Primary Causes & Pathophysiology
The fundamental mechanism of NAGMA is a primary reduction in serum bicarbonate (HCO3-) concentration without the addition of unmeasured organic acids. To maintain serum electroneutrality, the decrease in the negatively charged bicarbonate ion is offset by a compensatory increase in the reabsorption of chloride (Cl-) by the kidneys, leading to hyperchloraemia. This bicarbonate deficit arises either from direct losses via the gastrointestinal tract (e.g., severe diarrhoea, pancreatic fistulas) or via the kidneys (e.g., renal tubular acidosis, carbonic anhydrase inhibitors), or from a failure of the kidneys to excrete hydrogen ions (as in Type 4 RTA). The respiratory system compensates by increasing alveolar ventilation to blow off CO2, lowering the PaCO2 according to Winter's formula.
Direct loss of bicarbonate-rich fluid from the lower gastrointestinal tract, leading to a compensatory increase in serum chloride.
Impaired renal bicarbonate reabsorption (Type 2) or defective distal hydrogen ion secretion (Type 1 and 4), resulting in net acid retention and bicarbonate wasting.
Blockade of proximal tubular bicarbonate reabsorption, causing profound urinary bicarbonate loss and subsequent hyperchloraemic acidosis.
Loss of alkaline pancreatic and biliary secretions, which are normally rich in bicarbonate, into drains or the peritoneal cavity.
The bowel mucosa exchanges urinary chloride for bicarbonate, leading to systemic bicarbonate depletion and chloride retention.
Mild to moderate reductions in glomerular filtration rate can impair ammonium excretion before the retention of unmeasured uraemic anions (like sulphates and phosphates) becomes significant enough to elevate the anion gap.