Friday, 21 February 2020

Introduction to chemistry




Introduction to chemistry


1660-The Royal Society for improving Natural was founded in England.

1661-concept of element – Robert Boyle. He defined acid and base.
In 1754, Scottish chemist Joseph Black isolated carbon dioxide, which he called "fixed air".
In 1766, English chemist Henry Cavendish isolated hydrogen, which he called "inflammable air".
In 1773, Swedish chemist Carl Wilhelm Scheele discovered oxygen, which he called "fire air",
In 1774, English chemist Joseph Priestley independently isolated oxygen in its gaseous state, calling it "dephlogisticated air"

1779- oxygen theory of combustion by Lavoisier and
The discovery of law of conservation of mass in a chemical change.

Antoine Lavoisier revolutionized chemistry. He named the elements carbon, hydrogen and oxygen; discovered oxygen’s role in combustion and respiration; established that water is a compound of hydrogen and oxygen; discovered that sulfur is an element, and helped continue the transformation of chemistry from a qualitative science into a quantitative one.
Lavoisier announced a new fundamental law of nature in 1782;
The law of conservation of mass:
matter is conserved in chemical reactions
1800-disovery of Volta’s cell, a pile of dissimilar metals separated by salt soaked card boards;
a pile of such metals consisting of a pair of silver and zinc discs seperated by pieces of moist cardboard.
1800- By applying electric energy, Willium and Anthony, decomposed water into two different gases hydrogen and oxygen. They Confirmed that water is a compound and not an element.

The law of constant composition

Law of definite proportion while forming a compound-By Proust in1799; that the elements combine in a definite ratio by mass to make new compounds. Example; CuCO3 forms by Cu:C: O in a definite ratio, what ever be the method of making it.

1803-Daltons’s Atomic theory of elements and Computation of relative atomic weights of elements.
Dalton's fascination with gases gradually led him to formally assert that every form of matter (whether solid, liquid or gas) was also made up of small individual particles called Atoms.
The main points of Dalton's atomic theory, as it eventually developed, are:
  • Elements are made of extremely small particles called atoms.
  • Atoms of a given element are identical in size, mass and other properties; atoms of different elements differ in size, mass and other properties.
  • Atoms cannot be subdivided, created or destroyed.
  • Atoms of different elements combine in simple whole-number ratios to form chemical compounds.
  • In chemical reactions, atoms are combined, separated or rearranged.
In 1808,In A New System of Chemical Philosophy, Dalton introduced his belief that atoms of different elements could be universally distinguished based on their varying atomic weights. In so doing, he became the first scientist to explain the behavior of atoms in terms of the measurement of weight. He also uncovered the fact that atoms couldn't be created or destroyed.
1811-concept of gas molecule- Avogadro. Avogadro's law that equal volumes of gases contain equal number of particle[molecules].

1812- Discovery of new elements by Humphrey Davy using Volta’s Battery to decompose different salts.
Discovery of Na, K Mg, Ca, Sr and Ba. He also discovered chlorine.

1817- Swedish chemist, Berzelius simplified chemistry through his sugestion that elements be represented by symbols, using the first letter of each element’s Latin name. To indicate a proportion in a coumpound, he wrote the appropriate number as subscript. He was especialy noted for his determination of atomic weights and development of chemical symbols.

Berzelius gave the concept of catalysis for reactions which occur only in the presence of some third substance. He also suggested the name allotropy for the occurance of diferent forms of the same element.

In1834, Faraday’s Electro-chemistry and the Laws of electrolysis.

Faraday discovered that when electricity is passed through ionic solutions, the amount of chemical change produced was proportional to the quantity of electricity passed through it.

1840-Chemical society was founded and Royal college of chemistry opened.

1852-concept of valency by Edward Frankland.

1859-Bunsen discovered that each element produces its own characteristic set of lines in the spectrum.

1860 the first chemical congress called by Kekulay in Germany.
Following the Karlsruhe meeting, values of relative atomic weights, about 1 for hydrogen, 12 for carbon, 16 for oxygen, and so forth were adopted. This was based on a recognition that certain elements, such as hydrogen, nitrogen, and oxygen, were composed of diatomic molecules and not individual atoms.
An important long-term result of the Karlsruhe Congress was the adoption of the now-familiar atomic weights (actually, atomic masses) of approximately 1 for hydrogen, 12 for carbon, 16 for oxygen, Cl 35.5, K39, Ca 40, Br 80, Rb 85, Sr 88, I 127, Cs 133, Ba 137 and so forth.
1869- discovery of periodic properties of elements and periodic table of elements.
On March 6, 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 weight and valence.


