TiAl alloys were produced by investment casting method combined with induction skull melting (ISM) technique. In situ scanning electron microscopy (SEM) was utilized to study the fracture characteristics and crack...TiAl alloys were produced by investment casting method combined with induction skull melting (ISM) technique. In situ scanning electron microscopy (SEM) was utilized to study the fracture characteristics and crack propagation of a notched investment cast TiAl specimens in tension under incremental loading conditions. The whole process of crack initiation, propagation and failure during tensile deformation was observed and characterized. The results show that the fracture mechanism was sensitive to not only the microcracks near the notched area but also lamellar orientation to loading axis. The high tensile stress leads to the new microcracks nucleate along lamellar interfaces of grains with favorable orientation when local stress intensity reaches the toughness threshold of the material. Thus, both plasticity and high tensile stress are required to cause notched TiAl failure.展开更多
本文选取青岛市7个具有代表性的采样点,分时段进行大气颗粒物样本的采集,然后通过扫描电镜,进一步得到颗粒物的SEM(Scanning Electron Microscope)图像。通过对得到SEM图像的形貌特征进行观察分析,进而挑选出含有形貌特征明显的颗粒物的...本文选取青岛市7个具有代表性的采样点,分时段进行大气颗粒物样本的采集,然后通过扫描电镜,进一步得到颗粒物的SEM(Scanning Electron Microscope)图像。通过对得到SEM图像的形貌特征进行观察分析,进而挑选出含有形貌特征明显的颗粒物的SEM图像,共计334张图片。基于得到的大气颗粒物的SEM图像进行分析研究,根据其形貌特性的不同将颗粒物分为7类:链条状颗粒物、絮状颗粒物、纤维状颗粒物、球状颗粒物、类球状颗粒物、不规则矿物颗粒物、规则矿物颗粒物。将得到的SEM图片采用水平翻转、色彩平衡、亮度变换、模糊处理等相应的图像处理方法进行颗粒物SEM图像样本的扩展,生成新的图片样本,并将其添加到数据集中。从而建立起含有7类大气颗粒的SEM图像数据集,共含有2672张SEM图片。本文所建立的数据集可以用于采用机器学习等相关方法对大气颗粒物进行识别分类、分割等相关研究,也可为大气颗粒物相关研究提供基础数据资料。展开更多
[Objective] This study was to investigate the difference in microscopic features of pollen grain and stoma of four triticeae species, as well as the relationship between the sizes of pollen grain and stoma, and the ch...[Objective] This study was to investigate the difference in microscopic features of pollen grain and stoma of four triticeae species, as well as the relationship between the sizes of pollen grain and stoma, and the chromosome ploidy. [Method] Comparison of the micro-morphological characteristics of pollen grain and leaf epiderm among diaploid Thinopyrum elongatum, Elytrigia intermedia, hexaploid Triticum aestivum and octoploid Tritielytrigia types were carried out by observation under scanning electronic microscope(SEM). [Result] There were some differences among the four species in the micro-morphology, the size, the surface protuberance, the germ pore of pollen grain and the leaf epidermal stoma, in which diploid Thinopyrum elongatum was obviously different from the other three. Diploid, hexaploid and octoploid species of triticeae had remarkable differences in micro-morphological characteristics of pollen grain and stoma. However, some differences between hexaploid species and octoploid species were not significant. [Conclusion] Some microscopic characteristics of pollen grain and stoma could be used as the evidence to identify diaploid, hexaploid and octoploid spieces whose chromosome ploidy are hugely different.展开更多
We explored the potential use of combining wavelength-dispersive X-ray spectroscopy(WDX) and micromorphology of thin sections to identify minerals in peat soils. Peat soil minerals from three peats and swamps across G...We explored the potential use of combining wavelength-dispersive X-ray spectroscopy(WDX) and micromorphology of thin sections to identify minerals in peat soils. Peat soil minerals from three peats and swamps across Golestan Province in northern Iran were first characterized by micromorphological studies. Soils were composed mainly of quartz, muscovite, biotite, pyroxene,sericitized Fe-nodules, and iron-rich garnet. In addition,micromorphological results indicated that Galougah Coastal Swamp sections contained some inorganic residue with biological origin including oyster and limpet, which may be related to the swamp's location near Gorgan Gulf.In order to determine mineralogical properties of samples,twelve unknown grains were chosen for elemental concentration map studies. Quartz, garnet, ilmenite, calcite,and pyroxene in Suteh samples; epidote and Fe-nodule in Ghaleh-Ghafeh Peat Swamp; and barite, phyllosilicates,and calcite in Galougah were identified by WDX mapping of Si, Al, Fe, Ca, Mg, C, Ba, S, and Ti. Composition of the oysters' body was also analyzed by WDX for Si, Ca, Fe,and C. The results indicated that most of the minerals in all sections likely formed through weathering, inheriting their composition from the parent rock. This research suggests that merging micromorphology and SEM/WDX image techniques can be useful in confirming the presence of mineral particles in soil science.展开更多
