The Significant Events in the Development of Science of Geochemistry

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    ASSIGNMENTJanuary 3, 2012

    Submitted To: Dr Tehseenullah Khan Bangash

    The Significant

    Events In TheDevelopment of

    Science Of

    Geochemistry

    Geochemistry

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    The Significant Events In The Development

    of Science Of Geochemistry

    Geochemistry

    Group Members: Awais Nisar

    Zulqarnain Khaliq

    Hassam Mustafa

    Rana Bilal Ahmed

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    Table Of Contents

    Title: Page No:

    The Creation Of Earth 3

    Discovery Of Hydrogen 5

    Discovery Of Oxygen 6

    The Nineteenth Century 7

    F. W. Clarke 10

    Carnegie Institution, Washington. 11

    V. M. Goldschmidt 11

    V. I. Vernadsky 12

    References

    13

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    the matter that was squeezed inside it flew

    about. After that, the pieces of matter joined

    together to first form atoms, then from thoseatoms, stars, our sun, earth and the other

    planets. The scientists named this explosion the

    Big Bang. Everything in the universe was formed

    as a result of this Big Bang.

    Allah is the Maker of the Big Bang, the

    Organiser of the matter that scattered in space

    after the Big Bang. By bringing together all this

    matter, He is also the Creator of the sun, earth,

    planets and stars.

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    Discovery Of Hydrogen:

    Geochemistry did not come into its own as a

    science until the 1800s. The discovery

    of hydrogen opened the door for understanding

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    chemical elements and the concept of the atom.

    Hydrogen was first recognized as a distinct

    element in 1766 by Henry Cavendish, when heprepared it by reacting hydrochloric acid with

    zinc. He described hydrogen as "inflammable air

    from metals" and established that it was the

    same material regardless of which metal and

    which acid he used to produce it. Cavendish also

    observed that when the substance was burned, itproduced water.

    Lavoisier later named the element hydrogen

    (1783). The name comes from the Greek 'hydro'

    meaning water and 'genes' meaning forming -

    hydrogen is one of the two water formingelements.

    Discovery Of Oxygen:After the discovery of hydrogen, Oxygens

    discovery also played a vital role in setting a

    different label for the Geochemisterysience.

    on August 1, 1774, an experiment conducted

    by the british clergyman Joseph

    http://en.wikipedia.org/wiki/Joseph_Priestleyhttp://en.wikipedia.org/wiki/Joseph_Priestley
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    Priestleyfocused sunlight on mercuric

    oxide(HgO) inside a glass tube, whichliberated a gas he named "dephlogisticated

    air". He noted that candles burned brighter

    in the gas and that a mouse was more active

    and lived longer while breathing it. This gas

    was named Oxygen by Antoine Lavoisier in1777.

    Discoveries Of Antoine Lavoisier:

    Before the end of the eighteenth centuryLavoisier recognized some 39 elements.

    These elements included oxygen, nitrogen,

    hydrogen, phosphorus, mercury, zinc

    and sulfur.

    The Nineteenth Century:

    Completion Of The Periodic Table of D. I.Mendeleev.

    http://en.wikipedia.org/wiki/Joseph_Priestleyhttp://en.wikipedia.org/wiki/Mercury(II)_oxidehttp://en.wikipedia.org/wiki/Mercury(II)_oxidehttp://en.wikipedia.org/wiki/Mercury(II)_oxidehttp://en.wikipedia.org/wiki/Mercury(II)_oxidehttp://en.wikipedia.org/wiki/Joseph_Priestley
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    On 6 March 1869, Mendeleev made a formal

    presentation to the Russian Chemical Society,entitled The Dependence between the Properties

    of the Atomic Weights of the Elements, which

    described elements according to both atomic

    weight andvalence.This presentation stated that

    1.Theelements, if arranged according to theiratomic weight, exhibit an apparent periodicity

    of properties.

    2.Elements which are similar in regards to their

    chemical properties have atomic weights

    which are either of nearly the same value

    (e.g., Pt, Ir, Os) or which increase regularly(e.g., K, Rb, Cs).