Modern chemistry


Discovery of Sub-atomic particle, the electron.
In 1900 Electron was discovered as a subatomic particle.

Electron was discovered by J. J. Thomson in Cathode Ray Tube (CRT) experiment.
  1. Electrons are negatively charged particles with charge-to-mass ratio −1.76×108 C/gm
  2. The charge of an electron was measured by R. Millikan in Oil drop experiment.
  3. Charge of an electron is −1.60×10−19 C
  4. Mass of an electron is 9.1×10−28 gram.
  5. Electron is approximately 2000 times lighter than hydrogen.
Bohr's model of Hydrogen Atom:


In 1913, Neils Bohr, a student of Rutherford's, developed a new model of the atom. He proposed that electrons are arranged in concentric circular orbits around the nucleus. This model is patterned on the solar system and is known as the planetary model. The Bohr model can be summarized by the following four principles:
  • Electrons occupy only certain orbits around the nucleus. Those orbits are stable and are called "stationary" orbits.
  • Each orbit has an energy associated with it. The orbit nearest the nucleus has an energy of E1, the next orbit E2, etc.
  • Energy is absorbed when an electron jumps from a lower orbit to a higher one and energy is emitted when an electron falls from a higher orbit to a lower orbit.
  • The energy and frequency of light emitted or absorbed can be calculated by using the difference between the two orbital energies
Planck’s Quantum theory of Black Body radiation.
Photoelectric effect.
Theory of relativity
The bond theory.
Schrodinger wave equation and electronic configuration of elements.
1928-concept of Hybridization and multiple valency, and concept of crystallization.
1932-Electro-negativity figures calculated by Paulings.
1934-Artificial Radio activity by Fermi.
1942- Nuclear fission by Otto Hahn.


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Chemical industry

The scientific revolution has given birth to industrial revolution.
People began to use science to harnace The Nature, for profit.

1748- Coal mining started
1760- Iron smelting started
1765- steam Engine.
1781- James Watt’s Steam Engine and Industrial revolution. Steam locomotives for transport of large loads on rail roads. By 1800, the firm Boulton and Watts had constructed 496 steam engines.

Chamber process for Sulfuric acid:

In 1746 John Roebuck developed the lead chamber process for the manufacture of sulfuric acid. Prior to this time, sulfuric acid had been produced in glass bottles several pounds at a time. But the lead chamber process could produce sulfuric acid by the ton.
In the original lead chamber process, sulfur and potassium nitrate are ignited in a room lined with lead foil. Potassium nitrate, or saltpeter is an oxidizing agent oxidizes the sulfur to sulfur trioxide according to the reaction:
6 KNO3(s) + 7 S(s) -----> 3 K2S + 6 NO(g) + 4 SO3(g)
The floor of the room was covered with water. When the sulfur trioxide reacted with the water, sulfuric acid was produced:
SO3(g) + H2O(l) -----> H2SO4(aq)
This process was a batch process and resulted in the consumption of potassium nitrate
1791-Leblanc process for Soda ash:

The Leblanc process was an early industrial process for the production of soda ash (sodium carbonate) used throughout the 19th century, named after its inventor, Nicolas Leblanc. It involved two stages: production of sodium sulfate from sodium chloride, followed by reaction of the sodium sulfate with coal and calcium carbonate to produce sodium carbonate.

In 1823, a factory for alkali was set up in England. By 1840 soda was available in bulk quantity.
By the year1870, the British-soda output reached two lakh tons annually.

The Leblanc process was a batch process in which sodium chloride was subjected to a series of treatments, eventually producing sodium carbonate. In the first step, the sodium chloride was heated with sulfuric acid to produce sodium sulfate (called the salt cake) and hydrochloric acid gas, according to the chemical equation,

2 NaCl + H2SO4 Na2SO4 + 2HCl
in the second step, the salt cake was mixed with crushed limestone (calcium carbonate) and coal and fired. In the ensuing chemical reaction, the coal (carbon) was oxidized to carbon dioxide, reducing the sulfate to sulfide and leaving behind a solid mixture of sodium carbonate and calcium sulfide, called black ash.
Na2SO4 + CaCO3 + 2 C → Na2CO3 + CaS + 2 CO2
Because sodium carbonate is soluble in water, but neither calcium carbonate nor calcium sulfide is, the soda ash was then separated from the black ash by washing it with water. The wash water was then evaporated to yield solid sodium carbonate. This extraction process was termed lixiviation.
Bleaching powder for Textile industry:

Bleaching powder (formerly known as "chlorinated lime"), usually a mixture of calcium hypochlorite
(Ca(ClO)2), calcium hydroxide (Ca(OH)2), and calcium chloride (CaCl2) in variable amounts.
St. Rollox Chemical Works produced almost 10,000 tons of bleaching powder in 1804, improving exponentially its production of 52 tons in 1799. Created by Charles Tennant (who discovered the bleaching powder), it was considered as the first biggest chemical enterprise in the world.