Grout plays an important role in the transmission and maintenance of anchoring force,and in the protection of anchorage materials against corrosion.Thus,the hardening characteristics of grout directly affect the ancho...Grout plays an important role in the transmission and maintenance of anchoring force,and in the protection of anchorage materials against corrosion.Thus,the hardening characteristics of grout directly affect the anchoring effectivity and long-term reliability.We have excavated a prestressed anchorage which has been in service for 20 years,and have tested the grout which has worked for that long period under complicated geological conditions through strength tests and have analyzed its mineral composition using scanning electron microscopy(SEM) and X-ray diffraction(XRD).The results show that the mineral composition of the 12.5 m segment differs from other segments,and corresponds with poor coagulation characteristics of the 12.5 m segment grout.Analysis shows that unhydrated tricalcium silicate may be the reason for the localized poor coagulation.展开更多
Three types of rock specimens, three-point bending specimen, anti-symmetric four-point bending specimen and direct shearing specimen, were used to achieve Mode I, Mode II and mixed mode I–II fracture, respectively. M...Three types of rock specimens, three-point bending specimen, anti-symmetric four-point bending specimen and direct shearing specimen, were used to achieve Mode I, Mode II and mixed mode I–II fracture, respectively. Microscopic characteristics of the three fracture modes of brittle rock were studied by SEM technique in order to analyze fracture behaviors and better understand fracture mechanisms of different fracture modes of brittle rock. Test results show that the microscopic characteristics of different fracture modes correspond to different fracture mechanisms. The surface of Mode I fracture has a great number of sparse and steep slip-steps with few tearing ridges and shows strong brittleness. In the surface of Mode II fracture there exist many tearing ridges and densely distributed parallel slip-steps and it is attributed to the action of shear stress. The co-action of tensile and shear stresses results in brittle cleavage planes mixed with streamline patterns and tearing ridges in the surface of mixed mode I–II fracture. The measured Mode II fracture toughness K II C and mixed mode I–II fracture toughness K mC are larger than Mode I fracture toughness K I C · K II C is about 3.5 times K I C, and KmC is about 1.2 times K I C.展开更多
Nanoscale pore characteristics of the Upper Permian Longtan transitional mudrocks and their equivalent strata Wujiaping Formation marine mudrocks in and around the eastern Sichuan Basin was investigated using field em...Nanoscale pore characteristics of the Upper Permian Longtan transitional mudrocks and their equivalent strata Wujiaping Formation marine mudrocks in and around the eastern Sichuan Basin was investigated using field emission scanning electron microscopy(FE-SEM)and low-pressure N2 adsorption experiments.The results indicate that the Upper Permian mudrock is at a mature stage with total organic carbon(TOC)values ranging between 0.47%and 12.3%.The Longtan mudrocks mainly contain vitrinite,and their mineral composition is primarily clay.In contrast,the Wujiaping mudrocks are dominated by sapropelinite and solid bitumen,and their mineral compositions are mainly quartz and a notably high amount of pyrite.The FE-SEM reveals that clay mineral pores and microcracks are the common pore types in the Longtan mudrocks.The specific surface area and pore volume depend on the clay content but are negatively correlated with the TOC.The generation of nanometer pores in the Longtan mudrocks is caused by high clay mineral contents.Meanwhile,the Wujiaping mudrock mainly contains OM pores,and the pore parameters are positively correlated with the TOC.The OM pore development exhibits remarkable differences in the Longtan and Wujiaping mudrocks,which might be related to their sedimentary facies and maceral fractions.Vitrinite and inertinite appear as discrete particles in these mudrocks and cannot generate pores during thermal maturation.Sapropelinite often contains many secondary pores,and solid bitumen with large particles,usually with several pores,is not the major contributor to the pore system of the investigated mudrock.展开更多
基金Project(51001040)supported by the National Natural Science Foundation of ChinaProject(200802130014)supported by Specialized Research Fund for the Doctoral Program of Higher Education,China+1 种基金Project(HIT.NSRIF.2010116)supported by the Fundamental Research Funds for the Central Universities,ChinaProject(HITQNJS 2009022)supported by Development Program for Outstanding Young Teachers in Harbin Institute of Technology
文摘TiAl alloys were produced by investment casting method combined with induction skull melting (ISM) technique. In situ scanning electron microscopy (SEM) was utilized to study the fracture characteristics and crack propagation of a notched investment cast TiAl specimens in tension under incremental loading conditions. The whole process of crack initiation, propagation and failure during tensile deformation was observed and characterized. The results show that the fracture mechanism was sensitive to not only the microcracks near the notched area but also lamellar orientation to loading axis. The high tensile stress leads to the new microcracks nucleate along lamellar interfaces of grains with favorable orientation when local stress intensity reaches the toughness threshold of the material. Thus, both plasticity and high tensile stress are required to cause notched TiAl failure.
