XRD, Thermal Analysis and Clay Mineralogy | Thermal analysis
What does thermal analysis do?
Thermal analysis is a term for a group of methods that involve
measuring and interpreting a range of properties that occur when
a sample is subjected to a controlled heating programme, typically
from ambient – 1000 °C.
Thermal analysis techniques are employed to study both inorganic
and organic reactions and by comparison with reaction stoichiometry
can be used to identify, characterise and quantify the nature of
geological and soil materials.
For earth science applications, thermal analyses are particularly
useful in studying carbonate-, clay- and hydrated mineral-bearing
samples.
Thermal analyses are often most usefully performed in tandem with
X-ray diffraction analyses (click here for
more information).
How do thermal analyses work?
Thermogravimetric analysis (TGA) involves measuring the mass change
of a substance as a function of temperature through a controlled
heating programme. Results are presented as a plot of mass against
temperature or time and any mass loss or gain is therefore presented
as a step in the generated profile. Derivative (DTG) curves may also
be presented to indicate the rate of mass loss/gain and facilitate
the identification of overlapping reactions.
Allied techniques such as Differential Thermal Analysis (DTA) detect
thermal changes (exothermic or endothermic) in a sample in response
to heating or cooling by reference to an inert reference. Typically,
a DTA curve will be presented alongside a TG/DTG curves to aid interpretation.
Evolved Gas Analysis (EGA) measures and investigates the amount
of volatile products released by a sample during a controlled heating
programme. By calculating the masses of gas evolved, the presence
of very low levels of mineral species can be determined.
Equipment?
VState-of-the-art Mettler-Toledo SDTA/TGA 851e simultaneous
thermal analysis system, 34-position sample changer, high temperature
furnace (1500 ºC) for either routine or research analyses.
EGA system including Stanton Redcroft tube furnaces linked to separate
infrared detectors monitoring CO2, CO, H2O, SO2 and
NH3.
Applications?
The thermal analysis laboratory at Keyworth plays a key role in projects
that span the BGS science programme, for example:
detection and quantification of low levels of carbonate species
for radioactive waste disposal and CO2 capture/storage
quantification of kaolinite in beneficiation trials leading to
the development of industrial mineral deposits
characterisation of carbonate mineralogy as part of limestone assessment
surveys
determining the contribution of carbonate minerals to the engineering
behaviour of rocks and soils
Staff and facilities are also in constant demand for direct consultancy
analysis and interpretation by external clients including: oil, mineral
and mining companies, engineering and utility companies, consultancies,
university departments and local authorities.