Definitions
Weathering: processes that break up and corrode solid rock, transforming it into sedimentary rock
Erosion: the removal and transport of Earth’s surface materials by moving water, air, or ice
Weathering & Carbon Cycles: natural processes and the regulation of greenhouse gas, temperature
solid rock broken down contains C, release C once weathered
plant consumption in soil
into the atmosphere as a gas
Globally warm- the more plant growth, the more precipitation
increases the rate of rainfall
increase of CO2 removal by weathering
reduction of initial warming
Mechanical Weathering: Jointing, Wedging, Organism Activity, Abrasion
Definition: breaks down rock into smaller pieces, this does not effect the composition of minerals or chemicals found in the rock
Jointing/Exfoliation: natural cracks due to temperature/pressure change
Joints: are sets of cracks that are parallel, shows how/direction the pressure moved through the rock
Thermal expansion: increase of heat expands the outer layer as the rock is cooling and causes it to contract
need heat and cool
after forest fires, when magma passes by, the sun
Columnar Jointing: molten rock of a volcano starts to cool, the inside it hotter than the outside causes the outside to crack. They are vertical along the outside of a volcano, from the top each ridge has a hexagonal cap
Wedging: expansion in joints
Frost Wedging: ice causing expansion in joints, when water is put under pressure it exerts stress outwards. The the water at the top freezes first.
Root Wedging: roots causing expansion in joints, when roots grow into the joints of a rock
Salt Wedging: growth and expansion of salt crystals in pores and joints
Organism Activity: when organisms create and intensify rock breakage
Abrasion: when rock pieces collide as they are being transported, causing weathering
Chemical Weathering: Hydrolysis, Dissolution, Oxidation, Hydration
Definition: the breakage of rock into smaller pieces through a change in their chemical makeup, which creates more surface area which leads to more weathering
change in minerals, and chemical reaction
chemical changes to minerals that are unstable at Earth’s surface
Hydrolysis: a reaction between a mineral and water
H+ ions are added to the mineral and a chemical equivalent amount of cations are released into the solution
usually leaves pores behind in rocks
Dissolution: mineral breaks down completely into ions by dissolving into a fluid
Acid water, usually leaves large holes in rock
Oxidation: reaction between a mineral and O2
Iron minerals react with O2 to become iron oxide and iron hydroxide minerals, turning orange
Associated with a color change, Iron to orange, copper to green
Hydration: absorption of water into a structure
Clay, with the addition/subtraction of H2O