Lecture 12: Hydrologic Cycle Flashcards

-Properties of Water -Water Cycle and Balance -Water on the Land's Surface

1
Q

What is the chemistry of the water molecule?

A
  • formed by the covalent bonding of two hydrogens to and oxygen
  • Bent (104.5º)
  • Polar (more negative charge near the oxygen, more positive near the hydrogens)
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2
Q

What are the phases of water?

A
  • Ice
  • Liquid Water
  • Water Vapour
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3
Q

What transitions between phases absorb energy?

A

Evaporation, Melting, Sublimation

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4
Q

What transitions between phases release energy?

A

Condensation (water vapour to liquid water), Freezing, Condensation (water vapour to ice)

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5
Q

Latent heat

A

The energy absorbed or released by a body or thermodynamic system during a constant-temperature process.

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6
Q

Properties of liquid water

A

Due to its polarity, it:

  • Has a high surface tension
  • Is an excellent solvent
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7
Q

Properties of ice

A
  • Lower density than liquid water due to an open crystal lattice
  • Floats in liquid water
  • Expansion of freezing water can cause physical weathering
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8
Q

Evaporation

A

Solar energy causes water to evaporate from large bodies of water, moving it into the atmosphere.

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9
Q

Transpiration

A

The water vapour that is given off by plants.

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10
Q

Condenses

A

Water vapour condenses into clouds

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11
Q

Precipitation

A

The water falls back to land or the ocean as precipitation; rain, hail, or snow.

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12
Q

Infiltration

A

Some of the water infiltrates the ground, where it joins the ground-water reservoir and may eventually be locked up in the lithosphere in the form of the hydrous mineral.

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13
Q

Runoff

A

Some of the moisture flows back to the sea as surface runoff, while a small amount is captured by the biosphere.

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14
Q

Hydrologic reservoirs

A

Places in the water cycle where water is stored.

  • Nearly all the Earth’s water resides in the oceans
  • 75% is locked up as ice at the poles
  • Freshwater and surface water bodies comprise less than 3% of the total water on Earth
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15
Q

Residence time

A

The average amount of time that a water molecule stays in a particular reservoir

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16
Q

Flux

A

The rate at which water moves between reservoirs

17
Q

The residence time of Earth’s reservoirs

A
  • Atmosphere: days
  • Rivers and lakes: months to years
  • Shallow groundwater: decades to centuries
  • Oceans: thousands of years
  • Antarctic ice: tens of thousands of years
18
Q

Hydrologic balance

A

The relationship between flux, reservoir size, and residence times.
-relatively small water reservoirs can have high fluxes because the residence time is short

19
Q

Overland flow

A

The initial sheet-like movement of water downhill with gravity.
- Some of the rainfall and meltwater on the landscape begins to flow across the surface once the soil is saturated.

20
Q

Stream flow

A

Once the flow of water occurs in an establishmed channel

-Overland flow becomes channelized due to erosion, typicaly over relatively short distances.

21
Q

Surface runoff

A

When stream flow and overland flow together they create surface runoff.

22
Q

What are the two major sources for the flow of water in streams?

A
  1. Overland flow contributions

2. Baseflow

23
Q

Baseflow

A

The input of groundwater through the bed of a river, contributing to its flow.

24
Q

River systems

A
  • Streams organize into river systems

- Small streams (tributaries) typically merge downstream

25
Q

Drainage basin

A

Area drained by a major river and tributaries

26
Q

Drainage divides

A

Separate drainage basins

27
Q

Continental-scale basins

A

Topographic highs, such as continental divides typically separate water drainage basins the flow into different oceans

28
Q

What controls river behaviour?

A

The width, depth, gradient, velocity, and discharge of the river.

29
Q

Does the width and depth of a river increase or decrease downstream?

A

Increases, as tributaries join together.

30
Q

Does the gradient of a river increase or decrease downstream?

A

Decreases, steep mountain down to flat plains.

31
Q

Does velocity increase or decrease downstream?

A

Increases

32
Q

Does discharge increase or decrease downstream?

A

Increase

33
Q

What is discharge and how is it determined?

A

Discharge is the flux of water moving through the river at any given point.
It is determined by calculating the cross-sectional area of a river (width x depth), then multiplying that area by the velocity of the river
-This gives the units of discharge in units of volume per time.

34
Q

Dissolved load

A

Major ions in rivers. Primarily comes from dissolution of minerals.

35
Q

Suspended load

A

Comprised of particulate matters that remains in suspension in a river of stream.

  • Smaller particles settle more slowly than larger ones, and so are transported farther
  • Causes water to appear cloudy and opaque
36
Q

Bed load

A

Comprised of typically larger particles in a river system that are transported by moving along the bed.

37
Q

Different forms of transportation in bed load

A

Roll - rotate along the bed without leaving it.
Slide - move along the bed without leaving it.
Saltation - hopping along the bed, leaving it for short periods of time.

38
Q

Hydrographs

A

A record of river discharge at one point in the river continuously over many years.

39
Q

Trends in river mass transport

A
  • Faster flow velocity moves large particles
  • Large particles deposit near their source
  • Smaller particles deposit further downstream
  • Dissolved load is typically carried to sea