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Что такое Urine Osmolality Calculator?
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Urine osmolality is a measure of the concentration of all solutes dissolved in urine, expressed as milliosmoles per kilogram of water (mOsm/kg). It reflects the kidneys' ability to concentrate or dilute the urine in response to changes in body water balance, antidiuretic hormone (ADH or vasopressin) levels, and renal tubular function. Unlike urine specific gravity, which measures density and can be disproportionately affected by large molecules like glucose or contrast agents, osmolality accurately reflects the number of solute particles regardless of their molecular weight. Urine osmolality is measured in clinical laboratories by freezing point depression osmometry — the most accurate method — or estimated by the calculated formula using urine electrolytes, glucose, and urea. The normal kidneys can vary urine osmolality across an extraordinary range: from as low as 50 mOsm/kg during maximum water diuresis to greater than 1200 mOsm/kg during severe dehydration. This flexibility allows the body to handle large variations in water and solute intake. Clinically, urine osmolality is indispensable in the evaluation of hyponatraemia (SIADH vs other causes), hypernatraemia and diabetes insipidus, oliguria in AKI (pre-renal vs ATN), polyuria workup, and monitoring of the renal response to desmopressin (DDAVP) in the water deprivation test. Always interpret urine osmolality alongside plasma osmolality, clinical volume status, and serum sodium for a complete picture.
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Формула
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Calculated Uosm = 2 × (UNa + UK) + UGlucose/18 + UUrea/2.8 (all in mg/dL for glucose and urea; Na and K in mmol/L)Описание переменных
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| Символ | Имя | Единица | Описание |
|---|---|---|---|
| UNa | Urine Sodium | mmol/L | Major cation in urine; paired with chloride to contribute the largest portion of urine osmolality in normal conditions. |
| UK | Urine Potassium | mmol/L | Second major cation in urine; its contribution becomes significant in states of high aldosterone activity or potassium loading. |
| UGlucose | Urine Glucose | mg/dL | Normally absent in urine (threshold ~180 mg/dL plasma glucose). In glycosuria, glucose adds significantly to measured Uosm (each 180 mg/dL = approximately 10 mOsm/kg). |
| UUrea | Urine Urea | mg/dL | A major non-electrolyte contributor to urine osmolality, especially during protein catabolism or high protein intake. Urea recycling in the medulla is critical for the countercurrent concentration mechanism. |
| Uosm | Urine Osmolality | mOsm/kg | Total solute concentration in urine per kg of water. Measured by freezing point depression (gold standard) or calculated from the formula. Normal range is 50–1400 mOsm/kg depending on hydration state. |
Как Urine Osmolality Calculator
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- 1Measured urine osmolality is determined by freezing point depression osmometry in the laboratory — the most accurate method, preferred over calculation in clinical practice.
- 2Calculated urine osmolality uses: 2 × (UNa + UK) [from electrolytes] + UGlucose/18 [converts mg/dL to mmol/L] + UUrea/2.8 [converts mg/dL to mmol/L].
- 3The factor '2' before UNa + UK accounts for the accompanying anions (chloride and bicarbonate) that maintain electrical neutrality — each cation is paired with an anion, doubling the particle count.
- 4Interpret against plasma osmolality (normal 280–295 mOsm/kg): if urine osmolality is higher than plasma, the kidney is concentrating urine appropriately; if lower, the kidney is diluting.
- 5A urine osmolality >800 mOsm/kg with oliguria indicates maximal renal water conservation — consistent with pre-renal azotaemia or physiological response to dehydration.
- 6A urine osmolality <300 mOsm/kg with hypo-osmolar plasma strongly suggests diabetes insipidus (central or nephrogenic) — the kidney cannot concentrate despite low body water.
- 7In SIADH, urine osmolality is inappropriately high (>100 mOsm/kg, often >300) relative to a low serum osmolality — the hallmark diagnostic criterion.
Решённые примеры
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High Uosm with low UNa and oliguria supports pre-renal AKI. Measured osmolality likely >500 mOsm/kg.
The kidneys are responding normally to dehydration: maximal ADH release causes water reabsorption in the collecting duct, concentrating the urine. Urea excretion contributes substantially to osmolality here. IV fluid resuscitation should restore urine output and normalise osmolality.
