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Free Praseodymium student datasheetPrintable revision sheet with identity, structure, evidence notes, phase behavior, uses, isotopes and review prompts.
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Instant reference

Praseodymium atomic number, mass, electron configuration and key properties

Atomic number
59
Relative atomic mass
140.908
Electron configuration
[Xe] 4f³ 6s²
Common oxidation states
+3, +4
Density
6.77 g/cm³
Melting point
1204 K
Boiling point
3793 K
Ordinary crystal
Double hexagonal close-packed (DHCP) reference
ClassificationLanthanide
Reference isotope¹⁴¹Pr
State contextSoft silvery lanthanide metal
Evidence noteAtomic identity and reference values are source-reviewed. Material viewers are teaching representations, not crystallographic refinements. Search demand shapes headings and FAQs but never overrides measured/evaluated evidence or element-versus-compound distinctions.
Quick answers

Praseodymium: quick answers

How many protons, neutrons and electrons does praseodymium have?

Praseodymium’s atomic number is 59, so every praseodymium atom has 59 protons, and a neutral atom also has 59 electrons. Its most common natural isotope, praseodymium-141, has 82 neutrons (other isotopes have different neutron counts).

What is the symbol for praseodymium?

The chemical symbol for praseodymium is Pr.

Is praseodymium a solid, liquid or gas at room temperature?

Praseodymium is a solid at room temperature (about 25 °C).

What family (group) is praseodymium in?

Praseodymium is a lanthanide, in period 6 (the f-block row shown below the main table) of the periodic table.

What is the electron configuration of praseodymium?

The ground-state electron configuration of praseodymium is [Xe] 4f³ 6s².

Connect the facts

From atomic number to chemistry

Read these as a chain of causes, not as isolated facts. Each step links to the concept hub if you want the underlying idea explained.

Common misconceptionPraseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet. The green/yellow colors associated with Pr usually come from ions in compounds or host materials, not from the silvery metal itself.
Periodic-table position

Praseodymium in its period and family

Praseodymium is an early Period 6 lanthanide between cerium and neodymium. Its 4f³6s² atom most commonly forms Pr³⁺, while Pr⁴⁺ is also important in selected oxides.

Interactive Visual Lab

Praseodymium Visual Lab

Explore Pr across the teaching nucleus, isolated-atom orbitals, evidence-aware material structure and temperature/evidence views, then connect those models to uses, isotopes, search-led questions and source-backed context.

Overview · structure · orbitals · real world
How to read an element tile

Every mark points to one exact feature

159 2140.908 3Pr 4[Xe] 4f³ 6s² 5Praseodymium 6Double hexagonal close-packed (DHCP) reference 7Soft silvery lant…
1Atomic numberNumber of protons
2Relative atomic massStandard value or bracketed reference mass
3Chemical symbolPr
4Electron configurationGround-state shorthand or evidence-labelled prediction
5Element namePraseodymium
6Structure contextDouble hexagonal close-packed (DHCP) reference
7Physical-state contextSoft silvery lanthanide metal

The numbered markers explain the same information system used throughout Element Lookup. Unknown or predicted fields remain visibly labelled rather than being replaced with guesses.

Five things worth remembering

Praseodymium in one minute

01

Atomic number 59 means every praseodymium nucleus has 59 protons.

02

Neutral Praseodymium has the ground-state configuration [Xe] 4f³ 6s².

03

The representative teaching isotope is ¹⁴¹Pr.

04

Praseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet.

05

The ordinary material reference is Double hexagonal close-packed (DHCP) reference.

Atomic structure teaching model

¹⁴¹Pr nucleus · neutral Pr

Nucleus modelNucleon-count teaching view
59 p⁺ + 82 n⁰¹⁴¹Pr · schematic nucleus, not a literal nuclear geometry
Electron-count schematicPrincipal-shell populations

Shell rings organize electron counts. They are not electron trajectories or orbital shapes.

Nucleus, shell count and material structure are deliberately separated so one picture is not mistaken for another.
Connect picture → chemistry

2 · 8 · 18 · 21 · 8 · 2 electrons

n=12
n=28
n=318
n=421
n=58
n=62
Why this electron pattern matters

The displayed 4f_xyz orbital is one representative real f cubic harmonic. It is not a picture of the whole 4f subshell or the electronic bands in the bulk material.

