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#water movement

6 public questions tagged with this topic.

What happens to water movement in an isotonic solution?

Isotonic relationship exists when two compartments separated by semipermeable membrane possess identical effective osmolarity of impermeable solutes, typically around 300 milliosmoles per kilogram for mammalian cells corresponding to 0.9 percent sodium chloride or 5 percent dextrose clinically used for infusion. Osmotic pressure pi equals iCRT is identical on both sides, so water chemical potentials equal and thermodynamic driving force zero. Nevertheless molecular agitation does not cease; water molecules continuously cross lipid bilayer by solubility diffusion and through aquaporin-1 channels via single-file hydrogen bonded chain in both directions at rates exceeding ten to the ninth per second per pore due to thermal motion. Because probabilities of forward and reverse jumps are balanced by equal activity, influx equals efflux, net flux zero, and compartment volumes remain constant over time with no change in cell diameter. This dynamic equilibrium prevents shrinkage or swelling and preserves discoid shape and deformability for microcirculation. Hypertonic condition would cause net efflux and crenation, hypotonic influx and hemolysis. Physiological saline therefore formulated to be isotonic avoids damage during transfusion.

Ref: Alberts et al., Molecular Biology of the Cell, Chapter 11: Isotonic Solutions and Dynamic Equilibrium of Water Flux.

In a U-tube experiment, if Side A has 4M NaCl and Side B has 10M NaCl, what will be the movement of water?

Demonstration using U-tube separated by membrane permeable only to water nicely illustrates colligative water movement. Osmotic pressure approximated by van't Hoff law pi equals i times C times R times T proportional to total particle concentration. Solution A holding 4 molar NaCl dissociates into sodium and chloride giving factor near two, so effective osmolarity roughly 8 osmoles, solution B 10 molar near 20 osmoles, markedly higher. Chemical potential of water mu equals mu naught plus RT ln a water minus V bar P, and a water declines with solute. Therefore water potential higher in dilute arm and lower in concentrated arm. Spontaneous flux proceeds from high potential to low potential, meaning from dilute 4 molar side toward concentrated 10 molar side, attempting to equalize activities. Volume rises on high solute side, falls on low solute side until hydrostatic pressure difference compensates. Sodium chloride itself does not cross because membrane excludes ions. Analogous processes regulate cell volume. Hence in this scenario water moves from Side A containing 4M NaCl to Side B containing 10M NaCl following osmotic gradient toward higher solute concentration.

Ref: Nelson & Cox, Lehninger Principles of Biochemistry, Chapter 11: Osmosis and Water Movement Between Compartments.

What is the effect of hypertonic conditions on cells?

Tonicity governs cell volume by defining relative effective osmolarity of extracellular fluid compared with cytoplasm, usually near 300 milliosmoles. Hypertonic environment contains higher concentration of non-penetrating solutes like sodium chloride, mannitol or sucrose, leading to lower water potential described by psi equals psi solute plus psi pressure. Since water diffuses toward lower water potential via aquaporins and lipid bilayer, net efflux occurs from cell to surroundings. Loss of water concentrates intracellular proteins and solutes, decreases cell volume, increases ionic strength and may perturb enzyme activity and signaling cascades. Animal cells without rigid wall shrink, developing crenated or spiky morphology as cortical cytoskeleton collapses. In plants large central vacuole loses water, turgor pressure drops, plasma membrane retracts from cell wall during plasmolysis, causing wilting and growth arrest. Regulatory volume increase mechanisms involving NKCC, NHE and Cl transport may later import osmolytes to recover, but immediate physical response to hypertonic challenge is passive water loss leading to shrinkage and crenation.

Ref: Alberts et al., Molecular Biology of the Cell, Chapter 11: Hypertonic Effects on Cell Volume and Regulatory Mechanisms.

In reverse osmosis, water moves:

Natural osmosis describes spontaneous water flow from region of high water chemical potential, meaning low solute concentration, to low water potential, high solute, across semipermeable membrane until equilibrium. Reverse osmosis inverts this natural tendency by imposing mechanical energy. In purification devices impure feed solution with high total dissolved salts and industrial effluent contacts one side of thin film composite polyamide membrane with pores smaller than 0.1 nanometer that reject ions by charge repulsion and size exclusion. A high pressure pump applies hydrostatic pressure typically 15 to 70 bar exceeding inherent osmotic pressure defined by pi equals iCRT. When external pressure surpasses osmotic pressure, chemical potential gradient reverses and water forced opposite to spontaneous direction. Water leaves concentrated feed moving toward dilute permeate compartment producing fresh water while salts concentrated as brine rejected. This process relies on applied hydrostatic pressure overcoming colligative driving force. Therefore under reverse conditions water moves from high solute side to low solute side driven by external work input.

Ref: Voet & Voet Biochemistry, Chapter on Membrane Transport, Section: Reverse Osmosis Hydrostatic Pressure Overcoming Pi.

In a U-tube experiment, water moves from:

A classical U-tube experiment visualizes osmosis by dividing tube into two arms with a membrane impermeable to solute like sodium chloride but permeable to water via narrow pores or aquaporin analogues. Each arm filled with aqueous solution of different concentration. Water activity and chemical potential are inversely related to solute concentration; lower solute means more free water molecules with higher escaping tendency. Consequently random thermal motion results in greater diffusive flux of water from low solute concentration side where water concentration high toward high solute side where water concentration low. Solute molecules cannot follow due to size or polarity exclusion. Over time concentrated arm level rises while dilute arm falls, generating hydrostatic pressure difference that eventually balances osmotic driving force at equilibrium. No active transport or energy input is involved beyond existing gradient. This net flux demonstrates that water moves opposite to solute gradient. Hence water movement occurs from region of lower solute concentration to region of higher solute concentration until potentials equalize.

Ref: Lodish et al., Molecular Cell Biology, Chapter: Osmosis and U-Tube Demonstration of Water Movement.