Chapter 3: Matter Flashcards

1
Q

Define ‘Abiotic’.

A

Said of a compound that is of non-biologic (non-living) origin.

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2
Q

Define ‘Aerosol’.

A

A tiny liquid drop or tiny solid particle so small it remains suspended in air.

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3
Q

Define ‘Asthenosphere’.

A

The region of the mantle where rocks become ductile, having little strength, and are easily deformed. It lies at a depth of 100 to 350 km below the surface.

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4
Q

Define ‘Atom’.

A

The smallest individual particle that retains all the properties of a given chemical element.

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5
Q

Define ‘Biopolymer’.

A

Polymers that consist of organic compounds and are of biologic origin.

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6
Q

Define ‘Biotic’.

A

A compound that is of biologic (living) origin.

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7
Q

Define ‘Bond’.

A

The elemental forces that draw two atoms together.
Compounds form when one or more kinds of ion combine chemically in a specific ratio, typically through the sharing or exchange of electrons. The type and configuration of this sharing or exchange, called bonding, helps determine the properties of the compound.

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8
Q

Define ‘Carbohydrate’.

A

Organic compounds composed of C, H, and O, of which sugars, starches, and cellulose are examples. Carbs are formed by all green plants and constitute a major source of food for animals.

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9
Q

Define ‘Chemical element’.

A

The fundamental substances into which matter can be separated by ordinary chemical means.

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10
Q

Define ‘Chemical sediment’.

A

Sediment formed by precipitation of minerals from solutions in water.

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11
Q

Define ‘Clastic sediment’.

A

The loose fragmented debris produced by the mechanical breakdown of older rocks.

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12
Q

Define ‘Colloid’.

A

A gel consisting of extremely fine particles dispersed in a continuous medium, usually liquid.

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13
Q

Define ‘Compound’.

A

The combination of one or more kinds of anion with one or more kinds of cation in a specific ration, typically through the sharing (covalent bond) or exchange of electrons (ionic bond).

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14
Q

Define ‘Continental crust’.

A

The part of the Earth’s crust that comprises the continents, which has an average thickness of 45 km.

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15
Q

Define ‘Core’.

A

The spherical mass, largely metallic iron, at the center of the Earth.

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16
Q

Define ‘Crust’.

A

The outermost and thinnest of Earth’s compositional layers, which consists of rocky matter that is less dense than the rocks of the mantle below.

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17
Q

Define ‘Crystal’.

A

A solid compound composed of ordered, three-dimensional arrays of atoms or chemically bonded together and displaying crystal form.

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18
Q

Define ‘Density’.

A

The average mass per unit volume.

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19
Q

Define ‘Gas’.

A

State of matter that takes on the shape of the container in which it is contained, filling the container completely (or escaping into space if it is not contained), while its constituent atoms move freely and acquire a uniform distribution within the container.

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20
Q

Define ‘Gene’.

A

Regions of DNA coded for specific proteins that perform particular functions.

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21
Q

Define ‘Glass’.

A

Non-crystalline, amorphous solid.

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22
Q

Define ‘Hydrocarbons’.

A

Organic compounds that contain hydrogen and form carbon-hydrogen bonds.

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23
Q

Define ‘Igneous rock’.

A

Rock formed by the cooling and consolidation of magma.

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24
Q

Define ‘Inner core’.

A

The central, solid portion of the Earth’s core.

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25
Q

Define ‘Inorganic’.

A

Chemical compounds of non- biologic origin.

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26
Q

Define ‘Ion’.

A

An atom that has excess positive or negative charges caused by electron transfer.

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27
Q

Define ‘Isotope’.

A

Atoms of an element having the same atopic number but differing mass numbers.

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28
Q

Define ‘Lava’.

A

Magma that reaches the Earth’s surface through a volcanic vent.

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29
Q

Define ‘Lipid’.

A

A chemically diverse group of compounds that do not dissolve in water, including fats, oils, waxes, and steroids.

