AP Environmental Science Review

Descripción

Fichas sobre AP Environmental Science Review, creado por agrund3999303 el 11/10/2013.
agrund3999303
Fichas por agrund3999303, actualizado hace más de 1 año
agrund3999303
Creado por agrund3999303 hace alrededor de 11 años
39
1

Resumen del Recurso

Pregunta Respuesta
High quality energy organized and concentrated, able to perform useful work (ex: oil and nuclear)
Low quality energy disorganized dispersed (ex: heat)
Units of energy joules, calories, kilocalories, BTU’s, kilowatt-hours
Estimate of how long a radioisotope must be stored until it has decayed to a safe level 10 half lives
Parts of hydrologic (water) cycle evaporation (transpiration), condensation, precipitation
Carbon-silicate cycle very slow, geological cycle, C in oceans used by marine organisms, end up in ocean sediments and are subducted into Earth’s crust, eventually returned through volcanic venting
Nitrification ammonia is converted to nitrite (NO2) to nitrate (NO3)
Assimilation plants incorporate ammonia and nitrate ions into organic molecules (nucleic acids, amino acids)
Ammonification decomposer bacteria break down organic compounds into ammonia
Denitrification specialized bacteria convert nitrogen compounds into N2 and N2O which is released into the atmosphere
Phosphorous component of nucleic acids
P cycles more slowly no gaseous phase, mostly found in rocks as PO4, released by weathering
P major limiting factor for plant growth
Too much P in aquatic ecosystems from animal wastes, fertilizers, sewage can cause eutrophication
Major macronutrients Micronutrients and trace elements CHNOPS needed in small amounts
Plate tectonics Earth’s crust is broken into plates which move relative to each other, movement caused by convection currents dissipating Earth’s internal heat
Volcanoes and earthquakes occur at... plate boundaries
Divergent plate boundaries sea floor spreading, new crust generated, mid ocean ridges
Convergent plate boundaries oceanic plate subducts under ocean or continental plates, causes volcanoes and trenches. Continental plates produce mountains
Transform boundaries plates slide past each other, causes earthquakes
Rock cycle relationship of rocks and rock formation processes
Rock types according to origin igneous, sedimentary, and metamorphic
Minerals are not renewable
Ore concentration of mineral is high enough so that it is profitable to mine
Mineral reserve identified deposits, profitable to mine
Surface mining strip mining, cheaper, less dangerous to miners. Problems: toxic runoff, acid drainage
Soil texture size of soil particles; sand, silt, clay
Humus organic material in soil
Leaching removal of dissolved materials by water moving through
Permeability ability to transmit water
Porosity ability to hold water
Solution to soil problems contour plowing, crop rotation, conservation tillage, organic fertilizers
Troposphere 0-17 km above Earth’s surface, site of weather, organisms, most water vapor
Stratosphere 17-48 km above surface, contains ozone layer
Composition of Earth’s atmosphere 78% N2, 21% O2, 0.9% argon, 0.0035% CO2
Weather daily atmospheric conditions (temp and precip), Climate long term atmospheric conditions
Global circulation patterns caused by uneven heating of Earth’s surface and Earth’s rotation
ENSO El Niño Southern Oscillation; see-sawing of air pressure over Southern Pacific
Greenhouse gases (GHG) water vapor, CO2, methane, CH4, CFC’s; trap outgoing infrared radiation (heat), causing Earth to warm
Effects of global warming rising sea level, droughts, disruptions of ecosystems, shifts in vegetation
Ozone depletion caused by: CFC’s, methyl chloroform, carbon tetrachloride (CCl4), halons, methyl bromide all break down stratospheric ozone
Effects of ozone depletion increased UV radiation reaches Earth’s surface; causes increased skin cancer, cataracts, decreased plant growth and marine productivity
Stratospheric ozone layer approximately 20-30 km above the Earth’s surface (12-18miles)
Biotic/abiotic living and nonliving
Producer/autotroph organisms that CAN make their own food
Consumer/heterotroph organisms that CANNOT make their own food
Major trophic levels producers-primary consumers-secondary consumers-tertiary consumers-etc.
Energy flow in food webs solar energy converted to chemical energy, eventually returned as hear
Energy flow in food webs only 10% transferred to next trophic level
Mutualism interaction between 2 species in which both species benefit
Parasitism relationship in which one partner obtains nutrients at the expense of the host
Commensalism one partner benefits, the other is neither harmed nor benefited
Mostrar resumen completo Ocultar resumen completo

Similar

Historia Argentina
Nicolas Ñancucheo
Fichas de Inglés - Vocabulario Intermedio 2
maya velasquez
Tipos de Evaluación
Enrique Adolfo Simmonds Barrios
EL SIGLO XVIII EN ESPAÑA: LA MONARQUÍA BORBÓNICA
maya velasquez
VOCALES. Diptongo o Hiato...
JL Cadenas
GLOSARIO PARTE I PAA
Valeria de Leon
Artes Escénicas
amanda hernandez
EL MITO DE LA CAVERNA
Cardys Colorado
AMBIENTES VIRTUALES DE APRENDIZAJE (AVA)
naansara1993
Sistema óseo
Laura Mon
ANTZINAKO ERLIJIOAK (Txantxiloia)
Txemi López