2.1 2 atom mass spectrometer student

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  • 7/27/2019 2.1 2 Atom Mass Spectrometer STUDENT

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    S.MORRIS 2006

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    HISTORY OF THE ATOM

    460 BC Democritus develops the idea of atoms

    he pounded up materials in his pestle and

    mortar until he had reduced them to smaller

    and smaller particles which he called

    ATOMA

    (greek for indivisible)

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    HISTORY OF THE ATOM

    1808 John Dalton

    suggested that all matter was made up of

    tiny spheres that were able to bounce around

    with perfect elasticity and called them

    ATOMS

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    HISTORY OF THE ATOM

    1898 Joseph John Thompson

    found that atoms could sometimes eject a far

    smaller negative particle which he called an

    ELECTRON

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    HISTORY OF THE ATOM

    Thompson develops the idea that an atom was made up of

    electrons scattered unevenly within an elastic sphere surrounded

    by a soup of positive charge to balance the electron's charge

    1904

    like plums surrounded by pudding.

    PLUM PUDDINGMODEL

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    HISTORY OF THE ATOM

    1910 Ernest Rutherford

    oversaw Geiger and Marsden carrying out his

    famous experiment.

    they fired Helium nuclei at a piece of gold foil

    which was only a few atoms thick.

    they found that although most of them

    passed through. About 1 in 10,000 hit

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    HISTORY OF THE ATOM

    gold foil

    helium nuclei

    They found that while most of the helium nuclei passed

    through the foil, a small number were deflected and, to their

    surprise, some helium nuclei bounced straight back.

    helium nuclei

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    HISTORY OF THE ATOM

    Rutherfords new evidence allowed him to propose a more

    detailed model with a central nucleus.

    He suggested that the positive charge was all in a central

    nucleus. With this holding the electrons in place by electrical

    attraction

    However, this was not the end of the story.

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    HISTORY OF THE ATOM

    1913 Niels Bohr

    studied under Rutherford at the Victoria

    University in Manchester.

    Bohr refined Rutherford's idea by adding

    that the electrons were in orbits. Rather

    like planets orbiting the sun. With each

    orbit only able to contain a set number of

    electrons.

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    Bohrs Atom

    electrons in orbits

    nucleus

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    Marie Skodowska Curie

    TWO Nobel Prizes

    1903PHYSICS With

    her husband for radiation

    phenomena in Uraniumsalts

    1911CHEMISTRY

    On her own for

    discovering theradioactive elements,

    radium and polonium

    The first person to win

    TWO Nobel Prizes

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    HELIUM ATOM

    +

    N

    N

    +

    --

    proton

    electron

    neutron

    Shell

    NOTE: THIS IS NOT TO SCALE. The nucleus is extremely small relativeto the space the electrons are moving in. And electrons do not move innice concentric rings.

    POINT: THIS IS A MODEL that shows composition and relative position.

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    SUBATOMIC PARTICLES

    Particle

    proton

    neutron

    electron

    ?

    ?

    01

    ?

    5X10-4

    RelativeMass

    RelativeCharge

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    ATOMIC STRUCTURE

    the number of protons in an atom

    the number of protons andneutrons in an atom

    He

    4

    2

    number (A)

    number (Z)

    number of ________= number of protonsbut only for NEUTRAL atoms & compounds

    if no CHARGE is shown, assume neutrality

    number of _______= (atomic mass - number of protons)number of _________= atomic number

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    Mass SpectrometerSeparates particles relative to MASS:CHARGE (m/z)

    Used for:

    Determining mass of particlesElemental composition of a compound

    Chemical make-up of a sample

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    1. sample is vaporized

    2. sample is ionized by

    an electron beam; ideally every

    particle is 1+

    3. sample is accelerated

    by charged plates; ions move in a

    beam trough the spectrometer tube

    4. sample is deflected by

    a magnetic field; MOMENTUM:

    heavier particles resist change in

    direction and bend LESS

    5. particles of varied mass

    detected; relative frequencies of each

    is recorded

    Mass Spectrometer

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    Spectrometer Results

    Relative abundance ofmolecules in sea water Br2

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    Isotopes

    All atoms of a certain element have the same , but they

    may have different atoms of the same element that have different

    numbers of neutrons; they have different A, atomic masses

    12C is the atomic mass standard

    12C is set at EXACTLY 12 atomic mass units (amu)

    so, 1 amu = 1/12 the mass of12C1 amu = 1 dalton (Da)

    isotopic mass so how do we determine isotopic mass?

    spectrometer finds mass ratio relative to

    Aisotope = mass ratio X

    What is the isotopic mass of a pure sample of an Si

    isotope with a mass ratio of 2.331411?

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    Spectrometry Problems

    Rubidium has two common isotopes, 85Rb and 87Rb. Ifthe abundance of 85Rb is 72.2% and the abundance of

    87Rb is 27.8%, what is the average atomic mass of

    rubidium?

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    Uranium has three common isotopes. If the abundance of

    234U is 0.01%, the abundance of 235U is 0.71%, and theabundance of 238U is 99.28%, what is the average atomic

    mass of uranium?

    Spectrometry Problems

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    Titanium has five common isotopes: 46Ti (8.0%), 47Ti (7.8%),48Ti (73.4%), 49Ti (5.5%), 50Ti (5.3%). What is the average

    atomic mass of titanium?

    Spectrometry Problems

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    Isotopic Properties

    All isotopes of a given element have nearly identical

    chemical behavior

    (i.e. bonds involving lighter isotopes may break easier)

    Physical characteristics may vary between isotopes

    of the same element relative to mass (momentum) mass/volume

    molecules of liquid separate to gas form

    molecules move to disorder

    these varied physical properties can alter isotopic

    proportions in nature (i.e. global distribution of heavy

    water)

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    Isotope Example Hydrogen has three isotopes:

    1H protium

    2H deuterium

    3

    H tritium

    3H is RADIOACTIVE

    In this case, it is Beta () decayOne neutron turns into a proton and a -particle

    The proton stays, the -particle is emitted

    3

    H

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    Uses of

    Radioisotopes14C used for determining age of organic material

    half life is ~5700 years

    40

    K-40

    Arratios are used to date rockhalf life is ~1.25 billion years

    makes food safer to eat, have a longer shelf life

    60

    Co and

    137

    Cs kill microorganisms, likeE. co li

    125I and 131I for checking thyroid activity

    60Co produce gamma rays to destroy targeted

    cancer cells