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Free Rubidium student datasheetPrintable revision sheet with identity, structure, evidence notes, phase behavior, uses, isotopes and review prompts.
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Rubidium atomic number, mass, electron configuration and key properties

Atomic number
37
Relative atomic mass
85.468
Electron configuration
[Kr] 5s¹
Common oxidation state
+1
Density
1.53 g/cm³
Melting point
312.45 K
Boiling point
961 K
Crystal near room temperature
BCC
ClassificationAlkali metal
Reference isotope⁸⁵Rb
State contextSoft silvery alkali metal · solid at 20 °C
Evidence noteAtomic, isotope and ordinary bulk references are evaluated. The BCC view is a conventional teaching cell. Mineral-occurrence geography is conceptual because a few pins would falsely imply a dedicated native-rubidium mining map.
Quick answers

Rubidium: quick answers

How many protons, neutrons and electrons does rubidium have?

Rubidium’s atomic number is 37, so every rubidium atom has 37 protons, and a neutral atom also has 37 electrons. Its most common natural isotope, rubidium-85, has 48 neutrons (other isotopes have different neutron counts).

What is the symbol for rubidium?

The chemical symbol for rubidium is Rb.

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

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

What family (group) is rubidium in?

Rubidium is an alkali metal, in group 1, period 5 of the periodic table.

How many valence electrons does rubidium have?

Rubidium has 1 valence electron, the single electron in its outer shell, which matches its position in group 1.

What is the electron configuration of rubidium?

The ground-state electron configuration of rubidium is [Kr] 5s¹.

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 misconceptionRubidium metal, Rb⁺ salts and radioactive ⁸⁷Rb are related by element identity but are not the same chemical or nuclear object. The page keeps ion chemistry and isotope clocks separate.
Periodic-table position

Rubidium in its period and family

Rubidium is the Period 5 alkali metal below potassium and above cesium. The single 5s electron supports strong +1 chemistry and very low ionization energy relative to many elements.

Interactive Visual Lab

Rubidium Visual Lab

Toggle Rb to Rb⁺, rotate a ⁸⁵Rb teaching nucleus and BCC cell, inspect the spherical 5s probability cloud, then connect the atom to spectroscopy and the ⁸⁷Rb→⁸⁷Sr geological clock.

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

Every mark points to one exact feature

137 285.468 3Rb 4[Kr] 5s¹ 5Rubidium 6Rubidium metal · body-centred cubic 7Solid
1Atomic numberNumber of protons
2Relative atomic massStandard value or bracketed reference mass
3Chemical symbolRb
4Electron configurationGround-state shorthand or evidence-labelled prediction
5Element nameRubidium
6Structure contextRubidium metal · body-centred cubic
7Physical-state contextSoft silvery alkali metal · solid at 20 °C

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

Rubidium in one minute

01

Atomic number 37 means 37 protons.

02

Neutral rubidium ends in 5s¹ and commonly forms Rb⁺.

03

Rubidium metal is BCC near room temperature.

04

⁸⁷Rb is naturally radioactive and is used in Rb–Sr geochronology.

05

Rubidium also has important roles in atomic-physics and frequency-standard research.

Atomic structure teaching model

⁸⁵Rb nucleus · neutral Rb

Nucleus modelNucleon-count teaching view
37 p⁺ + 48 n⁰⁸⁵Rb · 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 · 8 · 1 electrons

n=12
n=28
n=318
n=48
n=51
Why this electron pattern matters

The 5s cloud is an isolated-atom probability model. It is not an electron orbit and does not depict conduction electrons in metallic rubidium.

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

Rubidium metal · body-centred cubic

Rubidium metal is represented with a body-centred-cubic conventional teaching cell near room temperature. Boundary atoms are shared between neighbouring cells.
Rubidium metal · body-centred cubicRubidium metal is represented with a body-centred-cubic conventional teaching cell near room temperature. Boundary atoms are shared between neighbouring cells.
What are you seeing?

Rubidium metal is represented with a body-centred-cubic conventional teaching cell near room temperature. Boundary atoms are shared between neighbouring cells.. 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

5s orbital

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

What this model does—and does not—show

The 5s cloud is an isolated-atom probability model. It is not an electron orbit and does not depict conduction electrons in metallic rubidium.

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 rubidium?

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

One
Spectroscopy

Spectroscopy

Rubidium has strong optical transitions used in laser spectroscopy and atomic-physics experiments.

