C5 Chemicals Of The Natural Environment

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C5 Chemicals Of The Natural Environment - Presentation Transcript

  1. C5 Chemicals of the natural environment GCSE SCIENCE Stephen Repacholi
  2. Part 1: Chemicals in four spheres
    • Learning Objectives
      • What are naturally occurring elements and compounds?
      • How abundant are elements in different spheres?
      • How do elements cycle between the spheres?
  3. Lithosphere
    • - The rigid outer layer of the Earth
    • - Made up of the crust and the part of the mantle just below it.
    • ~80 km deep
  4.  
  5.  
  6. Elements in the Lithosphere
    • Oxygen comprises 47% of the earth’s crust (by mass) that is made up by minerals that are oxygenated (silicates, carbonates, etc.)
    • Therefore it is the most abundant element.
    • Silicon is the next most abundant element – rocks of the lithosphere are mainly made out of silicates.
    • Other abundant elements are aluminium, iron, calcium, sodium, magnesium, potassium and titanium.
  7. Hydrosphere
    • All the water on Earth.
    • Includes oceans, lakes, rivers, underground reservoirs and rainwater.
    • Covers 2/3 of the globe.
  8.  
  9.  
    • The Earth’s ocean is 89% oxygen by element and contains dissolved oxygen.
    • The ocean is also vital for life as it contributes more than 50% of global photosynthetic oxygen production.
    • Look at the next diagram – what are the three most abundant elements in living tissue?
  10.  
  11. Biosphere
    • All the living things on Earth.
    • Includes all the plants, animals, and microorganisms.
  12.  
  13.  
  14. The Three most abundant elements in the biosphere are…
    • Hydrogen
    • Oxygen
    • Carbon
    • And then nitrogen, calcium, potassium, silicon, magnesium, phosphorus, sulphur, aluminium, sodium, iron and chlorine
  15. Atmosphere
    • The layer of gases that surround the Earth.
  16.  
  17.  
  18.  
  19. What elements are flowing or cycling between the spheres?
  20. Flowing between the spheres
    • Water – water cycle
    • Carbon dioxide – carbon cycle
    • Nitrogen – nitrogen cycle
    • Oxygen – oxygen cycle
  21.  
  22. Carbon Cycle
  23.  
  24.  
  25.  
  26.  
  27. Nitrogen fixing bacteria in root hairs
  28.  
  29. Part 2: Chemicals of the atmosphere
    • Learning objectives
      • What are the gases in the air?
      • What are the weak attractions between molecules?
      • What is strong covalent bonding?
  30. These gases are held within the atmosphere by the force of gravity from the Earth. These gases have low melting points and boiling points. The atmosphere, plus a suitable temperature (water is a liquid usually on Earth) means that the Earth can sustain a variety of life. Note: CH 4 is methane
  31. Molecules
    • Most non-metal elements and most compounds between non-metal elements are molecular.
    • In the atmosphere, there are diatomic molecules , such as N 2 and O 2 , as well as other small molecules such as CO 2 , and H 2 O.
    • Argon (Ar) is one of the exceptions – the noble gases exist as a single atom.
  32. Atoms and molecules in the air
    • All molecules have a slight tendency to stick together.
    • These attractive forces between molecules are weak. E.g. O 2 ---- O 2
    • This explains the low melting points and boiling points of gases in the atmosphere.
  33. Strong bonds in molecules
    • The forces inside molecules are many times stronger than the weak attractions between molecules.
    • Small atoms such as H 2 and O 2 do not split up, except at very, very high temperatures.
    Model of an oxygen molecule
  34. Hydrogen atoms share one electron each to make a stable outer shell
  35. Oxygen atoms share two electrons each to make a stable outer shell
  36. Water molecule
  37. These strong bonds from shared electrons are called COVALENT BONDS Hydrogen has one covalent bond (H-H) and oxygen has two (O=O). Water has single covalent bonds. Note the diagram is not balanced, it should be… 2H 2 + O 2  2H 2 0
  38. Carbon dioxide has what sort of bonds? With molecular models, by convention, hydrogen is white, oxygen is red and carbon is black.
  39. COVALENT BONDS! How many on the outside of each atom? Hint: C is in Gp 4 O is in Gp 6
  40. Carbon has 4 electrons in the outer shell, Oxygen has 6. Carbon needs 4 (4+4=8), Oxygen needs 2 (6+2=8). So each line represents one shared pair or 2 electrons. Count them to get 8 electrons in each outer shell.
  41. Nitrogen molecule What group is in in? Therefore, how many electrons in the outer shell? How many does it need to get a complete outer shell? So how many bonds?
