The Movement of water and Solutes in Plants

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The Movement of water and Solutes in Plants

Plants, like most living things, need to exchange gasses and transport minerals and substances to different parts of their structures.

Unlike Animals, plants don’t have a circulatory system. Diffusion is adequate for plants to exchange gasses, as they have a high surface area to volume ratio. Exchanging gasses is not a problem. The problem is moving water up stems that can be 100’s of meters tall without the aid of a pump (such as the heart). The answer is all to do with hydrostatic cohesion.

Before we look at how plants transport water and solutes, we must firstly know about the principles of water potential.

Water potential

Water potential(ψ) indicates which way water will move in a system. Water will always move from a high ψ to a low ψ. ψ can be measured in Kilopascals (kPa). Pure water has a ψ of 0 kPa. As solute is added, ψ is reduced (it becomes a negative number.)

e.g.

This is useful because you can add pressure to the equation.

If a pressure of 400 kPa is added to B (due to squeezing), the equation is

-1000 + 400 = -600

-600 = -600

Now that the forces are equal, there will be no water movement.

We will measure ψ using Molar Concentration which has a concentration of 0 - 1. Pure water has a ψ of 0M.

We already know what happens in the cell, so we also know what needs to be transported around the plant.

Water is taken from the roots to the rest of the plant.

Mineral ions are also absorbed through the root and taken to the rest of the plant, and the plant produces its very own organic solutes which it also needs to transport around.

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One of the first problems faced, is moving the water up very tall plants, without a pump. (after all, it takes a big fire engine which makes a lot of noise and uses a lot of energy to move water up to the top of a hose pipe a few hundred feet up, but forest trees constantly do that, silently).

The root itself has a thing called root pressure. This root pressure can push water up to the height of a meter or two. But how does the water get up the rest of the way?

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