Clinical review: Renal tubular acidosis – a physicochemical approach
© BioMed Central Ltd 2005
Published: 25 August 2005
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© BioMed Central Ltd 2005
Published: 25 August 2005
The Canadian physiologist PA Stewart advanced the theory that the proton concentration, and hence pH, in any compartment is dependent on the charges of fully ionized and partly ionized species, and on the prevailing CO2 tension, all of which he dubbed independent variables. Because the kidneys regulate the concentrations of the most important fully ionized species ([K+], [Na+], and [Cl-]) but neither CO2 nor weak acids, the implication is that it should be possible to ascertain the renal contribution to acid–base homeostasis based on the excretion of these ions. One further corollary of Stewart's theory is that, because pH is solely dependent on the named independent variables, transport of protons to and from a compartment by itself will not influence pH. This is apparently in great contrast to models of proton pumps and bicarbonate transporters currently being examined in great molecular detail. Failure of these pumps and cotransporters is at the root of disorders called renal tubular acidoses. The unquestionable relation between malfunction of proton transporters and renal tubular acidosis represents a problem for Stewart theory. This review shows that the dilemma for Stewart theory is only apparent because transport of acid–base equivalents is accompanied by electrolytes. We suggest that Stewart theory may lead to new questions that must be investigated experimentally. Also, recent evidence from physiology that pH may not regulate acid–base transport is in accordance with the concepts presented by Stewart.
Renal tubular acidoses (RTAs) are forms of metabolic acidoses that are thought to arise from a lack of urine excretion of protons or loss of bicarbonate (HCO3 -) due to a variety of tubular disorders. Characteristically, this causes a hyperchloraemic (non-anion gap) acidosis without impaired glomerular filtration. Molecular studies have identified genetic or acquired defects in transporters of protons and HCO3 - in many forms of RTA. However, at the same time these transporters have been found also to be involved in transport of Cl- and Na+. Furthermore, in a few cases RTA has been associated with primary defects in electrolyte transporters alone.
The core of Stewart theory is that transport of protons as such is unimportant to regulation of pH. In contrast, the theory states that acid–base homeostasis is directly regulated by electrolyte transport in the renal tubules. H+ is effectively a balancing requirement imposed by physical chemistry. Accounting for how this occurs will probably lead to an improved understanding of homeostasis.
We begin the review by describing the classical formulation of the renal regulation of acid–base homeostasis. We then describe the quantitative physical chemistry notion of acid–base as described by Stewart (henceforth called the 'physicochemical approach'). On this basis we analyze some of the mechanisms that are active in RTA. We show that the physicochemical approach may lead to new questions that can be pursued experimentally to supplement insights already gained with classical theory. Several authors have suggested that the physicochemical approach could be used to the benefit of our understanding of RTA [1, 2].
According to traditional concepts , daily acid production is calculated as the combined excretion of sulphate anion (SO4 2-) and organic anions in the urine, whereas renal elimination of acid equivalents is computed as the combined titrable acidity + ammonium - excreted HCO3 -, called net acid excretion (NAE). Cohen and coworkers  reviewed evidence indicating that the traditional view may be inconsistent with observations in patients in renal failure and in a number of experimental studies. In one of the studies assessed, Halperin and coworkers  examined rats loaded with extra alkali on top of already basic ordinary rat chow. Amazingly, increasing unmeasured organic anions had a 10-fold greater effect on alkali disposal than did changes in NAE, as traditionally computed. Similar findings had already been reported by Knepper and coworkers  in 1989. That acid–base balance is always accounted for by standard measurements may therefore be disputed. Although fervently rejected , this has given rise to a proposal of a new classification system for NAE that includes the regulation of loss of organic anions or potential HCO3 -.
Difficulties in measuring titrable acidity and organic anions are one main source of disagreement with regard to acid–base homeostasis  both in normal persons and in those with renal impairment . A recent Danish study  reinforced the concept from studies of healthy humans exposed to acid loads that nonmetabolizable base excretion is important to renal regulation of acid–base homeostasis.
