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8/13/2019 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
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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
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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_Priestley8/13/2019 The Significant Events in the Development of Science of Geochemistry
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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=18/13/2019 The Significant Events in the Development of Science of Geochemistry
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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/Silicon8/13/2019 The Significant Events in the Development of Science of Geochemistry
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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/