Vloeistofbeweging tussen compartimenten

Hydrostatic pressure, generated by the heart's pumping action, exceeds osmotic pressure at the arteriolar end of capillaries, pushing plasma and nutrients into surrounding tissues. At the venule end, hydrostatic pressure drops below osmotic pressure, allowing fluid and cellular wastes to reenter capillaries. This pressure gradient creates continuous fluid exchange between the intravascular and interstitial compartments.

Osmotic gradients, formed by differences in solute concentration across semipermeable membranes, regulate water movement between plasma, interstitial fluid, and intracellular fluid. Water moves from areas of low solute concentration to high solute concentration. These gradients shift constantly based on varying body conditions, redistributing water throughout tissues and maintaining fluid balance.

Hydrostatic pressure in kidney nephrons directly regulates blood filtration and urine production. Increased hydrostatic pressure drives more plasma from capillaries into the filtrate, increasing urine output. Conversely, extremely low pressure during dehydration reduces filtration capacity, compromising kidney function and potentially leading to reduced removal of nitrogenous wastes and acute kidney injury.

Active transport moves substances against concentration gradients using ATP energy, exemplified by the sodium-potassium pump. Passive transport, including facilitated diffusion, moves molecules down concentration gradients without energy. Glucose, amino acids, and ions use facilitated diffusion through specific protein channels, while dissolved gases and lipids permeate membranes directly.

Excess interstitial fluid not directly reabsorbed into capillaries is drained by the lymphatic system. The lymphatic vessels collect this fluid and return it to the vascular system at the subclavian veins, completing the fluid circulation cycle and preventing tissue swelling.

During dehydration, water loss increases solute concentration in body fluids, creating stronger osmotic gradients that pull water from cells. Reduced hydrostatic pressure in kidneys decreases filtration capacity, impairing waste removal. When rehydration occurs, water redistributes along osmotic gradients, replenishing all tissues and restoring normal kidney filtration.

Membrane permeability depends on molecular properties and size. Dissolved gases, lipids, and water easily permeate cell membranes directly. Larger or charged molecules like glucose, amino acids, and ions cannot cross without assistance and require facilitated transport through specific protein channels to move down their concentration gradients.