Generator

The column a dissolved thing holds up

One function in the fluids library, called 60 times across 10 essays. Below: what it draws at its defaults, what it draws at every branch an essay asks for, whether the site's own gate puts a claim to it, and everywhere it is called.

At its defaults it draws the column a dissolved thing holds up. Two arms of one vessel, joined below by a membrane that passes water and not solute. On the right is 10 mol/m³ of dissolved particles at 25 °C; on the left, pure water. Water crosses into the solution until the extra weight of the right-hand column has raised its pressure by the osmotic pressure — 24.8 kPa, which is 2.53 m of water, drawn here to scale. Nothing is pulling. The solvent is at a lower chemical potential where it is mixed, so it moves that way, and it stops when mechanical pressure has made up the difference. A solute a thousand times more dilute than seawater lifts a column taller than a person.

osmotic-cell is one function in lib/figures/fluids.js — matter that will not hold a shape, and the forces in it. Everything below came out of it during this build, at parameters taken from the essays rather than invented for this page. A figure here is the figure a reader meets in an essay, and if the generator changes, this page changes with it.

At its defaults

Drawn even though every essay passes options, because a default nothing exercises is a trap for the next essay to call this with none — which has happened here twice.

The column a dissolved thing holds up. Two arms of one vessel, joined below by a membrane that passes water and not solute. On the right is 10 mol/m³ of dissolved particles at 25 °C; on the left, pure water. Water crosses into the solution until the extra weight of the right-hand column has raised its pressure by the osmotic pressure — 24.8 kPa, which is 2.53 m of water, drawn here to scale. Nothing is pulling. The solvent is at a lower chemical potential where it is mixed, so it moves that way, and it stops when mechanical pressure has made up the difference. A solute a thousand times more dilute than seawater lifts a column taller than a person.

Two arms of one vessel, joined below by a membrane that passes water and not solute. On the right is 10 mol/m³ of dissolved particles at 25 °C; on the left, pure water. Water crosses into the solution until the extra weight of the right-hand column has raised its pressure by the osmotic pressure — 24.8 kPa, which is 2.53 m of water, drawn here to scale. Nothing is pulling. The solvent is at a lower chemical potential where it is mixed, so it moves that way, and it stops when mechanical pressure has made up the difference. A solute a thousand times more dilute than seawater lifts a column taller than a person.

A cell swells until its membrane runs out

The options are the ones The cell that bursts by geometry passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

A cell swells until its membrane runs out. The volume of a red cell of 90 fL against the salt concentration of the solution round it, in per cent sodium chloride by weight, with 0.9 per cent isotonic. By the Boyle–van 't Hoff law the water inside follows the outside's tonicity: the cell's volume is an inactive part, 40 per cent of the normal volume in haemoglobin and other solids, plus a part inversely proportional to the concentration. Its membrane's 135 μm² can enclose at most 147.5 fL, as a sphere (dashed). The swelling curve reaches that at 0.44 per cent salt: below it the cell has no more shape to give up and bursts. In a 1.5 per cent solution the same cell shrinks to 68 fL and crenates, with membrane to spare.

The volume of a red cell of 90 fL against the salt concentration of the solution round it, in per cent sodium chloride by weight, with 0.9 per cent isotonic. By the Boyle–van 't Hoff law the water inside follows the outside's tonicity: the cell's volume is an inactive part, 40 per cent of the normal volume in haemoglobin and other solids, plus a part inversely proportional to the concentration. Its membrane's 135 μm² can enclose at most 147.5 fL, as a sphere (dashed). The swelling curve reaches that at 0.44 per cent salt: below it the cell has no more shape to give up and bursts. In a 1.5 per cent solution the same cell shrinks to 68 fL and crenates, with membrane to spare.

One membrane, two volumes

The options are the ones The cell that bursts by geometry passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

One membrane, two volumes. A red blood cell in section, drawn from the profile Evans and Fung measured in 1972: a disc 7.8 μm across, 2.6 μm thick at the rim and 0.8 μm at the centre, enclosing 94 femtolitres inside 134 square micrometres of membrane. Beside it, the sphere with the same area: 6.56 μm across, holding 146 femtolitres. The disc uses 64 per cent of the volume its membrane could enclose. Every shape between the two has the same area, and the membrane can pass between them almost freely; it cannot become larger than the sphere's surface by more than about two per cent without tearing. A cell that takes in water therefore has room for about fifty-five per cent more, and then none.