1861Robert Bunsen and Gustav Kirchhoff discovered rubidium by spectroscopy, identifying characteristic red spectral lines.
20th centuryRubidium spectroscopy and isotope science became important research tools.
GeochronologyThe ⁸⁷Rb→⁸⁷Sr decay system became a major method for dating geological materials.
TodayRubidium is used mainly in specialized research, timing and electronic/atomic applications rather than bulk structural materials.
Evidence principleAtomic, isotope and ordinary bulk references are evaluated. The BCC view is a conventional teaching cell. Mineral-occurrence geography is conceptual because a few pins would falsely imply a dedicated native-rubidium mining map.
Signature science

Rb atom → Rb⁺ ion → ⁸⁷Rb geological clock

One outer 5s electron connects alkali-metal chemistry to atomic spectroscopy, while isotope identity adds a separate geological clock.

Evaluated

[Kr] 5s¹

Neutral rubidium has one outer 5s electron.

Reference properties

Rubidium 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 number37Source-reviewed; see Sources belowEvaluated
Relative atomic mass85.468Source-reviewed; see Sources belowEvaluated
Ground-state electron configuration[Kr] 5s¹Source-reviewed; see Sources belowEvaluated
Group / period / blockGroup 1 · Period 5 · s-blockPeriodic-table placementEvaluated
Electronegativity0.82Source-reviewed; see Sources belowEvaluated
Reference isotope⁸⁵RbSource-reviewed; see Sources belowEvaluated
PropertyValueContext / provenanceEvidence
State contextSoft silvery alkali metal · solid at 20 °CSource-reviewed; see Sources belowEvaluated
Density1.53 g/cm³Source-reviewed; see Sources belowEvaluated
Material / molecular structureRubidium metal · body-centred cubicRubidium metal is represented with a body-centred-cubic conventional teaching cell near room temperature. Boundary atoms are shared between neighbouring cells.Measured
ClassificationAlkali metalPeriodic-table / chemistry classificationEvaluated
Structure-model scopeRubidium metal is represented with a body-centred-cubic conventional teaching cell near room temperature. Boundary atoms are shared between neighbouring cells.Teaching visualization; exact crystallographic coordinates are not implied unless stated.Reviewed
PropertyValueContext / provenanceEvidence
Melting / transition reference312.45 KSource-reviewed; see Sources belowEvaluated
Boiling / gas reference961 KSource-reviewed; see Sources belowEvaluated
Phase-path contextAt approximately standard pressure, rubidium is BCC solid below 312.45 K, liquid to about 961 K, and gaseous above that boiling reference.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
Ordinary electrical behaviorMetallic conductorQualitative bulk behavior; exact resistivity depends on temperature, purity and alloy state.Measured
Conduction modelCollective solid-state electronsDo not interpret isolated-atom orbital clouds as literal current paths.Reviewed
Surface / compound caveatOxides, salts and alloys can behave differently from the pure metalMaterial contextReviewed
Engineering valuesCondition-dependentUse condition-specific materials data for engineering calculations.Reviewed
PropertyValueContext / provenanceEvidence
Common oxidation states+1Source-reviewed; see Sources belowEvaluated
Ion / common ion contextRb⁺Source-reviewed; see Sources belowEvaluated
Periodic chemistry contextRubidium is the Period 5 alkali metal below potassium and above cesium. The single 5s electron supports strong +1 chemistry and very low ionization energy relative to many elements.Element-specific interpretationReviewed
Chemistry cautionElemental form, ions and compounds are distinct chemical objects.Interpretive teaching ruleReviewed
PropertyValueContext / provenanceEvidence
⁸⁵RbStable natural isotopeReference teaching nucleus with 37 protons and 48 neutrons.Evaluated
⁸⁷RbVery long-lived radioactive natural isotopeDecays to ⁸⁷Sr and underpins Rb–Sr geochronology.Evaluated
Rubidium isotope contextTwo major natural isotopesNatural rubidium includes both ⁸⁵Rb and ⁸⁷Rb.Evaluated
Teaching nucleus⁸⁵Rb · 37 protons + 48 neutronsReference isotope used in the nucleus modelReviewed
Temperature explorer

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

At approximately standard pressure, rubidium is BCC solid below 312.45 K, liquid to about 961 K, and gaseous above that boiling reference.

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

Where on Earth is Rubidium found or produced?

World map
Heidelberg · 1861RSC historical context · 1861
Discovery and history

Who discovered Rubidium, and when?

1861

Robert Bunsen and Gustav Kirchhoff discovered rubidium by spectroscopy, identifying characteristic red spectral lines.

20th century

Rubidium spectroscopy and isotope science became important research tools.

Geochronology

The ⁸⁷Rb→⁸⁷Sr decay system became a major method for dating geological materials.

