Delisle to Rankine Converter

Convert degrees Delisle to degrees Rankine with our free online temperature converter.

Quick Answer

1 Delisle = 670.47 degrees Rankine

Formula: Delisle × conversion factor = Rankine

Use the calculator below for instant, accurate conversions.

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Last verified: February 2026Reviewed by: Sam Mathew, Software Engineer

Delisle to Rankine Calculator

How to Use the Delisle to Rankine Calculator:

  1. Enter the value you want to convert in the 'From' field (Delisle).
  2. The converted value in Rankine will appear automatically in the 'To' field.
  3. Use the dropdown menus to select different units within the Temperature category.
  4. Click the swap button (⇌) to reverse the conversion direction.
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How to Convert Delisle to Rankine: Step-by-Step Guide

Temperature conversions like Delisle to Rankine use specific non-linear formulas.

Formula:

First convert °De to °C: °C = 100 - °De × 2/3. Then convert °C to °R: °R = (°C + 273.15) × 9/5

Example Calculation:

Convert 10°De:
1. °C = 100 - (10 × 2/3) = 93.33°C
2. °R = (93.33 + 273.15) × 9/5 = 659.7°R

Disclaimer: For Reference Only

These conversion results are provided for informational purposes only. While we strive for accuracy, we make no guarantees regarding the precision of these results, especially for conversions involving extremely large or small numbers which may be subject to the inherent limitations of standard computer floating-point arithmetic.

Not for professional use. Results should be verified before use in any critical application. View our Terms of Service for more information.

What is a Delisle and a Rankine?

The Delisle scale (symbol: °De or °D) is an inverted temperature scale that divides the interval between the boiling point and freezing point of water into 150 equal divisions under standard atmospheric pressure, with numerical values decreasing as temperature increases.

Scale Calibration (Inverted)

Fixed Points:

  • Boiling point of water: 0 degrees Delisle (0°De) - the ZERO reference
  • Freezing point of water: 150 degrees Delisle (150°De) - 150° higher than boiling
  • Degree size: Each Delisle degree = 2/3 Celsius degree (or 0.667°C)

The Inversion: Unlike Celsius, Fahrenheit, Réaumur, and Kelvin, which all increase with temperature:

  • Hotter temperatures = LOWER Delisle numbers (approaching 0°De)
  • Colder temperatures = HIGHER Delisle numbers (above 150°De)
  • Temperature increases = Delisle decreases

Mathematical Relationships

Delisle to Celsius:

  • °C = 100 - (°De × 2/3)
  • Or: °C = 100 - (°De ÷ 1.5)

Celsius to Delisle:

  • °De = (100 - °C) × 3/2
  • Or: °De = (100 - °C) × 1.5

Delisle to Fahrenheit:

  • °F = 212 - (°De × 6/5)
  • Or: °F = 212 - (°De × 1.2)

Examples:

  • 0°De = 100°C (boiling water)
  • 75°De = 50°C (halfway between boiling and freezing)
  • 150°De = 0°C (freezing water)
  • 300°De = -100°C (extreme cold, -148°F)

Why 150 Degrees?

Delisle chose 150 degrees for the freezing point due to:

  1. Mercury contraction observation: His mercury thermometers showed 150 units of contraction between boiling and freezing
  2. Divisibility: 150 = 2 × 3 × 5², offering factors (2, 3, 5, 6, 10, 15, 25, 30, 50, 75, 150)
  3. Convenient fractional divisions: 150/3 = 50°, 150/2 = 75°, 150/10 = 15° for practical measurements
  4. Empirical basis: Based on actual instrument behavior rather than abstract decimal preference

Why Invert the Scale?

Delisle's inversion was methodological rather than arbitrary:

Calibration Process:

  • Started with boiling water (100°C) as reference point zero
  • Observed mercury column contraction as water cooled
  • Counted degrees of contraction downward from boiling
  • At freezing point (0°C), mercury had contracted 150 divisions

Result: A scale that measured "degrees of cooling" from boiling, making hotter temperatures numerically smaller. While counterintuitive by modern standards, it reflected the experimental process.

What Is the Rankine Scale?

The Rankine scale (symbol: °R or °Ra) is an absolute thermodynamic temperature scale where:

  • Zero point: Absolute zero (0 °R = −459.67 °F), the theoretical lowest possible temperature where all molecular kinetic energy ceases
  • Degree size: Equal to Fahrenheit degrees (1 °R increment = 1 °F increment)
  • Named after: William John Macquorn Rankine (1820-1872), Scottish engineer and physicist

Absolute Temperature Scales

An absolute temperature scale begins at absolute zero rather than an arbitrary freezing point:

Absolute scales (start at absolute zero):

  • Kelvin (K): Uses Celsius-sized degrees, 0 K = absolute zero, used worldwide in science
  • Rankine (°R): Uses Fahrenheit-sized degrees, 0 °R = absolute zero, used in some U.S. engineering

