Earth Mat Flashcards - Ch 12
relation of slopes to weathering
steep : short term and incomplete decomp
gentle : long term more thorough
The pressure exerted on buried rock objects at depth is referred to as
lithostatic pressure or confining pressure
the decrease in lithostatic pressure or load
unloading or confining pressure
fractures sub parralel to surface
sheet joints
sheet joints resembling onions
exfoliation
kind of frost action that occurs along fractures oriented steep to surface
frost wedging
kind of frost action that develops along bedding planes and/or sheet fractures
frost heaving
occurs when clays and micas expand and wetted
slaking
result from daily or seasonal changes in rock temp that cause significant amounts of disintigration
thermal volume changes / insolation
an example of interplay between disintigeration and decomposition where spaced rectangular joints develop into spheroidal forms
spheroidal weathering
most significant agent of decomposition
downward pecrolating water
occurs when a mineral or other soil component is wholly or partially dissolved during chemical decomposition
dissolution
Major decomp process
Dissolution
Ion Exchange
Hydrolysis
Hydration
Oxidation
Chelation
occurs when ions are directly exchanged between a mineral and a solution.
Ion exchange
is a chemical reaction between a mineral and water in which dissolved hydrogen ions and/or hydroxyl ions are added to form one or more new minerals.
hydrolysis
most abundant group of new minerals produced during chemical decomposition
clays
hydrolysis product of Feldspars? Mafics?
Kaolinite and Orthosilicic Acid
Pyrolusite and Orthosilicic acid
Orthosilisic acid is also known as
dissolved silica
involves the addition of water to a crystal structure during the reaction between a mineral and the aqueous solution.
Hydration
the anhydrous calcium sulfate mineral? its hydrated counterpart?
anhydrite; gypsum
the anhydrous iron oxide mineral? its hydrated counterpart?
hematite; goethite
chemical rxn where electrons are transferred from a cation in the mineral to an anion, increasing its valence
Oxidation
requirement of oxide mineral formation
loss of electrons
oxidation product of fayalite
hematite
oxidation product of rhodonite
manganite
hematite can also be the oxidation product of which sulfide
pyrite
how does hematite turn back to pyrite
through reduction rxn
combination with sulfate and the conversion of ferric (+3) to ferrous (+2)
organic hydrocarbon ring complexes produced by lichen and humus decay
chelates