A 50-year-old male with a history of chronic pancreatitis presents with several days of nausea and vomiting. His biochemistry profile is as follows:
Parameter |
Patient Value |
Normal Adult Range |
|
Arterial Blood Gas |
|||
FiO2 |
0.4 |
||
pH |
7.62* |
7.35 – 7.45 |
|
PCO2 |
62 mmHg* (8.2 kPa)* |
36 |
– 45 (4.6 – 6.0) |
PO2 |
133 mmHg (17.5 kPa) |
||
Bicarbonate |
65 mmol/L* |
21 |
– 28 |
Base Excess |
> 30 mmol/L* |
-3 – +3 |
|
Sodium |
149 mmol/L* |
135 – 145 |
|
Potassium |
3.3 mmol/L* |
3.5 – 5.2 |
|
Chloride |
53 mmol/L* |
95 |
– 110 |
Calcium ionised |
0.74 mmol/L* |
1.12 – 1.32 |
|
Lactate |
2.7 mmol/L* |
< 1.3 |
|
Venous biochemistry |
|||
Urea |
34.9 mmol/L* |
3.0 – 8.0 |
|
Creatinine |
431 micromol/L* |
60 |
– 110 |
Interpret the abnormalities in the above results and give likely underlying causes. (30% marks)
Severe metabolic alkalosis (raised SID)
Respiratory compensation (incomplete)
High anion gap (approx. 31) metabolic acidosis
Profound hypochloraemia
Gastric losses and fluid depletion causing chloride loss and metabolic alkalosis
Metabolic acidosis secondary to renal failure (acute? Acute on chronic?) +/- sepsis from pancreatitis and/or gastro-enteritis
CO2 retention as compensation for severe metabolic alkalosis
Let us dissect these results systematically.
So, in summary, the blood abnormalities are:
The college make a few strange statements here. For instance, the respiratory compensataion for this metabolic alkalosis is complete, but they think it is not. Are we using the same Boston equations? If we were to use the Copenhagen rules instead, we would expect the PaCO2 to be 40 + (30 ×0.6) = 58mmHg, and that would still be withing 4mmHg of the measured value.
So, it is difficult to tell exactly why the college think the compensation is incomplete. Certainly, complete compensation does not mean the normalisation of pH has been achieved.
In 1984, in his educational article for Kidney International John Harrington explored this issue, and concluded that the relationship between PaCO2 and HCO3- remains stable and near-linear for a broad range of values, extending even into the ridiculous. Every 1mmol/L rise in bicarbonate was matched by a 0.7mmHg increase in PaCO2. in a series of cruel human experiments on alkalotic volunteers who were either fed bicarbonate and THAM for many days by Goldring et al (1962), or had acetate administered via dialysis circuits by De Strihou et al (1973). If one plugs this rate of rise into an online calculator, one observes a rise of pH by about 0.01 for ever 1mmol increase in bicarbonate.
So, the pH will inevitably trend to alkalaemia. Furthermore, it is possible to demonstrate that the correction of pH back to 7.45 would require a PaCO2 of around 94mmHg, and this cannot be viewed as a physiologically beneficial move by any sane person. For this very sensible reason, respiratory compensation for truly severe metabolic alkalosis could never take place outside of mathematical models. To achieve a stable PaCO2 of 94mmHg the alkalotic person would have to be severely hypoxic on room air (with an alveolar oxygen tension no greater than 34 mmHg), and breathing at a rate of around 2 breaths per minute.
Goldring, Roberta M., et al. "Respiratory adjustment to chronic metabolic alkalosis in man." Journal of Clinical Investigation 47.1 (1968): 188.
De Strihou, C. Van Ypersele, and A. Frans. "The respiratory response to chronic metabolic alkalosis and acidosis in disease." Clinical Science 45.4 (1973): 439-448.
Harrington, John T. "Metabolic alkalosis." Kidney international 26.1 (1984): 88-97.