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Food
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Land use has increased exponentially with…
human population
What has happened more recently?
Traditional agriculture
Industrialized agriculture
Green Revolution
Traditional agriculture:
Making use of human and animal labor
Industrialized agriculture (1950s-present):
mass production by machines and technology
Green Revolution (1970s-1990s):
Widespread adoption across the world
Industrialized agriculture
Yield has increased faster than population
We currently produce enough food to meet the calorie needs of about 10 billion people
Yield
harvested product / unit land
Farming is the…
largest use of habitable land
Challenges in Agriculture
Population continues to grow! (expected to surpass 10 billion in 2060)
We have passed “peak agricultural land”
Livestock takes up more land than crops
How do we make the best use of the land we have?
Soils?
Pests?
Crops, animals to farm?
Nutrients
Elements and compounds needed by plants come from soils
Biogeochemical cycles:
exchange of elements between different parts of the Earth system (land, water, air)
Macronutrients of soil
nitrogen (N), phosphorus (P), potassium (K)
Other nutrients of soil
calcium (Ca), magnesium (Mg ), iron (Fe), zinc (Zn)
Parent material of soil
P, K, Ca Mg
Organic Material of Soil
N, P, K, Ca, Mg
Atmosphere Material
N
Nitrogen cycle
Only nitrate (NO3-) and ammonium (NH4+) are useable by plants
Formed by decomposers and nitrogen-fixing bacteria
Soluble in water
Denitrifying bacteria
Denitrifying bacteria
respiration converts nitrate back to N2 gas (often in low oxygen)
Nitrogen depletion
Harvesting of crops
Soil erosion
Leaching
Low aeration in soils
Overirrigation or flooded soils
Crop strategies for nitrogen
Leave fields to fallow
Crop rotation
Cover crops
Fertilizers
Crop rotation
Rotate fields between crops to limit nitrogen depletion
Cover crops
keep bacteria active ; take up nutrients to protect against leaching and soil erosion
Fertilizers
add more nutrients
Nutrients added by humans to supplement the supply in nature
Fertilizers
Organic fertilizer
made from the remains of living things elsewhere (e.g. compost, manure)
Inorganic (‘synthetic’) fertilizer
made from non-living materials by chemical processes
• Potassium and phosphorous were available before the Industrial Revolution
• Nitrates not available in fertilizer until 1913
Haber – Bosch process (1913):
Synthetic nitrogen
Industrial process to form ammonia from atmospheric nitrogen
A difficult chemical reaction - energy intensive!
Needed an iron catalyst at very high pressures
Enabled mass production of nitrogen fertilizer
Synthetic fertilizers
Estimated 4 billion people are fed due to synthetic fertilizer!
Supports growth of high-yield varieties of crops
Release rapidly into soils
Eutrophication
Excess fertilizers enters waterways
Small inputs collect in lakes, estuaries, and coasts until they cause algae blooms
Rise in decomposer populations as algae die
Eutrophication Impacts
“Dead zones” with low dissolved oxygen (hypoxia)
Harmful algal blooms (HABs)
Impact drinking water resources
Buildup of excess fertilizers in waterways
Eutrophication
Impacts of Eutrophication
Algal blooms – phytoplankton like dinoflagellates, diatoms,
cyanobacteria
Low dissolved oxygen (hypoxia)
Harmful algal blooms – algae that produce toxic compounds
Microcystin in cyanobacteria is a liver toxin!
Contamination of drinking water
Eutrophication - examples
Gulf of Mexico “dead zone”
Hypoxia impacts
Nonpoint source pollution
Harmful algal blooms
Lake Erie
Otterbein Lake (cyanobacteria blooms)
Soils are sensitive to chemical changes
Plants rely on the storage of cation nutrients (+) in soil
Organic matter and clay tend to have (-) charges, store cations
Cation exchange capacity
Ability of a soil to store cations used by plants
Cation exchange is sensitive to changes in soil
pH
Soil erosion
Removal of soil by wind or water
Impacts surface topsoil (O,A horizons) first
Agricultural fields are vulnerable to…
EROSION
• U.S. farmland: average loss of 4 tons/acre/year
Topsoil is eroding…
more quickly than it is formed
1 inch topsoil = at least 100 years to form
Once depleted, it is difficult for topsoil to regenerate
Tillage agriculture
Overturning or digging through the top layer of soil to prepare soil for planting
Promoted in 17th century Europe as a way to “bust up” nutrients in soil
Widely available machinery and tools
Consequences of tillage agriculture
Tillage was first promoted in humid, temperate soils of Europe
Not suited to other biomes (like grasslands!)
Mitigating soil erosion
Reduced or no-till agriculture
Cover crops
Contour farming
Reduced or no-till agriculture
Till in a limited way, use specialized equipment, or simply leave leftover crops to decompose in the field