针对红土镍矿在焙烧过程中物相转变及固结机制问题,对原矿进行了化学成分、X射线衍射(XRD)分析,得知红土镍矿主要以Fe2O3和单斜形蛇纹石矿物为主,另外含有部分十字沸石和利蛇纹石；通过热重(TG)、差热(DTA)测试,得到了在焙烧过程中,自然水、结晶水及羟基分别在195,293和612℃被脱除,在830℃时,部分硅酸盐发生物相转变；并用Factsage软件对红土矿在加热过程中液相的产生量进行了理论计算,当焙烧温度为1220℃时红土矿球团开始产生液相.在实验室中,利用箱式电阻炉进行球团焙烧实验,结果表明,焙烧球团的抗压强度和落下强度随着焙烧温度和时间的增加而增大,焙烧温度低于1200℃时,球团依靠固相反应和再结晶固结,抗压强度及落下强度较低；焙烧温度达到1300℃时,红土矿会产生34％的液相,冷却后使球团固结,抗压强度和落下强度大大增加；当焙烧温度一定时,球团抗压强度和落下强度随焙烧时间的延长而增加,但是球团的强度增加幅度较小.
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