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Alkanes. Constitutional Isomers. Have the same molecular formula. Have different atom arrangements (different structural formula). CH 3 CH 2 CH 2 CH 3. Butane. C 4 H 10. CH 3. 2-Methylpropane. CH 3 CHCH 3. C 4 H 10. Structural Isomer Practice.
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Constitutional Isomers • Have the same molecular formula. • Have different atom arrangements (different structural formula). CH3CH2CH2CH3 Butane C4H10 CH3 2-Methylpropane CH3CHCH3 C4H10
Structural Isomer Practice • On piece of your own paper, draw AND name ALL of the isomers for the following alkanes: • Pentane • Hexane • Heptane C5H12 C6H14 C7H16 3 5 9 Formulas isomers Dr Seemal Jelani Chem-160
Structural Isomers: Pentane (C5H12) pentane 2-methylbutane 2,2-dimethylpropane Dr Seemal Jelani Chem-160
Structural Isomers: Hexane (C6H14) hexane 2,3-dimethylbutane 2-methylpentane 2,2-dimethylbutane 3-methylpentane Dr Seemal Jelani Chem-160
Structural Isomers: Heptane (C7H16) heptane 2,2-dimethylpentane 2-methylhexane 2,3-dimethylpentane 3-methylhexane Dr Seemal Jelani Chem-160
Structural Isomers: Heptane (C7H16) 2,4-dimethylpentane 3-ethylpentane 3,3-dimethylpentane 2,2,3-trimethylbutane Dr Seemal Jelani Chem-160
Cyclic Hydrocarbon - Cycloalkane Cyclobutane = Cyclopentane = = Cyclohexane
Physical Properties of Alkanes • Nonpolar • Insoluble in water. • Lower density than water. • Low boiling and melting points. • Gases with 1-4 carbon atoms. • (methane, propane, butane) • Liquids with 5-17 carbon atoms. • (kerosene, diesel, and jet fuels) • Solids with 18 or more carbon atoms. • (wax, paraffin, Vaseline)
Boiling & melting points of Alkanes bp & mp ↑ Number of carbon atoms ↑ Number of branches ↑ bp & mp ↓ CH3 CH3CH2CH2CH3 CH3CHCH3
1- Combustion: • Alkanes react with oxygen. • CO2, H2O, and energy are produced. • Alkane + O2 CO2 + H2O + heat • CH4 + 2O2 CO2 + 2H2O + energy Chemical reactions of Alkanes Low reactivity
Halogenation Free Radical reaction Dr Seemal Jelani Chem-160
Chemical reactions of Alkanes Low reactivity 2- Halogenation: Alkanes react with Halogens. CH4 + Cl2CH3Cl + HCl Chloromethane Heat or light Dichloromethane CH3Cl+ Cl2CH2Cl2 + HCl Heat or light CH2Cl2+ Cl2CHCl3 + HCl Trichloromethane Heat or light CHCl3+ Cl2CCl4 + HCl Tetrachloromethane Heat or light
Halogenation • Reaction between a substance and a halogen in which one or more halogens atoms are incorporated into molecules of the substance • Product is Hydrocarbon derivative • Halogenation is an example of Substitution reaction It is a reaction in which part of a small reacting molecule replaces an atom or group of atoms on a hydrocarbons Dr Seemal Jelani Chem-160
General reaction heat or R-H + X2 R-X + H-X light R= Alkyl group Halogenation means: X2 where X = F, Br, Cl, I Dr Seemal Jelani Chem-160
Radical Halogenation Terms • Mechanism • How the reaction occurs through multiple steps (most reactions actually occur in many steps) • Chain Reaction • Reactions that occur on their own after some initiating event • Free Radicals • Atoms that have one free electron—highly reactive Dr Seemal Jelani Chem-160
Radical Halogenation Terms • Initiation Step • Step where a bond is split by heat/light, producing free radicals • Propagation Step • Step where free radicals react with non-radicals, producing more free radicals and continuing the “chain reaction” • Termination Step • Step where free radicals react with each other, producing non-radicals and terminating the “chain reaction” Dr Seemal Jelani Chem-160
Initiation • Reaction starts with one photon of light. • Must be UV • Wavelength less than 400nm • Energy less than 300kJ per mole • Reaction proceeds to completion after this. • Reason is the chlorine molecule • Light breaks the Cl-Cl bond • •Homolytic fission • Each atom takes an electron • Forms radicals. Dr Seemal Jelani Chem-160
Initiation • Homolytic fission forms radicals • Radicals are very reactive atoms or groups. • Cl2 2Cl. • Radicals react quickly with surrounding molecules. Dr Seemal Jelani Chem-160
Reactions of Alkanes CH4 + Cl2 CH3Cl + HCl Mechanism (chain reaction): Step 1 Cl2⇌ Cl· + Cl · Step 2 Cl· + CH4 CH3· + HCl Step 3 CH3· + Cl2 CH3Cl + Cl· Step 4 Cl· + Cl· Cl2 Type of Step Initiation Propagation Propagation Termination h Radical Halogenation of Alkanes (Free Radicals) Overall reaction: CH4 + Cl2 CH3Cl + HCl chloromethane Why not 1-chloromethane? Halogenated product is a haloalkane Naming: halogen atom is a substituent, replace –ine ending with –o -F fluoro -Cl chloro -Br bromo -I iodo Dr Seemal Jelani Chem-160
CHLORINATION OF METHANE Further propagationIf excess chlorine is present, further substitution takes place The equations show the propagation steps for the formation of... dichloromethaneCl• + CH3Cl ——> CH2Cl• + HCl Cl2 + CH2Cl• ——> CH2Cl2 + Cl• trichloromethane Cl• + CH2Cl2 ——> CHCl2• + HCl Cl2 + CHCl2• ——> CHCl3 + Cl• tetrachloromethane Cl• + CHCl3 ——> CCl3• + HCl Cl2 + CCl3• ——> CCl4 + Cl• Mixtures Because of the many possible reactions there will be a mixture of products. Individual haloalkanes can be separated by fractional distillation. Dr Seemal Jelani Chem-160
CRACKING Involves the breaking of C-C bonds in alkanes Converts heavy fractions into higher value products THERMALproceeds via a free radical mechanism CATALYTICproceeds via a carbocation (carbonium ion) mechanism CATALYTIC SLIGHT PRESSURE HIGH TEMPERATURE ... 450°C ZEOLITE CATALYST CARBOCATION (IONIC) MECHANISM HETEROLYTIC FISSION PRODUCES BRANCHED AND CYCLIC ALKANES, AROMATIC HYDROCARBONS USED FOR MOTOR FUELS ZEOLITES are crystalline aluminosilicates; clay like substances Dr Seemal Jelani Chem-160
At each level a mixture of compounds in a similar boiling range is taken off • Rough fractions can then be distilled further to obtain narrower boiling ranges • Some fractions are more important - usually the lower boiling point ones, high boiling fractions may be broken down into useful lower boiling ones - CRACKING Dr Seemal Jelani Chem-160
Sources of Alkanes • Natural gas • 90 to 95 percent methane • 5 to 10 percent ethane, and • a mixture of other low-boiling alkanes, chiefly propane, butane, and 2-methylpropane. • Petroleum • A thick liquid mixture of thousands of compounds, most of them hydrocarbons formed from the decomposition of marine plants and animals.