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

Atomic number
88
Reference mass
[226]
Electron configuration
[Rn] 7s²
Common oxidation state
+2
Density
≈5 g/cm³
Melting point
969 K
Boiling point
1773 K
Crystal
BCC (reported)
ClassificationRadioactive alkaline-earth metal
Reference isotope²²⁶Ra
State contextRadioactive solid metal
Evidence noteAll radium isotopes are radioactive. Atomic/nuclear values are source-reviewed, while scarce bulk-metal properties carry more uncertainty than common stable metals. Medical statements are descriptive, not treatment advice.
Quick answers

Radium: quick answers

How many protons, neutrons and electrons does radium have?

Radium’s atomic number is 88, so every radium atom has 88 protons, and a neutral atom also has 88 electrons. Radium has no stable isotopes, so the number of neutrons depends on which isotope you mean.

What is the symbol for radium?

The chemical symbol for radium is Ra.

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

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

What family (group) is radium in?

Radium is an alkaline earth metal, in group 2, period 7 of the periodic table.

How many valence electrons does radium have?

Radium has 2 valence electrons, the electrons in its outer shell, which matches its position in group 2.

What is the electron configuration of radium?

The ground-state electron configuration of radium is [Rn] 7s².

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 misconceptionRadium’s place in Group 2 explains aspects of its chemistry, but periodic trends do not predict radioactive half-life or make radium safe to handle.
Periodic-table position

Radium in its period and family

Radium sits at the bottom of Group 2 below barium. Its two outer 7s electrons support alkaline-earth +2 chemistry, but nuclear decay and isotope half-life are essential parts of any scientifically honest radium description.

Interactive Visual Lab

Radium Visual Lab

Decode radium’s tile, rotate a ²²⁶Ra teaching nucleus and reported BCC metal cell, inspect 7s and representative 6p core probability models, then connect radium to decay chains, discovery history, environmental monitoring and Ra-223 medicine.

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

Every mark points to one exact feature

188 2[226] 3Ra 4[Rn] 7s² 5Radium 6BCC (reported) 7Solid
1Atomic numberNumber of protons
2Relative atomic massStandard value or bracketed reference mass
3Chemical symbolRa
4Electron configurationGround-state shorthand or evidence-labelled prediction
5Element nameRadium
6Structure contextBCC (reported)
7Physical-state contextRadioactive solid 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

Radium in one minute

01

Atomic number 88 means every radium nucleus contains 88 protons.

02

The ground-state reference configuration is [Rn] 7s² and +2 is the characteristic oxidation state.

03

All radium isotopes are radioactive; ²²⁶Ra is a key long-lived natural isotope.

04

Radium occurs only in trace quantities as part of uranium/thorium decay series, not as large native-metal deposits.

05

Radium-223 has a regulated medical role in certain prostate-cancer settings involving bone metastases.

Atomic structure teaching model

²²⁶Ra nucleus · neutral Ra

88 p⁺ · 138 n⁰
Nucleus modelNucleon-count teaching view
88 p⁺ + 138 n⁰²²⁶Ra · 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 · 32 · 18 · 8 · 2 electrons

n=12
n=28
n=318
n=432
n=518
n=68
n=72
Why this electron pattern matters

The 7s view represents the occupied outer s orbital in a nonrelativistic hydrogen-like teaching approximation; 6p is an occupied core-region representative. For Z = 88, relativistic and many-electron effects matter, so the page labels these as qualitative orbital-shape models rather than scale-accurate electron densities.

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

BCC (reported)

Body-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarce
BCC (reported)Body-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarce
What are you seeing?

Body-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarce. 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

7s orbital

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

What this model does—and does not—show

The 7s view represents the occupied outer s orbital in a nonrelativistic hydrogen-like teaching approximation; 6p is an occupied core-region representative. For Z = 88, relativistic and many-electron effects matter, so the page labels these as qualitative orbital-shape models rather than scale-accurate electron densities.

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 radium?

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

Decay
Decay chains

Decay chains

Natural radium isotopes appear as daughter products in uranium/thorium radioactive decay series and occur only in trace concentrations.

1898Marie Curie and Pierre Curie announced radium after studying highly radioactive pitchblende residues.
1911Marie Curie and André Debierne isolated radium metal through specialized laboratory work.
Early 1900sRadium entered medicine and luminous paints before its hazards were adequately understood.
TodayModern use is limited and tightly controlled; Ra-223 has a specific role as a radiopharmaceutical in certain cancer care.
Evidence principleAll radium isotopes are radioactive. Atomic/nuclear values are source-reviewed, while scarce bulk-metal properties carry more uncertainty than common stable metals. Medical statements are descriptive, not treatment advice.
Signature science

From decay-series daughter to regulated medical isotope

Radium’s modern story is nuclear and historical; safe context matters as much as the numbers.