Today

Rubidium is used mainly in specialized research, timing and electronic/atomic applications rather than bulk structural materials.

Process / synthesis context

From mineral association to specialized rubidium products

1

Rubidium occurs as a minor constituent in minerals and brines associated with alkali metals.

2

Industrial recovery separates rubidium compounds from larger alkali-metal process streams.

3

High-purity compounds or metal are produced for specialized technical uses; this guide does not provide reactive-metal preparation procedures.

4

Atomic-physics applications use controlled laboratory systems, not bulk consumer rubidium.

Safety boundary: Rubidium metal is highly reactive. This page is educational and provides no handling, storage or preparation instructions.
Real-world applications

What is rubidium used for?

Atomic clocks

Rubidium frequency standards provide compact, stable timing references.

Research

Laser cooling, spectroscopy and quantum/atomic experiments use rubidium atoms.

Geochronology

⁸⁷Rb/⁸⁷Sr measurements constrain ages and geological histories.

Specialty electronics

Rubidium compounds have niche photoelectric and electronic uses.

Isotopes

Rubidium isotopes and natural abundance

⁸⁵Rb

Stable natural isotope

Reference teaching nucleus with 37 protons and 48 neutrons.

⁸⁷Rb

Very long-lived radioactive natural isotope

Decays to ⁸⁷Sr and underpins Rb–Sr geochronology.

Rubidium isotope context

Two major natural isotopes

Natural rubidium includes both ⁸⁵Rb and ⁸⁷Rb.

Learn it, don’t just read it

Five-question Rubidium check

What is rubidium’s atomic number?

What is the common ion?

What is the outer configuration?

Which isotope system is used in geochronology?

What structure is shown for room-temperature rubidium?

Questions answered

Rubidium 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 rubidium?

Short answer: Rubidium is element 37, a soft reactive alkali metal.

Atomic number 37 means every rubidium nucleus contains 37 protons. In the periodic table, Rubidium is classified here as an alkali metal in Period 5 and Group 1. Rubidium is the Period 5 alkali metal below potassium and above cesium. The single 5s electron supports strong +1 chemistry and very low ionization energy relative to many elements.

Key point: Rb is element 37; its periodic position and electron structure explain the rest of the page.

How many valence electrons does rubidium have?

Short answer: One, in the 5s¹ outer configuration.

The neutral-atom ground-state reference used on this page is [Kr] 5s¹. This is an isolated-atom reference: bonding and ion formation can change which outer electrons are present or chemically active. The listed common oxidation-state context is +1, which helps connect the atomic configuration to ordinary chemistry without treating electron counting as a single universal rule.

Key point: Electron configuration is a ground-state atomic reference, not a literal picture of every compound.

Is rubidium a metal?

Short answer: Yes. It is a Group 1 alkali metal.

This guide classifies Rubidium as an alkali metal. Its periodic position is Period 5, s-block, Group 1. Rubidium is the Period 5 alkali metal below potassium and above cesium. The single 5s electron supports strong +1 chemistry and very low ionization energy relative to many elements.

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

What is rubidium used for?

Short answer: Specialized uses include frequency standards, atomic-physics research and Rb–Sr geochronology.

Atomic clocks: Rubidium frequency standards provide compact, stable timing references. Research: Laser cooling, spectroscopy and quantum/atomic experiments use rubidium atoms. Rubidium metal, Rb⁺ salts and radioactive ⁸⁷Rb are related by element identity but are not the same chemical or nuclear object. The page keeps ion chemistry and isotope clocks separate.

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

Who discovered rubidium?

Short answer: Robert Bunsen and Gustav Kirchhoff in 1861 using spectroscopy.

In 1861, Robert Bunsen and Gustav Kirchhoff discovered rubidium by spectroscopy, identifying characteristic red spectral lines. In the 20th century, Rubidium spectroscopy and isotope science became important research tools.

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

Where is rubidium found?

Short answer: Dispersed in certain potassium- and lithium-bearing minerals and brines rather than as native metal.

Rubidium occurs as a minor constituent in minerals and brines associated with alkali metals. Mineral occurrence Rubidium occurs dispersed in potassium-rich and lithium-rich minerals rather than as native metal deposits.

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

Scientific sources and provenance

Scientific sources for Rubidium

Evidence rule: Atomic, isotope and ordinary bulk references are evaluated. The BCC view is a conventional teaching cell. Mineral-occurrence geography is conceptual because a few pins would falsely imply a dedicated native-rubidium mining map.
Keep the curiosity going

Questions to ask next about Rubidium

A good element lesson should lead to the next useful question, not end after a list of facts.

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