30
Q

Define ‘Liquid’.

A

State of matter that has definite volume but its constituent atoms are able to flow freely past one another; the material does not retain its own shape but conforms to the shape of its container.

31
Q

Define ‘Lithosphere’.

A

The outer 100 km of the solid Earth, where rocks are harder and more rigid than those in the plastic asthenosphere.

32
Q

Define ‘Magma’.

A

Molten rock, together with any suspended mineral grains and dissolved gases, that forms when temperatures rise and melting occurs in the mantle or crust.

33
Q

Define ‘Mantle’.

A

The thick shell of dense, rocky matter that surrounds the core.

34
Q

Define ‘Matter’.

A

Substance that has mass and occupies space.

35
Q

Define ‘Mesosphere’.

A

One of the four thermal layers of the atmosphere, lying above the stratosphere.

36
Q

Define ‘Metamorphic rock’.

A

Rock whose original compounds or textures, or both, have been transformed to new compounds and new textures by reactions in the solid state as a result of high temperature, high pressure, or both.

37
Q

Define ‘Mineral’.

A

Any naturally formed, crystal- line solid with a definite chemical com- position and a characteristic crystal structure.

38
Q

Define ‘Mineral assemblage’.

A

The variety and abundance of minerals present in a rock.

39
Q

Define ‘Molecule’.

A

Smallest unit that retains the properties of a given compound.

40
Q

Define ‘Nucleic acid’.

A

Giant organic polymers built from molecules called nucleotides, each of which contains a sugar group, a phosphate group, and a nitrogenous base.

41
Q

Define ‘Oceanic crust’.

A

The crust beneath the oceans.

42
Q

Define ‘Organic’.

A

Said of compounds consisting of carbon atoms that are joined to other carbon atoms by a covalent bond.
Organic compounds are generally of biologic origin and typically contain carbon-carbon and carbon-hydrogen bonds.Organic compounds, especially certain types of biopolymers, are extremely important in Earth processes. Four major categories of biologically important compounds are proteins, nucleic acids, carbohydrates, and lipids.

43
Q

Define ‘Outer core’.

A

The outer portion of the Earth’s core, which is molten.

44
Q

Define ‘Phase’.

A

Masses of material that can be separated from one another by a definable boundary.

45
Q

Define ‘Plasma’.

A

Ionized (electrically charged) gas with unique properties and characteristics.

46
Q

Define ‘Plutonic rock (intrusive)’.

A

Rock formed by the crystallization of magma underground. Tend to be much coarser- grained, with interlocking crystals.

47
Q

Define ‘Polymer’.

A

Large chain or network structures formed by the linking together of small molecules (called monomers).

48
Q

Define ‘Protein’.

A

Molecule formed through the polymerization of an amino acid.

49
Q

Define ‘Radioactive’.

A

Isotopes of certain chemical elements that transform spontaneously into another isotope of the same element, or to an isotope of a different element.

50
Q

Define ‘Regolith’.

A

The irregular blanket of loose, noncemented rock particles that covers the Earth.

51
Q

Define ‘Rock’.

A

Any naturally formed, nonliving, firm, and coherent aggregate mass of mineral matter that constitutes part of a planet.

52
Q

Define ‘Sediment’.

A

Regolith that has been trans- ported by any of the external processes.

53
Q

Define ‘Sedimentary rock’.

A

Any rock formed by chemical precipitation or by sedimentation and cementation of mineral grains transported to a site of deposition by water, wind, ice, or gravity.

54
Q

Define ‘Soil’.

A

The part of the regolith that can support rooted plants.

55
Q

Define ‘Solid’.

A

State of matter that is firm or com- pact in substance with a definite volume and density, and that tends to retain its shape even if it is not confined, because its constituent atoms are fixed in position relative to each other.

56
Q

Define ‘State’.

A

No def’n found. Solid, liquid, gas, etc…

57
Q

Define ‘Texture (of a rock)’.

