BIO 203 Lecture Notes - Lecture 20: Blood Plasma, Osmotic Concentration, Homeostasis
Document Summary
Osmosis- diffusion of water down osmotic gradient across a semipermeable membrane. Diffusion is independent movement of individual molecules by random thermal motion down a concentration or energy gradient. Net diffusive movement from solute to one side. Osmotic pressure- difference in energy of water due to dissolved solutes. Increasing solute concentration decreases energy of water (concentration) C=concentration of total solutes: unites for c: moles of solute/total moles. Non-dissol(cid:448)ed solids >rtc mmhg: non-metric;often medical atm: non-metric bar: metric (cgs) units, atm. Osmosis: diffusion of water down osmotic gradient across a semipermeable membrane. Water moves from low to high . Because high (cid:373)ea(cid:374)s lo(cid:449) (cid:449)ater co(cid:374)ce(cid:374)tratio(cid:374: water (cid:373)o(cid:448)es fro(cid:373) high (cid:449)ater co(cid:374)ce(cid:374)tratio(cid:374) (cid:894)lo(cid:449) (cid:895) to lo(cid:449) (cid:449)ater co(cid:374)ce(cid:374)tratio(cid:374) (cid:894)high (cid:895) Simple metazoans (hydra, sponge, ciliates: sponges body exposed to outside environment. Do not have blood: cell bathed directly by external medium. Water moves into cell: constant tendency to swell: solutions: pump out water as it comes in: contractile vacuole.