Matter cycles
Picture a walk across the Bog of Allen: the peat under your boots is carbon that plants fixed thousands of years ago, and the carbon in your breath today may once, millions of years ago, have been part of a dinosaur. Unlike energy, which is dissipated as heat and does not come back, the atoms of matter are not destroyed: they pass from living things to the atmosphere, the water or the rocks, and return again and again. These journeys are called biogeochemical cycles.
Reservoirs, fluxes and types of cycle
A mature forest stores tonnes of carbon in its trunks, but when the wood burns or decomposes, that mass disappears from view even though the atoms have not been destroyed. Where is the planet's matter stored, and by what mechanisms does it travel from one place to another?
Explain the difference between a gaseous and a sedimentary biogeochemical cycle, and classify the carbon, nitrogen, and phosphorus cycles into one of the two types,…
Explain the difference between a gaseous and a sedimentary biogeochemical cycle, and classify the carbon, nitrogen, and phosphorus cycles into one of the two types, justifying your choice.
Define reservoir and flow in a biogeochemical cycle, and identify a specific reservoir and a specific flow in the carbon cycle, explaining which process maintains that…
Define reservoir and flow in a biogeochemical cycle, and identify a specific reservoir and a specific flow in the carbon cycle, explaining which process maintains that flow.
Explain what the decomposition of organic matter is, which groups of organisms carry it out, and why the cycles of matter would come to a halt without them even if…
Explain what the decomposition of organic matter is, which groups of organisms carry it out, and why the cycles of matter would come to a halt without them even if producers were still present.
The carbon cycle
Carbon dioxide is also a controlling factor in plants: when CO₂ levels inside a leaf are low, the guard cells open the stomata so more CO₂ can enter for photosynthesis, and when CO₂ is high they tend to close. This is comparable to the way a rise in CO₂ in the blood makes the brain speed up breathing in humans.
Decomposers (bacteria and fungi) feed on dead organisms and waste. Their respiration returns carbon to the air as $\text{CO}_2$ and releases mineral nutrients to the soil. Without them, nutrients would stay locked in dead matter and producers would run out of raw materials. In waterlogged peat bogs, decomposition is slow, so carbon builds up as peat: a carbon sink, as are forests, algae and phytoplankton. Phytoplankton in the oceans photosynthesise and take up dissolved $\text{CO}_2$, which the sea replaces from the air: the oceans act like a sponge for atmospheric $\text{CO}_2$. Some of this carbon sinks as dead matter to the sea floor.
When you read a carbon-cycle diagram with unlabelled arrows, name each arrow by what happens at its two ends. An arrow from the atmosphere into producers is photosynthesis. An arrow from producers or consumers back to the atmosphere is respiration. An arrow from living things or dead matter to the soil and decomposers is death and waste (decomposition). An arrow from fossil fuels or peat into the atmosphere is combustion, and it is the flux that adds carbon from outside the fast cycle and upsets the balance.
The carbon cycle has a fast part (photosynthesis, respiration, decomposition, with fluxes of years to decades) and a slow part (sedimentary rock and fossil fuels, over millions of years). Residence time is how long carbon stays in a reservoir. A large reservoir does not make a small extra flux harmless: the atmosphere is a small reservoir, so burning fossil fuels, which moves carbon quickly into it, makes a large relative change and upsets the balance of the natural fluxes. Iron limits phytoplankton in some ocean regions; adding it would boost the biological carbon pump, but carbon only stays stored if it sinks to deep sediments instead of being recycled near the surface.
Write the overall chemical equations for photosynthesis and aerobic cellular respiration, and explain the role both processes play, in opposite directions, within the…
Write the overall chemical equations for photosynthesis and aerobic cellular respiration, and explain the role both processes play, in opposite directions, within the carbon cycle.
Petrol combustion and cellular respiration both release $\text{CO}2$. Explain what the two processes have in common chemically, how they differ, and why only one of them…
Petrol combustion and cellular respiration both release $\text{CO}_2$. Explain what the two processes have in common chemically, how they differ, and why only one of them has been part of the natural carbon cycle for millions of years.
