Certain conditions, such as exposure to a sudden downpour, can cause the influx of large amounts of water into a living cell. Like an overfilled balloon, the cell will rupture and die if it's not able to relieve the pressure. Many bacteria have evolved pressure-sensitive relief channels that allow water to flow out of the cell in response to increased pressure on the cell membrane. Under these extreme conditions, Staphylococcus aureus bacteria produce a compound made up of four proteins. As the pressure on the membrane increases nearly to the breaking point, the proteins arrange themselves into a pore allowing water and dissolved material to exit the cell.
"[H]elices lining the inside of the pore tilt towards the plane of the membrane as the channel moves from the closed to the pre-expanded state, and that the whole channel structure becomes flatter. The helices maintain this orientation as the cross-section of the channel expands to reach the open state...MscL is nonselective for the ions and small molecules it transports and is activated at membrane tensions close to the breaking point of the membrane bilayer. It is thus usually thought of as a bacterium’s last line of defence against hypo-osmotic shock...a domain of MscL [mechanosensitive channel of large conductance] known as the cytoplasmic bundle acts as a sieve that limits the passage of large molecules through the pore...the first physical transition generates a 'pre-expanded' state in which the cross-sectional area of the channel is slightly larger than in the closed state. This is likely to be the most tension-dependent state of the mechanism, as the probability that the channel will open should be proportional to −γΔA, where γ is the lateral tension in the membrane." (Vásquez and Perozo 2009:48)