Relative scales (start at arbitrary points):

  • Celsius (°C): 0 °C = water's freezing point (at standard pressure)
  • Fahrenheit (°F): 0 °F = freezing point of brine solution, 32 °F = water's freezing point

Why Absolute Scales Matter

Many fundamental physics equations require absolute temperatures because ratios and products become meaningful only when zero truly means "no thermal energy":

Ideal gas law: PV = nRT (T must be absolute) Carnot efficiency: η = 1 - T_cold/T_hot (requires absolute temperatures) Stefan-Boltzmann law: Power radiated ∝ T⁴ (absolute temperature to fourth power) Entropy calculations: ΔS = Q/T (T must be absolute to avoid division by zero)

Using relative scales (Fahrenheit, Celsius) in these equations produces nonsensical results. Absolute scales (Rankine, Kelvin) make the mathematics work correctly.

Official Definition

1 degree Rankine = 1 degree Fahrenheit (in size)

Relationship to Fahrenheit: °R = °F + 459.67

Relationship to Kelvin: °R = K × 9/5 (or °R = K × 1.8)

Relationship to Celsius: °R = (°C + 273.15) × 9/5


Note: The Delisle is part of the imperial/US customary system, primarily used in the US, UK, and Canada for everyday measurements. The Rankine belongs to the imperial/US customary system.

History of the Delisle and Rankine

The Delisle scale's 290-year history is inseparable from the development of Russian science and the Imperial Academy's early years.

Joseph-Nicolas Delisle (1688-1768)

Born in Paris to artistic parents, Delisle became one of France's leading astronomers, specializing in celestial mechanics and cartography. His work on planetary transits and lunar theory earned him election to the French Academy of Sciences (1714) and international recognition.

1725: Invitation to Russia

Tsar Peter the Great, determined to modernize Russia through Western science, invited Delisle to St. Petersburg to establish an astronomical observatory and help found the Imperial Russian Academy of Sciences. Delisle arrived in St. Petersburg in August 1725, months after Peter's death, but Empress Catherine I honored the invitation.

1725-1747: Russian Academy Directorship

As the Academy's first director of astronomy, Delisle:

  • Established St. Petersburg Observatory (1726)
  • Trained Russian astronomers and instrument makers
  • Standardized scientific measurements across the Russian Empire
  • Corresponded with European scientific societies

Creation of the Delisle Scale (1732)

The Problem: Russia's vast territory and extreme climate variations required standardized temperature measurements for meteorology, agriculture, and scientific research. Existing thermometers used inconsistent scales, making comparison impossible.

Delisle's Solution (1732):

  1. Boiling water reference: Started with boiling point as 0° (easiest to reproduce reliably)
  2. Mercury contraction: Observed mercury column shrinking as temperature decreased
  3. Freezing point calibration: Marked freezing water at 150° of contraction
  4. Uniform divisions: Divided the interval into 150 equal degrees

1732 Paper: Delisle presented his scale to the Imperial Russian Academy, arguing that starting from boiling point provided greater calibration accuracy than starting from freezing (where ice-water mixtures could vary slightly).

Official Adoption in Russia (1738-1840s)

1738: Imperial Decree

The Russian Imperial government officially adopted the Delisle scale for all government and scientific purposes, making Russia the first nation to standardize on a single temperature scale nationwide.

Implementation:

  • Meteorological stations: All Russian weather observation posts used Delisle thermometers
  • Scientific research: Academy publications reported temperatures in Delisle
  • Military applications: Army and Navy used Delisle for weather reporting
  • Educational institutions: Russian universities taught Delisle as standard

Geographic Spread: The scale's use extended across the Russian Empire:

  • St. Petersburg and Moscow (primary centers)
  • Baltic provinces (Estonia, Latvia, Lithuania)
  • Siberian outposts and exploration expeditions
  • Crimea and southern territories

Coexistence with Réaumur (1780s-1840s)

By the late 18th century, Western European science had largely standardized on Réaumur (continental Europe) or Fahrenheit (Britain), creating communication challenges for Russian scientists.

1780s-1820s: Gradual Transition

Russian instrument makers began producing dual-scale thermometers (Delisle/Réaumur) to facilitate:

  • International scientific correspondence
  • Translation of Western European research
  • Trade with European partners

1840s: Réaumur Dominance

By the 1840s, Réaumur had effectively replaced Delisle in Russian scientific practice:

  • Younger Russian scientists trained with Réaumur
  • International standardization pressure increased
  • French scientific influence (Réaumur) outweighed earlier German connections

Final Decline (1850-1917)

1850-1870: Delisle relegated to historical archives, antique thermometers, and elderly scientists' habit 1871: German unification's adoption of Celsius influenced Russian scientific circles 1900-1917: Celsius gaining ground in Russian universities and research institutions 1917-1925: Bolshevik Revolution brought metric system adoption, officially ending Delisle use

Legacy and Modern Recognition

The Delisle scale survives as:

  • Historical curiosity: The only inverted scale to achieve governmental adoption
  • Archival research: Russian meteorological data (1738-1840s) requires Delisle conversion
  • Thermometer collecting: Delisle/Réaumur dual-scale antique thermometers from Russia
  • Scientific history: Example of how methodology (cooling observation) shaped measurement design

William John Macquorn Rankine (1820-1872)

William Rankine was a Scottish engineer, physicist, and professor at the University of Glasgow who made foundational contributions to thermodynamics, civil engineering, and molecular physics.