The diagram represents the main reservoirs and fluxes of the carbon cycle. Name the processes marked with the letters a, b, and c, indicate which process corresponds to…
The diagram represents the main reservoirs and fluxes of the carbon cycle. Name the processes marked with the letters a, b, and c, indicate which process corresponds to the arrow marked with '?', and explain how this flux alters the balance of the cycle.
Explain the role phytoplankton plays in the oceanic carbon cycle and why the oceans are said to act as a sponge for atmospheric $\text{CO}2$.
Explain the role phytoplankton plays in the oceanic carbon cycle and why the oceans are said to act as a sponge for atmospheric $\text{CO}_2$.
Describe the possible journey of a carbon atom from being part of atmospheric $\text{CO}2$ to becoming incorporated into a muscle in your body and then returning to the…
Describe the possible journey of a carbon atom from being part of atmospheric $\text{CO}_2$ to becoming incorporated into a muscle in your body and then returning to the atmosphere, naming the biological process behind each step (photosynthesis, feeding, respiration...).
A mature forest fixes $10\ \text{t}$ of $\text{CO}2$ per hectare per year, but its trees and decomposers release $9.5\ \text{t}$ through respiration over the same…
A mature forest fixes $10\ \text{t}$ of $\text{CO}_2$ per hectare per year, but its trees and decomposers release $9.5\ \text{t}$ through respiration over the same period. Calculate the forest's net annual carbon sequestration and explain why a young, growing forest sequesters much more than a mature one even though it fixes less $\text{CO}_2$ in total.
Explain how the deforestation of a tropical basin disrupts both the carbon cycle and the water cycle at the same time: what happens to the carbon stored in the biomass,…
Explain how the deforestation of a tropical basin disrupts both the carbon cycle and the water cycle at the same time: what happens to the carbon stored in the biomass, to evapotranspiration, to the region's rainfall and to runoff.
Cattle emit methane ($\text{CH}4$) during digestion. Explain which anaerobic process produces it, which cycle of matter it belongs to, and why its emission is a concern…
Cattle emit methane ($\text{CH}_4$) during digestion. Explain which anaerobic process produces it, which cycle of matter it belongs to, and why its emission is a concern even though it is much smaller in quantity than that of $\text{CO}_2$ (compare their greenhouse warming potentials).
A science sceptic posts the following message: "The atmosphere contains about $850\text{ Gt}$ of carbon and the oceans more than $38\,000\text{ Gt}$. Our annual…
A science sceptic posts the following message: "The atmosphere contains about $850\text{ Gt}$ of carbon and the oceans more than $38\,000\text{ Gt}$. Our annual emissions from burning fossil fuels are barely around $10\text{ Gt}$. Since the planet's total carbon is constant and anthropogenic emissions are less than $0.03\,\%$ of the marine reservoir, it is absurd to claim that we can alter the global carbon cycle."
- a) Refute their argument by distinguishing between the dynamics of the biological (fast) cycle and the geological (slow) cycle: use the concepts of flux, residence time, and dynamic equilibrium to justify why $10\text{ Gt/year}$ destabilises the global climate.
- b) If natural sinks (biosphere and ocean surface) absorb on average $45\,\%$ of the anthropogenic carbon emitted each year, calculate how many ppm of $\text{CO}_2$ accumulate annually in the atmosphere, knowing that $1\text{ ppm} \approx 2.13\text{ Gt}$ of atmospheric carbon.
- c) Predict what will happen to the ocean's capacity to continue acting as a chemical sink for $\text{CO}_2$ as surface water temperature increases and its pH decreases, justifying through the chemical equilibrium of carbonic acid and carbonates.
To combat global warming, a geoengineering project has been proposed consisting of "fertilising" high-nutrient, low-chlorophyll (HNLC) oceanic zones by adding soluble…
To combat global warming, a geoengineering project has been proposed consisting of "fertilising" high-nutrient, low-chlorophyll (HNLC) oceanic zones by adding soluble iron salts to enhance the biological carbon pump.
