Chloride (Cl⁻) is the main negatively charged ion outside cells. Together with sodium it determines the osmolality of body fluids, and it plays a central role in acid–base balance: chloride and bicarbonate move in opposite directions to keep the blood electrically neutral. Chloride rarely changes on its own. Abnormal values usually point to a disturbance of water balance or of acid–base balance, which is why chloride is interpreted together with sodium and bicarbonate.
The anion gap is calculated as Na⁺ − (Cl⁻ + HCO₃⁻) and is normally about 8–12 mmol/L. The exact range depends on the laboratory method. In metabolic acidosis it helps separate two groups. In high-gap acidosis (ketoacidosis, lactic acidosis, kidney failure, poisoning with methanol, ethylene glycol or salicylates), extra acids are present and chloride is usually normal. In normal-gap (hyperchloraemic) acidosis (diarrhoea, renal tubular acidosis, large volumes of saline), bicarbonate is lost and chloride rises.
In critically ill patients, hyperchloraemia caused by intravenous fluids has been associated with kidney injury and worse outcomes, which is why balanced crystalloid solutions are often preferred.
An isolated, slightly abnormal chloride is rarely important. Your doctor will interpret it together with sodium, potassium, bicarbonate (or blood gas), kidney function and your symptoms. Seek urgent care for persistent vomiting, severe diarrhoea, confusion or rapid deep breathing.
This article is for general information and does not replace a consultation with a doctor. Laboratory results must be interpreted by a physician together with symptoms and other tests.
Published on 12 May 2024