The O-line model is usually applied to precipitation crystallography.Its application to investigation of martensite crystallography has received little attention.In this paper,the relationship between O-line model and...The O-line model is usually applied to precipitation crystallography.Its application to investigation of martensite crystallography has received little attention.In this paper,the relationship between O-line model and the prism matching model for martensite crystallography is established.The formulas in the O-line model are applicable to martensite crystallography.Analytical solution of the habit plane corresponding to the minimum shape strain has been derived.A calculation example of {3 10 15}f martensite in a ferrous alloy is provided.While the results are in agreement with the former models for martensite crystallography,the advantage of O-line model is that it offers analytical solutions,facilitating further systematic investigations.展开更多
目的探讨miR-21在肾透明细胞癌中的表达及其临床意义,以及如何通过调节程序性细胞死亡因子4(programmed cell death 4,PDCD4)的表达影响786-O肾透明细胞癌细胞系的增殖和凋亡。方法通过分析The Cancer Genome Atlas(TCGA)肾透明细胞癌...目的探讨miR-21在肾透明细胞癌中的表达及其临床意义,以及如何通过调节程序性细胞死亡因子4(programmed cell death 4,PDCD4)的表达影响786-O肾透明细胞癌细胞系的增殖和凋亡。方法通过分析The Cancer Genome Atlas(TCGA)肾透明细胞癌数据库,比较癌组织及正常癌旁组织中miR-21的表达水平;分析miR-21表达水平在不同临床病理分期肾癌组织中的差异;采用Kaplan-Meier法和对数秩和检验(Log-rank test)研究miR-21表达水平和患者生存之间的关系;通过转染miR-21抑制性核苷酸(AS-miR-21)下调miR-21表达水平,采用MTT和流式细胞术分别检测细胞增殖和凋亡,采用实时定量PCR(qRT-PCR)和Western blot测量PDCD4mRNA和蛋白质表达水平变化,采用双荧光素报告系统检测miR-21对PDCD4的直接调节。结果肾透明细胞癌组织中miR-21的表达水平显著高于癌旁组织(P<0.000 1)。miR-21在Ⅲ期和Ⅳ期肾癌组织中表达水平显著高于Ⅰ期(P均<0.000 1),miR-21表达水平与临床病理分期呈正相关(r=0.262,P<0.000 1)。miR-21表达水平与T分期(r=0.250,P<0.000 1)与淋巴结转移阳性(N1)以及远处转移均呈正相关(P均<0.001)。生存分析显示miR-21高表达患者中位生存时间显著短于miR-21低表达者中位生存时间(Log-rank,P<0.001)。下调miR-21后,786-O细胞的增殖能力较对照显著降低(P<0.05),凋亡显著增加(P=0.005),PDCD4mRNA(P=0.002)和蛋白质表达水平显著增高。双荧光素报告实验显示在转染AS-miR-21的细胞内PDCD4相对荧光强度较对照细胞显著升高(P=0.003)。结论 miR-21在肾透明细胞癌组织中表达升高,与患者临床病理分期呈正相关,和患者生存呈负相关;miR-21可能通过调节PDCD4表达水平,参与调节肾透明细胞癌细胞的增殖和凋亡。展开更多
Faceted interphase boundaries(IPBs)are commonly observed in lath-shaped precipitates in alloys consisting of simple face-centred cubic(fcc),body centred-cubic(bcc)or hexagonal closed packed(hcp)phases,which normally c...Faceted interphase boundaries(IPBs)are commonly observed in lath-shaped precipitates in alloys consisting of simple face-centred cubic(fcc),body centred-cubic(bcc)or hexagonal closed packed(hcp)phases,which normally contain one or two sets of parallel dislocations.The influence of these dislocations on interface migration and possible accompanying long-range strain field remain unclear.To elucidate this,we carried out atomistic simulations to investigate the dislocation-mediated migration processes of IPBs in a pure-iron system.Our results show that the migration of these IPBs is accompanied with the slip of interfacial dislocations,even in high-index slip planes,with two migration modes were observed:the first mode is the uniform migration mode that occurs only when all of the dislocations slip in a common slip plane.A shear-coupled interface migration was observed for this mode.The other interfaces propagate in the stick-slip migration mode that occurs when the dislocations glide on different slip planes,involving dislocation reaction or tangling.A quantitative relationship was established to link the atomic displacements with the dislocation structure,slip plane,and interface normal.The macroscopic shear deformation due to the effect of overall atomic displacement shows a good agreement with the results obtained based on the phenomenological theory of martensite crystallography.Our findings have general implications for the understanding of phase transformations and the surface relief effect at the atomic scale.展开更多
基金supported by the National Natural Science Foundation of China (Grant No. 50971076)
文摘The O-line model is usually applied to precipitation crystallography.Its application to investigation of martensite crystallography has received little attention.In this paper,the relationship between O-line model and the prism matching model for martensite crystallography is established.The formulas in the O-line model are applicable to martensite crystallography.Analytical solution of the habit plane corresponding to the minimum shape strain has been derived.A calculation example of {3 10 15}f martensite in a ferrous alloy is provided.While the results are in agreement with the former models for martensite crystallography,the advantage of O-line model is that it offers analytical solutions,facilitating further systematic investigations.
基金financially supported by the National Natural Science Foundation of China (Nos.51471097 and 51671111)the National Key Research and Development Program of China (No. 2016YFB0701304)
文摘Faceted interphase boundaries(IPBs)are commonly observed in lath-shaped precipitates in alloys consisting of simple face-centred cubic(fcc),body centred-cubic(bcc)or hexagonal closed packed(hcp)phases,which normally contain one or two sets of parallel dislocations.The influence of these dislocations on interface migration and possible accompanying long-range strain field remain unclear.To elucidate this,we carried out atomistic simulations to investigate the dislocation-mediated migration processes of IPBs in a pure-iron system.Our results show that the migration of these IPBs is accompanied with the slip of interfacial dislocations,even in high-index slip planes,with two migration modes were observed:the first mode is the uniform migration mode that occurs only when all of the dislocations slip in a common slip plane.A shear-coupled interface migration was observed for this mode.The other interfaces propagate in the stick-slip migration mode that occurs when the dislocations glide on different slip planes,involving dislocation reaction or tangling.A quantitative relationship was established to link the atomic displacements with the dislocation structure,slip plane,and interface normal.The macroscopic shear deformation due to the effect of overall atomic displacement shows a good agreement with the results obtained based on the phenomenological theory of martensite crystallography.Our findings have general implications for the understanding of phase transformations and the surface relief effect at the atomic scale.
