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erosion
the transport of rocks or other substances by different agents (water, wind, ice)
mechanical weathering
breaking material into smaller pieces without changing the original composition of the material. no change in chemical structure
surface area
determine the area (base x height) of each side and add them up
frost wedging
(mw) water works its way into the rocks, and upon freezing, expands and breaks rocks into smaller pieces
chemical weathering
the decomposition of substances into new substances through a chemical reaction
hydrolysis
(cw) hydrogen reacts with certain minerals, resulting in alteration, and dissolves some minerals completely
oxidation
(cw) oxygen reacts with certain elements resulting in alteration
carbonic acid
CO2 mixes with rain, making it slightly acidic, natural
sulfuric acid
sulfur emitted by industries mix with water can dissolve rocks and minerals
acid rain
sulfer in the air sticks to rain, making it acidic
humus
dead stuff and soil
porosity
amount of space between grains compared to the total value
permeability
how fast water moves through a substance
pore space
amount of space between grains
capillary water
water stuck between grains
water table
the tope of the zone of saturation
aquifer
permeable materials that contain and carry groundwater
aquiclude
impermeable materials, water cannot travel through
zone of saturation
the part of the ground where all pore spaces are filled with water
zone of aeration
area from the water table to the ground surface where the pores are filled with air `
cone of depression
around wells that are sucking up water - water table goes down
subsidence
when the ground surface goes down because pore space collapses
hydraulic gradient
slope of the water table
hydraulic conductivity
permeability
point source pollution
pollution that comes from one specific location
non - point source pollution
comes from many places
darcy’s law
equation used to measure groundwater movement