A red blood cell in section, drawn from the profile Evans and Fung measured in 1972: a disc 7.8 μm across, 2.6 μm thick at the rim and 0.8 μm at the centre, enclosing 94 femtolitres inside 134 square micrometres of membrane. Beside it, the sphere with the same area: 6.56 μm across, holding 146 femtolitres. The disc uses 64 per cent of the volume its membrane could enclose. Every shape between the two has the same area, and the membrane can pass between them almost freely; it cannot become larger than the sphere's surface by more than about two per cent without tearing. A cell that takes in water therefore has room for about fifty-five per cent more, and then none.

The pressure a full red cell can hold

The options are the ones The cell that bursts by geometry passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

The pressure a full red cell can hold. The excess pressure a red cell can hold once it has become a sphere, in kilopascals, against how far its membrane has been stretched beyond its resting area, from Laplace's law, Δp = 2τ/R, with a tension τ = K·strain and an area-expansion modulus K of 450 mN/m. The membrane tears at a tension of about 10 mN/m, a stretch of 2.2 per cent, where the pressure is 6.0 kPa. The osmotic pressure of the cell's contents is about 719 kPa: the membrane can hold back an imbalance of under 0.8 per cent of it. Before the cell is spherical the membrane is slack and holds no pressure at all; after, a further dilution of one per cent bursts it.

The excess pressure a red cell can hold once it has become a sphere, in kilopascals, against how far its membrane has been stretched beyond its resting area, from Laplace's law, Δp = 2τ/R, with a tension τ = K·strain and an area-expansion modulus K of 450 mN/m. The membrane tears at a tension of about 10 mN/m, a stretch of 2.2 per cent, where the pressure is 6.0 kPa. The osmotic pressure of the cell's contents is about 719 kPa: the membrane can hold back an imbalance of under 0.8 per cent of it. Before the cell is spherical the membrane is slack and holds no pressure at all; after, a further dilution of one per cent bursts it.

The osmotic fragility test, from geometry alone

The options are the ones The cell that bursts by geometry passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

The osmotic fragility test, from geometry alone. The fraction of red cells burst against the salt concentration, for three populations of 4,000 cells whose volumes and membrane areas scatter independently about their means, each cell bursting when its Boyle–van 't Hoff volume reaches the sphere its membrane allows plus two per cent. Half of the normal cells have burst at 0.42 per cent salt. Cells that have lost about an eighth of their membrane, as in hereditary spherocytosis, burst at 0.54 per cent; small, thin cells with membrane to spare, as in iron deficiency or thalassaemia, at 0.34. The clinical test that measures these curves is called a test of fragility, and what it measures is not the strength of the membrane, which is much the same in all three, but the ratio of membrane to contents.

The fraction of red cells burst against the salt concentration, for three populations of 4,000 cells whose volumes and membrane areas scatter independently about their means, each cell bursting when its Boyle–van 't Hoff volume reaches the sphere its membrane allows plus two per cent. Half of the normal cells have burst at 0.42 per cent salt. Cells that have lost about an eighth of their membrane, as in hereditary spherocytosis, burst at 0.54 per cent; small, thin cells with membrane to spare, as in iron deficiency or thalassaemia, at 0.34. The clinical test that measures these curves is called a test of fragility, and what it measures is not the strength of the membrane, which is much the same in all three, but the ratio of membrane to contents.

Where a cell bursts, set by area over volume

The options are the ones The cell that bursts by geometry passes. A branch drawn at its own defaults instead would be a picture no essay asked for and no assertion has been run against.

Where a cell bursts, set by area over volume. The salt concentration at which a red cell becomes a sphere and bursts, against its membrane area, for cells of 70, 90 and 110 fL, from the Boyle–van 't Hoff law with an inactive fraction of 0.4. A normal 90 fL cell with 135 μm² bursts at 0.44 per cent; with 120 μm² it bursts at 0.55, and below about 97 μm² it would be a sphere already and burst at isotonic salt. A 70 fL cell with the same 135 μm² survives to 0.32 per cent. Each curve rises steeply as the area approaches the smallest sphere that holds the cell, which is why a modest loss of membrane makes cells strikingly fragile.

The salt concentration at which a red cell becomes a sphere and bursts, against its membrane area, for cells of 70, 90 and 110 fL, from the Boyle–van 't Hoff law with an inactive fraction of 0.4. A normal 90 fL cell with 135 μm² bursts at 0.44 per cent; with 120 μm² it bursts at 0.55, and below about 97 μm² it would be a sphere already and burst at isotonic salt. A 70 fL cell with the same 135 μm² survives to 0.32 per cent. Each curve rises steeply as the area approaches the smallest sphere that holds the cell, which is why a modest loss of membrane makes cells strikingly fragile.

What checks it

physicscheck asserts something about osmotic-cell that could fail — it draws it and measures the result against a value reached some other way.