  42. Nitrogen Group 5 5 electrons in the OUTER SHELL It needs 3 electrons to get to 8. So each share 3 electrons = TRIPLE BOND! VERY STRONG INDEED
  43.  
  44. Whoops!
    • The electrostatic forces on the previous slide are from ions… - Some atoms give electrons e.g Na+
    • - Some atoms take electrons e.g. Cl-
    • Then ionic bonds form when opposites attract!
  45. With covalent bonds…
    • The electrostatic attraction is between the (positive) nuclei and the shared pair of (negative) electrons.
  46. Again, opposites attract!
  47. So, covalent bonds…
    • -- CO – together
    • -- VALENT –(from ‘valentia’ = strength)
    • They hold atoms together within molecules
    • The number of bonds depends on the number of shared pairs of electrons.
  48. Part 3 Chemicals in the Hydrosphere
    • Learning Objectives:
      • What are the unusual properties of water?
      • What are the sorts of bonding within a water molecule and between water molecules?
      • What happens to ions in solution?
  49. Properties of Water
    • Liquid at room temperature
    • Smaller mass than O 2 , N 2 or CO 2 .(gases)
    • Melts at 0 ○ C and boils at 100 ○ C
    • Water molecules tend to stick together
    • Ice is less dense that water, so it floats – very unusual property!
  50. Properties of Water
    • It is a good solvent for salts – most common solvents do not dissolve ions, but water does.
    • Pure water does not conduct electricity – it does not contain charged particles that are free to move around.  INSULATOR
  51. Water molecules
    • In the covalent bonds between hydrogen and oxygen, the electrons are not evenly shared –
    • oxygen has more than its fair share, so it has a slight negative charge.
    • hydrogen has a slight positive charge.
  52. Water molecules The greater share of the electrons by oxygen  angular shape of the molecule. Overall, the molecules are still electrically neutral. The small charges on opposite sides of the molecules cause slightly stronger attractive forces between the molecules. Hence, water is ‘sticky’ AND these small charges help water dissolve ionic compounds
  53. The charges on water help attract ions out of their crystals. Ions separate and can move freely when dissolved in water. In sea water there is a mixture of positive and negative ions.
  54.  
  55. Weathering slowly breaks down rocks. This exposes the inside of the rocks to water. Soluble chemicals in the rocks dissolve in the water and it get washed away. WHY IS SEA WATER SALTY? One litre of sea water has ~40 g of dissolved chemicals
  56. Some salts in sea water
    • Sodium chloride Na+ Cl-
    • Potassium chloride K+ Cl-
    • Potassium bromide K+ Br-
    • Potassium iodide K+ I-
    • Magnesium chloride Mg 2+ Cl-
    • Magnesium sulphate Mg 2+ SO 4 2-
    • Positively charged metals and negatively charged non-metals  salts e.g. MgSO 4
  57. Part 4: Chemicals in the lithosphere
    • Learning Objectives
      • What chemicals are in the crust of the Earth?
      • What is ionic bonding?
      • What is the importance of silica and silicates?
      • What are giant covalent structures?
  58.  
  59. Rocks and minerals
    • ‘ Lithos’ = stone or rock
    • The crust is the top of the lithosphere.
    • Rocks are made of one or more minerals
    • E.g. sandstone is mainly silicon dioxide (SiO 2 )
    • Limestone is mainly calcium carbonate
    • (CaCO 3 )
    • Minerals are naturally occurring chemicals – they may be elements (Ag, Au) or compounds (NaCl, SiO 2 ,Fe 2 O 3 )
  60. Granite
    • Granite is a mixture of quartz, feldspar and mica – it is a mixture of minerals.
    • The quartz is glassy grains of silica (silicon dioxide)
    • Mica is black
    • Feldspar is either pink or white
  61. Which minerals of granite are these?
  62. Which minerals of granite are these? MICA WHITE FELDSPAR PINK FELDSPAR QUARTZ
  63. Quartz Pure silicon dioxide is transparent and very hard.
  64. Amethyst
    • A form of quartz with traces of manganese and iron oxide  violet colour
  65. Haematite Fe 3 O 4 You may choose to believe this, but I am a sceptic!
  66. Calcite CaCO 3 calcium carbonate
  67. Iron pyrites FeS 2 FOOL’S GOLD!  This one is on some quartz
  68. Galena PbS
    • Lead sulphide!
  69. Quick Quiz
    • What is the most abundant metal in the lithosphere?
    • What is the most abundant non-metal in the lithosphere?
  70. Quick Quiz
    • What is the most abundant metal in the lithosphere?
    • SILICON (28%)
    • What is the most abundant non-metal in the lithosphere?
