The column a dissolved thing holds up
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.
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.
Most of a chain's counterions never leave it
The options are the ones The counterions that never leave the chain 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 fraction of a charged rod's counterions lying within a distance r of it, against r in rod radii on a logarithmic axis, for a charge parameter ξ = 4.2 — the Bjerrum length of water, 0.7135 nm, over a charge spacing of 0.17 nm, which is DNA's. Each curve is the Poisson–Boltzmann solution for the rod at the centre of a cell of radius 10², 10⁴, 10⁶ rod radii, with its counterions checked to neutralise it exactly. Diluting the solution widens the cell by four decades at a time, and a counterion free to go anywhere in the cell ought to spread with it; instead each curve keeps a plateau near the rod whose height does not change. At the inflection of every curve the enclosed fraction is 0.762, which is Manning's 1 − 1/ξ, and the plateau sits there: 76 per cent of the counterions stay bound to the chain however dilute the solution, and only 24 per cent spread through it.
Whether one counterion stays is whether an integral converges
The options are the ones The counterions that never leave the chain 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 probability that a single counterion, alone beside a charged rod, is found within a distance r0 of it rather than anywhere in a cell a million times wider, against how much thinner than r0 the rod is, on a logarithmic axis. The counterion's Boltzmann weight near a line charge goes as the distance to the power −2ξ, and the probability is a ratio of two integrals of that weight, each evaluated numerically and held against its closed form. For ξ = 0.5 it reaches 0.000; for ξ = 0.9 it reaches 0.063; for ξ = 1 it reaches 0.667; for ξ = 1.1 it reaches 0.996; for ξ = 2 it reaches 1.000 when the rod is a trillionth of r0. Below ξ = 1 the integral converges as the rod thins and the counterion wanders off into the cell, because the entropy it gains by going far away grows faster than the energy it pays. At ξ = 1 the two grow at the same logarithmic rate, and above it the integral diverges at the rod and the counterion is captured. Condensation is that divergence, and the other counterions, by screening the chain, are what stop it at ξ = 1.
The pressure the counterions are allowed to exert
The options are the ones The counterions that never leave the chain 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 coefficient of a solution of charged rods with no added salt — the osmotic pressure divided by what the counterions would exert as an ideal gas — against the charge parameter ξ, from the Poisson–Boltzmann cell model, where the pressure is the counterion density at the cell's edge times kT. Cells of 10², 10⁴, 10⁸ rod radii are successively more dilute. The solid line is Manning's limiting law: 1 − ξ/2 below the threshold and 1/2ξ above it. At ξ = 4.2 the computed coefficient is 0.154, 0.130, 0.122 for the three cells, falling towards Manning's 0.119. A solution of DNA with a mole of counterions therefore exerts roughly a tenth of the osmotic pressure a mole of free salt ions would, and the reason is not that the counterions are attached to anything but that the chain's field holds them within a few nanometres.
A superabsorbent holds a third of the pressure its charges promise
The options are the ones The counterions that never leave the chain 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 swelling pressure of a charged gel carrying 0.5 M of fixed charge on chains with ξ = 2.85 — sodium polyacrylate, a charge every 0.25 nm — against the salt in its bath, on logarithmic axes. The dashed curve counts every fixed charge in the Donnan balance; the solid curve counts only the charge left after condensation, the fixed charge divided by ξ. In a low-salt bath the pressure is the fixed charge counted as a gas, and condensation cuts it by ξ, from 1235 to 430 kPa at 1 mM. In a bath at physiological salt, 150 mM, the two give 702 and 118 kPa, a factor of 6.0, because the screening regime goes as the square of the charge. A nappy's absorbency in distilled water and in urine differs by both effects at once, and the charge the polymer was synthesised with is not the charge the water sees.
A trivalent counterion neutralises what a monovalent one cannot
The options are the ones The counterions that never leave the chain 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 fraction of a chain's charge neutralised by condensed counterions against the charge parameter ξ, for counterions carrying one, two and three charges. A counterion of charge z feels z times the chain's field, so it condenses until the effective charge parameter is 1/z and neutralises 1 − 1/zξ of the chain. For DNA, ξ = 4.2, the Poisson–Boltzmann cell at the inflection of each profile gives 76.2 per cent for monovalent ions, 88.1 per cent for divalent ions, 92.1 per cent for trivalent ions, matching Manning's form. The dashed line is 89 per cent, near which DNA in solution is observed to collapse from an extended chain into tightly packed toroids: sodium cannot take it there, magnesium falls just short, and the trivalent polyamine spermidine does, which is how DNA is packed into sperm heads and viral capsids.
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.
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.
FluidsThe 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.
FluidsThe 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.
FluidsThe 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.
FluidsThe 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.
FluidsWhat 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.