目的利用在体大鼠心肌缺血再灌注模型观察Bayk8644对大鼠心功能的影响。方法将18只大鼠随机分为3组:假手术组(sham组)、Bay k8644组(B组)和二甲基亚枫组(D组),分别在缺血30 m in时静脉持续泵入生理盐水、Bay k8644和二甲基亚枫,于缺血前...目的利用在体大鼠心肌缺血再灌注模型观察Bayk8644对大鼠心功能的影响。方法将18只大鼠随机分为3组:假手术组(sham组)、Bay k8644组(B组)和二甲基亚枫组(D组),分别在缺血30 m in时静脉持续泵入生理盐水、Bay k8644和二甲基亚枫,于缺血前,缺血5、20、40 m in以及再灌注5、30、60、90 m in时,分别测定心率(HR)、左心室收缩峰压(LVSP)、左心室舒张末压(LVEDP)、左心室压力变化最大速率(±dp/dtm ax),以评价心脏功能。结果缺血后HR变化不显著,LVSP和+dp/dtm ax降低(与缺血前和sham组比较差异有显著性P<0.05),LVEDP升高,-dp/dtm ax降低;再灌注时B组HR逐渐减慢,D组逐渐增快,两组比较差异无显著性(P>0.05);LVSP和+dp/dtm ax进行性升高,LVEDP升高,-dp/dtm ax降低,各时间点两组比较差异无显著性(P>0.05)。结论持续静脉注射Bay k8644(2μg.kg-1.m in-1)不影响缺血再灌注损伤大鼠的心脏功能。展开更多
Deciphering hydrocarbon generation and accumulation stage is of significance to understand oil and gas evolution and seek exploration targets.Taking the Upper Paleozoic buried-hills in the Huanghua Depression,Bohai Ba...Deciphering hydrocarbon generation and accumulation stage is of significance to understand oil and gas evolution and seek exploration targets.Taking the Upper Paleozoic buried-hills in the Huanghua Depression,Bohai Bay Basin,as a case study,hydrocarbon generation environment and detailed accumulation process are revealed by fluid inclusions observations,Laser Raman spectroscopy,Fourier Infrared spectroscopy,and K-Ar isotope measurements.The results show that both oil and gas inclusion were captured in the quartz overgrowth,dissolved feldspar and calcite microfractures,showing blue to dark brown fluoresce.The grains containing oil inclusions index(GOI)of oil,oil&gas and gas being 25%,65%,and 10%and the inclusions with abundant methyl groups and short chains,both indicate high thermal maturity.One series of fluids inclusion is generally observed,evidenced by the concentrated homogenization temperature of 135-145℃ and salinity of 3%-15 w.t.%NaCl equiv,indicating one primary charging stage.The gas and gas&liquid inclusions mainly contain CH_(4),with also peaks indicating CO_(2) and N_(2.)The Carboniferous and Permian biomarkers show reducing environment with brackish water,with organic matter sources both from marine and continental.The relative content ofααα20RC_(27),ααα20RC_(28),andααα20RC_(29) exhibit source contributions both from algae and higher plants,and mainly of II2 to III kerogen.Both coal derived gas and oil associated hydrocarbons are identified from most of the buried-hills.Combining the fluid homogenization temperature and salinity,as well as the thermal evolution history,the hydrocarbon generated from the Upper Paleozoic was concentrated at the end of the Eocene(40 Ma±),while the beginning of charging is 60 Ma±.The Wumaying Buried-hill is of only coal derived gas and has potential for inner coal measure natural gas exploration.The results provide a detailed understanding of hydrocarbon accumulations in the study area,which can also be reference for improving petroleum exploration efficiency in similar basins.展开更多
基金This study was supported by the National Natural Science Foundation of China(Grant No.42072194,U1910205)the Fundamental Research Funds for the Central Universities(800015Z1190,2021YJSDC02).
文摘Deciphering hydrocarbon generation and accumulation stage is of significance to understand oil and gas evolution and seek exploration targets.Taking the Upper Paleozoic buried-hills in the Huanghua Depression,Bohai Bay Basin,as a case study,hydrocarbon generation environment and detailed accumulation process are revealed by fluid inclusions observations,Laser Raman spectroscopy,Fourier Infrared spectroscopy,and K-Ar isotope measurements.The results show that both oil and gas inclusion were captured in the quartz overgrowth,dissolved feldspar and calcite microfractures,showing blue to dark brown fluoresce.The grains containing oil inclusions index(GOI)of oil,oil&gas and gas being 25%,65%,and 10%and the inclusions with abundant methyl groups and short chains,both indicate high thermal maturity.One series of fluids inclusion is generally observed,evidenced by the concentrated homogenization temperature of 135-145℃ and salinity of 3%-15 w.t.%NaCl equiv,indicating one primary charging stage.The gas and gas&liquid inclusions mainly contain CH_(4),with also peaks indicating CO_(2) and N_(2.)The Carboniferous and Permian biomarkers show reducing environment with brackish water,with organic matter sources both from marine and continental.The relative content ofααα20RC_(27),ααα20RC_(28),andααα20RC_(29) exhibit source contributions both from algae and higher plants,and mainly of II2 to III kerogen.Both coal derived gas and oil associated hydrocarbons are identified from most of the buried-hills.Combining the fluid homogenization temperature and salinity,as well as the thermal evolution history,the hydrocarbon generated from the Upper Paleozoic was concentrated at the end of the Eocene(40 Ma±),while the beginning of charging is 60 Ma±.The Wumaying Buried-hill is of only coal derived gas and has potential for inner coal measure natural gas exploration.The results provide a detailed understanding of hydrocarbon accumulations in the study area,which can also be reference for improving petroleum exploration efficiency in similar basins.