Uosm >100 mOsm/kg (and especially >plasma Osm) with serum hypo-osmolality fulfils the diagnostic criterion for SIADH.
In SIADH, ADH is secreted autonomously (often by ectopic tumour or CNS cause), forcing the kidney to concentrate urine regardless of serum osmolality. The diagnosis of SIADH requires: hypo-osmolality, inappropriately concentrated urine, euvolaemia, normal adrenal and thyroid function, and absence of diuretics.
Uosm <100 mOsm/kg with high serum Na and polyuria confirms failure to concentrate urine — central or nephrogenic DI.
Central DI results from ADH deficiency (posterior pituitary or hypothalamic damage). Administration of DDAVP (desmopressin) will raise Uosm to >300 mOsm/kg in central DI but will have no effect in nephrogenic DI — this is the basis of the desmopressin stimulation test.
Uosm 270–300 mOsm/kg (isosthenuria) with oliguria is the pattern of ATN — the tubules cannot concentrate or dilute urine.
Damaged tubular cells lose both their concentrating and diluting ability, producing urine close to plasma osmolality. Combined with high urine sodium and low urine/plasma creatinine ratio, this confirms ATN. Renal support may be needed.
Практическое применение
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Hyponatraemia workup: distinguishing SIADH (Uosm >plasma Osm) from primary polydipsia (Uosm <100) and hypovolaemic states — the first test ordered in any hyponatraemic patient evaluation., where accurate urine osmolality analysis through the Urine Osmolality supports evidence-based decision-making and quantitative rigor in professional workflows
Diabetes insipidus diagnosis: the water deprivation test relies entirely on serial urine osmolality measurements to confirm DI and distinguish central from nephrogenic forms using DDAVP challenge., where accurate urine osmolality analysis through the Urine Osmolality supports evidence-based decision-making and quantitative rigor in professional workflows
AKI differentiation: Uosm >500 mOsm/kg with oliguria strongly suggests pre-renal azotaemia; isosthenuria (~285 mOsm/kg) with oliguria suggests ATN — used alongside FENa and urine microscopy., where accurate urine osmolality analysis through the Urine Osmolality supports evidence-based decision-making and quantitative rigor in professional workflows
Monitoring desmopressin therapy: in patients with central DI on DDAVP, serial Uosm confirms adequate treatment (target >600 mOsm/kg) and guides dose titration., where accurate urine osmolality analysis through the Urine Osmolality supports evidence-based decision-making and quantitative rigor in professional workflows
Polyuria investigation: a 24-hour urine osmolality and volume allows calculation of daily osmolar excretion, classifying polyuria as water diuresis (Uosm <250), solute diuresis (Uosm >300 with high volume), or mixed.
Особые случаи
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SIADH vs Cerebral Salt Wasting
Both SIADH and cerebral salt wasting (CSW) present with hyponatraemia and an inappropriately high urine osmolality (>plasma Osm), making them difficult to distinguish on Uosm alone. The critical distinguishing feature is volume status: SIADH patients are euvolaemic with normal or low urine sodium; CSW patients are hypovolaemic (often with brain injury or subarachnoid haemorrhage) and have high urine sodium due to natriuresis. The treatment is opposite: SIADH requires fluid restriction; CSW requires fluid and sodium replacement. An error in direction can be dangerous.
Urine Osmolality in Hyperglycaemia
In poorly controlled diabetes mellitus, glucosuria dramatically elevates measured urine osmolality due to glucose's osmotic contribution (each 180 mg/dL of glucose adds approximately 10 mOsm/kg). This can make the urine appear 'concentrated' even when tubular concentrating ability is impaired. Always account for the glucosuria contribution (UGlucose/18) when interpreting Uosm in diabetic patients, or use the calculated Uosm excluding glucose to isolate tubular function.
Recovery Phase of ATN — Post-ATN Diuresis
As tubular cells regenerate after ATN, urine output increases dramatically (polyuric phase) but the new tubular cells cannot yet concentrate urine fully. Uosm during recovery is typically 200–350 mOsm/kg despite high urine volumes. This can cause massive free water and electrolyte losses. Careful monitoring and replacement of urine losses (particularly sodium and potassium) is essential to avoid secondary hypernatraemia or hypokalaemia during this phase.