- a) Justify what nutritional limitation iron relieves in these areas and describe the biogeochemical pathway that the fixed carbon must follow so that sequestration is effective on a geological timescale (centuries or millennia) rather than a mere rapid biological recycling.
- b) Analyse the benthic ecological risks: predict what will happen in the deep water column if a massive rain of organic marine snow descends to aphotic zones with a low rate of water turnover.
- c) Current global warming intensifies the thermal stratification of the surface ocean (creating a sharper thermocline). Predict and argue how this stratification will affect the natural functioning of the biological pump and what feedback it will cause on atmospheric $\text{CO}_2$.
An environmental impact assessment report compares two newly built hydroelectric dams: Dam A: Floods a rocky, mountainous valley in a temperate climate, where all tree…
An environmental impact assessment report compares two newly built hydroelectric dams:
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Dam A: Floods a rocky, mountainous valley in a temperate climate, where all tree biomass was previously felled and cleared. Average bottom water temperature: $9\ ^\circ\text{C}$.
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Dam B: Floods a tropical rainforest plain without clearing the vegetation or the thick soil humus layer. Average bottom water temperature: $26\ ^\circ\text{C}$.
During its first decade of operation, Dam B emits more greenhouse gases into the atmosphere per MWh produced than a natural gas thermal power plant.
- a) Justify biogeochemically why dissolved $\text{O}_2$ is depleted at the bottom of Dam B and which microbial consortia act so that the carbon stored in plant biomass is released as methane ($\text{CH}_4$) instead of carbon dioxide ($\text{CO}_2$).
- b) Knowing that the 20-year global warming potential of $\text{CH}_4$ is about 80 times greater than that of $\text{CO}_2$, critically discuss the common claim that "hydroelectric power is always a clean, carbon-neutral energy source."
- c) Design two pre-filling measures and one technical management measure at the turbine water intake (intake elevation) to prevent anoxic waters rich in dissolved gases from being discharged downstream and suddenly degassing.
The nitrogen cycle
Although the air you breathe contains $78\,\%$ nitrogen and plants are immersed in it, many crops turn yellow and stop growing if fertiliser is not added to the soil. Why does an element that is so abundant in the atmosphere turn out to be unavailable to plants, and how do they manage to take it in?
Describe the role of nitrogen-fixing bacteria and nitrifying bacteria, indicating which chemical transformation each group performs and why they are essential for plant…
Describe the role of nitrogen-fixing bacteria and nitrifying bacteria, indicating which chemical transformation each group performs and why they are essential for plant nutrition.
Name the main chemical forms nitrogen adopts throughout its cycle (atmospheric $\text{N}2$, ammonium, nitrite, nitrate and organic matter) and explain why most plants…
Name the main chemical forms nitrogen adopts throughout its cycle (atmospheric $\text{N}_2$, ammonium, nitrite, nitrate and organic matter) and explain why most plants cannot directly use the $\text{N}_2$ in the air.
Order the following stages of the nitrogen cycle as they occur in an ecosystem and briefly describe what each consists of: nitrification, fixation, denitrification, and…
Order the following stages of the nitrogen cycle as they occur in an ecosystem and briefly describe what each consists of: nitrification, fixation, denitrification, and ammonification.
The roots of legumes host nodules containing bacteria of the genus Rhizobium. Explain what the plant and the bacterium exchange in this symbiosis, which process of the…
The roots of legumes host nodules containing bacteria of the genus Rhizobium. Explain what the plant and the bacterium exchange in this symbiosis, which process of the nitrogen cycle the bacterium performs, and what agricultural advantage there is in including legumes in crop rotation.
An agricultural consortium discharges its runoff water loaded with nitrates ($80\text{ mg/L}$) and soluble phosphorus through a constructed wetland before reaching a…
An agricultural consortium discharges its runoff water loaded with nitrates ($80\text{ mg/L}$) and soluble phosphorus through a constructed wetland before reaching a protected coastal lagoon. At the outlet of the wetland, analyses indicate:
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Nitrate concentration reduced to $9\text{ mg/L}$.
