1/33
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
Flow eruptions
Coherent lava that is nonexplosive, branching lobe, and sheet-like
Domes eruptions
Circular mound-shaped coherent lava, more viscous (and dome collapse can trigger pyroclastic flows)
Pyroclastic
Fragments of igneous rocks are ejected from explosive volcano
Importance of volcanic gases
Hazardous since they are denser than atmospheric gasses and collect in depressions, hugging the ground, and suffocating organisms
Change in character can sere as eruptions precursor
Larger eruptions influence weather locally & globally
Long term primary source for atmosphere and hydrosphere
Types of Volcanos
Shield Volcanos:
Low angle slopes
Dominated by flows
smaller cinder cones common associate
Made up of basalts
Stratovolcanos:
Higher angle slopes
Dominated by pyroclastic rocks
Explosive eruptions
Larger calderas
Made up of andersite & rhyolite
Basalts
Low viscosity
High extrusion temp
Primarily flow
Denser
48-52% SiO2 content
Dark blackish color
Andersite & Dacite
Medium viscosity
Medium extrusion temp
Primarily as domes & pyroclastics
Less dense
52-68% SiO2 content
Grey in color
Rhyolite
High viscosity
Low extrusion temp
Primarily as domes & pyroclastic
Lower density
Light grey/reddish colored
Super volcanos
Eruptions of magnitude 8 on volcano explosively meaning <1000 km2 of magma are erupted
Hydrothermal Circulation associated w/ volcanoism
magma chamber @ depth provides source of eruption material
Hydrothermal circulation cell: magma chamber heats surrounding groundwater as hot air rises, setting a circulation of water through fractures and cavities of rock
Volcanic geohazards
Lava flows: slow moving ,can block roads, burn crops & homes
Volcanic gases: dense & collect “death” gullies released from caldera lakes
Lahars: intermediate speeds, long runouts, and follow drainage can destroy structures along rivers and contribute to dam failure
Ash: Travels far, can load on structures and collapse, health consequences and damage machinery, siltation changes river behaviors and habitat, and fertilizes plankton growth
Mitigation of volcanic geohazards
Monitoring & warning systems (responsibility of USGS in US)
Evacuation plans/facilities (produce hazard maps/models)
Public edu. abt possibility and how best to respond
Zoning (restriction of placement of critical facilities in certain areas)
Global climate & massive eruptions
Areas unaffected w/ volcanism can still be affected by catastrophic large eruptions bc eruptions send gas & ash into stratosphere that reflects sunlight causing global cooling of several C temp
Source rock
Organics need to be preserved in the rocks that happens in euxinic (O-poor) environments w/ slower anaerobic decay that factors preservation found in restricted marine bodies or lakes
Sulfur compounds are common in euxinic environments
Need a subsiding depression to bury and preserve the sed. & fossil organics
Black shales/limestone are common source rocks—often stinky when breaks fresh face open
Some 50% of source rocks formed in Cretaceous period
Thermal window history
Kerogen: Waxy and complex organics in source rock (immobile)
Kerogen need to be cooked into oil (low simmer) or gas (hotter)
Cooking increases mobility of organics, but temps too high can change organics into less useful forms
Reservoir/ Trap
Need reservoir rock and seal that the mobilized oil &/ gas collect in
Stratigraphic traps (e.g. reefs, channels, or offshore sand bodies) that have porosity
Structural traps: the classic anticline
Fracking technologies
Directional drilling- drills stem can be bent so it’ll drill along a oil rick layer for substantial lengths
Fracking by pumping water under high pressures that it intensely fractures the surrounding layers, creating a fracture porosity and permeability
Propants- Sand or other grains are included in water and left behind in the cracks to prop them open as pressure in reduced by pumping
Chemical additives- decrease the viscosity of oil making it easier to flow and pump, and biocides (active substances, including microorganisms that eliminate harmful organisms) so that microbial sludge won’t grow and plug up the works
Coal formation
Coal forms from peat, which forms in swamps, fens, and other types of wetlands
Euxinic waters (no O2, slow anaerobic decay generates CH4, partial organics accumulation to form peat
Peat→ lignite (soft brown coal)→ bituminous coal (black, harder)→ anthracite (black shiny)
—————————— (Compacting & heating w/ geological burial)——— ———→
Coal quality
Energy content: measured as btu (British thermal unit)/ pound, higher energy=better function of coal