文摘本文选取青岛市7个具有代表性的采样点,分时段进行大气颗粒物样本的采集,然后通过扫描电镜,进一步得到颗粒物的SEM(Scanning Electron Microscope)图像。通过对得到SEM图像的形貌特征进行观察分析,进而挑选出含有形貌特征明显的颗粒物的SEM图像,共计334张图片。基于得到的大气颗粒物的SEM图像进行分析研究,根据其形貌特性的不同将颗粒物分为7类:链条状颗粒物、絮状颗粒物、纤维状颗粒物、球状颗粒物、类球状颗粒物、不规则矿物颗粒物、规则矿物颗粒物。将得到的SEM图片采用水平翻转、色彩平衡、亮度变换、模糊处理等相应的图像处理方法进行颗粒物SEM图像样本的扩展,生成新的图片样本,并将其添加到数据集中。从而建立起含有7类大气颗粒的SEM图像数据集,共含有2672张SEM图片。本文所建立的数据集可以用于采用机器学习等相关方法对大气颗粒物进行识别分类、分割等相关研究,也可为大气颗粒物相关研究提供基础数据资料。
基金Supported by Key Projects in the National Science&Technology Pillar Program in the Eleventh Five-year Plan Period(2006BAD02A08-9)the Science and Technology Research and Development Program of Hebei Province(06230105)+1 种基金Program of Science and Technology from Education Department of Hebei Province(2006425)the Science and Technology Re-search and Development Program of Tangshan City(08120201A-8)~~
文摘[Objective] This study was to investigate the difference in microscopic features of pollen grain and stoma of four triticeae species, as well as the relationship between the sizes of pollen grain and stoma, and the chromosome ploidy. [Method] Comparison of the micro-morphological characteristics of pollen grain and leaf epiderm among diaploid Thinopyrum elongatum, Elytrigia intermedia, hexaploid Triticum aestivum and octoploid Tritielytrigia types were carried out by observation under scanning electronic microscope(SEM). [Result] There were some differences among the four species in the micro-morphology, the size, the surface protuberance, the germ pore of pollen grain and the leaf epidermal stoma, in which diploid Thinopyrum elongatum was obviously different from the other three. Diploid, hexaploid and octoploid species of triticeae had remarkable differences in micro-morphological characteristics of pollen grain and stoma. However, some differences between hexaploid species and octoploid species were not significant. [Conclusion] Some microscopic characteristics of pollen grain and stoma could be used as the evidence to identify diaploid, hexaploid and octoploid spieces whose chromosome ploidy are hugely different.
文摘We explored the potential use of combining wavelength-dispersive X-ray spectroscopy(WDX) and micromorphology of thin sections to identify minerals in peat soils. Peat soil minerals from three peats and swamps across Golestan Province in northern Iran were first characterized by micromorphological studies. Soils were composed mainly of quartz, muscovite, biotite, pyroxene,sericitized Fe-nodules, and iron-rich garnet. In addition,micromorphological results indicated that Galougah Coastal Swamp sections contained some inorganic residue with biological origin including oyster and limpet, which may be related to the swamp's location near Gorgan Gulf.In order to determine mineralogical properties of samples,twelve unknown grains were chosen for elemental concentration map studies. Quartz, garnet, ilmenite, calcite,and pyroxene in Suteh samples; epidote and Fe-nodule in Ghaleh-Ghafeh Peat Swamp; and barite, phyllosilicates,and calcite in Galougah were identified by WDX mapping of Si, Al, Fe, Ca, Mg, C, Ba, S, and Ti. Composition of the oysters' body was also analyzed by WDX for Si, Ca, Fe,and C. The results indicated that most of the minerals in all sections likely formed through weathering, inheriting their composition from the parent rock. This research suggests that merging micromorphology and SEM/WDX image techniques can be useful in confirming the presence of mineral particles in soil science.
