1. HOW DOES SOIL FORM? GLOBE NY Metro, 2008

2. Why do we study soil? Because It’s A(n) Great integrator Producer and absorber of gases (CO 2 and others) Medium for plant growth Medium of crop production Home to organisms (plants, animals and others) Waste decomposer Snapshot of geologic, climatic, biological, and human history Source material for construction, medicine, art, etc. Filter of water and wastes Essential natural resource Medium of heat and water storage

3. United States Department of Agriculture Soils are very different, depending on how they form

4. 5 FACTORS CONTROL THE TYPE OF SOIL TIME Soil forms by the interaction of the first four factors. It changes to create soil profiles unique for the conditions and elapsed time. A soil profile consist of layers called “soil horizons” TIME is the 5 th factor Soil forms by the interaction of the first four factors. It changes to create soil profiles unique for the conditions and elapsed time. A soil profile consist of layers called “soil horizons” During the GLOBE Soil Characterization protocol, you will describe, sample, and analyze soil horizons near your school Photo courtesy, Ray Weil, PhD Parent Material Topography Climate Living things 4 factors control soil- forming processes

5. ROLES OF THE FIVE FACTORS OF SOIL FORMATION Living things: Living things: Plant roots physically break rocks into small pieces; lichen dissolves rock; burrowing animals mix the soil and help aeration TIME TIME: When bedrock is exposed at the surface, chemical, biologic, and physical processes combine to produce a thin soil layer. Over time, the processes extend vertically downward, developing soil horizons whose position and thickness change over time. Parent material Parent material: Chemical changes during soil formation depend on what minerals and rocks are present. Example: Calcium-rich soils generally form from calcium-rich rocks (like limestone) but not from calcium-poor rocks like granite. Topography: Loose soil stays in place in flat areas, allowing more thorough physical and chemical alteration of its grains. On steep slopes, the soil moves downhill before complete alteration can occur Topography: Loose soil stays in place in flat areas, allowing more thorough physical and chemical alteration of its grains. On steep slopes, the soil moves downhill before complete alteration can occur. Climate: Climate: heat and water accelerate chemical changes (so moist, temperate areas like NYC have different soils than arid, tropical, or polar areas).

6. If all five factors are the same in two geographic regions, the soil will be the same in both. Some basic examples of different soil types include: Temperate deciduous soil Coniferous forest soil Grassland soil Coniferous forest soil Tropical rain forest soil Desert soil

7. Soil is an excellent place to study interactions in the Earth System, including contributions from the Atmosphere Atmosphere Dew (moisture from the air) begins chemical alteration of parent rock Rain erodes loose soil, preventing further alteration temperature controls rate and extent of chemical processes Hydrosphere Hydrosphere Water seeps into the ground, dissolving and redistributing elements evaporation dries soil, changing its physical characteristics Biosphere Biosphere plants add and remove chemicals plant roots anchor soil in place, enabling chemical reactions to be completed animals mix soil; transport seeds, etc. Geosphere Geosphere solid rock and unconsolidated sediment are the parent material for soil geologic processes (surface and internal) expose and bury rock, etc.

8. Hydrologic Cycle and the Soil Color Structure Bulk Density Texture pH Temperature Soil moisture Horizon Depths Soil Properties related to the hydrologic cycle.