USGS Mineral Resources Program
Niobium and Tantalum—Indispensable Twins
As part of a broad mission to
conduct research and provide
information on nonfuel mineral
resources, the U.S. Geological
Survey (USGS) supports science
to understand
• How and where niobium and
tantalum resources form and
concen trate in the Earth’s crust
• How niobium and tantalum
resources interact with the
environment to affect human
and ecosystem health
• Trends in the supply of and
demand for niobium and
tantalum in the domestic and
international markets
• Where undiscovered sources
of niobium and tantalum
might be found
Why is this information important?
Read on to learn about niobium
and tantalum and the important
role they play in the national
economy, in national security, and
in the lives of Americans every day.
Niobium and tantalum are transition metals almost always paired together in nature. These “twins”
are difficult to separate because of their shared physical and chemical properties. In 1801, English chemist
Charles Hatchett uncovered an unknown element in a mineral sample of columbite; John Winthrop
found the sample in a Massachusetts mine and sent it to the British Museum in London in 1734.
The name columbium, which Hatchett named the new element, came from the poetic name for North
America—Columbia—and was used interchangeably for niobium until 1949, when the name niobium
became official. Swedish scientist Anders Ekberg discovered tantalum in 1802, but it was confused
with niobium, because of their twinned properties, until 1864, when it was recognized as a separate
element. Niobium is a lustrous, gray, ductile metal with a high melting point, relatively low density, and
superconductor properties. Tantalum is a dark blue-gray, dense, ductile, very hard, and easily fabricated
metal. It is highly conductive to heat and electricity and renowned for its resistance to acidic corrosion.
These special properties determine their primary uses and make niobium and tantalum indispensable.
How Do We Use Niobium and Tantalum?
The steel industry uses nearly 80 percent of the
world’s produced niobium to manufacture high-
strength low-alloy steels. Niobium, a grain refiner
and precipitation hardener, enhances the steels’
mechanical strength, toughness, high-temperature
strength, and corrosion resistance for use in
pipelines, transportation, and structural applications.
Appreciable amounts (>20 percent) of niobium are
used in nickel-, cobalt-, and iron-based superalloys
for high-temperature applications in jet engines,
gas turbines, rocket subassemblies, turbocharger
systems, and combustion equipment. Niobium
alloys are used to manufacture superconducting
magnets for medical hardware such as magnetic
resonance imaging (MRI) and nuclear magnetic
resonance (NMR) instruments. A new use of
niobium is in a solid niobic acid that catalyzes the
conversion of palm oil to bio-diesel fuel. Niobium’s uses are specialized; substituting an alternative
can lead to reduced performance and increased cost.
Tantalum has a unique ability to store and release energy, which is why the electronics industry
consumes more than one-half of tantalum production. Tantalum-based components can be exceptionally
small, and other elements cannot serve as substitutes without degrading the performance of electronic
devices. As a result, tantalum is used in components for items as ubiquitous as cell phones, hearing aids,
and hard drives. Tantalum’s low mechanical strength and high biocompatibility allow it to coat stronger
substrates, like stainless steel, for medical applications. It is used for blood vessel support stents, plates,
bone replacements, and suture clips and wire. In the chemical industry, tantalum’s corrosion resistance makes
it useful as a lining for pipes, tanks, and vessels. Tantalum oxide can increase the refractive index of lens glass,
while the hardness of tantalum carbide makes it an ideal component in the manufacture of cutting tools.
Where Do Niobium and Tantalum Come From?
The average abundance of niobium and tantalum in bulk continental crust is low, with 8.0 parts per
million (ppm) niobium and 0.7 ppm tantalum. Their chemical characteristics reduce their potential to
substitute for more common elements in rock-forming minerals and make them practically immobile in
many aqueous solutions. Niobium and tantalum do not occur naturally as pure metals, but are concentrated
in rare oxide and hydroxide minerals and in a few rare silicate minerals. The economically important ore
minerals for niobium and tantalum production are all oxides. Niobium is primarily derived from the complex
oxide minerals of the pyrochlore group ((Na,Ca,Ce)
2
(Nb,Ti,Ta)
2
(O,OH,F)
7
), which are found in some
alkaline (igneous rocks containing certain sodium- or potassium-rich minerals) granite-syenite and carbon-
atite complexes (igneous rocks composed more than 50 percent by volume of primary carbonate minerals).
Tantalum is derived mainly from the mineral tantalite ((Fe,Mn)(Ta,Nb)
2
O
6
), which is found as an accessory
mineral in rare-metal granites and pegmatites enriched in lithium and cesium (termed the LCT family).
