What is Mendelevium?
Mendelevium (symbol Md) is element 101 on the periodic table, a actinide in period 7. The first element produced and identified one atom at a time. At room temperature it is a solid, and it is radioactive.
Structure
Not a diagram of dots on rings — a Monte-Carlo sample of the actual probability density |ψ|² for each occupied subshell. Drag to rotate. Blue and violet mark opposite signs of the wavefunction, which is what makes bonding possible.
Measured values
Every bar shows where mendelevium sits among all 118 elements for that property.
Sources: IUPAC 2021 standard atomic weights · CRC Handbook of Chemistry and Physics · NIST. Values marked ~ are predicted rather than measured.
Size, to scale
Radius 246 pm — that is 0.246 nm, so about 2033 million of them side by side would span a millimetre.
Thermal range
Mendelevium melts at 1100 K; its boiling point has not been measured.
The story
The first element produced and identified one atom at a time.
Mendelevium was discovered on February 19, 1955, by the legendary team of Albert Ghiorso, Glenn T. Seaborg, Gregory Robert Choppin, Bernard G. Harvey, and Stanley G. Thompson at the University of California, Berkeley. This discovery marked a pivotal moment in the Cold War race to synthesize new elements.
The discovery had dramatic origins in nuclear weapons testing. In 1952, the Ivy Mike thermonuclear test - a 10-megaton hydrogen bomb explosion - created enough neutron flux to produce previously unknown elements. Radioactive debris from this Pacific test contained einsteinium-253, the crucial target material needed for mendelevium synthesis.
Using Berkeley's 60-inch cyclotron, the team bombarded just one billion einsteinium atoms with alpha particles - the first time in history a new element was produced and identified "one atom at a time." On that historic February morning, they detected five characteristic fission events that proved element 101's existence.
The element was named after Dmitri Mendeleev, creator of the periodic table, honoring his prediction that elements beyond uranium would be discovered. This naming represented both scientific tribute and Cold War diplomacy, acknowledging Russian scientific contributions during tense US-Soviet relations.
Glenn T. Seaborg called the discovery "one of the most dramatic in the sequence of transuranium elements," establishing new techniques for superheavy element research that remain fundamental to modern nuclear physics. The achievement demonstrated humanity's ability to create matter that had never existed in the universe.
Applications
Mendelevium serves as a crucial stepping stone in superheavy element synthesis research, providing insights into nuclear shell structure and stability. Scientists use Md isotopes to understand the magic numbers that govern nuclear stability, particularly around the predicted "island of stability" for superheavy elements.
Research teams employ mendelevium in nuclear fission studies to investigate spontaneous fission processes and alpha decay chains. The element's relatively long half-life (77.7 minutes for 256Md) makes it invaluable for studying transuranium element chemistry and physics properties.
Mendelevium enables groundbreaking research into superheavy element chemistry, allowing scientists to study oxidation states, complex formation, and chemical behavior of elements beyond the actinide series. These studies help validate theoretical predictions about electron configuration and chemical bonding in extreme atomic environments.
Physicists use mendelevium data to refine nuclear models and calculations that predict the existence and properties of even heavier elements. This research drives the development of advanced particle accelerators and detection systems for future superheavy element discoveries.
While theoretical, understanding mendelevium's properties contributes to research on exotic matter that could potentially revolutionize space propulsion systems and energy generation technologies in the distant future.
Mendelevium's primary applications remain confined to specialized nuclear research facilities worldwide. Major laboratories including Berkeley Lab, GSI Helmholtz Centre, and RIKEN use mendelevium isotopes for fundamental nuclear physics research and superheavy element synthesis studies.
Research teams utilize mendelevium in nuclear spectroscopy experiments to measure gamma-ray emissions, alpha decay energies, and fission fragment distributions. These measurements provide critical data for understanding nuclear shell effects and predicting properties of undiscovered superheavy elements.
