GEOG 101: DAYS 7 Finishing Population and Starting Soils HOUSEKEEPING ITEMS Another Science and Technology Lecture – “An Overview of Global Fisheries and Aquaculture Production” – on Wednesday in Building 356, Room 209 (auditorium) from 7 to 8. This is a topic we will look at later in the semester as well. Food, Education and Development talks on February 2nd (Monday) in Building 355, Room 211: 10:30-11:45: Sara Dent – “The Power of Young Farmers in the Global Food Movement “ 12:00-1:15: Dawn Morrison – “Re-Indigenizing the Global Food Movement” 1:30-2:45: Brent Mansfield – “The University’s Role in the Global Food Movement” 3:00-4:15: Felix Martinez – “Temporary Foreign Agricultural Workers in Canada 5:00-6:15: Vanessa Goodall – “Seed Sovereignty in Canada” Building 355, Room 211 HOUSEKEEPING ITEMS Interesting item in the folder about how the death of the current king of Saudi Arabia may create space for reforms for women. Already 20% of the seats in the Saudi parliament are reserved for them. However, women are still not allowed to drive and are kept mostly segregated. Resource that might be useful for your alternative midterm assignment: http://enviro.nanaimo.ca/index.cfm?tab_ID=2&content_I D=15 (see whole thing). I would like to do the small group exercise around population issues before we move on. Also: we have been discussing whether population or over-consumption is the main contributor to environmental decline – keeping in mind that they are both factors. How would one go about answering that question? EXTRA CREDIT (VOLUNTARY) HOMEWORK • • • • • Outlines are due on Thursday. I have to cancel my office hour on Thursday to attend convocation, but e-mail me with any issues you have. There are lots of good films on soil and agriculture – Food Matters, Food Inc., The World According to Monsanto, The Future of Food, The Real Dirt on Farmer John, Food Fight, Fresh, King Corn, Super Size Me, The Garden, and Have You Got Milk? If you know of others, let me know. Check out any of them and write a two-page, single-space handwritten response to it, addressing whatever jumps out at you – things you didn’t know, particularly vivid images, ideas for enhancing and conserving soil, or whatever you like, as long as it’s relevant. Try to have it in to me by next Tuesday (Feb. 3rd). UPON SUCCESSFULLY COMPLETING THIS CHAPTER, YOU WILL BE ABLE TO (WE WILL ONLY HIT HIGHLIGHTS, THEN MOVE ON AGRICULTURE) Delineate the fundamentals of soil science, including soil-forming processes Describe some important properties of soil Characterize the role of soils in biogeochemical cycling State the importance of soils for agriculture and in supporting plant growth Identify the causes and predict the consequences of soil erosion and soil degradation Outline the history and explain the basic principles of soil conservation 7-5 SOIL AS A SYSTEM “The nation that destroys its soil destroys itself.” – Franklin D. Roosevelt, Former U.S. President Ganaraska wasteland before World War 2 (northeast of Toronto) Photo courtesy of John Bacher and Ed Borczon SOIL AS AN (ECO)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 It’s like an ecosystem on to itself 7-7 SOIL IS A COMPLEX, DYNAMIC MIXTURE Soil consists of mostly mineral matter with varying proportions of organic matter, the rest is pore space taken up by air, water, and other soil gases Parent material = the base geologic material of soil Determines the starting composition of the soil Organic matter includes living and dead microorganisms as well as decaying plant and animal material Water – is not pure, contains dissolved minerals and organics and is important for support of plant growth Air – soil air is not the same as air we breathe Soil can have an influence on a region’s ecosystem 7-8 SOIL FORMATION IS SLOW AND COMPLEX Soil formation begins when parent material is exposed to the effects of the atmosphere, hydrosphere, and biosphere Parent material can be lava, volcanic ash, rock, dunes or most commonly, 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 7-9 SOIL FORMATION IS SLOW AND COMPLEX (CONT’D) 7-10 SOIL FORMATION IS SLOW AND COMPLEX (CONT’D) Biological activity includes deposition, decomposition, and accumulation of organic matter Humus = a dark, spongy, crumbly mass of material formed by partial decomposition Erosion = the dislodging and movement of soil by wind or water Occurs when vegetation is absent When deposited elsewhere referred to as sediment 7-11 weighing the issues EARTH’S SOIL RESOURCES It can take anywhere from 500 to 100 years to produce 1 cm of natural topsoil, depending on local conditions. Much of Canada’s land area was scraped free of soil during the last glaciation by the passage of huge ice masses, which retreated about 10,000 years ago. Today much of interior and northern Canada still lacks soil. Given this very long renewal time, is soil truly a renewable resource? How should the very long renewal time influence soil management? 