Mineral content: flood in swamp can intro. mud w/ minter matter dispersing in coal, burnt forms fly ash that must be dealt
Sulfur content: Due to mineral pyrite that forms in euxinic enviro. contributes to acid mine runoff & rain. Coal from coastal swamps have more sulfur
coal exploration
surface geological mapping
drilling
have 100s of yrs of reserves (known as deposits in the ground) @ present U.S. rich in coal
Look for old deltas w/ unifromitanism
coal extraction
Underground: Typically $$$, but necessary if coal is @ depth. Enviro. Cost: Coal mine fires & explosions, black lung disease, coal mine collapse & surface subsidence
Surface/ Strip mining: $, safter for miners, works in shallow coal. Enviro. Cost: Destruction of surface soil & biota, acid mine tailing (waste rock from mine) drainages, and groundwater changes
Acid mine runoff
Mine runoff pH is typically 5, 3, and 2 (acidic)
Occurs not only w/ coal mines, but also common w. other mines
pyrite and other sulfide mineral entailing are culprits as they weather easily, oxidizing, and producing acidic water
Only extremophile microbial life can live in very acidic water, leach, and mobilize heavy metal
Acid mine runoff mitigation
limestone helps neutralize (geologic anti-acid)
Reclamation- returning of the mine land to some useable & desired form
Reshaping the landscape to desire from
Replacing topsoil (saved)
Seeding and/planting
Water to est. veg
monitoring
coal processing
Includes crushing, screening, and washing. Separation of lighter coal from heavier mineral
Sometimes use chem for frothing & flocculation, which aids separation (e.g MCHM is a coal cleaning chem)
Coal use
Particulate air pollution:
sig. health consequences
scrubbers (filters) clean power plant emission
High smoke stacks emit at high altitudes
Acid rain (Sulfuric acid):
Due to sulfur content of coal
widespread footprint
acidifies lakes & inf. tree health
mobilizes toxic forms of (Al)
Mercury Contamination:
@ low lvls in coal, but higher in backgrown
increasing lvls seen in lake sed. & biota
Hg bioaccumulates
disposal of coal waste
Coal ash either repurposed for most beneficial use (e.g cement) or storage in landfills
Nuclear proliferation
Plutonium- (can be) byproduct of nuclear operation that is very toxic & radioactive isotope
used as fuel for breeder reactor tech
Easily use to make nuclear bomb (must keep hidden)
Basic of radioactivity
Isotope- dif. Version of an element that has dif # of neutron and can be stable/unstable
Unstable isotopes “decay”- releases radiation and heat @ exponential decay rate (half life)
parent isotopes decays to daughter isotopes that is either radioactive/not (e.g uranium decays → stable lead isotope)
Forces vs. spontaneous decay & nuclear power
Atom bombs are critical masses, w/ exponential release of energy
Atomic power plants are sub-critical masses w/ constant and controllable energy release
Fuel & control rods in reactors absorb some radiation
Nuclear power plants are steam generators w/ H2O heated by reactors, where subcritical masses accelerate decay producing heat in controlled fashion
Radon
Naturally occurring radioactive gas
forms from U-238 decay
Lung cancer is correlated w/ prolong radon exposure
Mining fuel for nuclear power
Carnotite is common ore w/ various U oxide minerals
Crow Butte deposit is major U producers: euxinic causes U oxides to from while O rich waters dissolve and mobilizes U
Environmental concerns:
Waste rock can be enriched in U & other radioactive minerals
Oxidation mobilizes U → mining & exposure of rocks w/ increased surface area may cause increased U to move into groundwater
Radon exposure of miners
Designing high lvl waste site
(e.g. Yucca Mount) includes: No seepage of H2O through site (low permeability), position & stability of groundwater table, possibilities of volcanic & seismic activity, and low pop density
Low lvl radioactive waste
Material containing small concentration of radioactive substances, typically not requiring safety matures
Low lvl radioactive waste policy act of 1980: federal legislation est 5 states compact. By 1996 and non-member states chosen and dev disposal facility site that assumes title to a liability for all low lvl waste generated within boarders
Boyd county (NE’s compact site)
selected by consulting firm Bechtel Inc.
Pierre shale bedrock in Boyd county was host rock
Design focus on enhanced above grade vaults
Shallow perched aquifers, wetlands exist in area
NE denied permission for facility to be built, was sued by compact and had to pay $151 M & litigation cost of $25 M