Water-Bentonite Interaction of Iron Ore Green Pellets Through Micro-Structural Analysis

"The quality of pellets produced is affected by quality anssastd quantity of green pellets, amount of addition of binders, type of binders added, amount of moisture added along with the other variables like rotation, inclination and fineness of feed. The green pellet quality depends upon chemistry, mineralogy and granulometry of fines used for pellet making, the feed size, its moisture content and porosity. During firing of green pellets ingredients present within reacts to form different phases and microstructure. So in turn physical and metallurgical properties of pellets are influenced by amount and type of binder and flux addition, induration time and temperature. During iron making process, the metallurgical properties of fired pellets are decided by the type and amount of these phases and their chemistry. Green pelletizing and induration studies have been already carried out with hematite ore fines. Indian iron ores of high alumina content showing different pelletizing characters, these studies can’t be directly interpreted. The main objective of proposed research work is to understand the green pelletizing process and determine the water bentonite interaction at different levels. Detailed investigation on swelling behavior of bentonite and microstructure of the green pellets of iron ore fines from SAIL captive iron ore fines from the Barsua in the state of Odisha. To convert these ore fines into pellets, the key raw material, additives and process variables that influence the pellet quality needs to be identified.INTRODUCTION Pelletization is the unit operation of agglomerating iron bearing fines (generally below 150µ with 65-80% passing 40µ) by tumbling in horizontal rotating drums or inclined discs, (Sivrikaya and Arol, 2013; Bhuiyan et al., 2011; Forsmo et al., 2006; Sastry et al., 2003) and the pellets are approximately spherical lumps formed by this process in presence of water and binder, on subsequent induration at 1300°c (Sivrikaya and Arol, 2014; Sivrikaya and Arol, 2013; Sivrikaya and Arol, 2012; Sivrikaya and Arol, 2010; Sastry et al., 2003; Kawatra and Ripke, 2003; Iveson, 2001a; Iveson, 2001b)."