Biogeochem - Chapter 1: Water (Henrik) Flashcards

1
Q

What temp is waters highest density?

A

4ºC

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2
Q

What causes stratified bodies of water?

A

If the temperature difference and density gradient are big enough

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3
Q

When are temperate lakes stratified

A

In the summer (warm surface water) and in the winter (cooler surface water)

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4
Q

When do temperate lakes mix and what does this enable?

A

In autumn and spring
the water column has no
temperature gradients and can mix.
This allows oxygenated water to
get to the bottom of the water body.

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5
Q

What does a Amictic lake mean?

A

Bodies of water that never turn over. They are permanently covered in ice. These are usually found in Antarctica or at high altitudes in mountains

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6
Q

What is a cold monomictic lake?

A

A body of water that contains waters never exceeding 4ºC. They turn over one a year in the summer and are thermally stratified the rest of the year

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7
Q

Meaning of a dimitic lake?

A

A lake that turns over twice a year, in the spring and autumn. They are thermally stratified at other times in the year.

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8
Q

Where do you find dimitic lakes?

A

They are typically found in temperate climates and at high altitudes in the subtropics

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9
Q

What are warm monomictic lakes and when do they turn over?

A

A body of water that water temp is NEVER BELOW 4ºC. They turn over once a year in the winter and are thermally stratified the rest of the year.

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10
Q

What is a oligomictic lake and where do you find them?

A

they contain water that is significantly warmer than 4ºC. They turn over irregularly and are mostly found in tropical zones

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11
Q

What is a polymictic lake and where do you find them?

A

a lake that has water just over 4ºC and can turn over continually. These occur at high altitudes in equatorial regions.

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12
Q

What is a meromictic lake?

A

They are deep, narrow lakes with bottom waters that never mix with the waters above.

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13
Q

What are the properties of meromictic lakes?

A

Bottom waters generally have high dissolved salt concentrations which makes them dense and separates them from overlying waters by a chemocline. The upper waters in temperature climates may be thermally stratified in the summer and winter and undergo turnover in the spring and fall

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14
Q

Are tropical lakes usually thermally stratified

A

tropical lakes are not usually thermally stratified due to the lack of seasons with strong temperature differences

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15
Q

What does epilimnion refer to?

A

Epilimnion refers to the upper body of water

even during the stratification period, the epilimnion is usually fully mixed

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16
Q

What does hypolimnion refer to?

A

Hypolimnion refers to the deeper body of water

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17
Q

what is the thermocline?

A

the water layer where a steep temperature gradient is found

the larger the lake, the bigger the waves and the deeper the thermocline

18
Q

Is salinity a volatile or stable stratification?

A

Salinity (haline) stratification is usually stable and permanent, in contrast to temperature

19
Q

what does littoral mean/describe?

A

it describes zones close to the shore of the lake where light penetrates to the ground and the entire water column is above compensation depth (where photosynthesis > respiration)

20
Q

What sediment form the benthic zones (nb: sediment from which shore zones)

A

The littoral and profundal (permanently dark) sediment together form the benthic zone

21
Q

where do you find pelagic waters?

A

They are found above the compensation depth and above/on top of profundal waters

(this differs to littoral which is underlain by sediment!)

22
Q

What determines the epilimnion?

A

the lake size and energy input (wind)

23
Q

what determines the compensation depth?

A

(this separates the pelagic and profundal zones)

it is determined by the turbidity of the water in the lake

24
Q

What does stratification inhibit?

A

It inhibits the exchange of dissolved compounds (eg oxygen) between the different bodies of water

25
Q

how do the narrow veins of liquid water form in ice?

A

When ice crystals form, dissolved solids (salts and other compounds) are excluded from the ice crystals and become highly concentrated in the remaining liquid water which turns into brine.

the high salinity of brine lowers the freezing point, so tiny veins of liquid water are still present within the ice.

these liquid veins harbour complex microbial communities

26
Q

Properties of water due to hydrogen bonding

A

high boiling point (temp at which it goes from liquid to gas)

strong cohesion between molecules

large heat of evaporation (energy required to evaporate water)

capillary forces

27
Q

how high can water travel through capillary action?

A

120-130m high…. hence the height limit for trees is 120-130m tall

28
Q

How does H2S behave differently to H2O

(Hint: molecule weight and boiling point…)

A

H2S should behave similar to water… but as it is heavier it should have a higher evaporation energy and higher boiling point… this doesnt happen because it cant form efficient hydrogen bonds

29
Q

Difference between soil and sediment

A

Soil
- usually used for terrestrial habitats
- has 3 fractions: air, water and particles

Sediment
- usually used for deposits underlying a water body
- has 2 fractions: particles and water

30
Q

similarities between soil and sediments

A

both have a component of weathered rock materials
- soild mostly derived from underlying base rock
- sediments contain material that has often been transported over large distances

31
Q

Porosity definition

A

symbol = φ

describes the water content of a sediment (not usually used for soils)

the volume of pore water per volume of sediment

32
Q

porosity equation

A

φ = volume of pore space / total sample volume

33
Q

Porosity of surface sediments and water

A

Surface sediment porosity of between 0.4 - 0.8

pure water has a porosity of 1

34
Q

definition of tortuosity

A

described the effect of the shape and size of sediment particles on sediment diffusive fluxes

symbol = ϴ

35
Q

difference between sandy soils and peat

A

Sand
- usually have very little organic matter

Peat
- are usually/almost exclusively organic matter and contain very little mineral material

36
Q

Why can’t macropores retain water and what does this mean?

A

the diameter of the pores are too large for capillary action

this means water can drain freely as long as the soil is above the water table.

macropores are important for soil aeration

37
Q

why can micropores retain water?

A

they are small enough in diameter to retain water

(the smaller the diameter the stronger the capillary force keeping water inside)

38
Q

what is hygroscopic water

A

it is water that is not available to plants because it is held by strong intermolecular forces between soil particles (eg clays)

39
Q

whats the difference between soil saturation, field capacity and wilting point?

A

Soil saturation
- all pores filled with water
- gravitational water about to drain

Field capacity
- micropores filled with water
- macropores filled with air
- ‘suction’ forces in soil resist gravity flow of water

Wilting point
- most pores filled with air
- water present in small, unavailable quantities

40
Q

what does the term cyclic salt describe?

A

it describes salt that is transported by air currents (wind)