Teaching boundary: the nucleus uses colored spheres to make proton/neutron counts visible; the shell diagram only summarizes principal-shell populations. Neither is a literal picture of electron motion.
Material / molecular structure viewer

Double hexagonal close-packed (DHCP) reference

Ordinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.
Double hexagonal close-packed (DHCP) referenceOrdinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.
What are you seeing?

Ordinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.. The viewer is evidence-aware: measured structures are identified as such; unknown bulk structures stay unknown.

Teaching visualization; not a literal finite sample or thermal trajectory.
Probability-cloud teaching model

4f xyz orbital

One-electron teaching approximation; dots represent sampled probability density, not individual electrons.
Interpretation

What this model does—and does not—show

The displayed 4f_xyz orbital is one representative real f cubic harmonic. It is not a picture of the whole 4f subshell or the electronic bands in the bulk material.

Important: The cloud includes the expected nodal pattern for the named nonrelativistic orbital where applicable. Phase colors are not electric charge. For heavy and superheavy elements, relativistic/many-electron effects make these only teaching approximations.
Real-world archive

Where do I meet praseodymium?

Clickable learning cards connect the element to materials, environment, technology, biology or research - depending on what the evidence actually supports.

One
Permanent magnets

Permanent magnets

Pr can partly substitute or accompany Nd in high-performance rare-earth magnet materials.

1885Carl Auer von Welsbach separated “didymium” into praseodymium and neodymium.
Late 19th centurySpectroscopy and improved rare-earth separations established praseodymium as a distinct element.
20th centuryPr compounds became useful in glass, ceramics, alloys and optical materials.
TodayPr is important in selected magnet and advanced-material supply chains.
Evidence principleAtomic identity and reference values are source-reviewed. Material viewers are teaching representations, not crystallographic refinements. Search demand shapes headings and FAQs but never overrides measured/evaluated evidence or element-versus-compound distinctions.
Signature science

4f³ → Pr³⁺/Pr⁴⁺ → color and magnet materials

Praseodymium’s useful optical and magnetic roles usually arise from Pr ions inside compounds, alloys or host lattices rather than from elemental metal alone.

Evaluated

4f³6s²

Early-lanthanide open 4f shell.

Reference properties

Praseodymium properties: atomic, physical, thermal and chemical

Categories follow the science of this element rather than a fixed decorative template. Each row carries condition/provenance context and an evidence label; unknown values stay unknown.

PropertyValueContext / provenanceEvidence
Atomic number59Source-reviewed; see Sources belowEvaluated
Relative atomic mass140.908Source-reviewed; see Sources belowEvaluated
Ground-state electron configuration[Xe] 4f³ 6s²Source-reviewed; see Sources belowEvaluated
Group / period / blockGroup Lanthanide · Period 6 · f-blockPeriodic-table placementEvaluated
Electronegativity1.13Source-reviewed; see Sources belowEvaluated
Reference isotope¹⁴¹PrSource-reviewed; see Sources belowEvaluated
PropertyValueContext / provenanceEvidence
State contextSoft silvery lanthanide metalSource-reviewed; see Sources belowEvaluated
Density6.77 g/cm³Source-reviewed; see Sources belowEvaluated
Material / molecular structureDouble hexagonal close-packed (DHCP) referenceOrdinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.Measured
ClassificationLanthanidePeriodic-table / chemistry classificationEvaluated
Structure-model scopeOrdinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.Teaching visualization; exact crystallographic coordinates are not implied unless stated.Reviewed
PropertyValueContext / provenanceEvidence
Melting / transition reference1204 KSource-reviewed; see Sources belowEvaluated
Boiling / gas reference3793 KSource-reviewed; see Sources belowEvaluated
Phase-path contextAt approximately standard pressure, praseodymium is treated as a solid below 1204 K, liquid between melting and approximately 3793 K, and gas above the boiling reference. The ordinary crystal label applies to the stated material reference; unmodeled solid allotropy is not fabricated.Shared phase registry drives the slider, regions and markers.Evaluated
Condition warningTemperature and pressure define phase behavior; purity/allotropy may matter.Teaching condition statementReviewed
PropertyValueContext / provenanceEvidence
Common oxidation states+3, +4Source-reviewed; see Sources belowEvaluated
Ion / common ion contextPr³⁺Source-reviewed; see Sources belowEvaluated
Periodic chemistry contextPraseodymium is an early Period 6 lanthanide between cerium and neodymium. Its 4f³6s² atom most commonly forms Pr³⁺, while Pr⁴⁺ is also important in selected oxides.Element-specific interpretationReviewed
Chemistry cautionElemental form, ions and compounds are distinct chemical objects.Interpretive teaching ruleReviewed
PropertyValueContext / provenanceEvidence
¹⁴¹PrNatural isotopeEssentially all natural praseodymium is ¹⁴¹Pr.Evaluated
RadioisotopesArtificial isotopesUsed mainly in research contexts.Evaluated
Natural praseodymiumSingle-isotope natural elementRelative atomic mass is therefore close to the ¹⁴¹Pr isotopic mass.Evaluated
Teaching nucleus¹⁴¹Pr · 59 protons + 82 neutronsReference isotope used in the nucleus modelReviewed
PropertyValueContext / provenanceEvidence
Page evidence noteAtomic identity and reference values are source-reviewed. Material viewers are teaching representations, not crystallographic refinements. Search demand shapes headings and FAQs but never overrides measured/evaluated evidence or element-versus-compound distinctions.Evidence summary for this guideReviewed
Structure evidenceOrdinary praseodymium is represented with a DHCP teaching cell. Temperature-dependent solid allotropy exists; the phase track keeps the model conservative rather than extending one structure beyond its evidence.Measured structure, labelled schematic, prediction or explicit unknown as applicable.Reviewed
Map evidence ruleReal pins are reviewed examples; conceptual layers are used when pins would mislead.Geography Explorer 2.0Reviewed
Source set3 primary/reference links listed belowOpen the Sources section for the actual references.Reviewed
Temperature explorer