基金supported by National Key Technology R&D Program during the 11th Five-Year Plan Perio(Grant NO. 2008BAB29B01)State Key Program of National Natural Science of China(Grant NO. 41130745)Research foundation of the State Key Laboratory of Geohazard Prevention & Geoenvironment Protection (Grant NO.SKLGP2010Z008)
文摘Grout plays an important role in the transmission and maintenance of anchoring force,and in the protection of anchorage materials against corrosion.Thus,the hardening characteristics of grout directly affect the anchoring effectivity and long-term reliability.We have excavated a prestressed anchorage which has been in service for 20 years,and have tested the grout which has worked for that long period under complicated geological conditions through strength tests and have analyzed its mineral composition using scanning electron microscopy(SEM) and X-ray diffraction(XRD).The results show that the mineral composition of the 12.5 m segment differs from other segments,and corresponds with poor coagulation characteristics of the 12.5 m segment grout.Analysis shows that unhydrated tricalcium silicate may be the reason for the localized poor coagulation.
文摘Three types of rock specimens, three-point bending specimen, anti-symmetric four-point bending specimen and direct shearing specimen, were used to achieve Mode I, Mode II and mixed mode I–II fracture, respectively. Microscopic characteristics of the three fracture modes of brittle rock were studied by SEM technique in order to analyze fracture behaviors and better understand fracture mechanisms of different fracture modes of brittle rock. Test results show that the microscopic characteristics of different fracture modes correspond to different fracture mechanisms. The surface of Mode I fracture has a great number of sparse and steep slip-steps with few tearing ridges and shows strong brittleness. In the surface of Mode II fracture there exist many tearing ridges and densely distributed parallel slip-steps and it is attributed to the action of shear stress. The co-action of tensile and shear stresses results in brittle cleavage planes mixed with streamline patterns and tearing ridges in the surface of mixed mode I–II fracture. The measured Mode II fracture toughness K II C and mixed mode I–II fracture toughness K mC are larger than Mode I fracture toughness K I C · K II C is about 3.5 times K I C, and KmC is about 1.2 times K I C.
基金supported by the National NaturalScience Foundation of China(Grant No.41802163,41503033)Hunan Provincial Natural Science Foundation of China(Grant No.2018JJ3152)+1 种基金the Science and Technology Plan Project of Sichuan province(Grant No.2018JZ0003)the State Petroleum and Gas Specific Project(Grant No.2016ZX05061001-001)
文摘Nanoscale pore characteristics of the Upper Permian Longtan transitional mudrocks and their equivalent strata Wujiaping Formation marine mudrocks in and around the eastern Sichuan Basin was investigated using field emission scanning electron microscopy(FE-SEM)and low-pressure N2 adsorption experiments.The results indicate that the Upper Permian mudrock is at a mature stage with total organic carbon(TOC)values ranging between 0.47%and 12.3%.The Longtan mudrocks mainly contain vitrinite,and their mineral composition is primarily clay.In contrast,the Wujiaping mudrocks are dominated by sapropelinite and solid bitumen,and their mineral compositions are mainly quartz and a notably high amount of pyrite.The FE-SEM reveals that clay mineral pores and microcracks are the common pore types in the Longtan mudrocks.The specific surface area and pore volume depend on the clay content but are negatively correlated with the TOC.The generation of nanometer pores in the Longtan mudrocks is caused by high clay mineral contents.Meanwhile,the Wujiaping mudrock mainly contains OM pores,and the pore parameters are positively correlated with the TOC.The OM pore development exhibits remarkable differences in the Longtan and Wujiaping mudrocks,which might be related to their sedimentary facies and maceral fractions.Vitrinite and inertinite appear as discrete particles in these mudrocks and cannot generate pores during thermal maturation.Sapropelinite often contains many secondary pores,and solid bitumen with large particles,usually with several pores,is not the major contributor to the pore system of the investigated mudrock.