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Soil and Food Lecture 7 EB 2008

Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

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Page 1: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil and FoodSoil and Food

Lecture 7

EB 2008

Lecture 7

EB 2008

Page 2: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

AgendaAgenda

• Two fold– 1) Understanding soil– 2) Understanding farming and food production

• Two fold– 1) Understanding soil– 2) Understanding farming and food production

Page 3: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Case Study ACase Study A

• No-Till farming in Brazil• Started in Southern Brazil• Tried to follow the European method of farming -

plowing and planting• Failed - resulted in erosion - soil was washed or

blow away• Had to find alternative…• No-Till farming = leave it alone…• Reduced erosion by 90%

• No-Till farming in Brazil• Started in Southern Brazil• Tried to follow the European method of farming -

plowing and planting• Failed - resulted in erosion - soil was washed or

blow away• Had to find alternative…• No-Till farming = leave it alone…• Reduced erosion by 90%

Page 4: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Tilling No-till farming

Page 5: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil & farmingSoil & farming

• Agriculture = practice of raising crops and livestock for human use and consumption

• Cropland = land used to raise plants

• Rangeland = land used for grazing livestock

• Agriculture = practice of raising crops and livestock for human use and consumption

• Cropland = land used to raise plants

• Rangeland = land used for grazing livestock

Page 6: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Traditional vs. IndustrializedTraditional vs. Industrialized

• Traditional Agriculture = still uses man or animal power, with simple tool use

• Industrialized Agriculture = use of powerful machines and synthetic fertilizers

• Traditional Agriculture = still uses man or animal power, with simple tool use

• Industrialized Agriculture = use of powerful machines and synthetic fertilizers

Page 7: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

First farmersFirst farmers

• In human history

• We started agriculture about 10,000 years ago

• It seems that lots of tribe go the same idea about the same time…

• In human history

• We started agriculture about 10,000 years ago

• It seems that lots of tribe go the same idea about the same time…

Page 8: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

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Modern agriculture = more foodModern agriculture = more food

• 38% of the landmass of the planet is used for agriculture

• It is going to be hard to use the rest– Living land– Sensitive land– Unsuitable for some other reason– ???

• So we have to use this 38% more efficiently• However, bad practices lead to more problems.

– Run off, deforestation, desertification, pollution (air, land, water), toxic chemicals, erosion, etc.

• 38% of the landmass of the planet is used for agriculture

• It is going to be hard to use the rest– Living land– Sensitive land– Unsuitable for some other reason– ???

• So we have to use this 38% more efficiently• However, bad practices lead to more problems.

– Run off, deforestation, desertification, pollution (air, land, water), toxic chemicals, erosion, etc.

Page 11: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

EB’s need to understand SoilEB’s need to understand Soil

• Soil is complex and heavily infiltrated by living things.

• 2 parts– Inorganic matter

• Granulated rock• Minerals (50%)• Gases• Water (45%)

– Biotic component (5%)• Bacteria• Fungi• Waste• Dead matter

• Soil is complex and heavily infiltrated by living things.

• 2 parts– Inorganic matter

• Granulated rock• Minerals (50%)• Gases• Water (45%)

– Biotic component (5%)• Bacteria• Fungi• Waste• Dead matter

Page 12: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil formation is slow and complexSoil formation is slow and complex

• Rocks are weathered into soil• Rocks are weathered into soil

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Page 13: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Horizons? - Soil profilesHorizons? - Soil profiles

• Over time distinct layers develop

• These layers are known as horizons

• The total profile from top soil to bedrock is known as a soil profile…

• Over time distinct layers develop

• These layers are known as horizons

• The total profile from top soil to bedrock is known as a soil profile…

Page 14: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

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•The uppermost layer (the O horizon, or litter layer) consists mostly of organic matter deposited by organisms. •Below it lies the A horizon, or topsoil, consisting of some organic material mixed with mineral components. •Minerals and organic matter tend to leach out of the E horizon down into the •B horizon, or subsoil, where they accumulate. •The C horizon consists largely of weathered parent material unaltered or only slightly altered by the processes of soil formation. •The C horizon may overlie an R horizon of pure parent material.

Page 15: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

LayeringLayering

• Material moves from one layer to the next via leaching - carried by water

• This can be slow or very fast

• Sometimes too fast and the soil cannot support plant life…

• Material moves from one layer to the next via leaching - carried by water

• This can be slow or very fast

• Sometimes too fast and the soil cannot support plant life…

Page 16: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

THINK!THINK!

• It can take hundreds to thousands of years to produce just 1 inch of topsoil.

• Do you think such a resource should be considered ‘renewable’?

• How would you define a ‘renewable resource’? • How do you think soil’s long renewal time should

influence its management? • What types of practices encourage the formation

of new topsoil?

• It can take hundreds to thousands of years to produce just 1 inch of topsoil.

• Do you think such a resource should be considered ‘renewable’?

• How would you define a ‘renewable resource’? • How do you think soil’s long renewal time should

influence its management? • What types of practices encourage the formation

of new topsoil?