Is Praseodymium a solid, liquid or gas? State at temperature

At approximately standard pressure, praseodymium is treated as a solid below 1204 K, liquid between melting and approximately 3793 K, and gas above the boiling reference. The ordinary crystal label applies to the stated material reference; unmodeled solid allotropy is not fabricated.

Temperature293 K
Move the slider
The shared site-wide phase model controls the track, markers and readout.
Geography and evidence

Where on Earth is Praseodymium found or produced?

World map
Vienna, AustriaRSC historical context · historical
Discovery and history

Who discovered Praseodymium, and when?

1885

Carl Auer von Welsbach separated “didymium” into praseodymium and neodymium.

Late 19th century

Spectroscopy and improved rare-earth separations established praseodymium as a distinct element.

20th century

Pr compounds became useful in glass, ceramics, alloys and optical materials.

Today

Pr is important in selected magnet and advanced-material supply chains.

Process / synthesis context

From source material to Praseodymium applications: high-level material path

1

Praseodymium is obtained from mineral or metallurgical feedstocks in which it is chemically associated with other elements rather than mined as abundant native metal.

2

Industrial separation and refining produce element-specific compounds or metal feedstock; this guide does not provide operational extraction recipes.

3

The refined material is converted into the particular alloy, compound, doped host or component required by the application.

4

Recycling and recovery depend on the host product, concentration and economics; application materials must not be confused with pure element.

Safety boundary: This page is educational. Chemical, occupational, radiological or medical safety decisions require the specific material/isotope, its current safety data and qualified guidance.
Real-world applications

What is praseodymium used for?

Magnets

Pr is used with Nd and other elements in some high-performance permanent-magnet compositions.

Alloys

Pr-containing alloys can support specialized high-temperature and lightweight applications.

Optical glass

Pr ions provide characteristic absorption/color in glasses and filters.

Ceramics & pigments

Pr compounds provide durable colors in selected ceramic and enamel systems.

Isotopes

Praseodymium isotopes and natural abundance

¹⁴¹Pr

Natural isotope

Essentially all natural praseodymium is ¹⁴¹Pr.

Radioisotopes

Artificial isotopes

Used mainly in research contexts.

Natural praseodymium

Single-isotope natural element

Relative atomic mass is therefore close to the ¹⁴¹Pr isotopic mass.

Learn it, don’t just read it

Five-question Praseodymium check

What is Praseodymium’s atomic number?

Which classification best fits Praseodymium?

What is the representative teaching isotope?

Which statement respects the material evidence?

Which rule should guide real-world uses?