Discovery of coal and distillation to make coke
Destructive distillation of coal:
when coal is destructively distilled, coal gas, ammonia, coal tar and coke were obtained.
When coal-tar was fractionally distilled, light oil, middle oil, heavy oil were obtained.
Abraham Pineo Gesner, a Canadian geologist developed a process to refine a liquid fuel from coal, bitumen and oil shale. His new discovery, which he named kerosene, burned more cleanly and was less expensive than competing products, such as whale oil. In 1850, Gesner created the Kerosene Gaslight Company and began installing lighting in the streets in Halifax and other cities.

1828-Blast Furnace for pig-Iron extraction from iron-ore, using coke and hot air pumping[Hot blast process].

Discovery of crude oil and distillation to make kerosene to light the streets.
The first oil well is drilled successfully near Titusville, Pennsylvania in 1859. This oil well of 70 feet marked the beginning of the Petroleum Industry.

Bejamín Silliman, from New Haven, Conneticut, obtained valuable products from the destillation of petroleum in 1855. Between these valuable products were the naphthalene, gasoline, tar and other solvents.

Industrial organic chemistry and plastic materials.



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Sunday, 16 February 2020

Origin of Hydrocarbons




Origin of Hydrocarbons

Abraham Pineo Gesner, a Canadian geologist developed a process to refine a liquid fuel from coal, bitumen and oil shale. His new discovery, which he named kerosene, burned more cleanly and was less expensive than competing products, such as whale oil. In 1850, Gesner created the Kerosene Gaslight Company and began installing lighting in the streets in Halifax and other cities. By 1854, he had expanded to the United States where he created the North American Kerosene Gas Light Company at Long Island, New York.
Rapid burial of the remains of the single-celled planktonic plants and animals within fine-grained sediments effectively preserved them. This provided the organic materials, the so-called protopetroleum, for later diagenesis (a series of processes involving biological, chemical, and physical changes) into true petroleum.
The first, or immature, stage of hydrocarbon formation is dominated by biological activity and chemical rearrangement, which convert organic matter to kerogen. This dark-coloured insoluble product of bacterially altered plant and animal detritus is the source of most hydrocarbons generated in the later stages.
Deeper burial by continuing sedimentation, increasing temperatures, and advancing geologic age result in the mature stage of hydrocarbon formation, during which the full range of petroleum compounds is produced from kerogen and other precursors by thermal degradation and cracking (in which heavy hydrocarbon molecules are broken up into lighter molecules). Depending on the amount and type of organic matter, hydrocarbon generation occurs during the mature stage at depths of about 760 to 4,880 metres (2,500 to 16,000 feet) at temperatures between 65 °C and 150 °C (150 °F and 300 °F). This special environment is called the “oil window.” In areas of higher than normal geothermal gradient (increase in temperature with depth), the oil window exists at shallower depths in younger sediments but is narrower. Maximum hydrocarbon generation occurs from depths of 2,000 to 2,900 metres (6,600 to 9,500 feet). Below 2,900 metres, primarily wet gas, a type of gas containing liquid hydrocarbons known as natural gas liquids, is formed.
At the end of the mature stage, below about 4,800 metres (16,000 feet), depending on the geothermal gradient, kerogen becomes condensed in structure and chemically stable. In this environment, crude oil is no longer stable, and the main hydrocarbon product is dry thermal methane gas.
Oil and natural gas is believed to have been generated in significant volumes only in fine-grained sedimentary rocks (usually clays, shales, or clastic carbonates) by geothermal action on kerogen, leaving an insoluble organic residue in the source rock. The release of oil from the solid particles of kerogen and its movement in the narrow pores and capillaries of the source rock is termed primary migration.
The hydrocarbons expelled from a source bed next move through the wider pores of carrier beds (e.g., sandstones or carbonates) that are coarser-grained and more permeable. This movement is termed secondary migration and may be the result of rocks folding or raising from changes associated with plate tectonics.
The distinction between primary and secondary migration is based on pore size and rock type. In some cases, oil may migrate through such permeable carrier beds until it is trapped by a nonporous barrier and forms an oil accumulation.
Since nearly all pores in subsurface sedimentary formations are water-saturated, the migration of oil takes place in an aqueous environment.
The porosity (volume of pore spaces) and permeability (capacity for transmitting fluids) of carrier and reservoir beds are important factors in the migration and accumulation of oil. Most conventional petroleum accumulations have been found in clastic reservoirs (sandstones and siltstones).