7-12 A SOIL PROFILE CONSISTS OF LAYERS KNOWN AS HORIZONS Horizon = each layer of soil Soil profile = the cross-section of soil as a whole Topsoil = inorganic and organic material most nutritive for plants Leaching = dissolved particles move down through horizons Litter = surface deposits of leaves, branches, mosses, animal waste 7-13 A SOIL PROFILE CONSISTS OF LAYERS KNOWN AS HORIZONS (CONT’D) O Horizon – peat deposits A Horizon – topsoil B Horizon = subsoil, hardpan C Horizon = broken parent material R Horizon = unaltered parent material W Horizon = distinct layer of water in some soils Permafrost = some arctic soils contain a perennially frozen layer 7-14 SOILS VARY IN COLOUR, TEXTURE, STRUCTURE, AND PH Soils are classified into 10 orders based largely on the processes thought to form them Soils classified into various categories using properties such as: Color Texture Structure pH Near Nanaimo, the soils tend to be HumoFerric Podzols and Distric Brunisols 7-15 SOILS VARY IN COLOUR, TEXTURE, STRUCTURE, AND PH (CONT’D) Soil color = indicates its composition and fertility Black or dark brown = rich in organic matter Pale gray or white = indicates leaching 7-16 SOILS VARY IN COLOUR, TEXTURE, STRUCTURE, AND PH (CONT’D) • Soil texture = the size of particles - Clay (smallest), silt, sand (largest) • 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 • Silty soils with medium-size pores, or loamy soils with mixtures of pore sizes are best for plant growth and crop agriculture 7-17 SOILS VARY IN COLOUR, TEXTURE, STRUCTURE, AND PH (CONT’D) Soil structure (“tilth”= a measure of soil’s “clumpiness” Large clumps can discourage plant roots Repeated tilling compacts soil 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 7-18 BIOGEOCHEMICAL CYCLING IN SOIL 7-19 SOIL IS AN IMPORTANT TERRESTRIAL RESERVOIR FOR CARBON Soil plays a crucial role in the global carbon cycle Soil represents the largest terrestrial reservoir for carbon Main carbon fluxes in which soil is involved are driven by photosynthesis and the production of organic matter, followed by respiration and decay or organic matter Decay of soil organic matter produces soil gas that contains carbon Carbon dioxide Methane 7-20 One source I saw said twice that of atmospheric content and three times that of vegetation! See http://eusoi ls.jrc.ec.eu ropa.eu/pr ojects/SO CO/FactSh eets/ENFa ctSheet03.pdf SOIL DEGRADATION: A GLOBAL CONCERN 7-22 SOIL DEGRADATION: A GLOBAL CONCERN 7-23 SOIL DEGRADATION: A GLOBAL CONCERN Soil degradation results from deforestation, agriculture and overgrazing Over the past 50 years, soil degradation has reduced global grain production by 13% 7-24 REGIONAL DIFFERENCES AFFECT SOIL PRODUCTIVITY Rainforests have high primary productivity, but the nutrients are in plants, not the soil. If the forests are removed, the soils dry out and cannot readily be regenerated. 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 7-25 EROSION CAN DEGRADE ECOSYSTEMS AND AGRICULTURE Deposition = the arrival of eroded material at its new location Flowing water deposits sediment in river valleys and deltas Floodplains (e.g. Fraser Delta) are excellent for farming Erosion occurs faster than new soil is formed Erosion increases through: overcultivating fields, overgrazing rangelands, and clearing forested areas 7-26 SOIL ERODES BY SEVERAL MECHANISMS Wind (aeolian) erosion Water erosion (splash, sheet, rill, gully) Rill erosion moves the most topsoil, followed by sheet and splash erosion Gully erosion 7-27 SOIL EROSION IS WIDESPREAD Humans are the primary cause of erosion 19 billion hectares of croplands worldwide suffer from erosion Kazakhstan lost tens of millions of hectares to wind erosion Soil degradation over the next 40 years in Africa could reduce crop yields by half The on-farm cost of agricultural land degradation in Canada is $670 million per year 7-28 DESERTIFICATION REDUCES PRODUCTIVITY OF ARID LANDS Desertification A loss of more than 10% productivity from erosion, soil compaction, forest removal, overgrazing, salinization, climate change, depletion of water sources A type of land degradation Affects 1/3 of the planet’s land area Most prone areas are arid and semiarid lands Climate change could result in displacement of 50 million people in 10 years 7-29 THE DUST BOWL WAS A MONUMENTAL EVENT IN NORTH AMERICA (CONT’D) Native prairie grasses originally held erosion-prone soils in place 1879-1929: Widespread cultivation of wheat, and grazing of many thousands of cattle Great Depression brought a cycle of poverty and