Surficial Exam 2

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71 Terms

1
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What major processes control the chemical composition of natural waters?

Interaction with atmosphere, biological activity, mineral dissolution and precipitation, and human activities

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What are the three major types of chemical weathering?

Hydrolysis, dissolution, and oxidation.

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What are the main agents of chemical weathering?

Water, acids, dissolved oxygen

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What are key effects of chemical weathering?

Weakens rock —> more vulnerable to mechanical weathering/erosion, affects landforms, controls soil formation/fertility, changes water/soil chemistry, regulates climate over time

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Atoms

Basic building blocks of matter

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Molecules

Two or more atoms bonded together

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Ions

Charged atoms/molecules

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Chemical Elements

Pure substances of one type of atom

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Isotopes

Atoms of the same element with different numbers of neutrons

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What gives a charge to an atom or molecule?

An imbalance between the number of protons (+) and electrons (-).

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Why do atoms bond?

To reach a more stable, lower energy state, typically by filling their outermost valence electron shells.

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Atomic Weight

The weighted average mass of an atom of an element, based on the relative abundance of its isotopes.

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How do we calculate the molecular weight of a chemical compound?

By summing the atomic weights of all the individual atoms in the molecule's chemical formula.

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How do you calculate the number of moles from a given mass?

Divide the mass in grams by the molecular or atomic weight in g/mol.

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Thermodynamics

Study of energy and its transformation

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What type of information does Thermodynamics provide?

Describes physical and chemical state of matter. Predicts energy changes for a given transformation.

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What is a system

Part of the universe being studied.

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How do you define a phase in a system?

A physically distinctive, chemically homogeneous, and mechanically separable part of a system.

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<p>Phase Diagram</p>

Phase Diagram

As we cross the lines or curves on the phase diagram, a phase change occurs. 2 states of the substances coexist in equilibrium

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Internal Energy (U)

Total kinetic/potential energy

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Enthalpy (H)

U + PV; total heat of a system

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Entropy (S)

Measure of disorder

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Gibbs Free Energy (G)

Determines reaction spontaneity.

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1st Law of Thermodynamics

Energy can be neither created nor destroyed, it can only be transferred from a system to its surroundings

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2nd Law of Thermodynamics

In an isolated system, natural processes are spontaneous when they lead to an increase of entropy.

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Evaluate if a reaction will lead to an increase or decrease in entropy.

Entropy increases when solids become liquids/gases, or dissolved particles increase.

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What are conditions for spontaneous reactions?

Constant temperature, pressure, and Gibbs free energy is negative

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What is a chemical reaction?

Process transforming reactant substances into different product substances.

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What are common types of reactions?

Acid-base, solubility/precipitation, hydrolysis, redox, ion exchange

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How do you write a chemical equation?

Reactants on the left, products on the right, separated by an arrow with stoichiometric coefficients.

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What are the rules to balance a chemical equation?

Conserve mass and conserve electric balance

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<p></p>


Equilibrium Constant

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How is equilibrium related to thermodynamics?


<p></p>
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Write equilibrium constant of reactions using concentrations.

Right side divided by left side (except solids and liquids)

<p>Right side divided by left side (except solids and liquids)</p>
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How can you measure disequilibrium?

Compare Activity Product to Keq. AP/Keq < 1 favors dissolution; AP/Keq > 1 favors precipitation.

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What influences the composition of rainwater? Surface water? Groundwater?

Rainwater: atmospheric gases/aerosols. Surface water: weathering/runoff. Groundwater: prolonged rock-water interactions.

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What are common water quality parameters?

Color, turbidity, total dissolved solid (TDS), hardness, electrical conductivity (EC), pH, Alkalinity, dissolved oxygen

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What is included in a standard water chemical analysis?

Temperature, pH, EC, and major cations/anions.

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Major Cations in Natural Waters

Ca2+, Mg2+, Na+, K+

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Major Anions in Natural Waters

HCO3-, SO4 2-, Cl-

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<p>What are expected relative abundance of ions in the different types of water?</p>

What are expected relative abundance of ions in the different types of water?

Ca-Mg-SO4 waters - gypsum groundwater, CA-HCO3 waters - shallow fresh groundwater, Na-Cl waters - seawater - rainwater, Na-K,HCO3 waters

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What can impact the quality of a water analysis?

Sampling errors, contamination, delayed analysis, and instrumental limits.

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How can you check error in analysis?

Perform a charge balance calculation in meq/L.

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Convert concentrations to meq/L.

meq/L = (mg/L / Molar Mass) * Charge magnitude.

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<p></p>


Piper Diagram

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Acid

Substance that can donate a proton

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Base

Substance that can accept a proton

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Common Acids

Nitric Acid (HNO), Sulfuric Acid (H2SO4). Carbonic Acid (H2CO3), Formic Acid (CH2O2)

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Common Bases

Lime (CaO), Portlandite (CA(OH)2), Brucite (Mg(OH)2, Limestone (CaCO3)

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Recognize that a reaction is an acid or base dissociation reaction.

Look for a molecule splitting to release H+ or reacting with water to produce OH-.

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Write the expression of the equilibrium constant (dissociation constant) for acid or base dissociation reactions.


<p></p>
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Definition of pH


<p></p>
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What is buffering.

When the pH is held steady because of the presence of a conjugate acid/base pair

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What is hydrolysis?

H+ ions displace other ions to form a different mineral

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What are some examples of hydrolysis reactions in geology?

Weathering of K-feldspar into kaolinite

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How does a weathering profile develop?

1.) Solid bedrock (with original minerals like plagioclase)

2.) Water seeps in (percolation)

3.) Dissolves weak minerals (saprolite)

4.) Top layer builds (kaolinite and iron oxides)

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<p></p>


Weathering profile graph.

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<p>Activity Diagram</p>

Activity Diagram

Display the stability fields of a silicate mineral and its possible weathering products

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What are key factors controlling silicate weathering?

Minerology, fluid flow, temperature, source of acid, open/closed system, composition of water

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What are direct effects of silicate weathering on the environment?

Production of soils, 45% if total dissolved load of world’s rivers, mos pH-buffering mechanism, CO2 sink

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Ionic Bonding

Electrostatic attraction between oppositely charged ions

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Covalent Bonding

Sharing of valence electrons

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Metallic Bonding

Metal cations sharing a 'sea' of electrons

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Hydrogen Bonds

Weak electrostatic dipole-dipole interactions.

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Open System

Exchange of both energy and matter

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Closed System

No transfer of matter but possibilities for energy transfer

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Isolated System

No transfer of energy and matter across the boundaries of the system

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Intensive Properties

“Bulk” properties that can be specified at a particular point in the system. DON’T DEPEND on amount or size of system

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Extensive Properties

Constitute a property of the whole system body. They are additive. DEPEND on amount or size of system

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Examples of Intensive Properties

Temperature, pressure, density, concentration

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Examples of Extensive Properties

Volume, mass, heat capacity, energy