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Weathering and Soil

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AB
mechanical weatheringthe breakdown of rock into smaller pieces by physical means
oxidationa chemical reaction in which an element, such as iron, combines with oxygen to form an oxide
weatheringthe process by which rock materials are broken down by the action of physical or chemical processes
acid precipitationrain, sleet, or snow that contains a high concentration of acids
abrasionthe grinding and wearing away of rock surfaces through the mechanical action of other rock or sand particles
chemical weatheringthe process by which rocks break down as a result of chemical reactions
transported soilsoil that is blown or washed away from its parent rock
bedrockthe layer of rock beneath the soil
soila loose mixture of small mineral fragments, organic material, water, and air that can support the growth of vegetation
parent rockthe source of mineral fragments in the soil
soil conservationa method to maintain the fertility of the soil by protecting the soil from erosion and nutrient loss
soil texturesoil quality based on the relative size of soil particles
soil structurethe arrangement of soil particles
humusthe organic material formed in soil from the decayed remains of plants and animals
leachingthe removal from soil of substances that can be dissolved in water
Agents of Mechanical Weatheringice, abrasion, wind, water, gravity, plants, and animals
Agents of Chemical Weatheringwater, acid precipitation, acids in groundwater, acids in living things, air
4 steps of Ice Wedging1. Water seeps into cracks. 2. Water freezes and expands. 3. Ice widens cracks. 4. The rock splits apart.
Soil with a pH higher than 7The soil is basic.
Soil with a pH lower than 7The soil is acidic.
Soil with a pH of 7The soil is neutral.
lichensproduce acids that can slowly break down rock by chemical weathering
ice wedginga type of mechanical weathering which is also a type of frost action


Grade 6 Science
Madison Junior School
Madison, NJ

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