Key contributions:

  • Formulated the Rankine cycle (1859), describing the ideal thermodynamic cycle for steam engines
  • Developed the Rankine temperature scale (1859) as an absolute scale compatible with Fahrenheit
  • Wrote influential textbooks on applied mechanics, steam engines, and civil engineering
  • Co-founded the science of thermodynamics alongside Carnot, Clausius, Kelvin, and Joule

Rankine was a contemporary and correspondent of William Thomson (Lord Kelvin), who proposed the Kelvin absolute scale in 1848. The two scientists worked on similar thermodynamic problems but approached them from different engineering traditions—Kelvin from metric/Celsius contexts, Rankine from British imperial/Fahrenheit contexts.

The Need for an Absolute Scale (1840s-1850s)

The mid-19th century saw rapid developments in thermodynamics driven by the Industrial Revolution's reliance on steam engines:

Carnot's theorem (1824): Sadi Carnot demonstrated that heat engine efficiency depends on the temperature ratio between hot and cold reservoirs, implicitly requiring an absolute temperature scale

Joule's mechanical equivalent of heat (1843-1850): James Prescott Joule established that heat and mechanical work are interconvertible, laying foundations for the first law of thermodynamics

Thomson's (Kelvin's) absolute scale (1848): William Thomson proposed an absolute scale based on Carnot's theorem, using Celsius degree increments, with zero at −273.15 °C

These developments made clear that thermodynamic calculations required absolute temperature measurements, but Thomson's Kelvin scale was impractical for British and American engineers who worked exclusively in Fahrenheit.

Rankine's Proposal (1859)

In 1859, Rankine published his absolute temperature scale in engineering papers, presenting it as the practical solution for engineers who needed absolute temperatures but worked in imperial units:

Rankine's logic:

  1. Thermodynamic calculations require absolute zero as the baseline
  2. British and American engineers measure temperature in Fahrenheit
  3. Constantly converting Fahrenheit ↔ Celsius ↔ Kelvin introduces errors and inefficiency
  4. An absolute scale with Fahrenheit-sized degrees solves the problem elegantly

The result: 0 °R = absolute zero (−459.67 °F), with degree increments matching Fahrenheit

This allowed engineers to use familiar Fahrenheit measurements while accessing the mathematical benefits of absolute temperature.

Adoption in Engineering (1860s-1960s)

The Rankine scale became standard in British and American engineering disciplines throughout the late 19th and first half of the 20th centuries:

Steam engineering: Rankine cycle analysis (for steam turbines, power plants) used Rankine temperatures for efficiency calculations

ASME standards: The American Society of Mechanical Engineers incorporated Rankine into standard tables for steam properties, refrigeration cycles, and combustion calculations

Aerospace engineering: Early rocket and jet engine development (1940s-1960s) used Rankine for combustion chamber and exhaust nozzle temperature calculations

Cryogenics: Liquefied gas industries (oxygen, nitrogen, hydrogen) used Rankine when working with U.S. measurement systems

Thermodynamics textbooks: Engineering thermodynamics texts published in the U.S. and U.K. through the 1960s routinely presented equations in both Kelvin and Rankine

Decline and Modern Usage (1960s-Present)

Several factors led to Rankine's decline:

International metrication (1960s-1980s): Most countries adopted SI units (including Kelvin), making Rankine unnecessary outside the United States

Scientific standardization: The global scientific community standardized on Kelvin, making it the universal absolute scale for research and international collaboration

U.S. engineering education shift: Even American engineering programs increasingly taught Kelvin as the primary absolute scale, relegating Rankine to historical footnotes

Computing and automation: Modern engineering software typically works in SI units (Kelvin), reducing incentive to maintain Rankine compatibility

Where Rankine Survives Today

Despite its decline, Rankine persists in specific niches:

American aerospace engineering: NASA and aerospace contractors occasionally use Rankine in rocket propulsion calculations when working with U.S. customary units (pounds-force, BTU, etc.)

Cryogenic engineering: Liquefied natural gas (LNG) facilities and industrial gas companies in the U.S. may use Rankine for process calculations

Legacy documentation: Older engineering manuals, equipment specifications, and technical standards still reference Rankine, requiring continued familiarity

Thermodynamics education: Some U.S. engineering thermodynamics courses teach Rankine alongside Kelvin to demonstrate absolute temperature concepts with Fahrenheit context

Historical research: Engineers and historians studying 19th-20th century technology encounter Rankine in original documents and must understand conversions


Common Uses and Applications: degrees Delisle vs degrees Rankine

Explore the typical applications for both Delisle (imperial/US) and Rankine (imperial/US) to understand their common contexts.