Lithium-Induced Nephrogenic DI
Lithium is the most common drug cause of chronic nephrogenic DI. It blocks aquaporin-2 (AQP2) water channels in the collecting duct, impairing ADH-mediated water reabsorption. Patients develop persistent polyuria and polydipsia with Uosm typically <400 mOsm/kg. Unlike central DI, this does not respond adequately to DDAVP. Amiloride reduces lithium uptake into tubular cells and partially restores concentrating ability. Long-term lithium use can cause permanent concentrating defects even after discontinuation.
Mannitol and Contrast Agents
Mannitol and iodinated contrast agents are large osmotically active molecules excreted in the urine. They dramatically raise both measured urine osmolality and specific gravity without reflecting true tubular function. If Uosm is used to assess pre-renal vs ATN distinction (e.g., via urine/plasma osmolality ratio) in a patient who received mannitol or contrast, results will be misleadingly high. FEUrea or FENa are better indices in this scenario, as they are not affected by these agents.
Urine Osmolality Interpretation Guide
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| Uosm (mOsm/kg) | Clinical Meaning | Common Causes |
|---|---|---|
| > 800 | Maximally concentrated — renal water conservation | Dehydration, pre-renal AKI, physiological response to ADH |
| 500 – 800 | Moderately concentrated | Normal under mild fluid restriction; appropriate ADH response |
| 300 – 500 | Mildly concentrated to borderline | Mild dehydration, early renal impairment, transitional state |
| 280 – 300 | Isosthenuria (equals plasma) | ATN, advanced CKD, severe tubular dysfunction |
| 100 – 280 | Dilute but not maximal | Primary polydipsia, partial DI, early nephrogenic DI |
| < 100 | Maximally dilute — water diuresis | Complete central or nephrogenic DI, psychogenic polydipsia, post-obstructive diuresis |
Часто задаваемые вопросы
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Why is measured osmolality preferred over calculated?
Measured osmolality by freezing point depression captures all solutes, including those not in the standard formula (e.g., mannitol, contrast agents, NH4+, other organic solutes). The calculated formula only estimates the contribution of Na, K, glucose, and urea. In clinical practice — especially in the ICU or in polyuria workup — measured Uosm is always preferred. The calculated value is useful when measured Uosm is unavailable.
What is isosthenuria and what does it indicate?
Isosthenuria is urine osmolality approximately equal to plasma osmolality (280–300 mOsm/kg). It indicates loss of tubular concentrating and diluting ability. It is the hallmark of advanced tubular dysfunction seen in ATN, severe CKD, and other forms of intrinsic renal injury. Isosthenuric urine in an oliguric patient strongly suggests ATN rather than pre-renal disease.
What is the normal urine osmolality range?
Urine osmolality varies widely with water intake and physiological state. After overnight fasting and without excess water intake, it is typically 300–900 mOsm/kg in healthy adults. The minimum (maximum dilution) is ~50 mOsm/kg during a water load, and the maximum (maximum concentration) is 800–1400 mOsm/kg during dehydration. A random urine osmolality of >600 mOsm/kg generally indicates intact concentrating ability.
How is urine osmolality used in the water deprivation test?
In the water deprivation test (used to diagnose diabetes insipidus), the patient is deprived of fluid until plasma osmolality rises above 295 mOsm/kg or serum Na exceeds 145 mEq/L. Urine osmolality is measured hourly. A maximum Uosm <300 mOsm/kg despite hypernatraemia confirms DI. DDAVP is then given: if Uosm rises >50% (typically >750 mOsm/kg), central DI is confirmed; if no response, nephrogenic DI is diagnosed.
Can urine osmolality diagnose SIADH alone?
No. SIADH is a clinical diagnosis requiring all of: (1) serum hypo-osmolality (<275 mOsm/kg), (2) inappropriately concentrated urine (Uosm >100 mOsm/kg, usually >plasma Osm), (3) clinical euvolaemia, (4) elevated urine sodium (>40 mEq/L), (5) normal renal, adrenal, and thyroid function, and (6) absence of diuretics. An elevated Uosm alone does not diagnose SIADH — it must be interpreted in the context of low plasma osmolality and euvolaemia.