Page 17: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil can be characterized by color, texture, structure, and pHSoil can be characterized by color, texture, structure, and pH

• The color of soil can indicate its composition and sometimes its fertility.– Black or dark brown soils are usually rich in

organic matter, whereas a pale gray to white color often indicates leaching or low organic content.

• The color of soil can indicate its composition and sometimes its fertility.– Black or dark brown soils are usually rich in

organic matter, whereas a pale gray to white color often indicates leaching or low organic content.

Page 18: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil can be characterized by color, texture, structure, and pHSoil can be characterized by color, texture, structure, and pH

• Soil texture is determined by the size of particles and is the basis on which the United States Department of Agriculture (USDA) assigns soils to one of three general categories – Clay consists of particles less than 0.002 mm in diameter, – Silt of particles 0.002 ミ 0.05 mm, and – Sand of particles 0.05 ミ 2 mm.

• Sand grains, as any beachgoer knows, are large enough to see individually and do not adhere to one another. Clay particles, in contrast, readily adhere to one another and give clay a sticky feeling when moist.

• Soil with a relatively even mixture of the three particle sizes is known as loam.

• Soil texture is determined by the size of particles and is the basis on which the United States Department of Agriculture (USDA) assigns soils to one of three general categories – Clay consists of particles less than 0.002 mm in diameter, – Silt of particles 0.002 ミ 0.05 mm, and – Sand of particles 0.05 ミ 2 mm.

• Sand grains, as any beachgoer knows, are large enough to see individually and do not adhere to one another. Clay particles, in contrast, readily adhere to one another and give clay a sticky feeling when moist.

• Soil with a relatively even mixture of the three particle sizes is known as loam.

Page 19: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

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• Soil structure is a measure of the “clumpiness” of soil. Some degree of structure encourages soil productivity, and biological activity helps promote this structure.

• pH - The degree of acidity or alkalinity influences a soil’s ability to support plant growth.

• Soil structure is a measure of the “clumpiness” of soil. Some degree of structure encourages soil productivity, and biological activity helps promote this structure.

• pH - The degree of acidity or alkalinity influences a soil’s ability to support plant growth.

Page 21: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Regional differences in soil traits can affect agricultureRegional differences in soil traits can affect agriculture

• Soil characteristics and soil profiles vary from place to place

• Given a choice would you like to establish your farm in the Amazon with its lush forest, or in the central valley here?

• Soil characteristics and soil profiles vary from place to place

• Given a choice would you like to establish your farm in the Amazon with its lush forest, or in the central valley here?

Page 22: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Different environments - different outcomesDifferent environments - different outcomes

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ErosionDesertificationSalinizationWaterloggingnutrient depletionstructural breakdownpollution.

Page 23: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Erosion can degrade ecosystems and agricultureErosion can degrade ecosystems and agriculture

Erosion is the loss of topsoil…

• Overcultivating fields through poor planning or excessive tilling

• Overgrazing rangelands with more livestock than the land can support

• Clearing forests on steep slopes or with large clear-cuts

Erosion is the loss of topsoil…

• Overcultivating fields through poor planning or excessive tilling

• Overgrazing rangelands with more livestock than the land can support

• Clearing forests on steep slopes or with large clear-cuts

Page 24: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Soil erodes by several mechanismsSoil erodes by several mechanisms• Removing plant cover nearly always accelerates

erosion• Several types of erosion can occur, including wind

erosion and four principal kinds of water erosiona) Splash erosion occurs as raindrops dislodge soil particles

that fill in gaps between remaining clumps, decreasing the soil ユ s ability to absorb water.

b) sheet erosion, water flows in thin sheets over broad surfaces, washing topsoil away in uniform layers.

c) rill erosion, water runs along small furrows, deepening and widening them into channels called rills. Rills can merge to form larger channels and eventually gullies.

d) Gully erosion (d) cuts deeply into soil, leaving large gullies that expand as erosion proceeds.

• Removing plant cover nearly always accelerates erosion

• Several types of erosion can occur, including wind erosion and four principal kinds of water erosiona) Splash erosion occurs as raindrops dislodge soil particles

that fill in gaps between remaining clumps, decreasing the soil ユ s ability to absorb water.

b) sheet erosion, water flows in thin sheets over broad surfaces, washing topsoil away in uniform layers.

c) rill erosion, water runs along small furrows, deepening and widening them into channels called rills. Rills can merge to form larger channels and eventually gullies.

d) Gully erosion (d) cuts deeply into soil, leaving large gullies that expand as erosion proceeds.

Page 25: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Food ProductionFood Production

Page 26: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Facts of life…Facts of life…

• The population is expected to hit 9 billion by 2050• We have been able to produce food faster than

population growth (so far)• Still…

– 13% of the population is hungry• Some are undernourished• Others suffer from malnutrition• Someone dies every few seconds

– Some are overnourished• Fat (3/5)• Obese (1/4)• Heath effects, shorter life spans, expensive solutions.

