In the steady state, our total body water content and salt content remain constant. An increase or decrease in water and salt intake is paralleled by an equivalent change in renal water and salt excretion.[1]Homeostasis is achieved through the process of glomerular filtration of plasma to produce an ultrafiltrate. The tubules then process this ultrafiltrate so that the final urine flow rate and solute excretion meet the homeostatic needs of the body. Explanation: Osmolality and osmolarity are measurements of the solute concentration of a solution. In practice, there is negligible difference between the absolute values of the different measurements. For this reason, both terms are often used interchangeably, even though they refer to different units of measurement.Osmolality Osmolality is an estimation of the osmolar concentration of plasma and is proportional to the number of particles per kilogram of solvent; it is expressed as mOsmol/kg (the SI unit is mmol/kg but mOsmol/kg is still widely used). This is what is used when values are measured by a laboratory. Osmolality is measured by clinical laboratories using an osmometer - either a freezing point depression osmometer or a vapour pressure depression osmometer. The normal osmolality of extracellular fluid is 280-295 mOsmol/kg.Osmolarity Osmolarity is an estimation of the osmolar concentration of plasma and is proportional to the number of particles per litre of solution; it is expressed as mmol/L. This is what is used when a calculated value is derived. It is derived from the measured Na+, K+, urea and glucose concentrations. The osmolarity is unreliable in various conditions - eg, pseudohyponatraemia such as hyperlipidaemia in nephrotic syndrome, or hyperproteinaemia. The following equations can be used to calculate osmolarity: Calculated osmolarity = 2 (Na+) + 2 (K+) + Glucose + Urea (all in mmol/L); OR Calculated osmolarity = 2 (Na+) + Glucose + Urea (all in mmol/L). The doubling of sodium accounts for the negative ions associated with sodium and the exclusion of potassium approximately allows for the incomplete dissociation of sodium chloride. The term osmolarity has largely been superseded by osmolality, even when discussing calculated values. Osmolality is used for the rest of this article.Osmotic gap The osmotic gap (also called osmolal gap) is an arbitrary measure of the difference between the actual osmolality (measured by the laboratory) and the calculated osmolality. It is normally less than 10-15 mOsmol/kg (see local laboratory for range). Where the osmotic gap is increased, it indicates the presence of other osmotically active solutes which are not taken into account in the calculated osmolality - eg, in methanol or ethylene glycol ingestion.Clinical relevance of osmolality As cell membranes in general are freely permeable to water, the osmolality of the extracellular fluid (ECF) is approximately equal to that of the intracellular fluid (ICF). Therefore, plasma osmolality is a guide to intracellular osmolality. This is important, as it shows that changes in ECF osmolality have a great affect on ICF osmolality - changes that can cause problems with normal cell functioning and volume (may even induce cytolysis). In normal people, increased osmolality in the blood will stimulate secretion of antidiuretic hormone (ADH). This will result in increased water reabsorption, more concentrated urine and less concentrated blood plasma. Diabetes insipidus is a condition caused by hyposecretion of, or insensitivity to, the effects of ADH. Elevation may be associated with stroke mortality. A low serum osmolality will suppress the release of ADH, resulting in decreased water reabsorption and more concentrated plasma. An increase of only 2% to 3% in plasma osmolality will produce a strong desire to drink. A change of 10% to 15% in blood volume and arterial pressure is required to produce the same response.