Evaluated

Decay-series trace

Natural radium appears as a daughter in uranium/thorium decay chains and can enter rocks or groundwater.

Reference properties

Radium 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 number88Source-reviewed; see Sources belowEvaluated
Relative atomic mass[226]Source-reviewed; see Sources belowEvaluated
Ground-state electron configuration[Rn] 7s²Source-reviewed; see Sources belowEvaluated
Group / period / blockGroup 2 · Period 7 · s-blockPeriodic-table placementEvaluated
Electronegativity≈0.9 (context-dependent)Source-reviewed; see Sources belowEvaluated
Reference isotope²²⁶RaSource-reviewed; see Sources belowEvaluated
PropertyValueContext / provenanceEvidence
State contextRadioactive solid metalSource-reviewed; see Sources belowEvaluated
Density≈5 g/cm³Source-reviewed; see Sources belowPredicted
Material / molecular structureBCC (reported)Body-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarceMeasured
ClassificationRadioactive alkaline-earth metalPeriodic-table / chemistry classificationEvaluated
Structure-model scopeBody-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarceTeaching visualization; exact crystallographic coordinates are not implied unless stated.Reviewed
PropertyValueContext / provenanceEvidence
Melting / transition reference969 KSource-reviewed; see Sources belowEvaluated
Boiling / gas reference1773 KSource-reviewed; see Sources belowEvaluated
Phase-path contextA simplified approximately standard-pressure path uses 969 K as the melting reference and 1773 K as the boiling reference. These bulk values are far less experimentally routine than data for common stable metals.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+2Source-reviewed; see Sources belowEvaluated
Ion / common ion contextRa²⁺Source-reviewed; see Sources belowEvaluated
Periodic chemistry contextRadium sits at the bottom of Group 2 below barium. Its two outer 7s electrons support alkaline-earth +2 chemistry, but nuclear decay and isotope half-life are essential parts of any scientifically honest radium description.Element-specific interpretationReviewed
Chemistry cautionElemental form, ions and compounds are distinct chemical objects.Interpretive teaching ruleReviewed
PropertyValueContext / provenanceEvidence
²²⁶RaRadioactive · half-life ≈1600 yearsA major natural radium isotope in the ²³⁸U decay series and a key environmental-radiological reference.Evaluated
²²³RaRadioactive · half-life ≈11.4 daysAn alpha-emitting isotope used as radium-223 dichloride in specific regulated cancer therapy.Evaluated
²²⁴RaRadioactive · half-life ≈3.66 daysA naturally occurring radium isotope in the thorium decay series.Evaluated
Teaching nucleus²²⁶Ra · 88 protons + 138 neutronsReference isotope used in the nucleus modelReviewed
PropertyValueContext / provenanceEvidence
Page evidence noteAll radium isotopes are radioactive. Atomic/nuclear values are source-reviewed, while scarce bulk-metal properties carry more uncertainty than common stable metals. Medical statements are descriptive, not treatment advice.Evidence summary for this guideReviewed
Structure evidenceBody-centred cubic radium metal is commonly reported; bulk data are limited because radium is highly radioactive and scarceMeasured 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 set4 primary/reference links listed belowOpen the Sources section for the actual references.Reviewed
Temperature explorer

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

A simplified approximately standard-pressure path uses 969 K as the melting reference and 1773 K as the boiling reference. These bulk values are far less experimentally routine than data for common stable metals.

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

Where on Earth is Radium found or produced?

World map
Decay-series traceIAEA / environmental radionuclide context · conceptual
Discovery and history

Who discovered Radium, and when?

1898

Marie Curie and Pierre Curie announced radium after studying highly radioactive pitchblende residues.

1911

Marie Curie and André Debierne isolated radium metal through specialized laboratory work.

Early 1900s

Radium entered medicine and luminous paints before its hazards were adequately understood.

Today

Modern use is limited and tightly controlled; Ra-223 has a specific role as a radiopharmaceutical in certain cancer care.

Process / synthesis context

How radium enters science, environment and medicine - conceptual only

1

Natural radium forms in radioactive decay series associated with uranium and thorium.

2

Environmental science measures trace radium in rocks, soils and waters to understand exposure and geochemistry.

3

Historical isolation required extensive radiochemical separation, but Element Lookup does not reproduce operational separation procedures.

4

Modern medical radium-223 is manufactured and administered within regulated radiopharmaceutical systems; this page stays at the conceptual science level.

