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BAC1 tech · Biology, Geology and Environmental Sciences
Ecology and sustainability · Ecosystem dynamics

Matter cycles

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.

Before you start, make sure you know: The components of the ecosystem (3rd ESO)
Before you start, make sure you know: The causes of climate change (3rd ESO)

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?

Landscape with atmosphere, forest, soil, ocean and rocks: blue arrows show the gaseous flow of carbon and nitrogen through the atmosphere and green arrows show the sedimentary flow of phosphorus through soil, water and sediments. living things atmosphere N₂ CO₂ gaseous · C, N soil flux ocean rocks and sediments sedimentary · P zones: reservoirs · arrows: fluxes
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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.

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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.

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The carbon cycle

Diagram of the carbon cycle: producers take CO₂ from the atmosphere by photosynthesis and return it by respiration; the carbon passes to consumers through feeding and, from both, to the soil and the decomposers. atmosphere (CO₂) producers consumers soil and decomposers photosynthesis respiration feeding
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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.

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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.

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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.

ATMOSPHERE (CO₂) PRODUCERS CONSUMERS SOIL AND DECOMPOSERS FOSSIL FUELS a b c ?
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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?

Diagram of the nitrogen cycle: N₂ from the air becomes ammonium by fixation, nitrate by nitrification and organic matter by uptake; organic matter returns ammonium by ammonification and nitrate returns to the air as N₂ by denitrification. N₂ (air) ammonium NH₄⁺ nitrate NO₃⁻ organic matter fixation nitrification uptake denitrification ammonification
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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.

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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.

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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.

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The phosphorus cycle and other sedimentary cycles

Diagram of the sedimentary phosphorus cycle showing the slow weathering of phosphate rocks and their transport to the soil and bodies of water without passing through the atmosphere. phosphate rock erosion very slow soil rivers/sea no passage through the atmosphere
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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.

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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.

  1. 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.
  2. 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.
  3. 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.
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Eutrophication: when the cycles become unbalanced

After the neighbouring fields 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?

Cross-section of a eutrophic lagoon: at the top, fertiliser from a field reaches the water and algae cover the surface and block the light; at the bottom, the algae die and sink, the decomposers use up the oxygen at the bottom and the fish die. 1 Excess N and P no light O₂ 2 Algal bloom days later O₂ O₂ decomposers 3 Algae die 4 Anoxia → mortality
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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.

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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:

  • 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.

  • 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."

  1. a) Refute the technician's claim using biogeochemical arguments: justify why a massive autotrophic bloom inevitably leads to hypolimnetic and nocturnal anoxia.
  2. 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.
  3. c) Predict what immediate ecological consequences treating the lagoon with a chemical algaecide to eradicate phytoplankton would have on the matter cycle.
Solve
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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:

  • Option 1: Apply synthetic mineral fertiliser (urea/ammonium nitrate) produced industrially via the Haber-Bosch process.

  • 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.

  1. 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.
  2. 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.
  3. 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.
Solve

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.

Sulphur cycle: sulphate in the soil passes to plants and animals and returns through decomposition; volcanoes and combustion emit sulphur gases that are deposited with the rain; rocks and sulphide-oxidising bacteria supply sulphate. sulphur gases deposition volcano combustion producer consumer decomposers sulphate rocks and sediments sulphide anoxic environment oxidising bacteria

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.

Summary

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