Intro Flashcards

1
Q

Thermodynamics

A

predicts whether a particular chemical reaction can occur

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2
Q

Kinetics

A

information about the speed of reaction

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3
Q

Gibbs Free Energy

A

Energy (enthalpy) and/ or Entropy driven

delta G = deltaH = TdeltaS

Delta G is negative

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4
Q

Soil Processes: Intraphase

A

changes in element speciation within a phase

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5
Q

Soil Processes: interphase

A

transfer of matter between phases; ex- CO2 to plant biomass to SOM

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6
Q

Soil chemical POV: Multiphase

A

porous materials whose voids contain air and solution

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7
Q

Soil chemical POV: Multicomponent

A

soil matrix, soil air, and soil solution are each a mixture of reactive chemical compounds

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8
Q

Soil Chemical POV: open

A

exchange both matter and energy with the surrounding atmosphere, biosphere and hydrosphere

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9
Q

Soil Chemical POV: biogeochemical

A

biological and chemical transformations link soils with the atmosphere and hydrosphere producing fluxes that are of global significance

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10
Q

Electronegativity

A

increases bottom-up and left to right

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11
Q

Atomic radii

A

increases top to bottom and right to left

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12
Q

covalent bonding

A

sharing of electron pairs; occur between atoms of similar electronegativity; strongest 50-100 kcal/mol; short ranges; increases bond order proportional to increased strength of covalent bond

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13
Q

ionic bonding

A

occur between ions of opposite charge; opposite end of the periodic table; relatively strong bonds; long-range bonds; COMMON FOR SOIL MINERALS

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14
Q

If the ionic character % is 51 what does that mean

A

is means that the bonds are more covalent

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15
Q

ion-dipole bonding

A

shorter range; related to r^2; weaker than ionic and covalent

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16
Q

Dipole

A

a separation of charge within a molecule; ex water molecule

17
Q

examples of ion-dipole forces

A

cation and anion hydration in water- Al3+ will hydrate more strongly than K+ because it has a more dense charge radius

18
Q

dipole-dipole bonding

A

occurs by orienting oppositely charged ends towards one another

19
Q

H-bonding

A

weak electrostatic bond between H and highly electronegative atoms (N, O, Cl, F)

20
Q

Van Der Waals forces

A

weak attraction between nonpolar/apolar molecules; imbalances in electron distribution produce instantaneous dipoles; extremely short range

21
Q

The hydrophobic effect

A

The exclusion of nonpolar substances from an aqueous solution

22
Q

aggregation of hydrophobic molecules does what

A

frees up water molecules to increase the configural entropy of the system

23
Q

amphiphilic

A

assembly (molecules with both hydrophobic and hydrophilic portions): micelles, lipid bilayers, vesicles, proteins.

24
Q

bonding is rarely exclusively one of a kind

A

in soil minerals most bonds are composite of both covalent and ionic character