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Lake metabolism

Lake metabolism is a biology topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Lake metabolism rather than just read about it. In short: Lake metabolism represents a lake's balance between carbon fixation (gross primary production) and biological carbon oxidation (ecosystem respiration). Whole-lake metabolism includes the carbon fixation and oxidation from all organisms within the lake, from bacteria to fishes, and is typically estimated by measuring changes in dissolved oxygen or carbon dioxide throughout the day.

Lake metabolism — main illustration
Lake metabolism — illustration

Key takeaways

  • Lake metabolism belongs to biology; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Lake metabolism to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Lake metabolism from memory before moving on to harder problems.

Reference excerpt

Lake metabolism represents a lake's balance between carbon fixation (gross primary production) and biological carbon oxidation (ecosystem respiration). Whole-lake metabolism includes the carbon fixation and oxidation from all organisms within the lake, from bacteria to fishes, and is typically estimated by measuring changes in dissolved oxygen or carbon dioxide throughout the day. Ecosystem respiration in excess of gross primary production indicates the lake receives organic material from the surrounding catchment, such as through stream or groundwater inflows or litterfall. Lake metabolism often controls the carbon dioxide emissions from or influx to lakes, but it does not account for all carbon dioxide dynamics since inputs of inorganic carbon from the surrounding catchment also influence carbon dioxide within lakes.

Concept Estimates of lake metabolism typically rely on the measurement of dissolved oxygen or carbon dioxide, or measurements of a carbon or oxygen tracer to estimate production and consumption of organic carbon. Oxygen is produced and carbon dioxide consumed through photosynthesis and oxygen is consumed and carbon dioxide produced through respiration. Here, organic matter is symbolized by glucose, though the chemical species produced and respired through these reactions vary widely.

Photosynthesis: 6 C O 2 + 6 H 2 O →

l i g h t C 6 H 12 O 6 + 6 O 2 {\displaystyle 6CO_{2}+6H_{2}O{\xrightarrow[{}]{light}}C_{6}H_{12}O_{6}+6O_{2}}

Respiration: C 6 H 12 O 6 + 6 O 2 →

6 C O 2 + 6 H 2 O {\displaystyle C_{6}H_{12}O_{6}+6O_{2}{\xrightarrow[{}]{}}6CO_{2}+6H_{2}O}

Photosynthesis and oxygen production only occurs in the presence of light, while the consumption of oxygen via respiration occurs in both the presence and absence of light. Lake metabolism terms include:

GPP - gross primary production (e.g. total photosynthesis) R - total respiration ( R h + R a ) {\displaystyle (R_{h}+R_{a})}

R h {\displaystyle R_{h}} - heterotrophic respiration

R a {\displaystyle R_{a}} - autotrophic respiration NEP - net ecosystem production = GPP - R NPP - net primary production = GPP - R a {\displaystyle R_{a}}

Measurement techniques Estimating lake metabolism requires approximating processes that influence the production and consumption of organic carbon by organisms within the lake. Cyclical changes on a daily scale occur in most lakes on Earth because sunlight is available for photosynthesis and production of new carbon only for a portion of the day. Researchers can take advantage of this diel pattern to measure rates of change in carbon itself or changes in dissolved gases such as carbon dioxide or oxygen that occur on a daily scale. Although daily estimates of metabolism are most common, whole-lake metabolism can be integrated over longer time periods such as seasonal or annual rates by estimating a whole-lake carbon budget. The following sections highlight the most common ways to estimate lake metabolism across a variety of temporal and spatial scales and go over some of the assumptions of each of these methods.

… excerpt ends here. Continue reading the full article.