Launch of the Gemini 12 space
mission (image courtesy of NASA).
Thousands of pounds of niobium
have been used in advanced air
frame systems such as were used
in the Gemini space program.
Nb
[Kr]5s
1
4d
4
41
92.91
Ta
[Xe]6s
2
4f
14
5d
3
73
180.9
Central view of the ATLAS detector in the Large Hadron
Collider with its eight superconducting magnets (toroids)
around the calorimeter (note person standing in lower
center of photograph for scale). This is the world’s
largest superconducting magnet. (Image from European
Council for Nuclear Research [CERN]).
U.S. Department of the Interior
U.S. Geological Survey
Fact Sheet 2014 –3054
June 2014
Toroids
Did you know...
Niobium alloys are contained in the superconducting magnets used in particle accelerators
like
the
Large
Hadron
Collider
in
Europe.
Did you know...
Niobium is widely used for body piercing, and when put through an anodizing process results
in varying colors of jewelry without the use of toxic inks or dyes.
The Future of Niobium and Tantalum: Worldwide Supply and Demand
Estimated global reserves and resources of niobium and tantalum are large and more
than sufficient to meet global demand for the foreseeable future, possibly the next 500 years.
Therefore, geologic availability does not appear to be a major concern for the supply
of niobium or tantalum. Brazil, Canada, and Australia are the leading global producers
of niobium and tantalum mineral concentrates. Brazil produces the greatest amount of
niobium mineral concentrates (~90 percent), while Australia and Brazil together lead in
the production of tantalum mineral concentrates. A number of African countries—Burundi,
Democratic Republic of Congo, Ethiopia, Mozambique, Nigeria, Rwanda, Uganda—mine
for tantalum minerals (such as columbite-tantalite, also called coltan) through artisanal
mining or are establishing mining operations. Primary production of niobium or tantalum in
the United States has not been reported since the late 1950’s; therefore, the United States
has to meet its current and expected future needs by importing primary mineral concentrates
and alloys, and by recovering them from foreign and domestic alloy scrap.
Fluctuating market conditions, as with the recent worldwide economic
crises, interrupted operations at a number of production sites, and future
economic instability has the potential to generate supply problems. Other
possible disruptions include war, civil unrest, political changes, natural
disasters, environmental issues and market manipulation. For example, rebel
sales of “conflict coltan” in the Democratic Republic of Congo, amidst a civil
war, have led to discussions about supply-line transparency and traceability as
tools for excluding illegal columbite-tantalite while keeping the market open
for legitimate, small-scale artisanal mining in central Africa.
To help predict where future niobium and tantalum supplies might be
found, USGS scientists study how and where these resources are concentrated
in the Earth’s crust and then assess the likelihood that undiscovered resources
may exist. Techniques to assess mineral resource potential have been
developed by the USGS to support the stewardship of Federal lands and
better evaluate mineral resource availability in a global context. The USGS
also compiles statistics and information on the worldwide supply, demand,
and flow of niobium and tantalum. These data help support the U.S. economy
and national security.
ISSN 2327– 6932 (online)
http://dx.doi.org/10.3133/fs20143054
The USGS Mineral Resources Program is the principal
Federal provider of research and information on niobium,
tantalum, and other nonfuel mineral resources.
For more information, please contact:
Mineral Resources Program Coordinator
U.S. Geological Survey
913 National Center
Reston, VA 20192
Telephone: 703–648–6100
Fax: 703–648–6057
Email: minerals@usgs.gov
Home page: http://minerals.usgs.gov
For More Information
• On production and consumption of niobium and tantalum:
http://minerals.usgs.gov/minerals/pubs/commodity/niobium/
• On historical statistics on niobium and tantalum:
http://minerals.usgs.gov/ds/2005/140/
• On recycling of niobium and tantalum in the United States:
http://pubs.usgs.gov/circ/2004/1196am/
Any use of trade, firm, or product names is for descriptive purposes
only and does not imply endorsement by the U.S. Government.
Capacitor from Fotosearch Stock Images at www.fotosearch.com
Nb
[Kr]5s
1
4d
4
41
92.91
Ta
[Xe]6s
2
4f
14
5d
3
73
180.9
Text prepared by Klaus Schulz and John Papp.
High-purity niobium crystals, electrolytic made, as well
as a high-purity 1 cubic centimeter anodized niobium
cube for comparison (photograph from Wikipedia).
The large Mibra (Volta Grande) open-pit pegmatite mine operated
by Companhia Industrial Fluminense’s in Brazil (Itamar Resende).
(Image from Tantalum-Niobium International Study Center).