Polyuria

Fluid Compartments

As shown below, total body water (TBW) can be divided into two major compartments: intracellular and extracellular, the latter of which contains both the interstitial and intravascular spaces.

Osmolarity and Tonicity

While sodium and potasssium are capable of diffusing across cellular membranes, the sodium-potassium ATPase pumps within the cellular membranes maintain a gradient where sodium is primarily extracellular and potassium is primarily intracellular (left). In contrast, urea is an example of a solute that can freely distribute between fluid compartments (right).

 

While any dissolved solute may contribute to osmolarity (moles of solute/L), only solutes that respect the intra- and extra-cellular compartment boundaries contribute to "tonicity" by creating an osmotic gradient and cause the distribution of water witihn these compartmenets to shift. Use the INTERACTIVE ANIMATION below to see why sodium is an "effective osmole" (contributing to tonicity) but urea is not.

Since fluid shifts between the intra- and extra-cellular compartments can have clinical consequences, tonicity (or effective osmolarity) must be distinguished from total osmolarity, as shown in the equations below. NOTE: the correction factors for glucose and BUN are necessary to convert the units into mmol/L.

 

 

Water Balance

Although excess water can expand volume and excess solute can raise osmolality, we think of effective osmolality (~2 x Na) in terms of water balance we think of and total solute in terms of volume status becauase tonicity is regulated by water homeostasis (via mechanaisms such as thirst and anti-diuretic hormone activity) and the total solute balance is regulated by extracellular volume homeostasis (such as natriuretic peptide activity or RAAS).

 

 

Electrolyte Free Water Clearance

Recall that a solute diuresis may contribute to loss of free water if the solute is not an effective osmole, such as in the case of urea.

Calculating electrolyte free water clearance (EFWC) takes into account only effective osmoles to determine how much free water will be lost in the urine. EFWR is the opposite in the context of concentrated urine--how much free water is reabsorbed. See concepts and equations:

 

 

 

 

Back to the Case

 

Recall the patient's chemistries and volumes before and after ddAVP:

Initial Serum

Na 142

Initial Urine

Osm 322
Na 146
K 11
 

Initial 24Hr Urine

6.5L

Repeat Serum

Na 137

Repeat Urine

Osm 534
Na 223
K 31
Urea 58

Repeat 24Hr Urine

4.0L
 
 
 
 
 
 
 
 

Did the EFWC Change after ddAVP was given?

EFWC = UVol x [1 - (UNa + UK)/SNa)]

 
Before ddAVP, the EFWC was -0.65L / day
 
After ddAVP, the EFWC was -3.4L / day
 
Free water retention increased
 
 

Did the total daily osmolar output for sodium change?

 
The initial and subsequent total daily sodium output values are 947 and 895 mOmoles / day, respectively.
 
While ddAVP influenced free water retention in the kidney, there was no impact on sodium handling.
 
The sodium diuresis persisted at the same rate.
 
 
 

Tonicity Balance Simulation

This simulation assumes that plasma osmolarity is 2x serum sodium and that TBW is 0.6 x weight.

Click this link to view this simulation with additional parameters that are hidden in the view below.

This simulation should NOT be used as a clinical tool.

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