Central to renal acid–base physiology is excretion of ammonium. One view  is that ammonium is produced as NH4 + in large quantities from hydrolysis of peptide bonds, and its excretion in urine has no bearing on acid–base chemistry except for the fact that for nitrogen balance it would otherwise have to be converted to urea – a process seen to consume bicarbonate. Exactly this argument was used again by Nagami  in an authoritative review of renal ammonia production and excretion. Most recently a study of normal individuals  showed that ureagenesis increased during experimental acidosis produced by CaCl2. This contrasted with the authors' expectations because urea-genesis was supposed to cost alkali.
However, the traditional view is that NH4 + excretion is one ofthe most important mechanisms for eliminating metabolic acid equivalents because the leftover from deamination of glutamine is effectively bicarbonate and the process comes to a halt if NH4 + is not eliminated . As stated in recent accounts, this view also accounts for the bicarbonate toll of ureagenesis  but the details of regulation and overall stoichiometry are still debated. However, it seems that the handling of NH4 + in the kidney is of great importance because a complicated network of transport mechanisms have evolved . Most recently, a new group of putative NH4 + (and NH3?) transporters related to the rhesus group of proteins has been described . As far as we know, the result of missing one or more of these transporters on acid–base balance is not yet known, and because of redundancy it could be limited. Finally, apart from being a transported quantity that is of importance per se, NH4 + hasalso been found to influence a number of other tubular processesthat are involved in acid–base regulation [16, 17].
Hence, although there can be no doubt that excretion of is important to acid–base homeostasis, it is not entirely NH4 + clear why this is so. We suggest that the physicochemical approach to acid–base provides a more coherent picture of the role played by NH4 +.
Here we consider the approach to acid–base chemistry proposed by PA Stewart [18, 19]. Biological fluids are dominated by a high concentration of water, approximately 55 mol/l. Physical chemistry determines the dissociation of water into protons and hydroxyl ions. If the determinants of that equilibrium are unchanged, then concentration of protons, and therefore pH, will be as well.
A number of important substances (e.g. many salts) dissociate completely to ions, when dissolved in water, whereas water itself dissociates to a very minor degree. Nonetheless, the dissociation of water into H+ and OH- provides an inexhaustible source and sink of acid–base equivalents. The proton concentration, and hence pH, is determined by the requirement that positive and negative charges must balance and by the combined equations that govern dissociations of involved species. The approach is formally based on analysis of separate compartments and leads to the result that [H+] in a compartment of physiological fluid is determined by the concentrations of fully ionized substances (strong ion difference [SID]), partial CO2 tension (PCO2) and partly dissociated substances termed 'weak acids' in that compartment.
Hence, in a compartment/solution containing NaCl or similar salt solution, the proton concentration is simply determined by SID and the water ion product (Kw). Addition or removal of protons or hydroxyl ions may or may not be possible but will not change pH .
It is possible that the development of Stewart concepts to this extent will suffice for analysis of renal influences on acid–base homeostasis from a whole body or balance perspective. However, to present the theory of Stewart in a more complete form, we may also add weak acids and CO2 to this framework. A full account of the Stewart approach with some later adaptations is available in a previous issue of this journal (see the report by Corey ).
These equations have explicit entries of constants and concentrations or tensions, but the practical use of the framework must be developed with detail sufficient to deal with the problem at hand. In plasma, other strong ions (e.g. Ca2+ and lactate) and weak acids are frequently found but they are treated on an equal footing.
A number of studies have shown that this algebra yields an accurate description or prediction of acid–base measurements. More importantly, however, the physicochemical approach may lead to a better understanding of mechanisms that are active in disease and treatment. An example of what may be accomplished is the successful application of the physicochemical approach to exercise physiology. Here, the ability of the independent variables to predict measured pH has been proven (correlation 0.985), but more importantly changes over time and between the different body compartments in these independent variables explain how a range of interventions influence acid–base as a part of muscle physiology .
