scholarly journals An investigation into the permeability of a PGM slag freeze lining to sulphur

Author(s):  
H. Steenkamp ◽  
A.M. Garbers-Craig
Keyword(s):  
JOM ◽  
2021 ◽  
Author(s):  
Samant Nagraj ◽  
Mathias Chintinne ◽  
Muxing Guo ◽  
Bart Blanpain

AbstractFreeze lining is a solidified layer of slag formed on the inner side of a water-cooled pyrometallurgical reactor, which protects the reactor walls from thermal, physical, and chemical attacks. Because of the freeze lining's high thermal resistance, the reactor heat losses strongly depend on the freeze lining thickness. In a batch process such as slag fuming, the conditions change with time, affecting the freeze lining thickness. Determining the freeze lining thickness is challenging as it cannot be measured directly. In this study, a conceptual framework based on the morphology and microstructure of freeze lining and the rheology of the slag is discussed and experimentally evaluated to determine the freeze lining thickness. It was found that the bath/freeze lining interface lies just below critical viscosity temperature. The growth of the freeze lining is primarily controlled by the mechanical and thermal degradation of the crystals forming at the interface. The bath/freeze lining interface temperature for the measured slag lies in the range of 1035–1070°C.


Author(s):  
Liugang Chen ◽  
Muxing Guo ◽  
Shuigen Huang ◽  
Peter Tom Jones ◽  
Bart Blanpain ◽  
...  
Keyword(s):  

2013 ◽  
Vol 45 (3) ◽  
pp. 864-874 ◽  
Author(s):  
Ata Fallah-Mehrjardi ◽  
Jani Jansson ◽  
Pekka Taskinen ◽  
Peter C. Hayes ◽  
Evgueni Jak

2009 ◽  
Vol 40 (5) ◽  
pp. 632-642 ◽  
Author(s):  
Mieke Campforts ◽  
Evgueni Jak ◽  
Bart Blanpain ◽  
Patrick Wollants

2013 ◽  
Vol 53 (1) ◽  
pp. 1-10 ◽  
Author(s):  
J. Jansson ◽  
P. Taskinen ◽  
M. Kaskiala

2013 ◽  
Vol 53 (1) ◽  
pp. 11-16 ◽  
Author(s):  
J. Jansson ◽  
P. Taskinen ◽  
M. Kaskiala

2015 ◽  
Vol 51 (1) ◽  
pp. 41-48 ◽  
Author(s):  
J. Jansson ◽  
P. Taskinen ◽  
M. Kaskiala

The initial growth rate of freeze linings on water-cooled elements submerged in molten iron silicate slag is fast. The freeze lining microstructure forming on water cooled steel surface in a high-silica, slag cleaning furnace slag of a direct-to-blister copper smelter is mostly glassy or amorphous. It contains 5-30 ?m magnetite crystals, very small and larger copper droplets as well as small magnetite and silicate nuclei embedded in the glassy silica-rich matrix. Chemically the formed freeze linings are more silica-rich than the slag from which they were generated. Magnetite (spinel) is the primary phase of the solidifying SCF slag but it does not form a continuous network through the freeze lining. Its strength is given by the intergranular silica-rich phase which initially is glassy or microcrystalline. Due to only partial slag reduction in the SCF process, large magnetite crystals are present in the freeze lining and seem to interact physically with copper droplets.


2019 ◽  
Vol 116 (6) ◽  
pp. 635 ◽  
Author(s):  
Juhani Heimo ◽  
Ari Jokilaakso ◽  
Marko Kekkonen ◽  
Merete Tangstad ◽  
Anne Støre

In ilmenite smelting furnaces, a freeze lining of solidified slag is used to protect the furnace refractories against the aggressive titanium slag. Freeze lining thickness cannot be measured directly due to harshness of conditions inside the process, thus process modelling is required. Several parameters influence the thickness of the freeze-lining, one of them being thermal conductivity of the frozen slag. However, there is a lack of thermal conductivity values for high titanium slags −especially as a function of temperature. In this study, thermal conductivity of three titanium slag samples and an additional sample of freeze-lining was measured from room temperature to 1100/1400 °C with the laser flash analysis method. In addition, thermal expansion and microstructures of the samples were studied to provide an extensive understanding of how microstructure will affect thermal conductivity. The thermal conductivity of the slag samples was found to increase from 1.2 to a maximum of 2.4 W/(m K) when increasing temperature from room temperature to 1100 °C. An additional experiment at 1400 °C showed that the thermal conductivity increased further as the temperature increased. The freeze-lining sample behaves differently, with conductivity being the highest at room temperature, 2.2 W/(m K).


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