Difference between revisions of "GMOA Notes"
Line 198: | Line 198: | ||
|- | |- | ||
|} | |} | ||
+ | |||
+ | *Mineral formation | ||
+ | **Melting - Volcanic activity | ||
+ | **Evaporation - Salt water: Halite, Gypsum | ||
+ | **Biological activity - sulfur producing bacteria | ||
+ | **Oxidized - comes into contact with oxygen: Limonite | ||
+ | **Leached - as water moves through the soil it dissolves elements. A leech line forms due to mineral formation where the water stops: bauxite | ||
+ | **Metamorphic processes - formed by heat and pressure. Examples: graphite, chlorite, diamonds. Alters chemical composition and structure, called recrystallization | ||
+ | |||
+ | *Mineral Types | ||
+ | ** |
Revision as of 19:10, 4 October 2008
These are notes that cover Geology, Meteorology, Oceanography, and Astronomy.
Introduction
Earth's four spheres
Hydrosphere - dynamic mass of liquid that is always on the move
- Oceans - the most prominent feature of the hydrosphere
- 71% of Earth's surface is covered by ocean which is 97% of Earth's water
- Only 3% is fresh water - streams, lakes, glaciers and underground supplies
- Water Cycle - constantly recycles water
Atmosphere
- Provides us with the air we breath
- Protects us from the sun's intense heat and radiation
- Protects us from space
Biosphere
- Includes all life on Earth
- Interacts and influences the other 3 spheres
Lithosphere
- Earth's rigid outer layer called the crust and the upper mantle called the asthenosphere
- Solid earth consists of 4 layers:
- core
- inner, solid core
- outer, liquid core
- mantle
- lithosphere
- core
- Divisions of Earth's surface
- continents
- ocean basins
Sciences
Sciences involved in better understanding the earth integrate chemistry, physics, and biology into the following sciences:
Meteorology - the study of:
- the atmosphere
- weather and climate
Geology - the study of the Earth, and is broken into
- Physical geology
- minerals
- rocks
- Earth processes - mountain building, earthquakes, volcanoes, etc.
- Historical geology - Earth's origin and it's past
- physical
- biological
Oceanography - study of the Oceans
- Composition and movement of seawater
- Seafloor topography and sea life
Astronomy - the study of the universe
- Earth is a tiny object in a vast universe
- to understand Earth helps us to understand other planets and vice versa
Resources and Environmental Issues
Environment
- Physical environment (abiotic)
- water
- air
- soil
- rock
- Biological - living environment (biotic)
Resources
- Important environmental concern
- Include:
- water
- soil
- minerals
- energy
- Two broad categories of resources
- Renewable resources
- can be replenished
- Examples: plant (lumber) and wind energy
- Nonrenewable Resources
- Fixed quantities
- Examples: fuels and metals
- Renewable resources
Environmental Problems
- Local, regional, and global
- Human-induced and accentuated
- Urban air pollution
- Acid rain
- Ozone depletion
- Global Warming
- Natural Hazards
- Earthquakes
- Landslides
- Floods
- Huricanes
- World population pressures - in 30 years population increased from 4 to 7 billion
- US makes up 6% of that but uses 30% of the annual mineral and energy resources
- Alternate energy sources needed
Scientific Inquiry
Scientific Inquiry - scientific knowledge is gained through the following systematic steps called the scientific method, (PI-HE-RAC)
Gather facts through observation then ask why?
- Problem - state the problem
- Information about the problem
- Hypothesis (untested best guess as to why)
- Experimentation
- Record and Analyze results
- Conclusion - accept or reject hypothesis
Goal of science is to discover patterns in nature and use knowledge to predict what will happen under certain circumstances
- Theory - tested and confirmed
- Law - no known deviations have ever been found
Minerals
A mineral is a naturally occurring crystalline solid with a definite but not fixed chemical composition and ordered atmomic arrangement.
Chemistry and Mineral Terms
Chemistry Terms:
- Chemical Property - characteristics of a material, which depends upon how the material reacts with other materials
- Periodic Table - list of all known elements
- Element - matter made up of atoms that are essentially all the same and cannot be subdivided by ordinary chemical methods
- Atom - smallest part of an element
- Nucleus - central part of an atom made up of protons and neutrons
- Protons - subatomic particles with a positive charge
- Electrons - subatomic particles with a negative charge
- Neutrons - subatomic particles with a charge of 0
- Atomic number - the number of protons in an atom (above element symbol on periodic table)
- Atomic mass - the number of protons plus the number of neutrons (below element symbol on periodic table)
- Isotope - change in the number of neutrons in an atom. Example, and isotope of sodium may have 10 or 12 neutrons
- Electron Configuration - how the electrons are arranged around the atom in energy levels
- 1st energy level has 2 electrons
- all other energy levels have 8 electrons
- Ion - change in the number of electrons
- Atoms are most stable with 8 electrons in the outer energy level
- Will share, lose, or gain electrons to achieve this
- Ionic bonding - transfer of electrons
- example - Sodium and Chlorine
- Lewis Electron Dot Structure - Short hand for showing "chemistry" activity in the outer level by showing the number of electrons in the outer energy level
- Covalent bonding - sharing of electrons. VERY STRONG BOND
- example - bond between Hydrogen and Oxygen
- Metallic bonding - electrons do not belong to any particular nucleus, they float between nuclei
- example - two metals touching for a long time can "weld" to each other by metallic bonding. You can increase the speed of this by adding heat.
Mineral Terms:
- A mineral is a naturally occurring crystalline solid with a definite but not fixed chemical composition and ordered atomic arrangement
- Size of the ion is important because ions that are within 10% of the same size may be substituted in many minerals. This is why minerals of the same type have different chemical compositions.
- examples - Si,Al; Fe,Mg; Na, Ca
- Size of the ion is important because ions that are within 10% of the same size may be substituted in many minerals. This is why minerals of the same type have different chemical compositions.
Element | % by Weight |
---|---|
Oxygen, O | 47 |
Silicon, Si | 28 |
Aluminum, Al | 8 |
Iron, Fe | 6 |
Calcium, Ca | 4 |
Sodium, Na | 3 |
Magnesium, Mg | 2 |
Potassium, K | 2 |
- Mineral formation
- Melting - Volcanic activity
- Evaporation - Salt water: Halite, Gypsum
- Biological activity - sulfur producing bacteria
- Oxidized - comes into contact with oxygen: Limonite
- Leached - as water moves through the soil it dissolves elements. A leech line forms due to mineral formation where the water stops: bauxite
- Metamorphic processes - formed by heat and pressure. Examples: graphite, chlorite, diamonds. Alters chemical composition and structure, called recrystallization
- Mineral Types