Catchment Hydrology + The Processes of the Carbon Cycle Flashcards

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1
Q

What is evaporation and how does it transfer heat around the planet?

A

Evaporation is the process by which liquid water changes to vapour and is the main pathway by which water enters the atmosphere. It requires heat, which does not produce a rise in temperature in the water, but rather is absorbed as latent heat and released later in condensation. This process allows for huge quantities of heat to be transferred around the planet, from the oceans to the continents and from the tropics to the poles.

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2
Q

How does vegetation intercept precipitation?

A

Vegetation intercepts a proportion of precipitation, storing it temporarily on branches, leaves, and stems.

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3
Q

What are the two flowpaths of rainwater that does not enter storage?

A

Rainwater that does not enter storage follows one of two flowpaths to streams and rivers: infiltration by gravity into the soil and lateral movement or throughflow to stream and river channels, or overland flow across the ground surface either as a sheet or as trickles and rivulets to stream and river channels.

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4
Q

What are the two conflicting ideas regarding the flowpaths of rainwater?

A

Two conflicting ideas explain the flowpaths followed by rainwater. One relates overland flow to the soil’s infiltration capacity or the maximum rate it can absorb rain. Thus, it is argued that when rainfall intensity exceeds infiltration capacity, overland flow occurs. The second idea states that rainfall, regardless of its intensity, always infiltrates the soil.

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5
Q

What are the factors affecting interception loss according to Table 4.5?

A

According to Table 4.5, the factors affecting interception loss are the interception storage capacity, rates of evaporation increase with wind speed, turbulence also increases with wind speed causing additional throughfall, vegetation type, and tree species.

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6
Q

How does interception depend on the duration and intensity of a rainfall event?

A

Interception depends on the duration and intensity of a rainfall event. Before the onset of rainfall, vegetation surfaces are dry and their ability to retain water is at a maximum. Initially, most rainfall is intercepted. However, as vegetation becomes saturated, output of water through stemflow and throughfall increases.

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7
Q

How do wind speed and turbulence affect interception loss?

A

Rates of evaporation increase with wind speed, and turbulence also increases with wind speed causing additional throughfall.

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8
Q

What vegetation types have higher interception losses than others?

A

Interception losses are greater from grasses than from agricultural crops. Trees, which have a large surface area and aerodynamic roughness, have higher interception losses than grasses.

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9
Q

Why do evergreen conifers have far greater interception losses than broad-leaved, deciduous trees?

A

Interception losses are far greater from evergreen conifers (e.g. spruce, pine) than from broad-leaved, deciduous trees (e.g. oak, ash). This is because most conifers have leaves all year round and water adheres to the spaces between conifer needles (like water on a comb), which increases evaporation.

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10
Q

What is ablation?

A

Ablation is the loss of ice from snow, ice sheets, and glaciers due to a combination of melting, evaporation, and sublimation.

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11
Q

What is the main cause of flooding in adjacent lowlands in Britain during winter?

A

Rapid thawing of snow in upland Britain in winter is a common cause of flooding in adjacent lowlands.

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12
Q

What is photosynthesis?

A

Photosynthesis is the process by which green plants and marine phytoplankton convert light energy to chemical energy (glucose) using the Sun’s energy, CO2 from the atmosphere, and water.

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13
Q

What is respiration?

A

Respiration is the process in which plants release CO2 to the atmosphere while using energy in the form of glucose to maintain growth, reproduction, and other life processes.

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14
Q

What are the main processes involved in carbon exchanges?

A

The main processes involved in carbon exchanges (or fluxes) are precipitation, photosynthesis, weathering, respiration, decomposition, and combustion.

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15
Q

What is weathering?

A

Weathering is the in situ breakdown of rocks at or near the Earth’s surface by chemical, physical, and biological processes, and it involves rainwater which contains dissolved CO2 from the soil as well as the atmosphere.

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16
Q

What is interception?