• The population is expected to hit 9 billion by 2050• We have been able to produce food faster than

population growth (so far)• Still…

– 13% of the population is hungry• Some are undernourished• Others suffer from malnutrition• Someone dies every few seconds

– Some are overnourished• Fat (3/5)• Obese (1/4)• Heath effects, shorter life spans, expensive solutions.

Page 27: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Bad Practices in AgricultureBad Practices in Agriculture

• In the past people used polyculture…• Now over 25% of our farmland is

monoculture…• We are seeing signs that there is a

reduction in the food yield compared to the bumper crops of 1985– Soils are in decline and pollution on the

increase.– What will happen in the next 40 years?

• In the past people used polyculture…• Now over 25% of our farmland is

monoculture…• We are seeing signs that there is a

reduction in the food yield compared to the bumper crops of 1985– Soils are in decline and pollution on the

increase.– What will happen in the next 40 years?

Page 28: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Green revolutionGreen revolution

• The introduction of industrialized agriculture to the developing world.

• Designed to increase yields per acre• However, total yields rose 33% between

1900 and 2000• But consumption of energy to get these

gains by 800%• Had both positive and negative outcomes.• Is this worth it?

• The introduction of industrialized agriculture to the developing world.

• Designed to increase yields per acre• However, total yields rose 33% between

1900 and 2000• But consumption of energy to get these

gains by 800%• Had both positive and negative outcomes.• Is this worth it?

Page 29: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Pest and PollinatorsPest and Pollinators

• Pest - are organisms that damage our crops• Weeds - are plants that compete with our crops• Widespread use of chemicals to control these

– Insecticides– Pesticides– Herbicides– Fungicides

• Since 1960 the use of pesticides has shot up 400%

• Pest - are organisms that damage our crops• Weeds - are plants that compete with our crops• Widespread use of chemicals to control these

– Insecticides– Pesticides– Herbicides– Fungicides

• Since 1960 the use of pesticides has shot up 400%

Page 30: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Evolution of ResistanceEvolution of Resistance

• Chemicals may not kill 100% of the pests.• Those that survive will have babies that are also

resistant.• This will negate the effects of the chemicals very

quickly• Biological controls have the same outcome..in

some cases– Prickly pear example.

• Better weapon is IPM (Integrated pest management) - a custom solution to each problem.

• Chemicals may not kill 100% of the pests.• Those that survive will have babies that are also

resistant.• This will negate the effects of the chemicals very

quickly• Biological controls have the same outcome..in

some cases– Prickly pear example.

• Better weapon is IPM (Integrated pest management) - a custom solution to each problem.

Page 31: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Insects are importantInsects are important

• Plants may be wind pollinated or insect pollinated.

• Bees and the like perform pollination

• Remove the bees and we have a problem…

• Plants may be wind pollinated or insect pollinated.

• Bees and the like perform pollination

• Remove the bees and we have a problem…

Page 32: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

GM foodsGM foods

• Genetic engineering of plants and animals to aid us with food production

• Manipulate the DNA of the organism

• GM - Genetically Modified

• Place genes for desirable traits into our crops and livestock.

• Genetic engineering of plants and animals to aid us with food production

• Manipulate the DNA of the organism

• GM - Genetically Modified

• Place genes for desirable traits into our crops and livestock.

Page 33: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Feedlot AgricultureFeedlot Agriculture

• More wealth equals a greater demand for meats.• Feedlots = factory farms = churn out meat by

intensive, density driven, high calorie diet feed.• Reduce impact on the environment, but only of

managed properly• In the future we may have to give up meat every

day!!!• Energy loss from one trophic level to the next is

at 90%.• Land and water equivalents have been

calculated…

• More wealth equals a greater demand for meats.• Feedlots = factory farms = churn out meat by

intensive, density driven, high calorie diet feed.• Reduce impact on the environment, but only of

managed properly• In the future we may have to give up meat every

day!!!• Energy loss from one trophic level to the next is

at 90%.• Land and water equivalents have been

calculated…

Page 34: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

In you books there are some great figures comparing

a) The amount of feed input per kg of produceb) The amount of land needed to produce producec) The water usage per kg of produce

Please look these over for next weeks quiz…

Page 35: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

Sustainable AgricultureSustainable Agriculture

• A form of farming that does not deplete resources - land or water.

• Still uses low amounts of pesticides, fertilizers, growth hormones, etc.

• Organic farming uses none.

• More people are turning to organic produce.

• A form of farming that does not deplete resources - land or water.

• Still uses low amounts of pesticides, fertilizers, growth hormones, etc.

• Organic farming uses none.

• More people are turning to organic produce.

Page 36: Soil and Food Lecture 7 EB 2008 Lecture 7 EB 2008

ConclusionsConclusions

• Which way to go…

• How best to feed the growing population, without destruction of both the soil or the environment.

• A solution must be found now, before the collapse of agriculture.

• Which way to go…

• How best to feed the growing population, without destruction of both the soil or the environment.

• A solution must be found now, before the collapse of agriculture.