CO2 is transported in the body as a number of species and because the processes involved have variable latency (e.g. the Cl-/HCO3 - exchanger band3 in red blood cells ), widely differing values of PCO2 are found in the body . The physicochemical approach, focusing as it does on each compartment separately and having no special interest in the quantitatively lesser compartment of arterial blood, is at no disadvantage relative to conventional concepts in elucidating this difficult area. Although this is less of a problem when overall renal regulation of acid–base homeostasis is considered, notwithstanding that urine CO2 may be of utility when diagnosing variants of RTA , it is a major problem with respect to understanding the underlying cellular transport processes. Further, recent results showing the complicated organization of transporters together in physically connected complexes indicate that much work will be needed if we are to understand the integrated molecular details of anion transport and metabolism in renal CO2 tubules .
Whereas the physicochemical approach explains how pH is determined from independent variables, when applying this to urine the focus is not on regulation of urine pH but on the renal regulation of the independent variables that determine plasma and whole body acid–base balance. These independent variables are the SID, weak acids, and PCO2. Hence, from the point of view of the physicochemical approach, assessing urine with the aim of understanding the renal contribution to acid–base balance amounts to deducing its effects on the independent variables for a specified body compartment. It has been reported that the concepts of SID and weak acids may be blurred. For example, pH may influence the behaviour of species as either strong ions (components of SID) or weak acids , and this applies, for instance, to phosphates and proteins. Furthermore, neither Na+ nor Ca2+ is invariably and totally dissociated, as implied by the common SID construct .
One important but thus far undeveloped aspect of the Stewart approach to whole body acid balance problems is that the independent variables for the extracellular compartment normally in focus may be only partly relevant to the much larger intracellular compartment. Excretion of large amounts of potassium, for example, may be minimally relevant to SID in the extracellular compartment but may, depending on the circumstances, be crucial to intracellular SID .
It is evident that there will be differences in the approach to accounting for acid–base balance in the classical compared with the physicochemical approach. In the classical setting we must perform difficult titrations  and measurements of NH4 +, PCO2 and pH to compute a [HCO3 -] after correction of pK for ionic strength. Every part of this is complicated, and the overall results with regard to our understanding of whole body balance are not universally accepted . In the physicochemical approach, renal involvement in acid–base balance is manifested in its influence on independent variables – nothing more and nothing less. For a first approximation, this is the urine excretion of SID components, principally Na+ and Cl- when extracellular homeostasis alone is considered. It will be a practical matter to determine the extent to which the Stewart approach will be complicated by problems in computing both SID and weak acids in urine.
In the physicochemical approach, the urinary excretion of NH4 + or organic anions will be important for acid–base balance only to the extent that it influences SID in a body compartment. Excretion of organic anions is from this perspective a way to excrete Na+ without Cl- and thereby decrease SID in the body. This will result in increasing plasma H+, no matter what the nature of the organic anion is. This hypothesis can be tested experimentally. On a similar footing, NH4 + excretion could be understood as means to excrete Cl- without Na+ in order to increase SID in the body. However, apart from their influence on SID, the excretion of these substances may convey important information about underlying pathophysiological processes. Hence, Kellum  has proposed that, when analyzing the mechanism of hyperchloraemic acidosis, an initial distinction could be made between states in which the kidney reacted normally (i.e. increasing the excretion of Cl- relative to Na+ and K+ by augmenting NH4 + excretion and so causing urine SID to be more negative) and situations where, in spite of acidosis, the kidney continues to decrease whole body SID by excreting more Na+ and K+ than Cl-. This will typically be the case in distal RTA (dRTA) without increased NH4 + excretion during acidosis.