A

Interception is the process by which vegetation intercepts a proportion of precipitation, storing it temporarily on branches, leaves, and stems.

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17
Q

What is groundwater flow?

A

Groundwater flow is the slow migration of water through rock pores and joints as groundwater, eventually emerging at the surface as springs or seepages.

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18
Q

What is the process by which atmospheric CO2 dissolves in rainwater?

A

The process by which atmospheric CO2 dissolves in rainwater to form weak carbonic acid is a natural process.

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19
Q

What is abiotic storage?

A

Abiotic storage is the storage of water in soil, snow, and ice.

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20
Q

What is infiltration capacity?

A

Infiltration capacity is the maximum rate at which soil can absorb rainwater. When rainfall intensity exceeds infiltration capacity, overland flow occurs.

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21
Q

What is cryospheric processes?

A

Cryospheric processes are processes involving snow, ice, and permafrost.

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22
Q

What is the carbon flux from the atmosphere to land plants and phytoplankton via photosynthesis?

A

The flux of carbon from the atmosphere to land plants and phytoplankton via photosynthesis averages around 120 gigatonnes (GT) a year.

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23
Q

What is evaporation?

A

Evaporation is the phase change of liquid water to vapour and is the main pathway by which water enters the atmosphere.

24
Q

What is the process by which groundwater levels follow a distinct seasonal pattern in southern England?

A

Groundwater levels on the chalk in southern England follow a distinct seasonal pattern, with the water table beginning to rise as temperatures and evapotranspiration fall by late October. This recharge continues until late January, and groundwater levels then decline throughout the late winter, spring, and summer, reaching their lowest point in early autumn.

25
Q

What is overland flow?

A

Overland flow is the flow of rainwater across the ground surface either as a sheet or as trickles and rivulets to stream and river channels.

26
Q

What are the conflicting ideas that explain the flowpaths followed by rainwater?

A

Two conflicting ideas explain the flowpaths followed by rainwater: one relates overland flow to the soil’s infiltration capacity or the maximum rate it can absorb rain, and the other idea states that rainfall, regardless of its intensity, always infiltrates the soil.

27
Q

What is photosynthesis?

A

Photosynthesis is the process by which green plants and marine phytoplankton convert light energy to chemical energy (glucose) using the Sun’s energy, CO2 from the atmosphere, and water.

28
Q

What is the flux of carbon from the atmosphere to land plants and phytoplankton via photosynthesis?

A

The flux of carbon from the atmosphere to land plants and phytoplankton via photosynthesis averages around 120 gigatonnes (GT) a year.

29
Q

What is the equation for photosynthesis?

A

The equation for photosynthesis is 6CO2 + 6H2O → C6H12O6 + 6O2.

30
Q

What is respiration?

A

Plants use energy in the form of glucose to maintain growth, reproduction, and other life processes. In doing so, they release CO2 to the atmosphere in respiration.

31
Q

What are the main processes involved in carbon exchanges (or fluxes)?

A

The main processes involved in carbon exchanges (or fluxes) are precipitation, photosynthesis, weathering, respiration, decomposition, and combustion.

32
Q

What is weathering?

A

Weathering is the in situ breakdown of rocks at or near the Earth’s surface by chemical, physical, and biological processes.

33
Q

What is carbonation?

A

Carbonation is the process by which rainwater, which is a weak carbonic acid, slowly dissolves limestone and chalk, releasing carbon from limestones to streams, rivers, oceans, and the atmosphere.

34
Q

How does the effectiveness of solution weathering on limestone vary with soil cover?

A

The effectiveness of solution weathering on limestone is most effective beneath a soil cover because the higher concentration of CO2 in the soil makes rainwater highly acidic.

35
Q

What is physical weathering by freeze-thaw?

A

Physical weathering by freeze-thaw breaks rocks down into smaller particles but involves no chemical changes.

36
Q

What is the effect of physical weathering on chemical attack?

