In this paper, the microstructure change of one step-draw PET fiber has been studied byvarious methods, such as, Laser Raman Microscope, Wide-angle X-ray, Density-gradient andPolarizing Microscope. The computer has be...In this paper, the microstructure change of one step-draw PET fiber has been studied byvarious methods, such as, Laser Raman Microscope, Wide-angle X-ray, Density-gradient andPolarizing Microscope. The computer has been used to resolve overlapped bands in the Ramanspectra. Then the band changes have been correlated with trans, gauche and stressed trans-conformations indicated by a conformational index. Based on these indices, the relationshipbetween the conformation change of glycol units in the fiber structure and the macromechanicalproperties of fiber is expounded.展开更多
Based on results of microscopic observation and laser Raman analysis about fluid in-clusions,multiple special forms of immiscible inclusions that contain sulphur,liquid hydrocarbon,bi-tumen,etc.were discovered in samp...Based on results of microscopic observation and laser Raman analysis about fluid in-clusions,multiple special forms of immiscible inclusions that contain sulphur,liquid hydrocarbon,bi-tumen,etc.were discovered in samples collected from the H_(2)S gas reservoir-containing carbonates in the Lower Triassic Feixianguan Formation in the Jinzhu-Luojia area,Kai County,Sichuan Province.Based on the lithology and burial history of the strata involved as well as measurement results of homogenization temperature of fluid inclusions,bitumen reflectivity,etc.,it is concluded that the H_(2)S in the gas reservoir resulted from the thermal reaction between hydrocarbons in reservoir and CaSO_(4)in the gypsum-bearing dolostone section at the high temperature(140℃―170℃)oil-cracked gas for-mation stage in Late Cretaceous.Thereafter,research on a great number of immiscible inclusions in the reservoir reveals that elemental sulphur resulted from oxidation of part of the earlier-formed H_(2)S and further reaction between sulphates,hydrocarbons and H_(2)S in geological fluids in H_(2)S-bearing gas reservoir at a temperature of 86℃―89℃and a pressure of 340×10^(5)Pa and during the regional uplift stage as characterized by temperature decrease and pressure decrease in Tertiary.Meanwhile,gyp-sum,anhydrite and calcite formed at this stage would trap particles like elemental sulphur and result in a variety of special forms of immiscible inclusions,and these inclusions would contain information concerning the complexity of the fluids in the reservoir and the origin of H_(2)S and natural sulphur in the gas reservoir.展开更多
文摘In this paper, the microstructure change of one step-draw PET fiber has been studied byvarious methods, such as, Laser Raman Microscope, Wide-angle X-ray, Density-gradient andPolarizing Microscope. The computer has been used to resolve overlapped bands in the Ramanspectra. Then the band changes have been correlated with trans, gauche and stressed trans-conformations indicated by a conformational index. Based on these indices, the relationshipbetween the conformation change of glycol units in the fiber structure and the macromechanicalproperties of fiber is expounded.
基金This research was supported by the State Brainstorm Science Program for the Tenth Five-Year Pkn Period(Grant No.2001BA605A-0404)the Frontier Research Program Sponsared by Guangzhou Institute of Geochemistry of Chinese Ac ademy of Sciences(Grant No.GiGCX-04-08).
文摘Based on results of microscopic observation and laser Raman analysis about fluid in-clusions,multiple special forms of immiscible inclusions that contain sulphur,liquid hydrocarbon,bi-tumen,etc.were discovered in samples collected from the H_(2)S gas reservoir-containing carbonates in the Lower Triassic Feixianguan Formation in the Jinzhu-Luojia area,Kai County,Sichuan Province.Based on the lithology and burial history of the strata involved as well as measurement results of homogenization temperature of fluid inclusions,bitumen reflectivity,etc.,it is concluded that the H_(2)S in the gas reservoir resulted from the thermal reaction between hydrocarbons in reservoir and CaSO_(4)in the gypsum-bearing dolostone section at the high temperature(140℃―170℃)oil-cracked gas for-mation stage in Late Cretaceous.Thereafter,research on a great number of immiscible inclusions in the reservoir reveals that elemental sulphur resulted from oxidation of part of the earlier-formed H_(2)S and further reaction between sulphates,hydrocarbons and H_(2)S in geological fluids in H_(2)S-bearing gas reservoir at a temperature of 86℃―89℃and a pressure of 340×10^(5)Pa and during the regional uplift stage as characterized by temperature decrease and pressure decrease in Tertiary.Meanwhile,gyp-sum,anhydrite and calcite formed at this stage would trap particles like elemental sulphur and result in a variety of special forms of immiscible inclusions,and these inclusions would contain information concerning the complexity of the fluids in the reservoir and the origin of H_(2)S and natural sulphur in the gas reservoir.