Several types of RTA may be discerned : proximal (type 2), distal (type 1), mixed (type 3), and a heterogeneous group of disorders characterized by hyperkalaemia and acidosis (type 4). RTA is a hyperchloraemic rather than an anion-gap-type metabolic acidosis. Typically, renal function (glomerular filtration rate) is unimpaired and the acidosis is not simply caused by absence of renal clearance. RTA must be separated from other forms of hyperchloraemic acidosis, some of which (e.g. the hyperchloraemic acidosis that occurs following saline infusion) are very important in the intensive care setting [32, 33].
Proximal RTA is classically characterized by impaired proximal reclamation of bicarbonate. This may be isolated or combined with other proximal tubular defects, and it may be congenital or acquired.
Proximal bicarbonate reabsorption is still incompletely understood . Most of the bicarbonate  leaves the tubule lumen as CO2 following sodium dependent H+ secretion via Na+/H+ exchanger isoforms or (to a minor extent) vacuolar H+-ATPase, apical anion exchange via formate enhanced Slc26a6, or other mechanisms , but some bicarbonate transport may also be paracellular . The transport requires both membrane bound carbonic anhydrase (CA) type 4 and intracellular CA-2.
Among hereditary forms of RTA type 2  is a very rare autosomal dominant disorder, the mechanism of which is unknown, but isoform 3 of the Na+/H+ exchanger (solute carrier [SLC]9A3) is a candidate. More common is an autosomal recessive form with ocular abnormalities, related to mutations in kidney Na+/HCO3 - cotransporter (kNBC)1 (SLC4A4) gene, which encodes the basolateral, electrogenic Na+/3(HCO3 -) cotransporter. kNBC1 activity leads to a depolarization of the membrane and to extracellular accumulation of HCO3 -. A recently identified potassium channel, named TASK2, recycles K+ and repolarizes the potential, and mice that are deficient in this channel had metabolic acidosis associated with insufficient proximal bicarbonate reabsorption . Recent studies of the regulation of kNBC1 and integrated transport in the proximal tubule have shown that, in addition to a substrate interaction, there is also a true macromolecular interaction between CA-2 and kNBC1 .
Sporadic forms, which are not yet characterized, also occur. However, most cases of proximal RTA are secondary and a host of associations have been described. Blockade of CA-4 by acetazolamide leads predictably to proximal RTA. Important are other genetic diseases that cause a generalized proximal tubular syndrome (Fanconi's; e.g. cystinosis, fructose intolerance, etc.) and drugs and toxins (e.g. ifosfamide , lead, mercury and cadmium), but light chain disease occurs among the elderly with proximal RTA. A number of medications have been related to proximal RTA .
Characteristic of proximal RTA is the presence of bicarbonaturia, with a fractional bicarbonate excretion of more than 15% when bicarbonate is given. Eventually, acid–base balance and urine acidification is achieved as plasma bicarbonate drops low enough for reabsorption to keep pace. Treatment may be difficult because administered base is often excreted before the desired normalization is achieved.
Explaining acidosis in proximal RTA from the conventional point of view is straightforward because the defining loss of urinary bicarbonate will inevitably deplete the body and result in hyperchloraemic acidosis. From the point of view of the physicochemical approach, the reciprocal retention of Cl- and resulting decline in SID will also explain the findings.
In the conventional notion of acid–base regulation, proximal bicarbonate reabsorption is thought to be regulated by pH. However, based on studies of bicarbonate transport in the perfused rabbit proximal tubules, Boron and coworkers  concluded that the observed regulation would require both a CO2 sensor and a HCO3 - sensor. A pH sensor would not be enough. Stoichiometrically, a HCO3 - sensor transmits the same information as a hypothetical SID sensor, and the results thus indicate that the proximal tubule senses the two important independent variables in the Stewart model. These quite new results could indicate that the physicochemical approach is highly relevant to our understanding of the mechanisms that underlie regulation of acid–base physiology.
dRTA is characterized by impaired ability to acidify the urine in the distal tubules and it is often accompanied by hypokalaemia, low urinary NH4 + and hypocitraturia. In contrast to proximal RTA, nephrocalcinosis and nephrolithiasis frequently occur. Clinically, dRTA occurs as a primary (persistent or transient) or secondary disorder. Secondary dRTA occurs in a great number of circumstances related to autoimmune diseases, drugs and toxins, and genetic or structural disruptions of renal tubules. Treatment of dRTA is simple and involves substituting about 1 mEq/kg of alkali per day.
