Biogeochemical Cycles Flashcards
Definition of Flux
The rate of transfer of material within a system per unit of time (in units of mass/time)
Definition of Reservoir
Areas where elements are accumulated or held for a long period of time
Definition of Residence Time
Average time an element stays in a reservoir before cycling
Definition of feedbacks
processes in a system that can either amplify (+ve) or dampen (-ve) the system’s response to external influences
Example of Positive and Negative feedbacks
Runaway feedback = x amplifies or increases y which amplifies or increases x etc
EG: carbon-rich permafrost (frozen soil) and temperature, ice albedo feedback
Negative/Stabilizing feedback = reduces the effect of change and maintains balance
EG: CO2 and plant growth, silicate weathering feedback
Explain what the Redfield ratio is and how it is used.
Atomic ration of C:N:P found in phytoplankton and throughout deep oceans
Redfield ratio numbers = 106:16:1
Dictates the biogeochemical impacts of phytoplankton growth and decay & allows us to estimate the impact of a process on one nutrient concentration from knowledge of the impact on another nutrient
What is the importance of biology in the cycling of the elements relative to the sedimentary cycle and the anthropogenic effects on these cycles.
Important for degradation of biomatter and mineralisation of elements.
tends to accelerate elemental fluxes between reservoirs.
1) mining – accelerates chemical weathering lithospheric flux of elements (S & Fe) to the hydrosphere (rivers, ocean, lakes, atmosphere)
2) extraction of fertilizer (e.g., phosphate rock) for farming accelerates the rate of biomass production and degradation.
Why is the exchange of CO2 between the atmosphere and ocean important?
- Regulates earth’s temp
- Maintain CO2 concentration in the atmosphere
- Source of carbon for shell growth
What is Ksp, what information can it tell us about a reaction and what considerations are there when using this equation?
The solubility product constant, Ksp, is the equilibrium constant for a solid substance dissolving in an aqueous solution. It represents the level at which a solute dissolves in solution. The more soluble a substance is, the higher the Ksp value it has.
The K equation must always show the reversible reaction so that the value of K has meaning.
The concentrations used in the equation must be measured at equilibrium.
Solids, pure liquids & solvents are not included in the expression.
Products are favoured Ksp > 1
Reactants are favoured Ksp <1
Give the equation for the dissolution of carbon dioxide in water.
CaCO3(s) + CO2(aq) + H2O Ca2+ + 2HCO3-
Referring to the dissolution of CO2 equation, state what effect dissolving CO2 in the ocean has on the pH. What consequences does this have?
Acidifies the ocean. Drives the reaction to the right, dissolution of calcium carbonate (makes it harder for organisms to make their shells). Increased production of carbonate acid.
How do microorganisms drive the uptake of CO2 into the ocean?
Through photosynthesis, respiration, and decomposition. coccolithophores (single-celled algae)
Compare and contrast the amount of CO2 in the surface water of the ocean and the deeper ocean. In your answer include processes that are occurring, whether calcium carbonate is saturated, undersaturated or at equilibrium, and the pH relative to depth and the consequences for marine organisms.
Less CO2 at surface than at deep ocean. Carbon is exported from surface to depths where it is being respired, decreasing pH, and releasing nutrients. Calcium carbonate is saturated as reactants are favoured and SI is positive. The diatoms die and shells dissolve which returns the Carbon to the sea.
What affect does increased continental weathering have on the rate of calcium carbonate burial?
Can deepen CCD (calcite compensation depth) and lysocline increase ocean floor area over which carbonate can accumulate which increases carbon sequestration.
What does the term “biomass” mean?
total amount of living tissue within a given trophic level
Give a half reaction equation for the decomposition of biomass (oxidation reaction).
{CH2O} + 5H2O > CO2(g) + 4H3O+(aq) + 4e-