overly intensive agricultural practices Dust storms (black blizzards) travelled up to 2000 km Lung irritation, dust pneumonia, grasshopper infestations 7-30 THE DUST BOWL WAS A MONUMENTAL EVENT IN NORTH AMERICA (CONT’D) 7-31 PROTECTING SOILS 7-32 EROSION-CONTROL PRACTICES PROTECT AND RESTORE PLANT COVER Crop rotation Contour farming Intercropping and agroforestry Terracing Shelterbelts Reduced tillage 7-33 CROP ROTATION Intercropping Crop Rotation = alternating • Intercropping = planting the crops grown field from one different types of crops in season or year to the next alternating bands or other Cover crops protect soil spatially mixed arrangements to increase ground cover 7-34 Contour Farming • Contour Farming = plowing furrows sideways across a hillside, perpendicular to its slope, to prevent rills and gullies Terracing Terracing = level platforms are cut into steep hillsides, forming a “staircase” to contain water 7-35 SHELTERBELTS Shelterbelts or Windbreaks = rows of tall, perennial plants are planted along the edges of fields to slow the wind Alley cropping = shelterbelts + intercropping Reduced tillage • Reduced Tillage = furrows are cut in the soil, a seed is dropped in and the furrow is closed 7-36 IRRIGATION CAN CAUSE LONG-TERM SOIL PROBLEMS Irrigation = Artificially providing water to support agriculture Waterlogging = over-irrigated soils which suffocates roots Salinization = the buildup of salts in surface soil layers Salinization inhibits production of 20% of all irrigated cropland, costing more than $11 billion/year 7-37 IRRIGATION CAN CAUSE LONG-TERM SOIL PROBLEMS (CONT’D) Remedies for correcting salinization once it has occurred: Choose crops appropriate for the area Irrigate with low-salt water Irrigate efficiently Drip irrigation targets water directly to plants 7-38 OTHER CHEMICALS ALSO CONTRIBUTE TO SOIL CONTAMINATION Fertilizer = substances that contain essential nutrients but over-application can damage soils Inorganic fertilizers = mined or synthetically manufactured mineral supplements Organic fertilizers = the remains or wastes of organisms manure, crop residues, fresh vegetation Compost = produced when decomposers break down organic matter Not perfect when it gets into the water system, particularly manure 7-39 OTHER CHEMICALS ALSO CONTRIBUTE TO SOIL CONTAMINATION (CONT’D) Nitrogen and phosphorous runoff from farms and other sources can lead to algal blooms Nitrates can leach through soil and contaminate groundwater Pesticides are another source of soil contamination Industrial activity contaminates soil through inappropriate disposal of wastes and improper storage 7-40 GRAZING PRACTICES CAN CONTRIBUTE TO SOIL DEGRADATION Overgrazing is largely responsible for the permanent drying out of parts of the Mediterranean – e.g. Greece and Syria 7-41 CONCLUSION The preservation of arable soil is crucial for the maintenance of global food security Programs in Canada and worldwide have been successful in reducing topsoil erosion However, soil is still being degraded at a rate that threatens the sustainability of the resource The role of soil as a reservoir in biogeochemical cycling is also of increasing interest to scientists 7-42 QUESTION: REVIEW Physical weathering is characterized by: a) b) c) d) The chemical interaction of water with parent material Organisms breaking down parent material Wind or rain breaking down parent material The dislodging or movement of soil by wind 7-43 QUESTION: REVIEW Which horizon is the most valuable for agriculture? a) b) c) d) A horizon B horizon C horizon R horizon 7-44 QUESTION: REVIEW Erosion increases through all of the following, except: a) b) c) d) Excessive tilling Overgrazing Clearing forests All of the above increase erosion 7-45 QUESTION: REVIEW Which sustainable farming method involves planting rows of trees along field edges to slow the wind? a) b) c) d) Terracing Crop rotation Shelterbelts Contour farming 7-46 QUESTION: WEIGHING THE ISSUES Should developed nations fund reforestation projects in developing nations to combat erosion and deforestation? a) b) c) d) Absolutely, developing nations are facing a crisis No, not with money, but developed nations could give advice No, developed nations had to solve their problems, let the others solve their own problems I don’t care, it doesn’t really affect me 7-47 QUESTION: WEIGHING THE ISSUES Should the Canadian government provide farmers with financial incentives to use technologies such as no-till farming and crop rotation? a) b) c) d) Absolutely, farmers may be more likely to switch to these techniques Yes, but farmers must put any money received into the farm No, it’s not the government’s job to interfere with farming practices I don’t care, it doesn’t really affect me 7-48