[Metabolic alkalosis on the surface but metabolic acidosis in depth]. / Alcalose métabolique en surface, mais acidose métabolique en profondeur.

Our purpose in writing this article is to emphasize the acid-base consequences and total body imbalances which follow the selective depletion of HCl. The initial body balance is an equimolar deficit of chloride and gain of bicarbonate. Within a short period of time, body balance changes; the net deficits are closer to equimolar losses of potassium and chloride. Since the loss of potassium occurred without the simultaneous loss of existing body anions (chloride or phosphate), this negative balance of potassium is accompanied by an equimolar gain of hydrogen ions. Thus when the negative balance is that of KCl, acid-base balance is present but there is a surplus of bicarbonate in the extracellular fluid (ECF) together with an equal surplus of hydrogen ions in another compartment (the intra-cellular fluid (ICF)). Moreover, if the ECF volume is contracted, a more severe degree of acidosis of the ICF may occur due to a higher PCO2 in venous blood. Given the acid-base balance and a deficit of KCl, one should not view this disorder as being "corrected" by saline at any time other than in the acute phase before a large potassium deficit occurs. Sodium chloride should be restricted to repair a deficit of sodium chloride. The emphasis on therapy is obviously to replace the deficit of KCl.

Disorders of potassium homeostasis: an approach based on pathophysiology.

Disorders of potassium (K+) homeostasis are frequently encountered in clinical medicine and may have serious sequelae, particularly cardiac arrhythmias. Since long-term K+ balance depends on regulation of renal excretion of K+, the focus of this paper is to provide a novel way to analyze the K+ excretory process at the bedside in a noninvasive fashion. A fundamental aim was to incorporate recent new advances in K+ physiology to the clinical analysis of K+ disorders. In so doing, we have tried to replace eponyms and largely descriptive terms with more specific, but hypothetical pathophysiologic diagnoses. The approach we used focuses on an assessment of the components of K+ excretion in vivo. If the rate of excretion of K+ differs from the "expected" value for the stimulus of hypokalemia or hyperkalemia, one should determine whether the fault is with the flow rate and/or the [K+] in the terminal cortical collecting duct. The former is influenced primarily by the rate of excretion of osmoles when antidiuretic hormone acts, whereas the [K+] in the cortical collecting duct is determined by factors that modulate rate of electrogenic reabsorption of Na+ in that segment and its conductance for K+. By examining the extracellular fluid (ECF) volume status, the plasma renin activity, and the renal response to the induction of ECF volume contraction, we attempted to deduce whether the change in electrogenic reabsorption of Na+ was due to an altered Na+ transport or apparent permeability to chloride in the cortical collecting duct. We believe that an approach which draws heavily on pathophysiology can be of practical use at the bedside and, in addition, indicate areas in which more research could be fruitful. To illustrate these points, two clinical cases with hypokalemia and two with hyperkalemia were analyzed. Nevertheless, it is important to emphasize that the approach provided is speculative.

Does saline "correct" the abnormal mass balance in metabolic alkalosis associated with chloride depletion in the rat?

An elevated plasma pH and bicarbonate are the clinical hallmarks of metabolic alkalosis. Nevertheless, to fully define its pathophysiology, one needs a quantitative interpretation of events in 3 areas - the ECF, ICF, and urine. Accordingly, our purpose was to study mass balance in Cl--depletion metabolic alkalosis with normal initial balance for Na+ and K+. In the 20 h following the "exchange" of Cl- (loss, 2455 mumol) and HCO(3-) (gain, 2455 mumol), only 334 mumol HCO(3-) remained in the ECF and 337 mumol were excreted. The remaining 1784 mumol disappeared primarily via titration because 3051 mueq of endogenous anions were produced and excreted largely with K+. Accordingly, metabolic alkalosis was associated with a deficit rather than a surplus of HCO(3-). To reflect the shift of H+ into cells driven by the exit of K+, the cumulative deficit of Cl- was replaced as KCl or NaCl. The fall in plasma [HCO(3-)] was larger in the KCl group (13.2 vs. 9.4 mmol/L); it was largely due to H+ exit from cells; in contrast, disappearance of HCO(3-) from the ECF was due to new endogenous acid production in the NaCl group. Thus, there was an overall deficit of HCO(3-) in metabolic alkalosis associated with KCl depletion (extracellular alkalosis and intracellular acidosis); processes in the ICF were not corrected by NaCl.

What is responsible for the diurnal variation in potassium excretion?

Potassium excretion exhibits a diurnal pattern, with most excretion occurring close to noon in humans. Each component of the K+ excretion rate [urinary K+ concentration ([K+]) and flow rate] was measured and back-calculated to reflect events in the cortical collecting duct (CCD). Our purpose was to determine to what extent each component contributed to this diurnal variation in each 2-h portion of the day. In humans, K+ excretion rose threefold from nadir (0600 h) to peak (1200-1400 h), 18 h after the principal intake of K+. The variation in K+ excretion was due almost exclusively to changes in [K+] in the terminal CCD ([K+]CCD) rather than via changes in flow rate. In rats, the bulk of K+ excretion occurred shortly after eating. Both components of K+ excretion rose after meals; the rise in the [K+]CCD (3.3-fold) predominated at earlier times, and the rise in flow rate occurred later and was primarily a result of a higher rate of excretion of urea. The rise in [K+]CCD did not correlate with aldosterone levels or administration. A very large rise in the [K+]CCD only occurred in the presence of bicarbonaturia; the transtubular potassium concentration gradient was now close to 15 in the morning and evening.

Kaliuretic response to aldosterone: influence of the content of potassium in the diet.

The excretion of potassium (K+) decreased by 50% (30 v 63 mEq/d, P < .01) when subjects consumed a diet that was low in K+ for 3 days. Although part of this conservation of K+ was achieved in part by suppressing the release of aldosterone, nevertheless providing exogenous mineralocorticoids did not lead to a large kaliuresis when there was a modest degree of K+ depletion. Accordingly, the purpose of this study was to evaluate possible mechanisms for this antikaliuretic response to mineralocorticoids. The renal handling of K+ was examined by independent analysis of the two factors that influence its excretion, the driving force to secrete K+ and the urine volume. This driving force is reflected in a noninvasive fashion by the transtubular [K+] gradient (TTKG). Stimuli to increase the rate of excretion of K+ in subjects on a normal and a low-K+ diet included the administration of 200 micrograms fludrocortisone (9 alpha F), the induction of a high urine flow rate (9 alpha F+furosemide), the induction of bicarbonaturia (9 alpha F+acetazolamide), and the excretion of Cl(-)-poor urine (< 15 mEq/L). On the low-K+ diet, the peak value for the TTKG 3 to 4 hours after 9 alpha F was less than half that while on the normal diet (6.4 v 14, P < 0.01). In contrast, the TTKG was not significantly different on either diet when there was bicarbonaturia or the excretion of a Cl(-)-poor urine (18 v 17 and 17 v 16, respectively).(ABSTRACT TRUNCATED AT 250 WORDS)