The molecular details of some forms of primary dRTA are being pursued in great detail. α-Intercalated cells secrete H+ by means of a vacuolar-type H-ATPase  (and possibly also a H+/K+-type ATPase), and bicarbonate is exchanged for Cl- by means of anion exchanger (AE1) at the basolateral side. An autosomal dominant form of mutation in 17q21–22 of SLC4A1 leads to dysfunction of AE1 possibly related to mistargeting of the protein . Also, AE1 mutations causing autosomal recessive dRTA and haemolytic anaemia have been described . Otherwise, recessive forms of dRTA are related to mutations in the proton pump in α-intercalated cells. Some are accompanied by sensorineural deafness. The gene involved (ATP6V1B1) is located on chromosome 2, and encodes the B1-subunit of H+-ATPase expressed apically on α-intercalated cells and also in the cochlea. dRTA with less impaired hearing is related to mutation in ATP6V0A4 on chromosome 7, which encodes a4, an accessory subunit of H+-ATPase. As far as presently known, the H+ pumps are electrogenic and, at least under some circumstances, they also involve shunting of the potential by Cl-, although reverse transport of K+ may also occur [44, 47]. The Cl- shunt pathway has not been elucidated yet nor aligned with any of the many known Cl- channels . Likewise, functional Cl- channels (CIC5) are necessary to acidify transport vesicles in Dent's disease, pointing to the link between H+ and Cl- transport .
Jentsch and coworkers  recently presented a detailed examination of a mouse model that was knocked out for a K+/Cl- cotransporter, KCC4, which is located in the baso-lateral membrane in α-intercalated cells in the collecting duct. These animals had metabolic acidosis with alkaline urine, but electrolyte excretion in urine was unchanged compared with controls. The investigators measured a high intracellular [Cl-] and inferred a high intracellular pH also, driven by the basal HCO3 -/Cl- exchanger AE1. Although intracellular pH was not actually measured, and the defective cotransporter would be expected also to result in increased intracellular [K+], the results seem difficult to reconcile with a dominant effect of intracellular SID to set intracellular pH and with the notion that urine SID will have to change to explain acidosis in RTA. Details are awaited for this model; the authors also failed to document that conventional accounting for acid–base balance would explain the findings (decreased NAE would also change electrolyte excretion).
Recently, examination of the dRTA that is sometimes seen in cyclosporine A treatment has led to deeper insights into the tubular handling of protons and bicarbonate, but also – and importantly – that of Cl-. In a study  of perfused rabbit collecting ducts, cyclosporine A inhibited acidosis induced downregulation of unidirectional HCO3 - secretory flux in βintercalated cells and prevented downregulation of the linked Cl- resorption. Detailed examination of the apical and basolateral exchanges indicates that, rather than responding to, for example, intracellular pH, intracellular [Cl-] could be the regulated entity . If true, this interpretation is compatible with a Stewart-based perspective.
Type 3 RTA is caused by recessive mutation in the CA-2 gene on 8q22, which encodes carbonic anhydrase type 2 . It is a mixed type RTA that exhibits both impaired proximal HCO3 - reabsorption and impaired distal acidification, and more disturbingly osteopetrosis, cerebral calcification and mental retardation. The mechanisms that underlie the clinical picture in type 3 RTA, apart from much slower conversion of carbonic acid to and from bicarbonate, apparently also involve direct interaction between CA and the Na+/HCO3 - cotransporter kNBC1  or Cl-/HCO3 - exchanger SLC26A6 . From the physicochemical interpretation, acidosis is expected under these circumstances because of impaired transport of SID components.
