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Table 3 Peak temperatures of DSC endotherms for all samples and all four oven pressures used, arranged in order of increasing peak temperatures at 1000 mbar

From: The effects of instrument parameters and sample properties on thermal decomposition: interpreting thermal analysis data from Mars

Sample

Decomposition type (source of gas released)

DSC peak temperature (°C)

12 mbar

30 mbar

150 mbar

1000 mbar

Epsomite

H2O (structural H2O)

94.2

107.9

103.1

127.8

Montmorillonite

H2O (cation solvation water)

87.3

97.9

111.6

135.0

Goethite

H2O (structural OH)

297.8

304.4

312.0

327.4

Kieserite

H2O (structural H2O)

392.7

394.8

395.4

404.4

Kaolinite

H2O (structural OH)

503.6

506.3

509.5

524.7

Alunite

H2O (structural OH)

563.4

564.3

566.9

570.0

Magnesite

CO2 loss (carbonate decomposition)

595.0

605.3

615.3

628.6

Alunite

H2O (structural OH)

631.8

637.1

642.6

642.3

Montmorillonite

H2O (structural OH)

699.3

702.2

712.1

763.9

Alunite

SO2 loss (sulfate decomposition)

767.6

766.1

769.2

782.6

Calcite (<150 μm)

CO2 loss (carbonate decomposition)

719.0

736.2

766.2

807.0

Calcite (3 mm crystals)

CO2 loss (carbonate decomposition)

933.7

938.3

954.9

971.7

Epsomite

SO2 loss (sulfate decomposition)

951.9

972.3

1033.4

1105.7

Kieserite

SO2 loss(sulfate decomposition)

1062.6

1081.8

1100.4

1162.1

  1. Decomposition type shows what is being lost in the decomposition and measured by the EGA, with the source of the gas loss specified.