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Stemflow

Stemflow 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 Stemflow rather than just read about it. In short: In hydrology, stemflow is the flow of intercepted water down the trunk or stem of a plant. Stemflow, along with throughfall, is responsible for the transferral of precipitation and nutrients from the canopy to the soil.

Stemflow — main illustration
Stemflow — illustration

Key takeaways

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

Reference excerpt

In hydrology, stemflow is the flow of intercepted water down the trunk or stem of a plant. Stemflow, along with throughfall, is responsible for the transferral of precipitation and nutrients from the canopy to the soil. In tropical rainforests, where this kind of flow can be substantial, erosion gullies can form at the base of the trunk. However, in more temperate climates stemflow levels are low and have little erosional power.

Measurement

There are a variety of ways stemflow volume is measured in the field. The most common direct measurement currently used is the bonding of bisected PVC or other plastic tubing around the circumference of the tree trunk, connected and funneled into a graduated cylinder for manual or a tipping bucket rain gauge for automatic collection. At times the tubing is wrapped multiple times around the trunk is order to ensure more complete collection.

Determining factors Precipitation The primary meteorological characteristics of a rainfall event that influence stemflow are:

Rainfall continuity – the more frequent and extended are the gaps during the event where no rainfall occurs, the higher the likelihood that potential stemflow volume is lost to evapotranspiration; this is also governed by air temperature, relative humidity and most significantly, wind speed Rainfall intensity – the amount of total stemflow is diminished when the amount of rain in a given period surpasses the capacity of the flow paths Rain angle – stemflow generally starts earlier when rainfall is more horizontal; this is more of a determinant in an open forest with a lesser degree of crown closure Species

The species of the tree affects the amount of timing and stemflow. The particular morphological characteristics that are key factors are:

Crown size – stemflow potential is greater as crown size relative to the diameter at breast height increases. However, the greater the DBH, the more incident rainfall is needed to start stemflow. Leaf shape/orientation – leaves which are concave and elevated horizontally above the petiole are able to contribute to stemflow Branch angle – stemflow potential heightens as the angle of the branches and twigs in relation to the trunk decreases. Flow path obstructions – abnormalities on the flow path, such as detached pieces of bark or scars, on the underside of the branch can divert water from stemflow and become a component in throughfall Bark – stemflow is affected by the degree of absorptive ability and smoothness of the bark alongside the branch and stem. This is measured by using the Bark Relief Index, or BRI, which is the difference between the circumference of the tree and what the circumference would be if the tree had no bark. Stand characteristics In addition to the effects of individual tree species, the overall structure of the forest stand also influences the amount of stemflow that will ultimately occur, these factors are:

Species composition – the total stemflow for the stand is determined by the contributions of individuals and their species-specific traits Stand density – morphological characteristics such as branch angle and thickness are largely determined by the amount of density of competing trees in the stand Canopy structure – individuals located in the understory in a stand with multiple vertically-stratified stories will have a lessened amount of total stemflow due to the interception of dominant and codominant individuals Other

Seasonality – in the case of deciduous or mixed forests, stemflow rates are slightly higher in the dormant season when no leaves are present and evapotranspiration is reduced; this effect becomes more pronounced as the stem diameter increases Diurnality – variations in branch weight influence the amount of stemflow; branches are heavier in the morning (with dew) and lighter in the afternoon

Influence on soil Chemistry Nutrients that have accumulated on the canopy from dry deposition or animal feces are able to directly enter the soil through stemflow. When precipitation occurs, canopy nutrients are leached into the water because of the differences in nutrient concentration between the tree and the rainfall. Conversely, nutrients are taken up by the tree when concentration is lower in the canopy than the rainfall, the presence of epiphytes or lichens also contributes to uptake. The nutrients that enter the soil can also reflect the particular environmental conditions around them, for example, plants located in industrialized areas exhibit higher rates of sulfur and nitrogen (from air pollution), whereas those located near the oceans have higher rates of sodium (from seawater). Soil acidification can be seen around some stems, for example beech trees from dry deposition. Precipitation and morphological factors that influence stemflow timing and volume also affect the chemical composition; in general, stemflow water becomes more dilute during the course of a storm event, and rough-barked species contain more nutrients than smooth-barked species. Water distribution In forested areas, stemflow is considered a point-source input of water into the soil, thus water is more able to effectively penetrate past the topsoil into deeper layers of the soil horizon along tree roots and their subsequent creation of macropores (termed preferential flow). The loosening of the soil can result in minor landslides.

See also

Throughfall Canopy interception Forest floor interception

References

Illustrations

Stemflow: Stem flow measurement on a silver birch
Stem flow measurement on a silver birch
Stemflow: Stemflow in oaks is relatively low, due to their textured bark, few and horizontal branches, and high incidence of absorbent epiphytes.
Stemflow in oaks is relatively low, due to their textured bark, few and horizontal branches, and high incidence of absorbent epiphytes.

Worked examples

Example 1 — a first encounter with Stemflow

Start with the simplest possible case. Write down what Stemflow 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 Stemflow 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 Stemflow 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 Stemflow

In research
Stemflow 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 Stemflow 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
Stemflow is common in secondary-school and first-year university syllabi. It links to neighbouring topics Forest ecology, Hydrology, so understanding it makes those chapters shorter.
In everyday life
Look for Stemflow 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 Stemflow in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Stemflow 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 Stemflow out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Stemflow in simple terms?

In hydrology, stemflow is the flow of intercepted water down the trunk or stem of a plant. Stemflow, along with throughfall, is responsible for the transferral of precipitation and nutrients from the canopy to the soil.

Why does Stemflow 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 Stemflow?

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 Stemflow.

Tags

  • Forest ecology
  • Hydrology

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