Common Uses for degrees Delisle

Historical Russian Meteorology (1738-1840s)

The primary application of the Delisle scale was Russian weather observation:

Imperial Meteorological Network:

  • St. Petersburg Observatory: Daily temperatures recorded in Delisle
  • Moscow weather stations: Imperial Academy network standardized on Delisle
  • Siberian frontier posts: Military expeditions reported temperatures in Delisle
  • Black Sea and Baltic ports: Naval meteorological data in Delisle

Record Keeping: Archives from this period contain:

  • Handwritten logbooks with Delisle readings
  • Published annual weather summaries
  • Agricultural yield correlations with Delisle temperatures
  • Military campaign weather reports (e.g., Napoleon's 1812 invasion)

18th-Century Russian Scientific Research

Russian Academy scientists used Delisle for:

Physics Experiments:

  • Thermal expansion studies
  • Phase transition research (freezing, melting, boiling)
  • Instrument calibration standards

Biological Research:

  • Plant growth temperature requirements
  • Animal physiology studies
  • Seed germination experiments

Astronomical Observations:

  • Observatory temperature logs (affecting telescope precision)
  • Atmospheric refraction corrections based on temperature

Historical Document Interpretation

Modern researchers encounter Delisle in:

Russian Imperial Archives:

  • Government reports (1738-1840s)
  • Military campaign records
  • Agricultural survey data
  • Medical records from Russian hospitals

Scientific Publications:

  • Imperial Russian Academy journals
  • European scientific correspondence with Russian researchers
  • Exploration expedition reports (Bering, Kamchatka expeditions)

Literature and Personal Correspondence:

  • Letters between Russian aristocracy
  • Travel journals of European visitors to Russia
  • Historical novels set in 18th-19th century Russia

Antique Thermometer Collecting

Delisle thermometers are rare and valuable collectibles:

Rarity Factors:

  • Limited production period: 1732-1850s primarily
  • Geographic concentration: Almost exclusively Russian Empire
  • Destruction: Many lost during Russian Revolution, World Wars
  • Dual-scale models: Delisle/Réaumur thermometers from 1780s-1840s most sought

Market Value:

  • Original Delisle thermometers: $1,000-$10,000+ (extreme rarity)
  • Dual-scale Delisle/Réaumur: $800-$5,000 (more common)
  • Reproductions/modern curiosities: $50-$200

Education and Science Museums

Science museums use Delisle thermometers to teach:

  • History of measurement: Evolution of temperature scales
  • Scientific methodology: How observation shapes measurement design
  • Cultural context: Russian Empire's scientific development
  • Inverted scales: Challenging students' assumptions about "hotter = higher number"

Online Temperature Converters

Delisle appears in comprehensive temperature conversion tools:

  • Historical conversion calculators for archival research
  • "Exotic scales" demonstrations alongside Rømer, Newton scales
  • Educational tools teaching temperature scale diversity

When to Use degrees Rankine

1. Thermodynamic Cycle Analysis

Engineers analyzing heat engines and refrigeration cycles use Rankine when working in U.S. customary units:

Carnot efficiency calculation: η = 1 - T_cold/T_hot

Example (using Rankine for compatibility with imperial units):

  • Hot reservoir: 1160 °R (700 °F, combustion chamber)
  • Cold reservoir: 540 °R (80 °F, ambient air)
  • Maximum efficiency: η = 1 - 540/1160 = 1 - 0.465 = 53.5%

If you incorrectly used Fahrenheit (relative scale) instead: η = 1 - 80/700 = 88.6% ← Wrong! (impossibly high)

Rankine (absolute scale) gives the correct physical result.

Ideal gas law (PV = nRT): Requires absolute temperature T in Rankine or Kelvin Refrigeration coefficient of performance: COP = T_cold/(T_hot - T_cold), requires absolute T Entropy change: ΔS = Q/T, requires absolute T

2. Aerospace and Rocket Propulsion

NASA and aerospace contractors sometimes use Rankine in rocket engine calculations when working entirely in imperial units:

Rocket nozzle expansion:

  • Combustion chamber temperature: 6000 °R (5540 °F, liquid hydrogen/oxygen combustion)
  • Nozzle exit temperature: 1500 °R (1040 °F, after expansion)
  • Temperature ratio used in thrust calculations: 1500/6000 = 0.25

Specific impulse calculations: Rocket performance metrics sometimes expressed in U.S. units (pounds-force, BTU, Rankine)

Reentry heating analysis: Atmospheric friction temperatures calculated in Rankine for Space Shuttle and Apollo programs