Safety boundary: Radium is highly radioactive. This page deliberately avoids extraction, concentration, source fabrication or other operational radioactive-material instructions.
Real-world applications

What is radium used for?

Radium-223 medicine

Ra-223 dichloride is used in specific cases of prostate cancer metastatic to bone, under specialist clinical care.

Scientific history

Radium was central to early radioactivity research and helped transform understanding of atoms and nuclei.

Environmental tracing/monitoring

Radium isotopes can be measured in hydrogeology and environmental radioactivity studies.

Historical luminous paint

Former luminous-paint use is now primarily a radiation-safety and occupational-health lesson.

Isotopes

Radium isotopes and natural abundance

²²⁶Ra

Radioactive · half-life ≈1600 years

A major natural radium isotope in the ²³⁸U decay series and a key environmental-radiological reference.

²²³Ra

Radioactive · half-life ≈11.4 days

An alpha-emitting isotope used as radium-223 dichloride in specific regulated cancer therapy.

²²⁴Ra

Radioactive · half-life ≈3.66 days

A naturally occurring radium isotope in the thorium decay series.

Learn it, don’t just read it

Five-question Radium check

What is radium’s atomic number?

Does radium have stable isotopes?

Which oxidation state is characteristic for radium chemistry?

Which radium isotope has a modern regulated medical use?

Why is a “radium mine-production map” misleading?

Questions answered

Radium 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 radium?

Short answer: Radium is chemical element 88, a highly radioactive alkaline-earth metal in Group 2.

Atomic number 88 means every radium nucleus contains 88 protons. In the periodic table, Radium is classified here as a radioactive alkaline-earth metal in Period 7 and Group 2. Radium sits at the bottom of Group 2 below barium. Its two outer 7s electrons support alkaline-earth +2 chemistry, but nuclear decay and isotope half-life are essential parts of any scientifically honest radium description.

Key point: Ra is element 88; its periodic position and electron structure explain the rest of the page.

Why is radium dangerous?

Short answer: Radium is radioactive, and internalized radium can be especially hazardous because Ra²⁺ behaves chemically somewhat like Ca²⁺ and can be incorporated into bone, exposing nearby tissue as it decays.

The hazard is not just the word “radioactive.” It depends on isotope, activity, exposure route and where the material goes in the body. Radium decay can also produce radon, adding a decay-chain dimension. Historical luminous-paint exposures demonstrated why persistent internal deposition of alpha-emitting radionuclides is dangerous.

Key point: For radium, combine nuclear decay with its calcium-like ion chemistry and internal distribution.

Where is radium found?

Short answer: In nature it occurs only in trace amounts as part of uranium and thorium decay series, including in some rocks and groundwater.

Natural radium forms in radioactive decay series associated with uranium and thorium. Radium occurs only in trace quantities as part of uranium/thorium decay series, not as large native-metal deposits.

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

What is radium used for today?

Short answer: Modern uses are limited. Radium-223 dichloride has a regulated medical role in certain prostate-cancer bone-metastasis settings.

Radium-223 medicine: Ra-223 dichloride is used in specific cases of prostate cancer metastatic to bone, under specialist clinical care. Scientific history: Radium was central to early radioactivity research and helped transform understanding of atoms and nuclei. Radium is chemically related to other alkaline-earth metals, but its radioactivity dominates its practical handling and modern uses. Historical luminous-paint use is now a safety lesson, not a recommended application.

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

Why was radium used in old watch dials?

Short answer: Radium compounds were historically mixed with phosphors to make self-luminous paint. The serious radiation hazards were not initially understood, and this use was abandoned.

Luminous-paint history Radium was once used in luminous paints; severe occupational harms helped establish major lessons in radiation protection. Radium is chemically related to other alkaline-earth metals, but its radioactivity dominates its practical handling and modern uses. Historical luminous-paint use is now a safety lesson, not a recommended application.

Key point: Use the direct answer together with the material, isotope and evidence context shown elsewhere on the page.

Who discovered radium?

Short answer: Marie Curie and Pierre Curie announced the discovery in 1898 while studying pitchblende residues.

In 1898, Marie Curie and Pierre Curie announced radium after studying highly radioactive pitchblende residues. In 1911, Marie Curie and André Debierne isolated radium metal through specialized laboratory work.

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

Scientific sources and provenance

Scientific sources for Radium

Evidence rule: All radium isotopes are radioactive. Atomic/nuclear values are source-reviewed, while scarce bulk-metal properties carry more uncertainty than common stable metals. Medical statements are descriptive, not treatment advice.
Keep the curiosity going

Questions to ask next about Radium

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

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