Conserve water and particles across a cellular boundary
Intracellular fluid lies inside cell membranes; extracellular fluid includes interstitial fluid and plasma. Plasma is not the same as whole blood: blood cells contain intracellular fluid. Capillary walls separate plasma from interstitial spaces, while cell membranes separate intracellular from extracellular compartments. A substance can cross one boundary readily but not another, so a diagram must name both the compartment and the barrier.
Learning outcome: Compare initial shifts −0.5,0,+0.5 L at the same outside addition 300 mosmol. Retain initial concentrations, direction and final volumes. Identify which omitted pressure or permeability assumption would invalidate the calculation.
Starting recap
Use subject-relative anatomical directions, actual licensed tissue images, compartment conservation and explicit feedback/system boundaries; distinguish structural evidence from functional and clinical claims.
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With no initial shift and 300 mosmol added outside, total particles are 1800 and equilibrium concentration 360 mosmol/L. Outside volume becomes 900/360=2.5 L and inside volume 2.5 L: 0.5 L moves outward, while the two particle amounts remain 900 each.
Open the experimentPredict
Does changing initial water placement change the final equilibrium if total water and nonpenetrating particle amounts stay fixed?
Experiment
Compare initial shifts −0.5,0,+0.5 L at the same outside addition 300 mosmol. Retain initial concentrations, direction and final volumes. Identify which omitted pressure or permeability assumption would invalidate the calculation.
Conserve solute and water across a compartment boundary
Worked teaching model · synthetic values · Fictional closed 5 L two-compartment system, initially outside 2 L with 600 mosmol and inside 3 L with 900 mosmol. Only water crosses; added solute volume negligible; ideal particle amounts, no hydrostatic pressure difference or active regulation. Not a person, infusion plan or clinical reference.
Reset keeps your prediction, captures and practice history.
Water redistributes; impermeant particle amounts remain in their own compartments.
Outside solute addition raises the equilibrium outside volume, but the initial water shift determines the subsequent direction. Total volume and each particle amount are conserved after the specified addition; real body compartments include pressure and active solute transport.
| Quantity | Value | Unit |
|---|---|---|
| Initial outside concentration | 450 | mosmol/L |
| Initial inside concentration | 300 | mosmol/L |
| Equilibrium outside volume | 2.500000 | L |
| Equilibrium inside volume | 2.500000 | L |
| Water change outside | 0.5000000 | L |
| Common equilibrium concentration | 360 | mosmol/L |
Original bounded models, not measurements of the accompanying actual micrographs or any person. Retain settings, predictions and limitations in the notebook.
Water redistributes; impermeant particle amounts remain in their own compartments.
Outside solute addition raises the equilibrium outside volume, but the initial water shift determines the subsequent direction. Total volume and each particle amount are conserved after the specified addition; real body compartments include pressure and active solute transport.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
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With no particle addition, 0.5 L was initially moved outside. Find initial concentrations, final volumes and subsequent direction.
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