Micro-diamonds were only found ten years ago in eclogite associated with marble at Xindian in the Dabie Mountains. This paper reports our new finding of micro-diamonds not only in eclogites at Maobei in the Sulu regio...Micro-diamonds were only found ten years ago in eclogite associated with marble at Xindian in the Dabie Mountains. This paper reports our new finding of micro-diamonds not only in eclogites at Maobei in the Sulu region and at Xindian and Laoyoufang in the south part of the Dabie Mountains (South Dabie), but also in eclogites at Baizhangya and Huangweihe in the northern part of the Dabie Mountains (North Dabie) that has usually been considered not to experience ultrahigh pressure metamorphism. Except the micro-diamond at Huangweihe that was found from the artificial heavy sands of zircons used for isotopic dating, the micro-diamonds from other localities were identified in thin sections of the eclogites. Besides a few interstitial grains, most of the micro-diamond grains in thin sections occur as inclusion in garnet. Three crystals of micro- diamond at Maobei in the Sulu region are sized in 120, 60 and 30 mm, respectively. Crystal forms look like octahedron and the composite of octahedron and hexahedron. The largest micro-diamond crystal comes from Xindian, which is measured to be 180 mm in diameter with distinct zonal structure and inclusions. The zonal structure occurs as an inclined octahedron inside rounded by an incomplete hexagonal girdle. A smaller micro-diamond inclusion occurs inside the central octahedron, and a larger graphite inclusion is within the outer zone. The Laoyoufang micro-diamond is partially retrograded to graphite. Micro-diamond from the Baizhangya eclogite in the ultramafic rock belt of North Dabie is an aggregate of 70 mm×90 mm in size. All the micro-diamonds are confirmed by the Raman spectrum analysis. The occurrence of the micro-diamonds from the eclogites in the ultramafic rock belt of North Dabie demonstrates that this region was also subjected to ultrahigh pressure metamorphism as well as the South Dabie did.展开更多
Primary high-density fluid inclusions were identified in garnet from ultrahigh pressure eclogite in the southern part of the Sulu terrane. They occur isolatedly or in cluster together with relatively low-density two-p...Primary high-density fluid inclusions were identified in garnet from ultrahigh pressure eclogite in the southern part of the Sulu terrane. They occur isolatedly or in cluster together with relatively low-density two-phase inclu-sions. The eutectic temperature of the inclusions is as low as ≤ -52℃. A bubble was nucleated in a liquid inclusion dur-ing the specific stage of cyclic cooling-heating runs, and the liquid-gas homogenization temperature was measured to be ≤-12.5℃. The composition of the inclusions modeled by the system CaCl2-NaCl-H2O, yields the fluid density of 1.27g/cm3 that corresponds to a pressure of ca. 2.4 GPa at thetemperature of peak eclogite-facies metamorphism, close tothe ultrahigh pressure metamorphic conditions. During theexhumation of the eclogite the inclusions reacted with thehost mineral, forming hydrous silicate minerals that resulted in lowering of the fluid density and its transformation to multi-phase inclusions.展开更多
为缩短蒜片热风干燥时间,提高干制蒜片品质,将超高压与超声波技术应用到蒜片干燥前处理,并利用低场核磁共振技术(Low Field Nuclear Magnetic Resonance,LF-NMR)分析预处理对蒜片干燥过程中内部不同状态水分迁移的影响。结果表明:干燥...为缩短蒜片热风干燥时间,提高干制蒜片品质,将超高压与超声波技术应用到蒜片干燥前处理,并利用低场核磁共振技术(Low Field Nuclear Magnetic Resonance,LF-NMR)分析预处理对蒜片干燥过程中内部不同状态水分迁移的影响。结果表明:干燥前超声或超高压预处理有利于加快干燥过程,超声、超高压和超高压-超声预处理的干燥时间分别比没有预处理的对照组降低了37.50%、43.75%、62.50%;三种预处理均可以降低干燥能耗,尤以超高压-超声最为显著(P<0.05),相比对照降低了32.31%。低场核磁共振测定结果表明,预处理后蒜片中存在三种状态的水分,自由水占的比例最大,不易流动水次之,结合水最少。干燥过程中脱除的主要是自由水,超声和超高压均降低了自由水的脱除时间,超高压-超声预处理脱除自由水的时间最少,为90 min,说明超高压和超声联合更有利于减弱蒜片组织对水分的束缚并增强水分的流动性。通过扫描电镜发现,超高压使蒜片细胞间隙增大,细胞壁破坏严重,而经超声预处理的蒜片组织出现疏松多孔的结构,超高压-超声扩增了蒜片的显微通道,验证了超高压-超声更有利于提高水分的流动性。经超高压或超声预处理后,干制蒜片的色差降低,复水比和蒜素含量显著提高(P<0.05),超高压与超声联合预处理得到的干制蒜片品质较优,色差值为16.11,大蒜素含量为2.67 mg/g,复水比为2.90 g/g。研究结果为高效节能、高品质的大蒜干燥技术提供理论参考。展开更多
基金supported by the National Natural Science Foundation of China(Grant No.40172079)the Scientific Investigation of Chinese Continental Scientific Drilling Project(Grant No.2001 CCB00900).
