APES 150 Flashcards
First Law of Thermodynamics
energy is neither created nor destroyed, may be converted from one form to another
Second Law of Thermodynamics
when energy is changed from one form to another, some useful energy is degraded into lower-quality energy (usually heat) Entropy is increased
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
Power
the rate of doing work. Units of power: watts and kilowatts
Electromagnetic radiation
a form of energy, travel as waves-radio waves, IR, visible light, UV, gamma ray
Ionizing radiation
has enough energy to knock electrons from atoms, forming ions, and capable of doing damage to DNA. (Gamma rays, X-rays, UV)
Radioactive decay
unstable radioisotopes decay releasing gamma rays, alpha and beta particles
Half-life
the time it takes for ½ of the mass of a radioisotope to decay
Estimate of how long a radioisotope must be stored until it has decayed to a safe level
10 half-lives
Nuclear fission
nuclei of isotopes are split apart into smaller nuclei; used in nuclear reactors
Nuclear fusion
2 isotopes of light elements are forced together at high temperatures; not technologically available now
Parts of hydrologic (water) cycle
evaporation (transpiration), condensation, precipitation
The fate of precipitation
runoff or infiltration, percolation
Aquifer
underground water-bearing layer Water table- the upper surface of groundwater
Cone of depression
lowering of the water table around a pumping well
Saltwater intrusion
over-pumping of groundwater near the coast causes saltwater to move into an aquifer
Ways to conserve water
Agriculture- drip irrigation
industry- recycling,
home use- fix leaks, use gray water, low flow fixtures
Distribution of water on Earth
97% seawater, 2% in icecaps and glaciers, <1% in groundwater, surface, organism, and atmosphere
Carbon
component of all organic molecules
The largest reservoir of carbon
sedimentary rocks, second the ocean
Photosynthesis
the process by which plants convert CO2 to carbohydrates, removes C from the atmosphere
Cellular respiration
organisms break down carbohydrates; releases energy, returns C to the atmosphere
Processes that releases C back into the atmosphere
cellular respiration and decomposition, fires, burning fossil fuels, volcanoes
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
Nitrogen
component of proteins and amino acids
The largest reservoir of nitrogen
the atmosphere (78% N2)
Nitrogen fixation
N2 is converted to ammonia NH3. bacteria does this
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 (nitrogen) and N2O (nitrous oxide) which are released into the atmosphere
Phosphorous
component of nucleic acids and a limiting factor for plant growth
P cycles more slowly
no gaseous phase, mostly found in rocks as PO4 (phosphate), released by weathering
Too much P in aquatic ecosystems
P from animal waste, fertilizers, sewage can cause eutrophication (excessive nutrients in body of water that causes dense growth of plants and death of animals due to lack of oxygen)
Major macronutrients
CHNOPS: carbon, hydrogen, nitrogen, oxygen, phosphorus, sulfur
Micronutrients and trace elements
needed in small amounts
Earth is 4.5 billion years old
1st cells appeared 3.5 billion years ago
Plate tectonics
Earth’s crust is broken into plates that move relative to each other, movement caused by convection currents dissipating Earth’s internal heat
plate boundaries
Volcanoes and earthquakes occur at
Divergent plate boundaries
seafloor spreading, new crust generated, mid-ocean ridges
Convergent and continental plate boundaries
oceanic plate subducts under oceanic 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
mineral resource, profitable to mine
Surface mining
strip mining (stopping a layer of soil), cheaper, less dangerous to miners. Problems: toxic runoff, acid drainage
Soil texture
the size of soil particles; sand, silt, clay
Humus
organic material in the soil
Leaching
removal of dissolved materials by water moving through
Permeability and Porosity
ability to transmit water. Porosity: ability to hold water
The 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 the surface, contains the ozone layer
Composition of Earth’s atmosphere
78% N2, 21% O2, 0.9% argon, 0.0035% CO2
The original atmosphere was H2 and He, Organisms have altered atmosphere
increases O2 and N2 decreased
Weather
daily atmospheric conditions (temp and precip), Climate long term atmospheric conditions