1 (also grade especially in North American English)the degree to which the ground slopes, especially on a road or railwaya steep gradienta hill with a gradient of 1 in 4 (or 25%)2 (technical)the rate at which temperature, pressure, etc. changes, or increases and decreases, between one region and another
It is a type of passive diffusion, as the water travels along a concentration gradiant. As opposed to active transport, where the substances can pass against a concentration gradiant.
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Divide the height of the ramp by the length of the ramp (rise over run).
A concentration gradiant is a common term used in biology to signify that one side of a membrane contains a significantly higher amount of ions/atoms/molecules than the other side. This esentially means that in a concentration gradient you have stored energy. This is a common term used when talking about the formation of ATP.
They are fake hearts...mainly found in earthworms, these pump blood around the body to maintain a high concentration gradiant.
There is less friction from the bed and banks of the river downstream (where the gradiant decreases) so the velocity increases.
Osmosis is a passive form of diffusion as it travels downa concentration gradiant, as opposed to active transport; a type of diffusion that can go against a conc. grad.
Because it allows the creation of an osmolar gradiant between the outermost and the innermost parts of the renal medulla. This process is important in the dilution of urine.
Osmosis is the movement of water across a partially permeable membrane down the concentration gradiant from an area of high concentration to an area of low concentration until an equilibrium is achieved.
It means that they are directly proportional to each other. As one variable increases, the other variable increases/decreases at a constant rate. The constant rate is determined by the gradiant of the straight line.
I sugest you look up "steam tables". Since convection currents are caused solely by diferences in density ... yes, it is assumed that tempreture diferences CAUSED the density gradiant - but that is not always true.
A straight line will have a constant gradiant, so its change in height over time will be some multiple of x. We'll call this bx. The other point of consideration is where the line crosses the y axis (x=0). We'll call this point a. So the equation of a straight line can be given as y=a+bx