Properties of water Flashcards

1
Q

‘Hydrogen Bonds’

A

Form between the changed ends of molecules. Covalent bonding within water molecules distorts electrical charge on water molecule creating dipole molecule.

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2
Q

Surface tension in water

A

High level

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3
Q

Dipolar

A

A water molecule is said to be dipolar because it has a positive and a negative pole as a result of the uneven distribution of electrons within it
The dipole nature within a water molecule creates attractive forces known as hydrogen bonding, allowing them to stick together

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4
Q

Unique properties of water

A
  • High heat capacity
  • Higher melting and boiling point relative to other hydrogen compounds
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5
Q

Bonding of H2O

A

Covalent

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6
Q

Asymmetrical shape

A

Two hydrogen molecules are at one end, separated by 105 degreed when in the gaseous or liquid phase and 109.5 degrees when ice

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7
Q

Oxygen end of molecule

A

Negatively charged

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8
Q

Hydrogen end of molecule

A

Positively charges

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9
Q

Dipole structure of water

A

Produces an electrostatic bond (hydrogen bond) between water molecules with cluster together

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10
Q

Clumps of water molecules

A

Act to increase the viscosity of water

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11
Q

Breaking hydrogen bonds

A

More energy is required than normal to break up hydrogen bonds

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12
Q

As temperature decreases….

A
  • Atoms or molecules move closer
  • Density increases because there is more mass (atoms) in the same volume
  • Until formation of ice moves them apart
  • Maximum density caused by hydrogen bonding
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13
Q

What controls density?

A

Temperature

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14
Q

Water dissolves salts by:

A
  • Halite (NaCl) ionic bond
  • Surrounding the atoms in the salt molecule
  • Neutralising the ionic bond holding the molecule together
  • Dissolved salts form cations and anions
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15
Q

What lowers the freezing point of water

A

Adding salt- salt ions intefere with the formations of the hexagonal structure of ice

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16
Q

Hydration

A

The process of water surrounding an ion

17
Q

Seawater salinity

A

The temperature of maximum density is at the freezing point

18
Q

Surface Cooling

A

Dense water sinks and surface cooling >4C increases density and promotes overturning. Sinking water is replaced by upwelling

19
Q

Lakes 0-4C

A
  • Cooling <4C lowers density
  • Stratified cold layer promotes surface freezing
  • Deep water isolated from the surface and remains ‘warm’ throughout winter
20
Q

Density changes in lakes

A

Causes biannual overturning, and prevent lakes from totally freezing

21
Q

Seasonally fresh water

A

Reaches maximum density twice a year; while freezing (autumn) and whilst thawing (spring)
e.g. overturning in lakes

22
Q

When sea water freezes to form sea ice…

A

Salt is rejected during freezing as salt ions interfere with the formation of the hexagonal structure of ice

23
Q

Salt ejection

A

Leads to salty brine solution- aids overturning circulation- thermocline
- Density of water increases as salinity increases