Questions answered

Praseodymium questions students commonly ask

Each answer starts with the direct fact, then explains the chemistry, evidence or material context so the result is understandable rather than merely memorized.

What is praseodymium?

Short answer: Praseodymium is chemical element 59, symbol Pr, a soft silvery lanthanide metal.

Atomic number 59 means every praseodymium nucleus contains 59 protons. In the periodic table, Praseodymium is classified here as a lanthanide in Period 6 and Group Lanthanide. Praseodymium is an early Period 6 lanthanide between cerium and neodymium. Its 4f³6s² atom most commonly forms Pr³⁺, while Pr⁴⁺ is also important in selected oxides.

Key point: Pr is element 59; its periodic position and electron structure explain the rest of the page.

What is praseodymium used for?

Short answer: It is used in rare-earth magnets, specialty alloys, colored glass, ceramics and optical filters.

Magnets: Pr is used with Nd and other elements in some high-performance permanent-magnet compositions. Alloys: Pr-containing alloys can support specialized high-temperature and lightweight applications. Praseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet. The green/yellow colors associated with Pr usually come from ions in compounds or host materials, not from the silvery metal itself.

Key point: Always distinguish the pure element from the compound, alloy, isotope or device material that actually performs the application.

Where is praseodymium found?

Short answer: It occurs mixed with other lanthanides in minerals such as monazite and bastnäsite and is separated during rare-earth processing.

Praseodymium is obtained from mineral or metallurgical feedstocks in which it is chemically associated with other elements rather than mined as abundant native metal. Praseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet. The green/yellow colors associated with Pr usually come from ions in compounds or host materials, not from the silvery metal itself.

Key point: Natural occurrence, resources, production and recycling are different geography questions.

Who discovered praseodymium?

Short answer: Carl Auer von Welsbach separated praseodymium from didymium in 1885.

In 1885, Carl Auer von Welsbach separated “didymium” into praseodymium and neodymium. In the late 19th century, Spectroscopy and improved rare-earth separations established praseodymium as a distinct element.

Key point: Discovery credit follows the historical evidence and accepted attribution, not just the earliest claim.

Is praseodymium a metal?

Short answer: Yes. It is a lanthanide metal, not a nonmetal or metalloid.

This guide classifies Praseodymium as a lanthanide. Its periodic position is Period 6, f-block, Group Lanthanide. Praseodymium is an early Period 6 lanthanide between cerium and neodymium. Its 4f³6s² atom most commonly forms Pr³⁺, while Pr⁴⁺ is also important in selected oxides.

Key point: Periodic-table classification describes recurring atomic/chemical behavior; it does not make every element in a column physically identical.

How did praseodymium get its name?

Short answer: The name comes from Greek words associated with “green” and “twin,” reflecting the green salts and its origin from didymium.

Praseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet. The green/yellow colors associated with Pr usually come from ions in compounds or host materials, not from the silvery metal itself. Praseodymium is obtained from mineral or metallurgical feedstocks in which it is chemically associated with other elements rather than mined as abundant native metal.

Key point: Element names record scientific history; the name itself does not determine the element’s chemistry.

How many electrons does praseodymium have?

Short answer: A neutral atom has 59 electrons; its ground-state configuration is [Xe] 4f³ 6s².

A neutral atom has the same number of electrons as protons, so neutral Praseodymium has 59 electrons. Its ground-state reference configuration is [Xe] 4f³ 6s²; ions have different electron counts because electrons have been removed or added.

Key point: Electron count changes in ions; proton count does not.

What color is praseodymium?

Short answer: The elemental metal is silvery; many Pr compounds/ions have distinctive green or yellow-green colors.

The ordinary elemental-material description used here is: Soft silvery lanthanide metal. Praseodymium metal is not the same material as praseodymium oxide, Pr-containing glass or a rare-earth magnet. The green/yellow colors associated with Pr usually come from ions in compounds or host materials, not from the silvery metal itself.

Key point: Elemental appearance can differ from the colors of its ions, compounds, oxide films or host materials.

Scientific sources and provenance

Scientific sources for Praseodymium

Evidence rule: Atomic identity and reference values are source-reviewed. Material viewers are teaching representations, not crystallographic refinements. Search demand shapes headings and FAQs but never overrides measured/evaluated evidence or element-versus-compound distinctions.
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