3. Cryogenic and Liquefied Gas Engineering

Engineers working with liquefied natural gas (LNG), liquid nitrogen, or liquid oxygen may use Rankine in American industrial contexts:

LNG storage:

  • Methane boiling point: 201.1 °R (−258.6 °F, 111.7 K)
  • Storage tank insulation must maintain temperatures below 210 °R

Nitrogen liquefaction: Process temperatures from ambient (528 °R) down to liquid nitrogen (140 °R)

Oxygen separation: Cryogenic air separation units cool air from 520 °R to 163 °R (oxygen boiling point)

4. Steam Power and HVAC Engineering

Historical and some modern steam system calculations use Rankine:

Steam turbine efficiency: Calculating ideal Rankine cycle efficiency for power plants Boiler performance: Heat transfer calculations involving steam temperatures in Rankine HVAC refrigeration cycles: Coefficient of performance calculations requiring absolute temperatures

5. Combustion and Internal Combustion Engines

Engine designers analyzing combustion processes may use Rankine when working in U.S. units:

Compression ratio effects: Calculating temperature rise during compression stroke Exhaust temperatures: Modeling exhaust gas temperatures for turbocharger design Flame temperatures: Analyzing combustion chamber temperatures in Rankine for compatibility with BTU energy units

6. Materials Science and Heat Treatment

Metallurgists and materials engineers working with U.S. specifications:

Heat treatment processes: Tempering, annealing, and hardening temperatures sometimes specified in Rankine in older American standards Thermal expansion: Calculating expansion coefficients with temperature in Rankine Phase transitions: Melting and solidification temperatures in absolute scale for thermodynamic calculations

7. Historical Engineering and Technical Documentation

Engineers working with legacy systems, historical restoration, or archival research:

Old ASME standards: Early 20th century steam tables and equipment specifications used Rankine Vintage aviation: WWII and early jet age aircraft engine documentation may use Rankine Technical history: Understanding historical engineering achievements requires Rankine fluency


Additional Unit Information

About Delisle (°De)

What are the freezing and boiling points of water in Delisle?

Water boils at 0°De and freezes at 150°De. This is inverted compared to all other major temperature scales (Celsius, Fahrenheit, Réaumur, Kelvin), where higher numbers indicate hotter temperatures.

Why does the Delisle scale decrease with increasing temperature?

Delisle's methodology determined the scale's direction:

  1. Calibration process: He started with boiling water (100°C) as his zero reference point
  2. Cooling observation: He watched mercury contract as water cooled from boiling
  3. Counting contraction: Each unit of contraction represented one Delisle degree
  4. Result: At freezing point, the mercury had contracted 150 divisions from boiling

The scale thus measured "degrees of cooling" from boiling water, making hotter temperatures numerically smaller. While counterintuitive, it reflected his experimental procedure.

How does Delisle relate to Celsius?

Conversion formulas:

  • Delisle → Celsius: °C = 100 - (°De × 2/3)
  • Celsius → Delisle: °De = (100 - °C) × 1.5

Relationship: Each Delisle degree = 2/3 Celsius degree (0.667°C), but running in opposite direction.

Example:

  • 0°De = 100°C (boiling)
  • 150°De = 0°C (freezing)
  • 75°De = 50°C (midpoint)

The "100 -" in the formula accounts for the inversion.

Was the Delisle scale ever widely used?

Yes, in Imperial Russia (1738-1840s):

The Delisle scale was the official temperature standard of the Russian Empire for approximately one century. It was mandatory for:

  • All government meteorological stations
  • Imperial Russian Academy scientific research
  • Military weather reporting
  • Educational institutions

Not widely used elsewhere: Aside from Russia, Delisle remained a curiosity. Western Europe used Réaumur or Fahrenheit; Delisle was essentially a Russian phenomenon.

Why didn't other countries adopt the Delisle scale?

Several factors limited adoption:

  1. Counterintuitive: The inversion (hotter = lower number) confused users
  2. Late arrival: By 1732, Fahrenheit (1714) and Réaumur (1730) were established
  3. Geographic isolation: Russia's distance from Western European scientific centers
  4. Communication barriers: Language and political isolation limited dissemination
  5. No compelling advantage: The inversion offered no practical benefit over conventional scales

The scale succeeded in Russia due to Delisle's position at the Imperial Academy and government decree, not scientific merit.

How do you convert a Delisle temperature to Fahrenheit?

Two-step method:

  1. Convert Delisle to Celsius: °C = 100 - (°De × 2/3)
  2. Convert Celsius to Fahrenheit: °F = (°C × 9/5) + 32

Direct formula: °F = 212 - (°De × 6/5) or °F = 212 - (°De × 1.2)

Example: 120°De (Russian "room temperature")

  • Step 1: °C = 100 - (120 × 2/3) = 100 - 80 = 20°C
  • Step 2: °F = (20 × 1.8) + 32 = 36 + 32 = 68°F

Direct: 212 - (120 × 1.2) = 212 - 144 = 68°F ✓

Can you still find Delisle thermometers?

