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The kidney's juxtamedullary nephrons produce dilute urine when the fluid intake is high.
In the renal cortex, the osmolarity of the interstitial fluid and that of the tubular fluid in the proximal convoluted tubule PCT is the same.
However, the osmolarity of the interstitial fluid in the renal medulla is significantly higher than that of the filtrate, creating a gradient for water reabsorption in the descending limb of the nephron loop.
As a result, as water moves out, the osmolarity of the filtrate increases.
As the filtrate reaches the ascending limb, reabsorption of ions takes place. However, this portion of the renal tubule is impermeable to water, so with the loss of ions, the filtrate becomes dilute, and its osmolarity decreases.
This continues as the early distal convoluted tubule DCT is also permeable to ions but impermeable to water.
Further, in the absence of antidiuretic hormone or ADH, during overhydration, the late DCT and collecting ducts also become impermeable to water, but ion reabsorption continues.
Due to a lack of water reabsorption, dilute urine is produced in large volumes.
The formation of dilute urine is a critical renal adaptation that maintains fluid balance, particularly during periods of high fluid intake. This proc…
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