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Continuous release of diatomic nitrogen ($\text{N}_2$) into the atmosphere with near-zero $\text{N}_2\text{O}$ emissions.
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Net carbon accumulation in the sediment at a rate of $400\text{ g C/m}^2\times\text{year}$.
- a) Analyze the biogeochemical microzonation of the wetland: justify how the oxidized rhizosphere of aquatic macrophytes and the underlying anoxic mud interact spatially to successfully complete sequential nitrification and denitrification.
- b) Explain the mechanism by which wetlands retain and accumulate carbon over millennia at rates higher than those of many mature forests, relating water saturation to the low activity of bacterial and fungal hydrolytic enzymes.
- c) Predict and discuss the biogeochemical consequences on the nitrogen and carbon cycles if this wetland were artificially drained to convert it into developable land.
The phosphorus cycle and other sedimentary cycles
Phosphorus is often the limiting nutrient in terrestrial ecosystems. Explain what it means for a nutrient to be 'limiting', why the phosphorus cycle is so slow, and what…
Phosphorus is often the limiting nutrient in terrestrial ecosystems. Explain what it means for a nutrient to be 'limiting', why the phosphorus cycle is so slow, and what consequence its lack of a gaseous phase has.
Unlike carbon and nitrogen, the phosphorus cycle is predominantly sedimentary. In an agricultural region, a paradox is observed: soil analyses show a high accumulation…
Unlike carbon and nitrogen, the phosphorus cycle is predominantly sedimentary. In an agricultural region, a paradox is observed: soil analyses show a high accumulation of total phosphorus after decades of phosphate fertilization, but crops show symptoms of chlorosis and phosphorus deficiency unless mineral fertilizers continue to be added, while adjacent surface waters suffer from eutrophication.
- a) Justify why the lack of a significant gaseous phase constrains the natural recycling rate of phosphorus back to the continents, and explain which biological and geological processes allow its return to dry land on a macroscopic scale.
- b) Explain the process of phosphorus fixation or insolubilization in soil: explain how pH (highly acidic or strongly calcareous soils) influences the formation of insoluble salts with iron, aluminium, or calcium, making phosphorus unavailable for root uptake.
- c) Given the anticipated depletion of apatite mines ("peak phosphorus"), design two circular economy measures for an agricultural-livestock farm aimed at mobilizing the phosphorus already retained in its soils and recovering it from wastewater effluents without relying on synthetic fertilizers.
Eutrophication: when the cycles become unbalanced
After the neighbouring fields beside a Midlands lake have been heavily fertilised, a pond of clear water becomes covered within a few days by a dense, opaque green layer, and soon afterwards dead fish appear floating at the edge. How can a massive input of nutrients, which stimulates the primary producers, end up wiping out the aquatic fauna?
An environmental monitoring team studies a coastal lagoon after an agricultural runoff discharge and records the following data: Day 5: Surface reactive phosphorus…
An environmental monitoring team studies a coastal lagoon after an agricultural runoff discharge and records the following data:
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Day 5: Surface reactive phosphorus concentration of $0.8\text{ mg/L}$ and chlorophyll $a$ of $65\ \mu\text{g/L}$; dissolved $\text{O}_2$ saturation of $145\,\%$ at noon in the top $40\text{ cm}$ of depth.
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Day 20: Surface $\text{O}_2$ saturation of $35\,\%$ at dawn; extreme turbidity ($40\text{ NTU}$); dissolved $\text{O}_2$ at the bottom ($3\text{ m}$) at $0.3\text{ mg/L}$, with the release of hydrogen sulfide ($\text{H}_2\text{S}$) and benthic fauna die-off.
A municipal technician states: "It is impossible for fish to die of asphyxiation if algae produce plenty of oxygen through photosynthesis; the cause must be direct chemical toxicity from nitrate."
- a) Refute the technician's claim using biogeochemical arguments: justify why a massive autotrophic bloom inevitably leads to hypolimnetic and nocturnal anoxia.
