Stemflow

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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.[ citation needed ]

Contents

Measurement

Stem flow measurement on a silver birch Stammabflussmesser18.jpg
Stem flow measurement on a silver birch

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. [1]

Determining factors

Precipitation

The primary meteorological characteristics of a rainfall event that influence stemflow are: [2]

Species

Stemflow in oaks is relatively low, due to their textured bark, few and horizontal branches, and high incidence of absorbent epiphytes. Quercus agrifolia-4.jpg
Stemflow in oaks is relatively low, due to their textured bark, few and horizontal branches, and high incidence of absorbent epiphytes.

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

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: [3]

Other

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). [4]

Soil acidification can be seen around some stems, for example beech trees from dry deposition. [5]

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

Related Research Articles

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<i>Eucalyptus regnans</i> Species of eucalyptus

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<span class="mw-page-title-main">Arboriculture</span> Management and study of trees and other woody plants

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<span class="mw-page-title-main">Interception (water)</span> Precipitation that is intercepted by vegetation before reaching the soil

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<span class="mw-page-title-main">Canopy (biology)</span> Aboveground portion of a plant community or crop

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<span class="mw-page-title-main">Canopy interception</span> Rainfall that is intercepted by the canopy of a tree

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<span class="mw-page-title-main">Throughfall</span> Process where wet leaves drop water onto the ground

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<span class="mw-page-title-main">Woody plant</span> Plant that produces wood and has a hard stem

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<span class="mw-page-title-main">Tree</span> Perennial woody plant with elongated trunk

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<span class="mw-page-title-main">Forest floor interception</span>

Forest floor interception is the part of the (net) precipitation or throughfall that is temporarily stored in the top layer of the forest floor and successively evaporated within a few hours or days during and after the rainfall event. The forest floor can consist of bare soil, short vegetation or litter. This throughfall is especially rich in nutrients which makes its redistribution into the soil is an important factor for the ecology and water demand of surrounding vegetation. As a hydrological process it is crucial for water resource management and climate change.

Monodominance is an ecological condition in which more than 60% of the tree canopy comprises a single species of tree. Monodominant forests are quite common under conditions of extra-tropical climate types. Although monodominance is studied across different regions, most research focuses on the many prominent species in tropical forests. Connel and Lowman, originally called it single-dominance. Conventional explanations of biodiversity in tropical forests in the decades prior to Connel and Lowman's work either ignored monodominance entirely or predicted that it would not exist.

A canopy root, also known as an arboreal root, is a type of root that grows out of a tree branch underneath an epiphytic mat. These adventitious roots form in response to moist, dark, nutrient-rich conditions that are found in “canopy soils”. Canopy roots have been found in species of maple, poplar, alder, myrtle, beech, and spruce, among many others. They are structurally similar to roots found on the forest floor and likely serve a similar purpose for water and nutrient uptake, though their specific functions are still being studied.

References

  1. Williams, Matthew B. (2004), Investigating the contribution of stemflow to the hydrology of a forest catchment (PDF), vol. Dissertation, University of Southampton
  2. Crockford, R.H.; Richardson, D.P (1990), "Partitioning of rainfall in a Eucalypt forest and pine plantation in southeastern Australia: II Stemflow and factors affecting stemflow in a dry sclerophyll eucalypt forest and a Pinus radiata plantation", Hydrological Processes, 4 (2): 145–155, Bibcode:1990HyPr....4..145C, doi:10.1002/hyp.3360040205
  3. André, Frédéric; Jonard, Mathieu; Ponette, Quentin (2008). "Influence of species and rain event characteristics on stemflow volume in a temperate mixed oak-beech stand". Hydrological Processes. 22 (22): 4455–4466. Bibcode:2008HyPr...22.4455A. doi:10.1002/hyp.7048. ISSN   0885-6087. S2CID   128756723.
  4. 1 2 Johnson, Mark S.; Lehmann, Johannes (2006), "Double-funneling of trees: Stemflow and root-induced preferential flow", Écoscience, 13 (3): 324–333, doi:10.2980/i1195-6860-13-3-324.1, S2CID   10931068
  5. Deposition and soil leaching in stands of Norway spruce and European Beech: Results from the Höglwald research in comparison with other European case studies