RTA type 4 or hyperkalaemic RTA is a heterogeneous group of disorders that is characterized by low urine NH4 +, which is probably caused by the hyperkalaemia or by aldosterone deficiency or defective signalling. Causes include various types of adrenal failure or pseudohypoaldosteronism (PHA)1 due to defects in the mineralocorticoid receptor or the epithelial Na+ channel, all characterized by salt loss and hypotension. A similar picture may be seen in obstructive uropathy or drug-induced interstitial nephritis. Furthermore, a number of drugs may impair signalling in the renin–aldosterone system and cause hyperkalaemia and metabolic acidosis (e.g. potassium sparing diuretics, trimethoprim, cyclo-oxygenase inhibitors, angiotensin converting enzyme inhibitors).
Lately, much interest has been given to a group of rare autosomal dominant diseases characterized by hyperkalaemia and acidosis and age-related hypertension . In spite of hypervolaemia, aldosterone is not low and the disorders have been collectively termed pseudohypoaldosteronism type 2 (PHA2) . Two of the mutations have been mechanistically characterized in some detail. Mutations in 17q21 in the WNK4 gene may change the function of the protein, whereas a mutation in the intron to the WNK1 gene at 12p increases transcription of the protein. Briefly, WNK4 normally inhibits the thiazide-sensitive cotransporter (TSC) in the distal convolute tubule (DCT), and inhibits the renal outer medullar K+ channel (ROMK) in the collecting duct (CD), but enhances paracellular Cl- transport in both DCT and CD. Mutations in the WNK4 gene that cause PHA2 are found to release the normal inhibition of TSC, but at the same time PHA2 enhances the inhibition of ROMK and enhances the paracellular Cl- flux (but not Na+ flux) through claudins. Hence, the hyperkalaemia is explained both by inhibition of ROMK and by decreased delivery of Na+ to CD because of enhanced absorption in the DCT, and the good effect of thiazides on the hypertension is readily explained. The normal explanation for metabolic acidosis is based on the decreased delivery of Na+ to CD and thereby inhibition of generation of lumen negative potential to enhance H+ secretion in combination with the decreased delivery of NH4 + secondary to the hyperkalaemia .
The effect of the molecular abnormalities on Cl- transport is barely considered in the explanation of the findings using the conventional model of acid–base. From the physicochemical approach it is evident that acidosis is well explained by the dominant and primary enhancement of Cl- absorption in this disorder. Even if only the TSC effect were invoked, an isotonic expansion of body volume with Na+ and Cl- would be expected to yield acidosis. In any case, SID in plasma will decrease and pH will too. Very recently it was described that WNK1 activates the epithelial Na+ channel , and this was felt to explain the finding that not all patients with PHA2 are equally sensitive to thiazides. This would be expected to relieve the voltage imposed inhibition of H-ATPase in CD and likewise lessen the degree of hyperkalaemia. Electrolyte and NAE balance studies across different mutations may help to clarify how acid–base balance is actually constructed in these rare diseases.
Traditionally, dRTA is recognized by the inability to decrease urine pH below 5.5 in spite of metabolic acidosis. These patients are also characterized by an inability to augment NH4 + excretion . A high urine PCO2 after bicarbonate loading has traditionally been the criterion for declaring distal H+ secretion to be normal , and it was also recently found to identify patients with confirmed dRTA due to a proton pump problem .
Proximal RTA is characterized by high fractional excretion of bicarbonate (>15%) during loading, and an ability to achieve a urine pH below 5.5 during acidosis. Approaches are well described by Soriano  and Smulders and coworkers .
When assessing urine to gauge whether the physicochemical approach or the classical theory is best able to explain the acidosis in RTA, it is possible that both will do so successfully. From the physicochemical approach, the lack of urine NH4 + in distal RTA will force excretion of urine with a relatively high SID and this will explain the acidosis. An old study did in fact indicate that, in type 1 RTA, Na+ loss and to a lesser degree Cl- handling was abnormal in spite of long-term correction of acidosis .
