Read the notes, then try the practice. It adapts as you go.When you're ready.
Session Length
~17 min
Adaptive Checks
15 questions
Transfer Probes
8
Soil science is the study of soil as a natural resource, encompassing its formation, classification, physical and chemical properties, biological processes, and role in sustaining terrestrial life. Often called pedology when focused on soil formation and morphology, or edaphology when examining how soils influence living organisms, the discipline integrates concepts from geology, chemistry, biology, and ecology. Soil is far more than inert dirt beneath our feet; it is a dynamic, living system composed of minerals, organic matter, water, air, and an astonishing diversity of microorganisms that together regulate nutrient cycling, water filtration, carbon storage, and plant productivity.
The formation of soil, known as pedogenesis, unfolds over centuries to millennia through the interplay of five soil-forming factors identified by Hans Jenny: climate, organisms, relief (topography), parent material, and time. These factors drive weathering of rock into mineral particles, accumulation and decomposition of organic matter, and the development of distinct soil horizons visible in a soil profile. Scientists classify soils into twelve major orders under the USDA Soil Taxonomy system, ranging from young and minimally developed Entisols to the highly weathered Oxisols of tropical regions. Understanding these classification systems is essential for predicting soil behavior across landscapes.
Soil science has profound practical importance for agriculture, environmental management, and climate change mitigation. Healthy soils underpin global food security by supplying essential nutrients and water to crops, while degraded soils threaten both productivity and ecosystem stability. Soil organic carbon represents one of the largest terrestrial carbon pools, and practices such as cover cropping, reduced tillage, and composting can sequester atmospheric carbon dioxide in soils. As the world confronts challenges of feeding a growing population, remediating contaminated land, and adapting to shifting climate patterns, soil science provides the foundational knowledge necessary for sustainable land management.
One step at a time.
Distinct horizontal layers within a soil profile, each differing in color, texture, structure, and chemical composition. The major horizons are O (organic), A (topsoil), E (eluviation), B (subsoil), C (parent material), and R (bedrock).
Example: Digging a pit in a forest reveals a dark, humus-rich A horizon at the surface, underlain by a lighter E horizon from which minerals have leached, above a reddish-brown B horizon where those minerals accumulate.
The relative proportions of sand, silt, and clay particles in a soil sample. Texture governs water-holding capacity, drainage, aeration, and nutrient retention, and is classified using the USDA soil texture triangle.
Example: A sandy loam drains quickly and warms up fast in spring, making it ideal for early-season vegetable production, whereas a clay soil retains moisture longer but is prone to waterlogging.
A measure of a soil's ability to hold and supply positively charged nutrient ions (cations) such as calcium, magnesium, potassium, and ammonium. Higher CEC indicates greater fertility potential.
Example: A soil dominated by montmorillonite clay may have a CEC of 80-120 cmol/kg, readily supplying nutrients to crops, while a kaolinite-dominated soil may have a CEC below 10 cmol/kg and require frequent fertilization.
The fraction of the soil composed of plant and animal residues at various stages of decomposition, along with living microbial biomass. SOM improves soil structure, water retention, nutrient supply, and biological activity.
Example: Adding compost to a garden increases soil organic matter, which darkens the soil color, improves its ability to hold water during dry spells, and feeds beneficial earthworms and microorganisms.
The natural process of soil formation through the weathering of rock and the accumulation and transformation of organic material over time, driven by the five soil-forming factors: climate, organisms, relief, parent material, and time.
Example: Volcanic ash deposited on a tropical hillside gradually weathers into andisol over thousands of years as rainfall, vegetation, and microbial activity transform the mineral material into distinct soil horizons.
A measure of the acidity or alkalinity of a soil solution on a scale from 0 to 14. Soil pH strongly influences nutrient availability, microbial activity, and plant growth, with most crops thriving between pH 6.0 and 7.5.
Example: Blueberries require acidic soil with a pH of 4.5 to 5.5, so growers often amend soil with elemental sulfur or acidic peat moss to lower the pH to the desired range.
The series of biogeochemical transformations by which nitrogen moves between the atmosphere, soil organic matter, and living organisms, including fixation, mineralization, nitrification, denitrification, and immobilization.
Example: Rhizobium bacteria in the root nodules of legumes fix atmospheric nitrogen gas into ammonium, which is then converted by Nitrosomonas and Nitrobacter bacteria into nitrate that neighboring plants can absorb.
The arrangement of individual soil particles (sand, silt, clay) into aggregates or peds of various shapes and sizes. Good structure creates pore spaces that facilitate root growth, water movement, and gas exchange.
Example: A well-structured granular topsoil in a no-till field has abundant macropores from earthworm channels and root decay, allowing rainwater to infiltrate rapidly rather than running off the surface.
More terms are available in the glossary.
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