Urine osmolality

Urine osmolality depends on the amount of osmotically active particles excreted in the urine, regardless of their weight, size or electric charge. Osmolality is expressed in mmol / kg. It is only approximately dependent on urine density. Its measurement is more accurate compared to density, has a greater informative value and is preferred.

If we compare the two quantities, the osmolality reflects the total mass concentration of all solutes, while the density reflects their total mass concentration. Therefore, we can simply say that osmolality will be more affected by changes in the concentration of low molecular weight substances (in practice, especially sodium, glucose and urea), while density will be more significantly affected by the presence of protein in the urine.

Normal osmolality values ​​at normal fluid intake are 300-900 mmol / kg. Urine osmolality depends on the dilution and concentration of the kidneys. The extreme values ​​of osmolality at maximum dilution or maximum concentration are in the range of 50-1200 mmol / kg. If the osmolality of the urine is approximately the same as the osmolality of the blood, it is isoosmolar urine. Urine hypoosmolální has a lower osmolality than blood, i.e. less than about 290 mmol / kg. As hyperosmolální urine indicates urine osmolality higher than blood exhibits.

Theoretically, we can imagine that definitive urine arises from isoosmolar glomerular filtrate, to which pure, so-called solute-free water is added or resorbed in the renal tubules.

The transport of solute-free water expresses its clearance. We will explain what this quantity means using the following considerations: First, let us define the clearance of osmotically active substances. It is a quantity analogous to the commonly used clearance of endogenous creatinine : the clearance of osmotically active substances represents the theoretical volume of blood plasma, which is completely deprived of all osmotically active particles in the kidneys per unit time. The following will apply (derivation is similar to that of endogenous creatinine clearance):
 * $$Cl_{osm}=\frac{U_{osm} \cdot V}{P_{osm}}$$,

If the primitive urine has the same osmolality as the plasma and we neglect the contribution of proteins to the total osmolality of the plasma, the volume of filtered primitive urine must be the same as the clearance of the osmotically active Cl eight particles.

As the clearance of solute-free water refers to the difference between the actual volume of final urine excreted per unit time and osmolální clearance:
 * $$Cl_{H_2O}=V-Cl_{osm}$$

If the clearance of solute-free water is negative, it means that part of the solute-free water has been resorbed from the primitive urine, so that the definitive urine is more osmotically concentrated. Conversely, if the clearance of solute-free water were positive, hypoosmolar urine would form, against blood plasma diluted with solute-free water. Physiological values ​​range between ,00.027 and ,000.007 ml / s.

The kidneys are able to excrete large amounts of solute-free water to prevent hyponatremia. Conversely, in the absence of water, its excretion is limited and particles are excreted in a smaller volume of water.

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