    • OXYGEN (47%)
  71. SEA SALT
  72. Sea Salt
    • When sea water evaporates, ionic compounds crystallize
    • E.g. NaCl (rock salt), which is the mineral halite
  73. Salt mine in Cheshire
  74. Gypsum
    • Calcium sulphate CaSO 4
    • It is the main ingredient of plaster and plaster-board.
  75. The structure of salt
    • Sodium chloride is an ionic compound that forms from ionic bonding.
    • Na gives an e-  Na+
    • Cl takes an e-  Cl-
    • The Na+ attracts other Cl- ions that are close to it.
    • In fact 6 Cl- ions can fit around one Na+ ion, and vice versa..
  76. 6 to 1, half a dozen to the other… 6 Cl- ions are attracted around each Na+ ion 4 are on the same plane, in a square like formation 1 is above and 1 is below each ion. The converse is true: 6 Na+ are attracted around each Cl- ion  Cubic crystals form with a giant ionic structure
  77. Properties of salts
    • There are millions of ions held together with very strong attractive forces
    • It takes a lot of energy to break down the regular arrangement of ions
    • So it has a reasonably high melting point and boiling point
    • E.g. NaCl melts at 808 degrees Celcius
  78. Silica and silicates
    • Quartz is the commonest crystalline form
    • Is found in sand and used to make glass
    • Important role in computers (Silicon Valley)
    • 95% if rocks in the Earth’s crust are formed by silica and silicate minerals.
  79. Silicon Dioxide (SiO 2 ) Each Si atom is covalently bonded to four O atoms. Each O atom is bonded to 2 Si atoms. Si-O covalent bond is very strong, so this giant covalent structure is very strong and rigid.
  80. Silica glass used as an insulator in electrical devices No free electrons or ions to carry electricity Electrical insulator Sandstone used as building stone Resists weathering, ending up as sand in rivers, beaches & deserts Insoluble in water Used to make linings for furnaces and high –temperature laboratory glassware Strong, rigid structure; difficult to break down High melting (1610 ○C) and boiling ( 2230 ○C) points Used as abrasive in sandpaper and scouring powders Strong rigid structure; will scratch steel Very hard Uses Comments Property of SiO 2
  81. Deccan traps in India – layer upon layer of basalt (made from silicate minerals)
  82. Part 5 - Chemicals of the Biosphere
    • Learning objectives
      • What chemicals are found in living things?
      • What are the chemicals found in carbohydrates, proteins and DNA?
  83. Biochemistry
    • The study of chemicals of life
    • Most biochemicals are based on three elements – carbon, hydrogen and oxygen
    • Sometimes these large molecules will have nitrogen, sulphur and/or phosphorus
    • Biochemicals start with a carbon skeleton…
  84.  
  85. Carbon
    • Carbon is the element on which all life is based.
    • Carbon atoms can form chains by joining them together (the carbon skeleton)
    • Carbon forms 4 strong covalent bonds, so other atoms can join onto the chains – very often these are hydrogen atoms.
    • A whole branch of chemistry is based on this property of carbon (organic chemistry)
  86. Some organic molecules Acetone – the active ingredient in nail polish remover. Glyceraldehyde – one of the breakdown products of carbohydrate metabolism.
  87. Glucose and Starch Sometimes we don’t write in the carbons on our diagrams, e.g. starch above, as you would get sore fingers! Glucose (left) is really ring-shaped and starch stores glucose…
  88. Glucose Courtesy of the sun and the action of photosynthesis!
  89. Carbohydrate
    • Glucose, starch and cellulose are all examples
    • ‘ Carbo’ – carbon
    • ‘ hydrate’ – water
    • Glucose – very soluble sugar
    • Starch – insoluble polymer – made of long chains of glucose units
    • Cellulose – polymer found in plant walls, that we cannot digest  dietary fibre
  90. Proteins are built from 20 different amino acids Besides, carbon, oxygen and hydrogen, amino acids have nitrogen in them – hence it is something that is very important to get in the diet (thank goodness for nitrogen-fixing bacteria!
  91.  
    • DNA has three parts
    • A deoxyribose sugar
    • A phosphate group
    • (these two form the backbone)
    • and
    • A nitrogenous base
    • (see next slide)
  92. The four bases found in DNA
  93. Quick Quiz
    • How many bonds are formed by each
      • Carbon atom?
      • Oxygen atom?
      • Nitrogen atom?
    • What elements are present in DNA?
  94. Quick Quiz
    • How many bonds are formed by each
      • Carbon atom? FOUR
      • Oxygen atom? TWO
      • Nitrogen atom? THREE
    • What elements are present in DNA?
    • - Carbon, Hydrogen, Oxygen, Nitrogen, Phosphorus
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