Net osmotic pressure stays about the same and net hydrostatic pressure decreases.
Osmotic rate refers to the speed at which solvent molecules move across a semi-permeable membrane in response to differences in solute concentrations between the two sides. It is influenced by factors such as solute concentration gradient, temperature, and surface area of the membrane. A higher osmotic rate means that solvent molecules are moving more rapidly across the membrane to equalize the concentrations on either side.
Animals that have a hydro-static skeleton have a fluid filled body cavity and a muscular body wall. This skeleton has no hard parts but a animal can squeeze the fluid from one area of the body to another under pressure to give him support.
The cell is in a state of dynamic equilibrium. This means that while molecules are constantly moving in and out of the cell, there is no overall change in the concentration inside the cell because the rate of movement in both directions is equal.
Osmosis can affect a cell by causing it to either swell or shrink depending on the concentration of solutes inside and outside the cell. When water moves into or out of the cell through osmosis, it can change the cell's volume and shape, potentially impacting its function and stability. An imbalance in osmotic pressure can lead to cell damage or even cell death.
Hemolysis is the bursting of red blood cells (hemo- blood and lysis- bursting). There are three types of solutions that blood can be put into: hypertonic, hypotonic and isotonic. The names of these give you some clue as to how the cell will behave in solution. Hypertonic solutions have greater osmotic pressure than the cells they contain, which will cause the cell to shrivel as its contents diffuse into the solution. Hypotonic solutions have less osmotic pressure than the cells inside of them, so the contents of solution will diffuse across the cell membrane and into the cell, eventually causing it to swell and burst (hemolysis). Isotonic solutions have osmotic pressure equal to that of the solutes they contain, so no net change is observed.
Because it will change the osmotic pressure .
Pressure increases with depth due to the weight of the overlying material pushing down. This is known as hydrostatic pressure. The deeper you go underwater or underground, the greater the pressure because there is more material above exerting force.
A capillary tube in an air conditioner serves as a metering device to regulate the flow of refrigerant into the evaporator coil. It helps to maintain the proper pressure and temperature levels needed for the refrigeration cycle to operate effectively. By creating a pressure drop, the capillary tube assists in the cooling process by facilitating the phase change of the refrigerant from liquid to gas.
Osmotic change refers to the movement of water across a membrane in response to differences in solute concentration on either side of the membrane. This process is driven by osmosis, where water flows from an area of low solute concentration to an area of high solute concentration to equalize the concentration on both sides of the membrane. Osmotic changes can affect the volume and pressure of cells and organisms.
The elasticity of the balloon's material allows it to expand and take on different shapes when filled with water. As the balloon fills with water, the pressure from the water pushes against the sides of the balloon, causing it to stretch and change shape.
Osmotic rate refers to the speed at which solvent molecules move across a semi-permeable membrane in response to differences in solute concentrations between the two sides. It is influenced by factors such as solute concentration gradient, temperature, and surface area of the membrane. A higher osmotic rate means that solvent molecules are moving more rapidly across the membrane to equalize the concentrations on either side.
Translocation is caused due to the change in the osmotic pressure in the upper and lower part of a tree/plant.when there is a difference of water content in the upper part and the lower part then the water will move towards the upper region where endosmosis has taken place. this translocation takes place with the help of sieve tubes.
Isotonicity refers to a solution having the same osmotic pressure as another solution, resulting in no net movement of water across a semi-permeable membrane. Isoosmosis, on the other hand, refers to the equal movement of solvent molecules in opposite directions across a semi-permeable membrane, leading to no change in concentration on either side. In summary, isotonicity relates to solute concentration and osmotic pressure, while isoosmosis involves the movement of solvent molecules.
Blood flow in the circulatory system is as follows: arteries->arterioles->capillaries->venules->veins. if you dilate the arteriole you are in fact lowering the resistance of the vessel (Poiseuille's Law), and it follows that net flux will increase. If capillary resistance remains the same, but the net flux has increased, then there will be an upwards change in pressure (Ohm's law). As far as veins go, it has a high compliance, which means that it can store large amounts of blood without raising venal pressure. If your question asked whether or not capillary pressure increases when venous dilates then the answer is no. Capillary blood flow will be less restricted as they flow into venules->vein and therefore will not have an increased pressure. If the question asked whether or not the venal pressure increases, then the answer is yes, but it is negligible (it has high compliance).
Pressure increases with depth below the surface of a fluid due to the weight of the fluid above pushing down. This relationship is described by the hydrostatic pressure formula P = ρgh, where P is pressure, ρ is density, g is acceleration due to gravity, and h is depth.
The basic hydrostatic equation relates the pressure variation with depth in a fluid at rest. It states that the change in pressure with depth is equal to the product of the fluid density, acceleration due to gravity, and the height difference. This equation is fundamental in understanding fluid behavior, especially in geophysics and meteorology.
Molality is independent of temperature, so when you are trying to find changes in boiling and freezing points you need something that will stay constant regardless of the change in temperature. Molarity is temperature dependent and also is based on the volume of a solution, both of which are needed to calculate pressure using the ideal gas law, PV=nRT. Osmotic pressure is similar but we substitute the number of moles of the solution and the volume by using the molarity, you cannot do this with molality, since it is dependent on mass, not volume.