Why does urine osmolality differ from urine specific gravity?
Specific gravity measures the density of urine relative to water and is influenced disproportionately by large molecules (glucose, protein, contrast agents, dextran). A patient with heavy glycosuria may have a high specific gravity (1.030) but a normal or only mildly elevated osmolality. Osmolality measures only the number of particles, not their mass. For accurate assessment of tubular concentrating ability, osmolality is far superior to specific gravity.
What is the urine-to-plasma osmolality ratio?
The urine-to-plasma osmolality ratio (U/P Osm) is a simple clinical tool: a ratio >1.5 suggests appropriate concentration (pre-renal or physiological response); a ratio close to 1 suggests isosthenuria (ATN or severe CKD); a ratio <1 suggests dilute urine (water diuresis, DI, or recovery from ATN). It is used alongside FENa and clinical context in AKI evaluation.
How does nephrogenic DI differ from central DI on urine osmolality?
In both central and nephrogenic DI, urine osmolality is inappropriately low (<300 mOsm/kg) in the face of high serum osmolality. The key distinction is the response to DDAVP: in central DI (ADH deficiency), DDAVP causes a >50% rise in Uosm (tubules are intact and respond to exogenous ADH). In nephrogenic DI (ADH resistance), Uosm does not rise significantly because the tubules are insensitive to ADH regardless of the source. Lithium and demeclocycline are classic drug causes of nephrogenic DI.
Распространённые ошибки
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- !Using urine specific gravity as a proxy for osmolality in the presence of glucose, protein, or contrast — specific gravity can be falsely high while true osmolality is normal; use a laboratory osmolality measurement instead.
- !Diagnosing SIADH based on high Uosm alone without confirming low serum osmolality, euvolaemia, and normal adrenal/thyroid function — Uosm >plasma Osm is necessary but not sufficient for SIADH.
- !Ignoring that Uosm can be high in pre-renal AKI but also in SIADH — context (volume status, serum Na, serum Osm) is essential to distinguish the two.
- !Not accounting for glucose or mannitol when interpreting Uosm — glucosuria raises measured Uosm substantially, potentially masking underlying tubular dysfunction.
- !Misinterpreting isosthenuria as a normal finding — Uosm equal to plasma osmolality in an oliguric or polyuric patient is always abnormal and reflects tubular dysfunction.
- !Using a random urine sample without noting fluid intake — Uosm varies widely over the day; a first-morning void after overnight fasting is the most reproducible sample for assessing maximal concentrating ability.
Совет профессионала
In the workup of hyponatraemia, the urine sodium AND urine osmolality together define the aetiology far better than either alone. The classic SIADH pattern is Uosm >100 mOsm/kg (usually >plasma Osm) + UNa >40 mEq/L in a euvolaemic hyponatraemic patient. If Uosm <100 mOsm/kg, SIADH is essentially excluded — the hyponatraemia is from excessive free water intake (primary polydipsia).
Знаете ли вы?
The inner medulla of the kidney achieves its extraordinarily high osmolality gradient (up to 1200 mOsm/kg in humans, and up to 9000 mOsm/kg in some desert rodents like the kangaroo rat) through the countercurrent multiplication system. This gradient was only fully elucidated by Wirz, Hargitay, and Kuhn in 1951 — a discovery that revolutionised understanding of how the kidney can produce urine vastly more concentrated than plasma without violating the second law of thermodynamics.
Regional Guides
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Источники
- ›Spasovski G et al. — Clinical practice guideline on diagnosis and treatment of hyponatraemia. Eur J Endocrinol 2014
- ›Fenske W, Allolio B — Clinical review: Current state and future perspectives in the diagnosis of DI. J Clin Endocrinol Metab 2012
- ›UpToDate — Evaluation of patients with polyuria
- ›Rose BD, Post TW — Clinical Physiology of Acid-Base and Electrolyte Disorders, 5th Ed. McGraw-Hill, 2001
- ›KDIGO AKI Guidelines 2012 — Diagnosis and evaluation of AKI
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