Does capillary length limit water rise in very thin capillaries?

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SUMMARY

The discussion centers on the mechanics of water transport in very thin capillaries, particularly in trees, where capillary action and transpiration play crucial roles. It is established that adhesive forces between water and the capillary walls are stronger than gravitational forces in small radius tubes, allowing water to rise. However, the capillary length does exist and is influenced by the meniscus, which is the only area where adhesive forces act. Transpiration from leaves creates a low-pressure zone that further aids in water ascent, overcoming gravitational pull.

PREREQUISITES
  • Understanding of capillary action and its principles
  • Knowledge of fluid dynamics, particularly in relation to adhesive and gravitational forces
  • Familiarity with the role of transpiration in plant physiology
  • Basic concepts of hydrostatic pressure in fluid systems
NEXT STEPS
  • Research the mechanics of capillary action in various materials, focusing on wood and plant structures
  • Study the role of transpiration in water transport within trees and its impact on hydrostatic pressure
  • Explore the effects of meniscus formation on fluid dynamics in capillaries
  • Investigate the relationship between capillary diameter and water ascent in different plant species
USEFUL FOR

Botanists, fluid dynamicists, environmental scientists, and anyone interested in the mechanics of water transport in plants.

Medicago
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Considering very thin capillaries, such as found in wood to transport water (~100Micron), I understand that the two main factors in play are gravity and the adhesive forces between the water and the surface of the capillary tube.

I understand that gravity is proportional to volume that is (radius)^2 whereas adhesive forces are proportional to inner surface area of tube that is (radius)^1.

So for some small radius adhesive forces are stronger than gravitational pull.

However it seems as if this is independent of length. It seems that since both gravitational pull and adhesive forces, being proportional to volume and surface area, are directly proportional to some ΔL, then the length of the tube is irrelevant and the water will climb up until the tube ends. However, we still define a certain capillary length for capillaries.

Does this capillary length exist for very thin capillaries? Or would water climb indefinitely in a very thin perfect tube?

And if it does exist why would it depend on length anyway?

Thanks.
 
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Well I've found the answer myself.

Apparently the opposing adhesive forces act only on the meniscus!

I thought it was a shear force that acts all along the surface of the tube.

But here's another question:

If I take a tube and split it to two tubes somewhere in the middle, creating two menisci, would that raise the water higher? Considering the diameter doesn't change.

I'm simply looking into the mechanics of water transport in trees and I'm really missing some essential fluid dynamics background so I'm trying to make up for it here..

Thanks.
 
In trees, a lot of the vertical transport is accomplished by more than pure capillary action. The evaporation (transpiration actually) of moisture out of the leaves also plays an effect. Transpiration causes low pressure at the top of the column which in effect sucks the water up the capillaries. The stomata on the leaves open and close to control transpiration, and therefore vertical flow.
 
negligible in terms of pressure gradient, chris.

One can assume that gravity is balanced entirely by adhesive forces, whereas transpiration contributes to the actual flow.
 
Yes, a greater length of contact for the same cross-sectional area will support a taller column of water. That's why the capillaries are narrow.
As Medicago says, capillary action draws water up until the tube is filled, but evaporation from the top makes the capillary action draw up more to keep it filled.
 
From Wikipedia:

"In taller plants and trees however, the force of gravity can only be overcome by the decrease in hydrostatic (water) pressure in the upper parts of the plants due to the diffusion of water out of stomata into the atmosphere"
 

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