文摘Micro-diamonds were only found ten years ago in eclogite associated with marble at Xindian in the Dabie Mountains. This paper reports our new finding of micro-diamonds not only in eclogites at Maobei in the Sulu region and at Xindian and Laoyoufang in the south part of the Dabie Mountains (South Dabie), but also in eclogites at Baizhangya and Huangweihe in the northern part of the Dabie Mountains (North Dabie) that has usually been considered not to experience ultrahigh pressure metamorphism. Except the micro-diamond at Huangweihe that was found from the artificial heavy sands of zircons used for isotopic dating, the micro-diamonds from other localities were identified in thin sections of the eclogites. Besides a few interstitial grains, most of the micro-diamond grains in thin sections occur as inclusion in garnet. Three crystals of micro- diamond at Maobei in the Sulu region are sized in 120, 60 and 30 mm, respectively. Crystal forms look like octahedron and the composite of octahedron and hexahedron. The largest micro-diamond crystal comes from Xindian, which is measured to be 180 mm in diameter with distinct zonal structure and inclusions. The zonal structure occurs as an inclined octahedron inside rounded by an incomplete hexagonal girdle. A smaller micro-diamond inclusion occurs inside the central octahedron, and a larger graphite inclusion is within the outer zone. The Laoyoufang micro-diamond is partially retrograded to graphite. Micro-diamond from the Baizhangya eclogite in the ultramafic rock belt of North Dabie is an aggregate of 70 mm×90 mm in size. All the micro-diamonds are confirmed by the Raman spectrum analysis. The occurrence of the micro-diamonds from the eclogites in the ultramafic rock belt of North Dabie demonstrates that this region was also subjected to ultrahigh pressure metamorphism as well as the South Dabie did.
文摘Primary high-density fluid inclusions were identified in garnet from ultrahigh pressure eclogite in the southern part of the Sulu terrane. They occur isolatedly or in cluster together with relatively low-density two-phase inclu-sions. The eutectic temperature of the inclusions is as low as ≤ -52℃. A bubble was nucleated in a liquid inclusion dur-ing the specific stage of cyclic cooling-heating runs, and the liquid-gas homogenization temperature was measured to be ≤-12.5℃. The composition of the inclusions modeled by the system CaCl2-NaCl-H2O, yields the fluid density of 1.27g/cm3 that corresponds to a pressure of ca. 2.4 GPa at thetemperature of peak eclogite-facies metamorphism, close tothe ultrahigh pressure metamorphic conditions. During theexhumation of the eclogite the inclusions reacted with thehost mineral, forming hydrous silicate minerals that resulted in lowering of the fluid density and its transformation to multi-phase inclusions.
文摘为缩短蒜片热风干燥时间,提高干制蒜片品质,将超高压与超声波技术应用到蒜片干燥前处理,并利用低场核磁共振技术(Low Field Nuclear Magnetic Resonance,LF-NMR)分析预处理对蒜片干燥过程中内部不同状态水分迁移的影响。结果表明:干燥前超声或超高压预处理有利于加快干燥过程,超声、超高压和超高压-超声预处理的干燥时间分别比没有预处理的对照组降低了37.50%、43.75%、62.50%;三种预处理均可以降低干燥能耗,尤以超高压-超声最为显著(P<0.05),相比对照降低了32.31%。低场核磁共振测定结果表明,预处理后蒜片中存在三种状态的水分,自由水占的比例最大,不易流动水次之,结合水最少。干燥过程中脱除的主要是自由水,超声和超高压均降低了自由水的脱除时间,超高压-超声预处理脱除自由水的时间最少,为90 min,说明超高压和超声联合更有利于减弱蒜片组织对水分的束缚并增强水分的流动性。通过扫描电镜发现,超高压使蒜片细胞间隙增大,细胞壁破坏严重,而经超声预处理的蒜片组织出现疏松多孔的结构,超高压-超声扩增了蒜片的显微通道,验证了超高压-超声更有利于提高水分的流动性。经超高压或超声预处理后,干制蒜片的色差降低,复水比和蒜素含量显著提高(P<0.05),超高压与超声联合预处理得到的干制蒜片品质较优,色差值为16.11,大蒜素含量为2.67 mg/g,复水比为2.90 g/g。研究结果为高效节能、高品质的大蒜干燥技术提供理论参考。