A

The overall appearance that a rock has because of the size, shape, and arrangement of its constituent mineral grains.

58
Q

Define ‘Vapor’.

A

Gas.

59
Q

Define ‘Volcanic rock (extrusive)’.

A

Rock formed from the volcanic eruption of lava or tephra; often very fertile. Can be recognized by their very fine grain sizes or glassy texture.

60
Q

The common states of matter on Earth are solid, liquid, and gas. What are some others?

A

Other forms and states of matter, including plasmas, gels, colloids, and aerosols, are also important in Earth processes.

61
Q

Are mixtures and solutions the same as compounds?

A

They are not the same as compounds because the materials in the mixture do not undergo chemical reactions and they can usually be separated from one another by physical means.

62
Q

The overall composition of Earth is inherited from its location in the solar nebula. As a terrestrial planet, the composition of Earth is predominantly ___ and ___.

A

Rocky and metallic.

63
Q

Earth has internal layers that originated as a consequence of the chemical differentiation of the partially molten early planet. The layers can be distinguished from one another on the basis of differences in composition—___, ___, ___; rock strength—___, ___, ___; and state of matter—___ ___ (solid), ___ ___ (liquid).

A

Core, mantle, crust.
Mesosphere, asthenosphere, lithosphere.
Inner core (solid), outer core (liquid).

64
Q

What 12 elements comprise 99.23 % of the continental crust? These are the abundant elements, which control the compositions of many common Earth materials.

A

12 elements—oxygen, silicon, aluminum, iron, calcium, magnesium, sodium, potassium, titanium, hydro- gen, manganese, and phosphorus.

65
Q

Minerals are conveniently identified and classified on the basis of their physical properties, which, in turn, depend on their chemical compositions and crystal structures. How are they identified?

A

The proper ties most often used to identify minerals are crystal form, growth habit, cleavage, luster, color, hardness, and specific gravity.

66
Q

What are the 3 families of rocks?

A

There are three families of rock: igneous rocks, which form by the cooling and consolidation of molten rock; sedimentary rocks, which form by the chemical precipitation of material carried in solution by lake, river, or ocean water, or by the deposition of particles transported in suspension by water, wind, or ice; and metamorphic rocks, which have been changed as a result of high temperatures, high pressures, or both.

67
Q

How are rocks identified?

A

A rock can be identified and classified on the basis of its texture (the size, shape, and arrangement of constituent mineral grains), and mineral assemblage, which reflect the conditions under which the rock was formed and/or later modified.

68
Q

How are rocks identified?

A

A rock can be identified and classified on the basis of its texture (the size, shape, and arrangement of constituent mineral grains), and mineral assemblage, which reflect the conditions under which the rock was formed and/or later modified.

69
Q

What are two factors that can be recognizable in metamorphic rocks? Sedimentary rocks?

A

Metamorphic rocks often are recognizable because they show evidence of chemical and/or physical alteration due to exposure to very high temperatures and pressures, such as recrystallization or layering.

Sedimentary rocks can usually be identified on the basis of textural evidence of individual accumulated particles that have become stuck or cemented together. Fossils also provide strong evidence of sedimentary origins.

70
Q

Regolith is composed of ___(decomposed rock in situ); ___(loose, unconsolidated particulate matter); and ___(regolith that contains organic matter and can support rooted plant life).

A

Saprolite, sediment, and soil.

71
Q

What are the two fundamental types of sediment?

A

There are two fundamental types of sediment: clastic, composed of bits of broken rock and mineral particles; and chemical, derived from material transported in solution and deposited when the dissolved minerals are precipitated.

72
Q

Energy drives the continuous cycling of materials among Earth’s reservoirs: geosphere, hydrosphere, atmosphere, and biosphere. ___ cycles are the pathways that chemical elements follow as they move through the Earth system.

A

Biogeochemical.
The key that unifies biogeochemical cycles is the involvement of the four prin- cipal components of the Earth system: rocks, air, water, and life.