Original antiques: Extremely rare and valuable

  • Russian-made Delisle thermometers (1738-1850): $1,000-$10,000+
  • Dual-scale Delisle/Réaumur (1780-1840): $800-$5,000
  • Most survive in Russian museums, private collections, or academic institutions

Modern reproductions: Very limited availability

  • Some specialty scientific instrument makers produce educational replicas
  • Mostly for museum exhibits or science education purposes
  • Generally not commercially available

Why so rare:

  • Short production period (≈110 years)
  • Limited geographic area (Russian Empire only)
  • Wars and revolutions destroyed many (1812, 1917, WWII)
  • Glass fragility means few survived intact

What does negative Delisle mean?

Negative Delisle = Above boiling point (>100°C):

Since 0°De = 100°C (boiling), temperatures above boiling would be negative:

  • -15°De = 110°C (230°F) - pressurized water
  • -30°De = 120°C (248°F) - autoclave sterilization
  • -150°De = 200°C (392°F) - hot oven

Rarely used: Delisle's original design focused on ambient and cooling temperatures. High-temperature applications were uncommon in 18th-century Russia, so negative Delisle values are virtually absent from historical records.

How do historians handle Russian weather data in Delisle?

Conversion workflow:

  1. Identify Delisle readings in archival documents (e.g., "180 градусов Делиля" = 180 degrees Delisle)
  2. Apply conversion formula: °C = 100 - (180 × 2/3) = 100 - 120 = -20°C
  3. Convert to Fahrenheit if needed: (-20 × 1.8) + 32 = -4°F
  4. Document both original and converted values for scholarly accuracy

Example from historical record:

  • Original: "Санкт-Петербург, 15 января 1740, 195°De" (St. Petersburg, January 15, 1740, 195°De)
  • Conversion: 100 - (195 × 2/3) = 100 - 130 = -30°C = -22°F (severe cold)

Why is Delisle important to the history of science?

Scientific significance:

  1. Methodological diversity: Demonstrates how experimental procedure shaped measurement design
  2. Governmental standardization: First empire-wide temperature scale adoption (1738)
  3. Cultural context: Reflects Russian Empire's scientific modernization under Peter the Great's legacy
  4. Measurement evolution: Shows the pre-standardization diversity of temperature scales
  5. Unique inversion: Only inverted scale to achieve widespread official use

Lessons:

  • Measurement standards require international consensus, not just local adoption
  • Intuitive design matters for widespread acceptance
  • Historical contingency (Delisle's Academy position) can temporarily override scientific merit

Are there any other inverted temperature scales?

No other major inverted scales achieved significant use.

Minor historical attempts:

  • Some early thermometers were calibrated from hot to cold simply due to construction methods
  • Individual scientists occasionally created personal inverted scales for specific experiments

Why Delisle is unique:

  • Only inverted scale adopted by a government (Imperial Russia, 1738)
  • Only inverted scale used for over a century
  • Only inverted scale with substantial archival presence

All other successful temperature scales (Fahrenheit, Celsius, Réaumur, Kelvin, Rankine) use conventional orientation where higher numbers = hotter.

About Rankine (°R)

What is absolute zero on the Rankine scale?

Answer: 0 °R (exactly)

Absolute zero is the lowest possible temperature, where all classical molecular motion ceases and a system has minimal quantum mechanical zero-point energy. On the Rankine scale, this is defined as exactly 0 °R.

Absolute zero in other scales:

  • Rankine: 0 °R (by definition)
  • Fahrenheit: −459.67 °F
  • Kelvin: 0 K (by definition)
  • Celsius: −273.15 °C

The Rankine scale, like Kelvin, is an absolute scale, meaning its zero point represents true zero thermal energy (in the classical thermodynamic sense), not an arbitrary freezing point like Celsius or Fahrenheit.

How does Rankine relate to Fahrenheit?

Answer: °R = °F + 459.67 (Rankine is Fahrenheit shifted to start at absolute zero)

The Rankine and Fahrenheit scales use identical degree sizes—a change of 1 °R equals a change of 1 °F. The only difference is where zero is placed:

  • Fahrenheit: 0 °F is the freezing point of a brine solution (arbitrary choice from 1724)
  • Rankine: 0 °R is absolute zero, the lowest possible temperature

Key reference points:

  • Absolute zero: −459.67 °F = 0 °R
  • Water freezes: 32 °F = 491.67 °R
  • Water boils: 212 °F = 671.67 °R
  • Room temperature: 68 °F = 527.67 °R

Temperature changes: Because degree sizes are equal, a temperature rise of 50 °F is also a rise of 50 °R.

How does Rankine relate to Kelvin?