Across the library: 100 interrogated, 2 exercised only, 1 untouched, of 103. Read out of the gate's source by the gate's own two patterns — and the gate's last claim fails the build if that read disagrees with what it was handed while running.

Where it is called

Changing this generator changes every figure on this list. That is what makes the list worth publishing rather than keeping in a check script.

Fluids

The cell that bursts by geometry

Put a red blood cell in salt water weaker than blood and water flows in. The cell does not stretch to take it, because its membrane will not stretch: it can change shape almost for nothing and change its area by about two per cent before it tears. So the cell swells by changing shape, from a dimpled disc towards a sphere, and when it reaches the sphere its membrane can enclose, it has no more shape to spend. That happens at about 0.44 per cent salt, half the strength of blood, and the clinical test that measures it — called a test of fragility — turns out to measure a ratio of area to volume, not the strength of anything.

Fluids

The counterions that never leave the chain

Dilute a solution of DNA a million times and its counterions ought to scatter through the whole volume. Three quarters of them do not. A line of charges closer together than the Bjerrum length — 0.71 nm in water — holds on to its counterions however much room they are given, until the chain's charge is cut back to one per Bjerrum length, and every osmotic pressure, swelling gel and packed virus built from such chains is set by that length rather than by the chemistry.

Fluids

The like charges that pull together

Two surfaces carrying the same charge, with nothing between them but the ions that neutralise them, ought to repel, and the standard mean-field theory proves that they always do. With calcium or spermine as the counterions they attract, and come to rest a fraction of a nanometre apart. The mean field misses it because it averages the ions into a smooth cloud, and multivalent ions are too strongly repelled by each other to form one. Each keeps a patch of surface to itself, and the pressure between the plates becomes a single ion's business.

Fluids

The membrane that almost holds

Van 't Hoff's law gives the osmotic pressure a perfectly selective membrane would develop, and no membrane is. What a real one develops is a fraction of it — a number between zero and one that belongs to the membrane and the solute together, and that decides whether a solution is isotonic in effect or only on paper.

Fluids

The pressure that comes from counting

Dissolve a teaspoon of anything in a litre of water, put a membrane between it and pure water, and the solution will hold up a column of water two and a half metres tall. Nothing is pulling. The pressure does not depend on what was dissolved, only on how many particles it made — which is the ideal gas law, with the solute in place of the gas.

Fluids

The pressure that stops counting molecules

Van 't Hoff's law counts dissolved particles, and for a dilute polymer each chain is one particle, however many thousand segments it has. That is how osmometers weigh polymers. Concentrate the solution until the coils overlap and the count changes. The pressure stops depending on how long the chains are and grows as the 2.3 power of the concentration, the same for chains a thousand segments long and a hundred thousand. The unit being counted is no longer a molecule. It is a stretch of chain as long as the mesh of its neighbours allows, and it has no chemical identity at all.

Fluids

The stem that stands by pressure

A lettuce leaf has no bones, and a young sunflower stem has hardly any wood, yet both hold their shape against gravity and wind. They do it with pressure. Each cell holds more dissolved solute than the water around it, water flows in until the cell wall pushes back, and the wall ends up stretched taut by a pressure of seven or eight atmospheres — three times a car tyre's. A tube of membrane under tension resists bending in exact proportion to its pressure, whatever the membrane is made of, so a soft plant is stiff exactly as long as its cells are full. Lose a few per cent of their water and the pressure is gone, and the plant wilts.

Fluids

The swelling a membrane cannot stop

Give the thing a membrane holds back an electric charge and the small ions that can cross are no longer free to distribute themselves. Two conditions — neutrality on each side, and equal chemical potential for the salt — fix where every ion goes, and they leave the charged side with more particles than the other. That excess is what holds a joint apart, and it is why a cell has to spend a third of its energy pumping.

Fluids

The waterfall at every river mouth

Where a river meets the sea, fresh water mixes into salt and the free energy of mixing is released as nothing more useful than a little warmth and stirring. It is not a little energy: a cubic metre of river water entering the sea gives up as much as if it fell 290 metres. A desalination membrane run backwards can catch some of it, and the arithmetic of doing so is the arithmetic of every source with an internal resistance — the most power comes at half the pressure, and half the work is the price of getting it quickly.

Fluids

What it costs to take the salt out

Salt dissolves in water because mixing is overwhelmingly the more probable arrangement, and separating the two again means paying back what the mixing gave away. The bill can be computed before any apparatus is chosen — 0.79 kilowatt-hours for the first cubic metre from seawater — and it rises with every further cubic metre taken, because what is left behind is saltier than what was started with.

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