposition = the arrival of eroded material at its new location

• Flowing water deposits sediment in river valleys and deltas– Floodplains are excellent for farming

• But, erosion is a problem because it occurs faster than new soil is formed

• Erosion increases through: excessive tilling, overgrazing, and clearing forests

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Soil erodes by several methods

• Plants protect soils form erosion– Removing plants accelerates erosion

• Rill erosion moves the most topsoil, followed by sheet and splash forms of erosion

• Water erosion occurs most easily on steep slopes• Erosion in the U.S. declined between 1982 and 2001

– Soil conservation measures

Despite conservation measures, the U.S. still loses 6 tons of soil for every ton of grain harvested

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Various types of soil erosionSplashSheetRillGully

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Soil erosion is a global problem

• Humans are the primary cause of erosion– It is occurring at unnaturally high rates

• In Africa, erosion over the next 40 years could reduce crop yields by half– Coupled with rapid population growth, some observers

describe the future of agriculture as a crisis situation


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