    3.The arrangement of the elements in groups

    of elements in the order of their atomic

    weights corresponds to their so-called

    valencies, as well as, to some extent, to theirdistinctive chemical properties; as is

    apparent among other series in that of Li, Be,

    B, C, N, O, and F.

    http://en.wikipedia.org/w/index.php?title=Russian_Chemical_Society&action=edit&redlink=1http://en.wikipedia.org/wiki/Atomic_weighthttp://en.wikipedia.org/wiki/Atomic_weighthttp://en.wikipedia.org/wiki/Valence_(chemistry)http://en.wikipedia.org/wiki/Chemical_elementhttp://en.wikipedia.org/wiki/Chemical_elementhttp://en.wikipedia.org/wiki/Valence_(chemistry)http://en.wikipedia.org/wiki/Atomic_weighthttp://en.wikipedia.org/wiki/Atomic_weighthttp://en.wikipedia.org/w/index.php?title=Russian_Chemical_Society&action=edit&redlink=1
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    4.The elements which are the most widely

    diffused have small atomic weights.5.The magnitude of the atomic weight

    determines the character of the element,

    just as the magnitude of the molecule

    determines the character of a compound

    body.6.We must expect the discovery of many yet

    unknown elementsfor example, two elements,

    analogous to aluminium andsilicon,whose

    atomic weights would be between 65 and 75.

    7.The atomic weight of an element may

    sometimes be amended by a knowledge of

    those of its contiguous elements. Thus the

    atomic weight of telluriummust lie between

    123 and 126, and cannot be 128. Here

    Mendeleev seems to be wrong as the "atomic

    mass" of tellurium (127.6) remains higherthan that of iodine(126.9) as displayed on

    modern periodic tables, but this is due to the

    way atomic masses are calculated, based on a

    http://en.wikipedia.org/wiki/Siliconhttp://en.wikipedia.org/wiki/Telluriumhttp://en.wikipedia.org/wiki/Iodinehttp://en.wikipedia.org/wiki/Iodinehttp://en.wikipedia.org/wiki/Telluriumhttp://en.wikipedia.org/wiki/Silicon
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    weighted average of all of an element's

    common isotopes, not just the one-to-one

    proton/neutron-ratio version of the elementto which Mendeleev was referring.

    8.Certain characteristic properties of elements

    can be foretold from their atomic weights.

    Mendeleev published his periodic table of all

    known elements and predicted several new

    elements to complete the table.

    Discovery of the Radioactive Elements:

    Many Radioactive elements and isotopes had

    been discovered by the end of nineteenth

    century hich led to the separartion and

    building of the science if the geochemistry.

    F. W. Clarke:

    In 1884, the US Geological Survey

    appointed a Chief Chemist, F. W. Clarke,

    and set up a laboratory to investigate thechemistry of the planet.

    It was to be concerned with analyses of all

    kinds of materials sent in by the Survey's

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    field officers, and it amassed a wealth of

    sample data.

    Carnegie Institution, Washington:

    In 1904, the Geophysical Laboratory was

    established in Carnegie Institution,Washington.

    The reason was to apply the principles of

    physical chemistry on the study of

    geological processes, especially the

    evolution of the rock-forming minerals.

    V. M. Goldschmidt:

    A few years later V. M. Goldschmidt at the

    University of Oslo applied the phase rule to

    mineralogical changes brought about duringcontact metamorphism of sedimentary rocks.

    His subsequent studies in metamorphism all

    showed that metamorphic changes could be

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    interpreted in terms of the principles of

    chemical equilibrium.

    V. I. Vernadsky:

    In 1915 in the USSR, a school of

    geochemistry was developed energetically

    by V. I. Vernadsky and his successors, suchas A. P. Vinogradov.

    Their work was largely directed towards

    the search for and exploration of mineral

    resources.

    Vernadsky was an expert in mineralogy and

    was the first to relate chemical elements

    to the formation of minerals in nature.

    Russia stakes claim V. I. Vernadsky to the

    founder of geochemistry.

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    After the Second World War, there was a

    surge of interest in radioactivity withinthe Earth, and new methods of analysis and

    instrumentation, such as the electron

    probe, were invented.

    Two of the most significant and rapidly

    expanding fields of research today areorganic geochemistry and biogeochemistry

    Organic materials are found in many

    sedimentary rocks of all ages from the

    Archaean onwards.

    Organic geochemical research has beenconcerned primarily with the origin and

    evolution of living materials and their fate

    after burial.

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    References: http://www.geo.cornell.edu

    http://en.wikipedia.org

    http://science.jrank.org http://www.encyclopedia.com

    http://geofrontiers.com

    http://sustainability.asu.edu

    Thank

    You

    http://www.geo.cornell.edu/http://www.geo.cornell.edu/http://en.wikipedia.org/http://en.wikipedia.org/http://science.jrank.org/http://science.jrank.org/http://www.encyclopedia.com/http://www.encyclopedia.com/http://geofrontiers.com/http://geofrontiers.com/http://sustainability.asu.edu/http://sustainability.asu.edu/http://sustainability.asu.edu/http://geofrontiers.com/http://www.encyclopedia.com/http://science.jrank.org/http://en.wikipedia.org/http://www.geo.cornell.edu/