A

Physical weathering increases the surface area exposed to chemical attack.

37
Q

What is chelation?

A

Chelation is a biological weathering process that contributes to rock breakdown.

38
Q

How do humid acids attack rock minerals?

A

Humid acids formed by rainwater mixed with dead and decaying organic material in the soil attack rock minerals.

39
Q

What is respiration?

A

Respiration is the process in which carbohydrates (e.g. glucose) fixed in photosynthesis are converted to CO2 and water.

40
Q

What is the reverse of photosynthesis?

A

The reverse of photosynthesis is respiration.

41
Q

What are the two most important processes in the fast carbon cycle?

A

The two most important processes in the fast carbon cycle are respiration and photosynthesis.

42
Q

What is decomposition?

A

Decomposition is the breakdown of dead organic matter by decomposer organisms such as bacteria and fungi.

43
Q

What factors affect the rate of decomposition?

A

The rate of decomposition depends on climatic conditions, with the fastest rates occurring in warm, humid environments such as the tropical rainforest.

44
Q

What is combustion?

A

Combustion occurs when organic material reacts or burns in the presence of oxygen.

45
Q

What are some natural uses of combustion in ecosystems?

A

Wildfires caused by lightning strikes are essential to the health of some ecosystems such as the coniferous forests of the Rocky Mountains.

46
Q

What is the main cause of combustion from human activities?

A

The combustion of fossil fuels is the main cause of combustion from human activities.

47
Q

How much CO2 is transferred from fossil fuel burning to the atmosphere, oceans, and biosphere each year?

A

Currently, the burning of fossil fuels transfers nearly 10 GT of CO2 a year from geological store to the atmosphere, oceans, and biosphere.

48
Q

What are the two mechanisms by which the oceans take up carbon?

A

The oceans take up carbon by two mechanisms referred to as a “physical pump” and a “biological pump”.

49
Q

What is the physical carbon pump?

A

The physical carbon pump involves the mixing of surface and deep ocean waters by vertical currents, creating a more even distribution of carbon in the oceans. Initially, CO2 enters the oceans from the atmosphere by diffusion. Surface ocean currents then transport the water and its dissolved CO2 polewards where it cools, becomes more dense and sinks.

50
Q

Where does downwelling occur in the oceans?

A

Downwelling occurs in only a handful of places in the oceans, one of which is in the North Atlantic between Greenland and Iceland.

51
Q

What happens to dissolved carbon that is carried to the ocean depths by downwelling?

A

Dissolved carbon is carried to the ocean depths by downwelling, where individual carbon molecules may remain for centuries.

52
Q

What is the biological carbon pump?

A

Carbon is exchanged between the oceans and atmosphere through the actions of marine organisms, which is referred to as the biological carbon pump.

53
Q

What marine organisms drive the biological pump?

A

Phytoplankton, floating near the ocean surface, combine sunlight, water and dissolved CO2 to produce organic material. Coccolithophores, molluscs, and crustaceans also contribute to the biological pump.

54
Q

What happens to carbon that is locked in phytoplankton?

A

Carbon locked in phytoplankton either accumulates in sediments on the ocean floor or is decomposed and released into the ocean as CO2.

55
Q

Where are huge stores of carbon found on land?

A

Huge stores of carbon are found in land plants, especially trees in the rainforests and boreal forests.

56
Q

What is carbon sequestration?

A

Carbon sequestration is the process by which carbon is removed from the atmosphere and stored in a stable form, such as in vegetation, soils, or oceans.

57
Q

How does carbon sequestration occur in oceans?

A

Carbon sequestration in oceans occurs through the physical and biological pumps, where carbon is either mixed and distributed throughout the ocean depths or is exchanged through the actions of marine organisms. Marine organisms also extract carbonate and calcium ions from seawater to manufacture plates, shells, and skeletons of calcium carbonate, which eventually ends up in ocean sediments and is ultimately lithified to form chalk and limestone