3 - Biogeochemical Cycle and Life Processes Flashcards

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1
Q

This refers to a movement on a global scale where the elements and compounds that sustain us are cycled endlessly through living things and through the environment.

A

Biogeochemical cycling

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2
Q

It explains the water exchange through the Earth’s ocean, and and atmosphere.

A

Hydrological cycle

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3
Q

In the hydrological cycle, its is responsible for metabolic processes within cells, for maintaining the flow of key nutrients through ecosystems and for global distribution of heat and energy.

A

Hydrological cycle

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4
Q

It refers to the structural component of organic molecules and chemical bonds in carbon compounds that provide metabolic energy.

A

Carbon

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5
Q

It is a process that refers to the transfer of carbon among plants, animals, and microbes, as well as minerals within the earth and the atmosphere.

A

Carbon cycle

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6
Q

It is the most abundant element in the atmosphere, occupying 78% of it. It is also present in soil, the water we consume, and the air we inhale.

A

Nitrogen

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7
Q

It is a continuous cycle of events in which nitrogen circulates through various living and non-living entities, such as the atmosphere, soil, water, plants, animals, and bacteria.

A

Nitrogen cycle

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8
Q

It is the natural process that explains the changes and movement of phosphorus within soil, water, and living as well as decaying organic matter.

A

Phosphorus cycle

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9
Q

It illustrates how sulfur moves within the earth’s geosphere and biosphere.

A

Sulfur cycle

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10
Q

These are defined as “the biological and chemical reservoirs”, “agents of change”, and “pathway of flow” from one another reservoir of a chemical on earth to another reservoir.

A

Biogeochemical cycles

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11
Q

These describe the amount of material stored, produced, or consumed within the repository, as well as the conversion of material from one repository to another.

A

Biogeochemical cycles

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12
Q

It refers to the science that treats the waters of the earth, their occurrence, circulation, and distribution, their chemical and physical properties, and their reaction with the environment, including the relations to living things.

A

Hydrology

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13
Q

It is the mixture of gases extending from the surface of the Earth towards space.

A

Atmosphere

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14
Q

It refers to the soil crust that lies on the surface of the planet where we live.

A

Lithosphere

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15
Q

It refers to the portion of the Earth that accounts for most of the water storage and consists of oceans, lakes, streams, and shallow groundwater bodies.

A

Hydrosphere

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16
Q

It describes the movement of water from one biogeochemical cycle to another.

A

Hydrological cycle

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17
Q

It refers to the process of converting liquid water from surface water sources to gaseous water that resides in the atmosphere.

A

Evaporation

18
Q

It occurs when water is conveyed from living plant tissue, especially leaves, to the atmosphere.

A

Transpiration

19
Q

It represents the overall pathways of water moving into the atmosphere, which includes evaporation and transpiration from plants.

A

Evapotranspiration

20
Q

It refers to the conversion of water in the gas phase to liquid water by cooling the water molecules.

A

Condensation

21
Q

It occurs when the atmosphere becomes completely saturated with water and the droplets have enough mass to fall from the atmosphere.

A

Precipitation

22
Q

It is a process when some fraction of precipitation seeps into the ground.

A

Infiltration

23
Q

It refers to the topographic area that collects and discharges stream flow through one outlet or mouth.

A

Watershed / drainage basin / catchment

24
Q

It refers to the region that collects rainfall.

A

Watershed / drainage basin / catchment

24
Q

It is formed by precipitation that is not absorbed by the soils, which becomes the source water for all human to use for agriculture, drinking water, and energy production.

A

Runoff

25
Q

These flow into groundwater-based streams or river systems.

A

Intermittent streams

26
Q

It refers to the conversion of atmospheric nitrogen (N2) which is primarily available in an inert form, into the usable form-ammonia (NH3).

A

Nitrogen fixation

27
Q

A type of nitrogen fixation and a natural phenomenon where the energy of lightning breaks the nitrogen into nitrogen oxides, which are then used by plants.

A

Atmospheric fixation

28
Q

A type of nitrogen fixation and a man-made alternative that aids in nitrogen fixation by the use of ammonia.

A

Industrial nitrogen fixation

29
Q

A type of nitrogen fixation in which the nitrogen is not used directly from the air by plants and animals. Bacteria like Rhizobium and blue-green algae transform the unusable form of nitrogen into other compounds that are more readily available.

A

Biological nitrogen fixation

30
Q

It is a process of converting ammonia (NH3) by the presence of bacteria in the soil.

A

Nitrification

31
Q

These are formed by the oxidation of ammonia with the help of Nitrosomonas bacteria species.

A

Nitrites

32
Q

The reaction involved in the process of Nitrification

A

(2)NH3 + (3)O2 → (2)NO2(–) + 2H(+) + (2)H2O
(2)NO2(–) + O2 → (2)NO3(–)

33
Q

This process involves plants taking in the nitrogen compounds from the soil with the help of their roots, which are available in the form of ammonia, nitrite ion, nitrate ions, or ammonium and are used in the formation of the plant and animal proteins.

A

Assimilation

34
Q

It is a process in which when plants or animals die, the nitrogen present in the organic matter is released back into the soil, convert the organic matter back into ammonium.

A

Ammonification

35
Q

The process in which the nitrogen compounds make their way back into the atmosphere by converting nitrate (N2O) into gaseous nitrogen (N2) and nitrous oxide (N2O).

A

Denitrification

36
Q

This process of nitrogen cycle is the final stage and occurs in the absence of oxygen.

A

Denitrification

37
Q

It causes algal blooms and excess plant growth in water bodies.

A

Eutrophication

38
Q

It causes serious loss of soil nutrients such as calcium and potassium; acidification of rivers and lakes; and rising atmospheric concentrations of nitrous oxide, a greenhouse gas.

A

Excess nitrogen input

39
Q

It is present mainly in rocks, soil, and water, which is released into the atmosphere by the burning of fossil fuels, volcanic activities, and decomposition of organic materials.

A

Sulfur

40
Q

On land, it is stored in underground rocks and minerals. It is released by precipitation, weathering of rocks and geothermal vents.

A

Sulfur