Answer: °R = K × 9/5 (or K = °R × 5/9)

Rankine and Kelvin are both absolute scales (zero at absolute zero), but they use different degree sizes:

  • Kelvin: Uses Celsius-sized degrees
  • Rankine: Uses Fahrenheit-sized degrees (which are 9/5 the size of Celsius degrees)

Conversion formula: °R = K × 9/5 (or K × 1.8)

Examples:

  • 0 K = 0 °R (absolute zero aligns)
  • 273.15 K (water freezes) = 491.67 °R
  • 373.15 K (water boils) = 671.67 °R
  • 300 K (room temp) = 540 °R

No offset needed: Unlike Fahrenheit-Celsius (which requires both multiplication AND addition), Rankine-Kelvin only requires multiplication because both start at absolute zero.

Why was the Rankine scale created?

Answer: To provide an absolute temperature scale compatible with Fahrenheit for British and American engineers

William Rankine created the scale in 1859 to solve a practical problem:

The problem:

  • Thermodynamic calculations (heat engines, gas laws, entropy) require absolute temperatures
  • Lord Kelvin had created an absolute scale in 1848, but it used Celsius degree intervals
  • British and American engineers worked in Fahrenheit, not Celsius
  • Constantly converting Fahrenheit → Celsius → Kelvin was error-prone and inefficient

Rankine's solution:

  • Create an absolute scale (zero at absolute zero) using Fahrenheit-sized degrees
  • Result: Engineers could use familiar Fahrenheit measurements with the benefits of an absolute scale

Historical context: In the 19th and early 20th centuries, this was essential for steam engine design, refrigeration engineering, and thermodynamic analysis in imperial-unit countries.

Is the Rankine scale still used today?

Answer: Rarely—primarily in specialized American engineering contexts and legacy documentation

Rankine has largely been replaced by Kelvin in modern engineering and science, but persists in specific niches:

Where Rankine is still used:

  • American aerospace engineering: Some NASA and contractor calculations when working in U.S. customary units
  • Cryogenic engineering: U.S. liquefied gas industries (LNG, liquid nitrogen/oxygen)
  • Legacy documentation: Older ASME standards, vintage equipment manuals, historical references
  • Thermodynamics education: Some U.S. engineering courses teach both Rankine and Kelvin

Why it declined:

  • Global metrication (1960s onward) made Kelvin the international standard
  • Scientific community exclusively uses Kelvin
  • Modern engineering software typically works in SI units
  • International collaboration requires Kelvin for compatibility

Current status: Rankine is a "legacy unit" maintained primarily for continuity with older American engineering systems, not for new designs.

What are the key temperatures on the Rankine scale?

Answer: Important reference temperatures in Rankine:

| Physical Point | Rankine | Fahrenheit | Description | |----------------|---------|------------|-------------| | Absolute zero | 0 °R | −459.67 °F | Theoretical minimum temperature | | Liquid helium boils | 7.6 °R | −451.9 °F | Coldest commonly used cryogenic liquid | | Liquid nitrogen boils | 139.3 °R | −320.4 °F | Common cryogenic refrigerant | | Dry ice sublimes | 389.0 °R | −109.3 °F | Solid CO₂ turns directly to gas | | Water freezes | 491.67 °R | 32 °F | Ice point at standard pressure (exact) | | Room temperature | 527.67 °R | 68 °F | Typical comfortable indoor temp | | Human body | 558.27 °R | 98.6 °F | Normal body temperature | | Water boils | 671.67 °R | 212 °F | Boiling point at standard pressure (exact) |

Exact values: Water's freezing and boiling points are defined exactly in Fahrenheit (32 °F and 212 °F), so they're also exact in Rankine (491.67 °R and 671.67 °R).

How do I convert Rankine to Celsius?

Answer: °C = (°R × 5/9) − 273.15

Step-by-step process:

  1. Convert Rankine to Kelvin: K = °R × 5/9
  2. Convert Kelvin to Celsius: °C = K − 273.15

Combined formula: °C = (°R × 5/9) − 273.15

Examples:

  • 491.67 °R (water freezes) = (491.67 × 5/9) − 273.15 = 273.15 − 273.15 = 0 °C
  • 671.67 °R (water boils) = (671.67 × 5/9) − 273.15 = 373.15 − 273.15 = 100 °C
  • 527.67 °R (room temp) = (527.67 × 5/9) − 273.15 = 293.15 − 273.15 = 20 °C

Alternative method: First convert to Fahrenheit, then to Celsius:

  1. °F = °R − 459.67
  2. °C = (°F − 32) × 5/9

Both methods give the same result.

Can I use negative numbers in Rankine?

Answer: No—negative temperatures don't exist on the Rankine scale (or Kelvin)

Because Rankine is an absolute scale starting at absolute zero (0 °R), there are no temperatures below zero. Negative Rankine temperatures would represent temperatures colder than absolute zero, which is physically impossible according to thermodynamics.