Mendelevium serves as a benchmark element for testing quantum mechanical calculations and nuclear models. Scientists compare experimental data from mendelevium isotopes with theoretical predictions to refine their understanding of nuclear forces and electron behavior in superheavy atoms.
The study of mendelevium drives innovation in ultra-sensitive detection systems, including time-of-flight mass spectrometry, alpha-particle detectors, and sophisticated particle identification systems that advance our ability to study extremely rare nuclear processes.
Where it comes from
0 mg/kg of Earth's crust · more abundant than 0% of elements
Mendelevium does not occur naturally on Earth or anywhere in the observable universe. This superheavy element can only be created through artificial nuclear synthesis in sophisticated particle accelerators, making it one of the rarest substances ever produced by humanity.
Scientists create mendelevium by bombarding einsteinium-253 targets with alpha particles (helium-4 nuclei) in cyclotrons or linear accelerators. The Berkeley team's original 1955 synthesis used just one billion einsteinium atoms, producing mendelevium literally "one atom at a time" - a remarkable achievement in nuclear physics.
The most stable mendelevium isotope, 258Md, has a half-life of only 51.5 days, meaning any mendelevium atoms that might have existed during Earth's formation would have decayed billions of years ago. Current production yields are measured in individual atoms or small clusters.
Worldwide production of mendelevium is estimated at fewer than a few thousand atoms per year across all research facilities combined. The element's synthesis requires rare einsteinium targets, advanced particle accelerators, and enormous amounts of energy, making it astronomically expensive to produce.
Unlike lighter elements formed in stellar nucleosynthesis, mendelevium cannot be created in stars or supernovae due to its extremely short half-life and the specific nuclear reactions required for its synthesis. It represents purely human-made matter that pushes the boundaries of atomic existence.
Handling
Mendelevium is radioactive. It has no stable isotope — every nucleus decays. Handling requires appropriate shielding and licensing.
DANGER: Mendelevium is an extremely radioactive synthetic element that poses severe health risks through alpha radiation, gamma emissions, and spontaneous fission. Even microscopic quantities require specialized containment and handling protocols in licensed nuclear facilities.
Mendelevium isotopes emit high-energy alpha particles that can cause severe radiation burns, genetic damage, and cancer if they contact living tissue. Internal contamination through inhalation or ingestion would be immediately life-threatening due to concentrated radiation dose to organs.
Research requires specialized hot cells, remote handling equipment, and continuous radiation monitoring. Personnel must wear complete radiation protection gear and work behind heavy shielding. Emergency decontamination procedures and medical radiation treatment must be immediately available.
Despite its short half-life, mendelevium contamination creates persistent radioactive hazards through decay products and fission fragments. Specialized waste disposal protocols are required for all materials that contact mendelevium, including laboratory equipment and protective clothing.
Quick answers
Mendelevium (symbol Md) is element 101 on the periodic table, a actinide in period 7. The first element produced and identified one atom at a time. At room temperature it is a solid, and it is radioactive.
[Rn] 5f¹³ 7s², giving 7 occupied shells holding 2, 8, 18, 32, 31, 8, 2 electrons respectively.Mendelevium melts at 1100 K (826.9 °C) and boils at not measured.
Mendelevium has no stable isotope, so it has no standard atomic weight. The figure quoted, 258, is the mass number of its longest-lived known isotope.
Mendelevium has a density of 10.3 g/cm³. Water is 1.0 g/cm³, so a block of mendelevium is about 10.3× heavier.
Mendelevium has a Pauling electronegativity of 1.3. The scale runs from 0.70 (francium, the least greedy for electrons) to 3.98 (fluorine, the most). Values in this middle band tend to form covalent rather than strongly ionic bonds.
Mendelevium was discovered in 1955 by Ghiorso et al.. It is named after dmitri Mendeleev.
Mendelevium does not occur naturally on Earth in any meaningful quantity — it is made in a reactor or an accelerator.
Yes. Mendelevium has no stable isotope — every one of its nuclei decays. It does not occur in usable quantities in nature and must be synthesised.