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Title: Kinetic%20Methods


1
Kinetic Methods
2
Rates
  • In order to use a reaction for analytical
    purposes, the reaction must have a rate slow
    enough to measure but fast enough to get it done
    in a reasonable time.
  • There must be some way of monitoring the
    reactions progress.
  • The rate law for the reaction must be known.
  • Rate is defined so as to always be a positive
    quantity. Thus for Reactant ? Product,
  • Rate -d(Reactant)/dt or d(Product)/dt

3
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4
Rate Laws
  • Reaction rates depend upon reactant
    concentrations in often complicated ways.
  • This is because reactions rarely proceed by one
    simple step but rather through several steps.
  • The dependence of rate on concentration really is
    a matter of what is involved in the slowest, or
    rate determining step.
  • If there are several reactants (A, B, etc.) we
    can write Rate k(A)a(B)b where the sum ab
    is referred to as the reaction order.
  • The reaction order must always be determined
    experi-
  • mentally and may have little to do with the
    molecularity of the reaction, i.e., the balancing
    coefficients.

5
Some reaction orders
  • Zero order Rate k(reactant)0 constant
  • This is often characteristic of heterogeneously
    catalyzed reactions.
  • First order Rate k(reactant)1
  • These reactions follow ln(At) ln(A0) - kt if A
    is the reactant. Also, k 0.693/t½, where t½ is
    the half-life of the reaction, the time required
    for half the reactant to disappear.
  • Second order Rate k(reactant)2 or k(A)1(B)1.
  • The first type follows 1/(At) 1/(A0) kt.

6
Pseudo-first-order Kinetics
  • It is sometimes possible to use such a great
    excess of one reactant that its concentration
    doesnt change during the analysis and thus the
    rate depends on only the other reactant. Such
    conditions are called pseudo-first-order.
  • It may even be possible to adjust conditions so
    as to make the reaction pseudo-zero-order.

7
Analytical Methods
  • It is possible to use kinetic methods in many
    different ways (see diagram in text, p.626).
  • For example, one can measure the reactant
    concentration at some particular time and use the
    integrated rate law to calculate what the value
    was at t0. This can sometimes be accomplished
    by stopping the reaction chemically to give time
    to measure (At).
  • An alternative is to measure the time required
    for some amount of reactant to disappear.

8
Radiochemical Methods
  • Isotopes of many elements are radioactive. Thus
    the presence of such isotopes makes for a
    sensitive way of detecting and quantifying them.
  • In substances where only very small amounts of
    radioactive isotope are present, it is possible
    to activate the sample by bombarding with
    neutrons to produce more radioactivity and thus
    make the analysis easier.
  • Radioactive compounds can also be added to
    samples to enable one to see how effective
    certain transfer procedures are.

9
Radiation
  • Alpha particles, helium nuclei, 4He2
  • Beta particles, electrons
  • Gamma rays, high energy electromagnetic
    radiation, ?
  • Radioactive decay follows first order kinetics.
  • A ?N and Nt N0e-?t
  • where A is activity, ? is decay constant (in
    disintegrations per unit time), and N is the
    number of radioactive atoms. The decay constant
    is related to half-life by
  • ? 0.693/t½

10
Neutron Activation Analysis
  • An analysis method based on bombarding a sample
    with neutrons to make it radioactive and then
    measuring the disintegrations, generally as gamma
    radiation.
  • The sample is bombarded in a nuclear reactor or
    with a slow neutron instrument. It is allowed to
    cool for a period to make it safe to handle and
    permit short-term interferences to decay to
    background.
  • The method is applicable to nearly all elements
    and is a nondestructive technique.

11
Neutron Activation Analysis
  • The rate of production of radioactive atoms
    depends on several parameters
  • Rate FsN
  • where F is the neutron flux, s is the reaction
    cross-section and N is the number of atoms
    originally present in the sample.
  • The initial radioactivity, A0, after radiation
    for some time, t, is given by
  • A0 FsN(1-e-?t)
  • Thus, if one can determine A0, and know the other
    parameters, one can calculate N, the number of
    atoms present in the sample.

12
Isotope Dilution Analysis
  • In this technique, a radioactive tracer is added
    to an analyte sample.
  • After the analyte has been treated to isolate it
    for final quantification, the radioactivity of
    the sample can be used to determine what fraction
    of the original analyte was lost in the
    analytical process, e.g. precipitation,
    filtration, or extraction.

13
Isotope Dilution Analysis
  • A mass, wT, of tracer with known activity, AT, is
    added to the unknown mass, wx, of analyte and the
    sample is made homogeneous.
  • If after the analysis it is found that wA grams
    of analyte were found, and one finds the activity
    of the isolated substance is AA, then following
    relationship will hold
  • AA AT wA/(wx wT)
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