The classical theory also explains the acidosis by a lack of amplification of NH4 + excretion. Likewise, for proximal RTA bicarbonate loss and high SID excretion will be equivalent. It was recently suggested that even though it may be difficult mechanistically to separate the implications of the theories, by using the physicochemical approach the focus is forced toward movements of Na+ and Cl-, and this may lead to a new understanding . Indeed, analysis of WNK mutations confirms this expectation.
From the clinical viewpoint, the advantage of employing the physicochemical approach is that the renal contribution to acid–base homeostasis, even in complicated settings, can be ascertained in principle by simple chemical analysis of the urine. It is possible to explain RTA in general as a hyperchloraemic form of metabolic acidosis that can be described as a low SID acidosis, which has focused attention primarily on the net handling of SID constituents, namely Na+, K+, and Cl-. This handling of SID constituents has not had a central position in our understanding of the various disease states, and in some cases only seems to be a consequence of anions necessarily being filled in by Cl- as HCO3 - goes down and reversely. However, in the future efforts will focus on which transport mechanism is active (e.g. is Cl- moving with H+ or K+ or against it to shunt the potential generated by the vacuolar H-ATPase ) and on which moiety is actually regulated by the tubular processes. A number of studies have recently focused on apical anion handling in the collecting duct via a newly characterized transporter, namely pendrin . This exchanger seems well poised to react to Cl- balance  and could therefore also be sensitive to the independent variable in acid–base regulation (i.e. SID) .
One defining point in the physicochemical approach that has an impact on the interpretation of acid–base phenomena is the concept of [H+] as a dependent variable, which tends to imply that clinical or physiological phenomena might more fundamentally depend on the baseline independent variables (e.g. SID, weak acids and PCO2). The necessity when analyzing renal phenomena to differentiate metabolic and respiratory acidosis may be an indicator that pH as such is not actually the sensed quantity.
In fact, how derangements in acid–base balance are sensed by the kidneys remains elusive, although there it is a general belief that such detection happens there. Quite recently, a protein, Pyk2, that was sensitive to pH and that regulated isoform 3 of the Na+/H+ exchanger in the proximal tubules was described . Furthermore, in experiments identifying this alleged pH sensor, SID was directly varied but PCO2 did not change. Hence, it is not evident that pH was really sensed, and in an accompanying editorial Gluck  expressed reservations regarding this notion. As explained above in relation to proximal RTA, recent studies conducted by Boron and coworkers  indicate that that bicarbonate and PCO2 are the regulated entities, rather than pH, which is in accordance with the physicochemical approach to acid–base physiology insofar as bicarbonate and SID are equivalent.
Finally, if whole body acid–base balance is to be untangled, then the intracellular domains, which are likely to vary, must also be understood. In exercise physiology  advances have been made using the Stewart approach in elucidating plasma acid–base balance as it is perturbed by transfer of putative independent influences, but modelling cells or whole organs themselves from this point of view has not been done. This will entail such difficulties as determining water structure in cells and small confines  and modelling the pH effects of the structural proteins and nucleic acids as they fold and integrate. Modelling potassium balance in order to draw inferences regarding intracellular SID will likewise be necessary and interesting.
A recent study of patients in acute renal failure , employing state of the art methods, found that almost 80% of total body water appeared to be extracellular. This indicates that a great deal of experimental work must be done before analytical solutions  to the whole body multicompartment system can be derived and applied in clinical practice. We suggest that the physicochemical approach will prove useful in formulating hypotheses for future work aimed at developing a coherent, unpretentious and practical understanding of mechanisms involved in renal acid–base regulation.
total concentration of weak acids
distal convoluted tubule
distal renal tubular acidosis
kidney Na+/HCO3 -; cotransporter
net acid excretion
partial CO2 tension
renal outer medullar K+ channel
renal tubular acidosis
strong ion difference