Illustrations

Lake metabolism: Lake Mendota in Madison, Wisconsin. One of the most well-studied lakes in the world including estimates of lake metabolism.
Lake Mendota in Madison, Wisconsin. One of the most well-studied lakes in the world including estimates of lake metabolism.
Lake metabolism: Example of O2 and CO2 cycle within a lake upper mixed layer (epilimnion). During the day, gross primary production outpaces lake respiration resulting in a net production of O2 and consumption of CO2. Later in the day when solar radiation is reduced and during the night when there is no light, respiration still occurs in the absence of gross primary production resulting in net consumption of O2 and production of CO2. Data for this figure are from Harp Lake on August 1, 2014.[5]
Example of O2 and CO2 cycle within a lake upper mixed layer (epilimnion). During the day, gross primary production outpaces lake respiration resulting in a net production of O2 and consumption of CO2. Later in the day when solar radiation is reduced and during the night when there is no light, respiration still occurs in the absence of gross primary production resulting in net consumption of O2 and production of CO2. Data for this figure are from Harp Lake on August 1, 2014.[5]
Lake metabolism: Lake cross-sectional diagram of the factors influencing lake metabolic rates and concentration of dissolved gases within lakes. Processes in gold text consume oxygen and produce carbon dioxide while processes in green text produce oxygen and consume carbon dioxide. Physical processes can both increase or decrease dissolved gas concentration, for example atmospheric gas exchange can increase or decrease lake dissolved oxygen depending on whether the lake is undersaturated or oversaturated in dissolved oxygen compared to the atmosphere, respectively. The panel on the right shows how light, temperature, and nutrients tend to change with depth for a stratified lake, which in turn results in variation in metabolic rates vertically within a lake.
Lake cross-sectional diagram of the factors influencing lake metabolic rates and concentration of dissolved gases within lakes. Processes in gold text consume oxygen and produce carbon dioxide while processes in green text produce oxygen and consume carbon dioxide. Physical processes can both increase or decrease dissolved gas concentration, for example atmospheric gas exchange can increase or decrease lake dissolved oxygen depending on whether the lake is undersaturated or oversaturated in dissolved oxygen compared to the atmosphere, respectively. The panel on the right shows how light, temperature, and nutrients tend to change with depth for a stratified lake, which in turn results in variation in metabolic rates vertically within a lake.
Lake metabolism: Temperature sensitivity of gross primary production (GPP) and respiration (R) based on average activation energies reported in Yvon-Durocher et al. (2012).[5] As water temperature increases, R increases more rapidly than GPP due to the higher average activation energy for R. In this figure, GPP and R temperature responses are reported as relative to GPP and R rates at 15 °C (59 °F). A doubling of metabolic rates compared to metabolic rate at 15°C (horizontal dashed line) occurs with just a 7.6°C increase for R but requires a 14.8°C increase to double GPP.
Temperature sensitivity of gross primary production (GPP) and respiration (R) based on average activation energies reported in Yvon-Durocher et al. (2012).[5] As water temperature increases, R increases more rapidly than GPP due to the higher average activation energy for R. In this figure, GPP and R temperature responses are reported as relative to GPP and R rates at 15 °C (59 °F). A doubling of metabolic rates compared to metabolic rate at 15°C (horizontal dashed line) occurs with just a 7.6°C increase for R but requires a 14.8°C increase to double GPP.
Lake metabolism: Conceptualized indirect effects of dissolved organic carbon (DOC) on gross primary productivity through interacting effects of DOC impacts on light and nutrient availability in lakes. Figure is redrawn from Kelly et al. 2018[34]
Conceptualized indirect effects of dissolved organic carbon (DOC) on gross primary productivity through interacting effects of DOC impacts on light and nutrient availability in lakes. Figure is redrawn from Kelly et al. 2018[34]

Worked examples

Example 1 — a first encounter with Lake metabolism

Start with the simplest possible case. Write down what Lake metabolism claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In biology, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Lake metabolism before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Lake metabolism ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Lake metabolism

In research
Lake metabolism appears in biology research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Lake metabolism in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Lake metabolism is common in secondary-school and first-year university syllabi. It links to neighbouring topics Aquatic ecology, Lakes, Limnology, so understanding it makes those chapters shorter.
In everyday life
Look for Lake metabolism outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Lake metabolism in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Lake metabolism means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Lake metabolism out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Lake metabolism in simple terms?

Lake metabolism represents a lake's balance between carbon fixation (gross primary production) and biological carbon oxidation (ecosystem respiration). Whole-lake metabolism includes the carbon fixation and oxidation from all organisms within the lake, from bacteria to fishes, and is typically esti…

Why does Lake metabolism matter?

Because it connects several biology ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Lake metabolism?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Lake metabolism.

Tags

  • Aquatic ecology
  • Lakes
  • Limnology
  • Limnology and Oceanography articles
  • Metabolism

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