- b) Explain which trophic group proliferates from day 15 onwards and which anaerobic metabolic pathways account for the presence of $\text{H}_2\text{S}$ at the bottom.
- c) Predict what immediate ecological consequences treating the lagoon with a chemical algaecide to eradicate phytoplankton would have on the matter cycle.
A maize farm requires an input of $180\text{ kg N/ha}$. The agronomist is hesitating between two management options: Option 1: Apply synthetic mineral fertiliser…
A maize farm requires an input of $180\text{ kg N/ha}$. The agronomist is hesitating between two management options:
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Option 1: Apply synthetic mineral fertiliser (urea/ammonium nitrate) produced industrially via the Haber-Bosch process.
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Option 2: Sow a cover crop of common vetch (Vicia sativa, a legume) in autumn-winter, chop it as green manure in spring, and supplement with composted pig slurry.
- a) Compare both options in terms of energy consumption and carbon footprint: justify how the $\text{N}\equiv\text{N}$ bond is chemically broken in industry compared to how symbiotic nitrogenase does it in root nodules.
- b) Following a spring storm, nitrate concentrations of $95\text{ mg/L}$ (the safe threshold is $50\text{ mg/L}$) and emission peaks of nitrous oxide ($\text{N}_2\text{O}$) into the atmosphere are recorded in wells near plots treated exclusively with Option 1. Explain which microbial transformations of the nitrogen cycle give rise to both problems from the surplus fertiliser.
- c) Design a combined strategy that takes advantage of the immediate availability of mineral fertiliser and the sustainability of biological fertiliser, minimising leaching and gaseous losses.
The sulphur cycle
Sulphur is part of amino acids such as cysteine and methionine. Plants take up sulphate from the soil and the sulphur passes to consumers through feeding; decomposition returns it to the environment. Microorganisms transform reduced and oxidised compounds: in anoxic environments sulphide can be produced, and oxidising bacteria convert it into sulphate. Burning coal releases $\text{SO}_2$, which forms acid rain (pH below 5.6). Where bedrock is limestone (calcium carbonate), it neutralises the acid: carbonate reacts with the H⁺ ions, so the water pH stays near neutral (a buffering effect). Natural rain is already slightly acidic (about pH 5.6) because dissolved CO₂ forms carbonic acid. Where it is granite, the water stays acidic and dissolves toxic aluminium ions ($\text{Al}^{3+}$) from the soil, which harm fish and amphibians. Acid rain is a concern for Irish lakes and rivers on granite, such as those in the Wicklow Mountains.
Two high-mountain lakes, located at equal distances from an industrial park with coal-fired power plants, receive continuous precipitation with an average pH of $4.1$.…
Two high-mountain lakes, located at equal distances from an industrial park with coal-fired power plants, receive continuous precipitation with an average pH of $4.1$. Biological and chemical monitoring reveals very contrasting data:
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Lake A (situated on a granitic basin): Has lost its salmonid and amphibian populations; a dissolved $\text{Al}^{3+}$ concentration of $0.35\text{ mg/L}$ is detected in its waters.
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Lake B (situated on a limestone basin): Keeps its fish richness intact and shows no detectable dissolved aluminium.
- a) Justify on a lithological and chemical scale why the same flux of acid rain causes a biological collapse in lake A but proves harmless in lake B.
- b) Explain the biogeochemical mechanism by which acidification of the surrounding soil mobilises toxic ions such as $\text{Al}^{3+}$ and leaches essential nutrients ($\text{Ca}^{2+}$, $\text{Mg}^{2+}$), and predict the impact of this phenomenon on the forest in basin A.
- c) To restore lake A, an association proposes periodically adding large volumes of slaked lime or calcium carbonate directly to the water. Argue the limitations and potential harmful effects of this measure compared to reducing $\text{SO}_2$ emissions at the source.
Back to the beginning: The carbon atom you breathe out today could have belonged to a dinosaur because, after the reptile died and decomposed, that carbon passed into the atmosphere as $\text{CO}_2$ or was trapped in sedimentary rocks; millions of years later, a plant fixed it again by photosynthesis and it reached you through the food chain.