磁性材料及器件
磁性材料及器件
자성재료급기건
JOURNAL OF MAGNETIC MATERIALS AND DEVICES
2013年
3期
49-52,61
,共5页
陈杰%程玲莉%张明%徐光亮%高旭山
陳傑%程玲莉%張明%徐光亮%高旭山
진걸%정령리%장명%서광량%고욱산
NdFeB 磁体%热退磁%磁通%金相形貌%磁畴结构
NdFeB 磁體%熱退磁%磁通%金相形貌%磁疇結構
NdFeB 자체%열퇴자%자통%금상형모%자주결구
NdFeB permanent magnet%thermal demagnetization%flux%metallurgical morphology%magnetic domain structure
对高磁能积 NdFeB 永磁体的热退磁机理进行了分析。首先测量并研究永磁体开路磁通随温度的宏观变化,然后采用多功能显微镜、热分析仪及 X 射线衍射仪观察了高温金相形貌并分析了物相和表面成分变化,借助磁力显微镜观察了磁畴结构,从而分析了永磁体的热退磁机理。高温金相观察结果表明,在320℃以内,除金相形貌的颜色发生变化外,晶粒形状及尺寸均未发生明显变化;XRD 分析表明,金相形貌的颜色变化是表面氧化所致,说明磁体在320℃以内的热退磁现象与金相结构无关,即热退磁不是由金相结构变化引起的。320℃以后,XRD 及高温金相分析表明表面氧化变严重,尤其在580℃时有富 Nd 相熔融物析出,晶界模糊、大晶粒吞并小晶粒,金相结构发生明显变化。但磁畴观察结果表明,320℃内热退磁前后磁化强度方向发生偏转,方向一致性变差,是热退磁的原因所在。
對高磁能積 NdFeB 永磁體的熱退磁機理進行瞭分析。首先測量併研究永磁體開路磁通隨溫度的宏觀變化,然後採用多功能顯微鏡、熱分析儀及 X 射線衍射儀觀察瞭高溫金相形貌併分析瞭物相和錶麵成分變化,藉助磁力顯微鏡觀察瞭磁疇結構,從而分析瞭永磁體的熱退磁機理。高溫金相觀察結果錶明,在320℃以內,除金相形貌的顏色髮生變化外,晶粒形狀及呎吋均未髮生明顯變化;XRD 分析錶明,金相形貌的顏色變化是錶麵氧化所緻,說明磁體在320℃以內的熱退磁現象與金相結構無關,即熱退磁不是由金相結構變化引起的。320℃以後,XRD 及高溫金相分析錶明錶麵氧化變嚴重,尤其在580℃時有富 Nd 相鎔融物析齣,晶界模糊、大晶粒吞併小晶粒,金相結構髮生明顯變化。但磁疇觀察結果錶明,320℃內熱退磁前後磁化彊度方嚮髮生偏轉,方嚮一緻性變差,是熱退磁的原因所在。
대고자능적 NdFeB 영자체적열퇴자궤리진행료분석。수선측량병연구영자체개로자통수온도적굉관변화,연후채용다공능현미경、열분석의급 X 사선연사의관찰료고온금상형모병분석료물상화표면성분변화,차조자력현미경관찰료자주결구,종이분석료영자체적열퇴자궤리。고온금상관찰결과표명,재320℃이내,제금상형모적안색발생변화외,정립형상급척촌균미발생명현변화;XRD 분석표명,금상형모적안색변화시표면양화소치,설명자체재320℃이내적열퇴자현상여금상결구무관,즉열퇴자불시유금상결구변화인기적。320℃이후,XRD 급고온금상분석표명표면양화변엄중,우기재580℃시유부 Nd 상용융물석출,정계모호、대정립탄병소정립,금상결구발생명현변화。단자주관찰결과표명,320℃내열퇴자전후자화강도방향발생편전,방향일치성변차,시열퇴자적원인소재。
The demagnetization mechanism of high energy product NdFeB permanent magnet was analyzed. Firstly, changes of open-circuit magnet flux with temperature were studied. And then high-temperature metallurgical phase as well as surface composition changes were observed and analyzed using multi-functional metallographic microscope, thermal analysis instrument and X-ray diffraction, respectively. Finally we studied the phase magnetic domain structure of sintered NdFeB permanent magnet after magnetization and high-temperature treatment using magnetic force microscopy (MFM). The experimental results showed that in addition to changes in color of microstructure morphology, no obvious change occurs in grain shape and size below 320℃. XRD analysis showed that the color change is due to surface oxidation, which indicates that thermal demagnetization below 320℃ has nothing to do with the metallurgical structure. XRD and metallographic analysis also showed that surface oxidation becomes serious above 320℃, especially at 580℃ melting Nd-rich phase precipitates, the grain boundary became fuzzy and large grain annexes small one. However, magnetic domain observation showed that, magnetization direction changes after thermal demagnetization below 320℃, which is the fundamental reason for thermal demagnetization.