Comparison to other scales:

  • Rankine/Kelvin (absolute): Only positive values (0 and up)
  • Fahrenheit/Celsius (relative): Can have negative values (arbitrary zero points)

Lowest possible temperature: 0 °R (absolute zero) = −459.67 °F = −273.15 °C = 0 K

Note on exotic physics: In specialized quantum systems, "negative absolute temperatures" can exist in a technical sense (inverted population distributions), but this is a quantum statistical mechanics concept unrelated to everyday thermodynamics, and still doesn''t produce Rankine values below zero in the conventional thermal sense.

What''s the difference between °R and °Ra symbols?

Answer: Both °R and °Ra represent Rankine; °R is more common in American usage

Symbol variations:

  • °R: Most common symbol in American engineering contexts
  • °Ra: Sometimes used to avoid confusion with other units (electrical resistance in ohms: Ω or R)
  • R (without degree symbol): Occasionally seen in older texts but discouraged

Current standard: Most modern references use °R (with degree symbol), matching the pattern of °F, °C, and K (though Kelvin dropped its degree symbol in 1968).

Avoiding confusion:

  • Electrical resistance: ohm (Ω), not R
  • Gas constant: R (universal gas constant, context makes it clear)
  • Rankine temperature: °R or °Ra (degree symbol helps distinguish)

Recommendation: Use °R for Rankine temperatures in modern technical writing.

Why doesn''t Kelvin use a degree symbol but Rankine does?

Answer: In 1968, the kelvin was redefined as a base SI unit, dropping the degree symbol; Rankine wasn''t part of SI and retained its symbol

Historical evolution:

Before 1968: Both scales used degree symbols

  • Kelvin: °K (degrees Kelvin)
  • Rankine: °R or °Ra (degrees Rankine)

After 1968: The 13th General Conference on Weights and Measures (CGPM) redefined the kelvin as a base SI unit (like meter, kilogram, second), removing the degree symbol:

  • Kelvin: K (kelvin, no degree symbol)
  • Rankine: °R (still degrees Rankine, not an SI unit)

Reasoning: Celsius (°C) retained its degree symbol because it's defined relative to kelvin (°C = K − 273.15). But kelvin itself, as a fundamental unit, doesn't use degrees—you say "300 kelvin" not "300 degrees kelvin."

Rankine status: Since Rankine isn't part of the International System of Units (SI), it never underwent this redefinition and still uses the degree symbol: °R.

Is Rankine more accurate than Fahrenheit for engineering?

Answer: Neither is more "accurate"—Rankine is better for thermodynamic calculations because it''s an absolute scale

Accuracy vs. suitability:

  • Both Rankine and Fahrenheit can be measured to arbitrary precision (accuracy)
  • The difference is mathematical correctness for thermodynamic equations

Why Rankine is better for thermodynamics:

  • Equations like PV = nRT, η = 1 - T_cold/T_hot, and ΔS = Q/T require absolute temperature
  • Using Fahrenheit (or Celsius) produces physically meaningless results (negative efficiency, division by zero, etc.)
  • Using Rankine (or Kelvin) produces correct physical results

Example (ideal gas law: PV = nRT):

  • At 0 °F (459.67 °R), pressure P is proportional to 459.67
  • If you incorrectly used 0 °F in the equation, you'd get P = 0 (no pressure), which is wrong!
  • Using 459.67 °R gives the correct pressure

Conclusion: For everyday temperature measurement, Fahrenheit is fine. For thermodynamic calculations, you must use Rankine (or Kelvin).

Will Rankine ever become obsolete?

Answer: Likely yes—it''s already obsolete in most contexts and will fade as U.S. engineering fully metrifies

Current trajectory:

  • 1960s-1990s: Rapid decline as global metrication occurred
  • 2000s-present: Niche survival in specific American engineering contexts
  • Future: Continued decline as remaining U.S. industries standardize on SI units (Kelvin)

Factors driving obsolescence:

  • International collaboration: Global engineering requires common units (Kelvin)
  • Software standardization: Modern CAD/simulation tools default to SI units
  • Educational shift: Engineering schools increasingly teach only Kelvin
  • Generational change: Engineers trained primarily in Rankine are retiring

Where it might persist longest:

  • Historical preservation (understanding old documents)
  • Legacy systems (maintaining equipment with Rankine specifications)
  • Specialized American aerospace/cryogenics (slow to change due to established procedures)

Likely outcome: Rankine will become a "historical unit" known primarily to engineering historians, similar to how the "degree Réaumur" (°Ré) is now obsolete despite 18th-19th century prominence.


People Also Ask

How do I convert Delisle to Rankine?

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What is the conversion factor from Delisle to Rankine?

The conversion factor depends on the specific relationship between Delisle and Rankine. You can find the exact conversion formula and factor on this page. Our calculator handles all calculations automatically. See the conversion table above for common values.

Can I convert Rankine back to Delisle?

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What are common uses for Delisle and Rankine?

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Last verified: February 19, 2026