热处理
熱處理
열처리
HEAT TREATMENT
2014年
3期
1-7
,共7页
马氏体相变%切变%表面浮凸%不变平面应变%马氏体相变晶体学表象理论%惯习面
馬氏體相變%切變%錶麵浮凸%不變平麵應變%馬氏體相變晶體學錶象理論%慣習麵
마씨체상변%절변%표면부철%불변평면응변%마씨체상변정체학표상이론%관습면
martensitic transformation%shear%surface relief%invariable plane strain%phenomenological theory of martensite crystallography%habit plane
自20世纪20年代以来,基于马氏体相变产生的浮凸和在母相中预先刻制的直线变成在相界面上连续的折线,提出了以切变为基础的马氏体相变的晶体学特征-“不变平面应变”的概念。随后,以该概念为基础建立了马氏体相变晶体学表象理论( PTMC)。然而,刘宗昌等基于相同的实验,即马氏体相变后的直线刻痕仍为直线和浮凸形态为帐篷形,分别在2010年和2013年《热处理》杂志上发表文章,否定马氏体相变的“切变”机制进而否定马氏体相变的“不变平面应变”。如所周知,否定马氏体相变的“切变机制”就是否定“不变平面应变”,因此刘宗昌等于2013年发表的文章彰显出他们的轻率。本文作者已在3篇文章中列举用原子力显微镜和透射电镜观察的结果驳斥了他们的错误观点,至少可以说,他们没有理解我们文章中的实验和理论。为此,本文再次引用Yang 和Wayman的透射电镜实验结果,即单变体马氏体使预存在的层错迹线(直线)变成折线,而自协调的多个马氏体可使迹线仍为直线;单变体马氏体的浮凸为N形,但多变体马氏体的浮凸可以是帐篷形或更为复杂的形态,由此可以说明刘宗昌等错误观点的原因。最近,本文作者及其合作者基于PTMC计算了Mn80Fe15Cu5热弹性合金马氏体相变的惯习面,并与实验结果相符,由此确认了“不变平面应变”是马氏体相变晶体学特征的正确性。
自20世紀20年代以來,基于馬氏體相變產生的浮凸和在母相中預先刻製的直線變成在相界麵上連續的摺線,提齣瞭以切變為基礎的馬氏體相變的晶體學特徵-“不變平麵應變”的概唸。隨後,以該概唸為基礎建立瞭馬氏體相變晶體學錶象理論( PTMC)。然而,劉宗昌等基于相同的實驗,即馬氏體相變後的直線刻痕仍為直線和浮凸形態為帳篷形,分彆在2010年和2013年《熱處理》雜誌上髮錶文章,否定馬氏體相變的“切變”機製進而否定馬氏體相變的“不變平麵應變”。如所週知,否定馬氏體相變的“切變機製”就是否定“不變平麵應變”,因此劉宗昌等于2013年髮錶的文章彰顯齣他們的輕率。本文作者已在3篇文章中列舉用原子力顯微鏡和透射電鏡觀察的結果駁斥瞭他們的錯誤觀點,至少可以說,他們沒有理解我們文章中的實驗和理論。為此,本文再次引用Yang 和Wayman的透射電鏡實驗結果,即單變體馬氏體使預存在的層錯跡線(直線)變成摺線,而自協調的多箇馬氏體可使跡線仍為直線;單變體馬氏體的浮凸為N形,但多變體馬氏體的浮凸可以是帳篷形或更為複雜的形態,由此可以說明劉宗昌等錯誤觀點的原因。最近,本文作者及其閤作者基于PTMC計算瞭Mn80Fe15Cu5熱彈性閤金馬氏體相變的慣習麵,併與實驗結果相符,由此確認瞭“不變平麵應變”是馬氏體相變晶體學特徵的正確性。
자20세기20년대이래,기우마씨체상변산생적부철화재모상중예선각제적직선변성재상계면상련속적절선,제출료이절변위기출적마씨체상변적정체학특정-“불변평면응변”적개념。수후,이해개념위기출건립료마씨체상변정체학표상이론( PTMC)。연이,류종창등기우상동적실험,즉마씨체상변후적직선각흔잉위직선화부철형태위장봉형,분별재2010년화2013년《열처리》잡지상발표문장,부정마씨체상변적“절변”궤제진이부정마씨체상변적“불변평면응변”。여소주지,부정마씨체상변적“절변궤제”취시부정“불변평면응변”,인차류종창등우2013년발표적문장창현출타문적경솔。본문작자이재3편문장중열거용원자력현미경화투사전경관찰적결과박척료타문적착오관점,지소가이설,타문몰유리해아문문장중적실험화이론。위차,본문재차인용Yang 화Wayman적투사전경실험결과,즉단변체마씨체사예존재적층착적선(직선)변성절선,이자협조적다개마씨체가사적선잉위직선;단변체마씨체적부철위N형,단다변체마씨체적부철가이시장봉형혹경위복잡적형태,유차가이설명류종창등착오관점적원인。최근,본문작자급기합작자기우PTMC계산료Mn80Fe15Cu5열탄성합금마씨체상변적관습면,병여실험결과상부,유차학인료“불변평면응변”시마씨체상변정체학특정적정학성。
Since 1920’ s, based on the fact that both the surface relief produced by martensitic transformation and a previously marked straight-line scratch changing into a continuous fold line at martensite-austenite interface , the concept of invariable plane strain as the crystallography characteristic of martensitic transformation on the basis of the shear was proposed .Subsequently , the phenomenological theory of martensite crystallography ( PTMC ) was built on the basis of the invariable plane strain .In 2010 and 2013 in《Heat Treatment》,however , LIU Zongchang et al published papers where they denied the shear mechanism and further denied the invariable plane strain for martensitic transformation according to their experimental results that a straight-line scratch do not change and the relief exhibits tent-shaped after the martensitic transformation .It is well known that to deny the shear mechanism of martensitic transformation is to deny the invariable plane strain and , therefore , LIU et al publishing paper in 2013 is from haste . Author of this paper criticized their wrong viewpoints by results obtained from atomic force microscopy and transmission electron microscopy observations in three published papers .It is at least said that LIU et al do not understand experiments and the related theories in three papers mentioned above . Therefore , experimental results of Yang and Wayman , that is, the trace of stacking fault (straight line) will change into the fold line when it is shorn by a single martensitic variant , but still is a straight line when it is shorn by multiple martensitic variants with self-accommodation , and the surface relief may exhibit N -shaped for a single martensitic variant and tent-shaped or more complex shape for two or more martensitic variants , were cited again in this paper , which may reveal the origin of LIU et als ’ wrong viewpoint .Recently , the habit plane of martensitic transformation in a Mn80Fe15Cu5 thermoelastic alloy is calculated by author and co-authors of this paper based on PTMC , and the calculated result was well consistent with the experimental result , which may confirm that the invariable plane strain is crystallography characteristic of martensitic transformation .