- Be able to predict the
thermodynamic favorability of a chemical reaction.
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- Distinguish between: (a)
elementary and overall reactions; (b) homogeneous and heterogeneous
reactions.
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- Use
Pauling’s Rules to predict ion coordination.
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- Be
able to calculate various parameters related to phyllosilicate clay
minerals (net
negative charge, CEC, molecular weight, and clay activity) and predict
the
mineralogy in the sample.
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- Understand
the relationship of clay mineralogy to potassium (K+)
fixation and
water sorption.
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- Know
different surface area methods and relate to clay mineral structure.
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- Differentiate between soil
organic matter (SOM) fractions and be aware of diagnostic humification
indicators.
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- Discuss major functional groups
on SOM that contribute to the observed CEC as a function of pH.
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- Calculate ionic strength (I) for
both symmetrical and nonsymmetrical electrolytes.
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- Be able to perform pH calculations for weak
acids/bases and strong acids/bases (of the monoprotic type).
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- Understand
the relationship between ion activities and concentrations.
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- Given
equilibrium expressions for common metal oxides and clay minerals in
soils,
derive equations necessary to plot solubility diagrams and be
prepared to make
interpretations.
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- Given
equilibrium expressions for complexation and hydrolysis of metals and
nonmetals, be able to perform calculations of free and complexed
species.
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- Know
the purpose for each reagent used in the soil fractionation procedure
and diagnostic
features for identification of soil minerals.
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- Know
the definitions of Lewis acids and bases and how these terms are
applied to
soil components.
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- Understand
the procedures and calculations involved to calculate CEC of your soil
in the
lab.
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- Be
prepared for basic analytical calculations employed in the lab.
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- Distinguish
between different adsorption isotherm and ion exchange equations. Be able to calculate thermodynamic parameters
related to sorption.
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- Know
definitions of PZNC, PZNPC, PZC, PZSE and methods of determination.
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- What
are the effects of I on the thickness of the double layer (1/k)? Know
those parameters which influence 1/k.
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- Understand
the chemistry of soil components such as reactive sites, surface charge
components of solid particle surfaces, and solution chemistry of
inorganic
solutes to predict reactivity.
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- Be
able to explain the ion preference patterns for group I alkali metals.
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- Predict
sorption mechanisms for cations and anions on soil mineral surfaces.
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- Distinguish
between heterovalent and homovalent ion exchange.
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- Be
prepared to derive and calculate half-lives (t1/2) for first
and
second order reactions and rate constants.
Also, write expressions for the overall rate given a
reaction. Be familiar with the equation
used to express
the temperature dependence of rates.
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- Given
reduction half-reactions, be able to construct and sketch Eh/pe versus pH
diagrams, and predict the direction
of the reaction.
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- Understand
the general controls on the redox state of natural waters.
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- Be
acquainted with the soil N, Mn, Fe, and C cycles and how they can
impact
contaminant fate.
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