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构造生烃 被引量:1
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作者 熊斌辉 《海洋石油》 CAS 2009年第2期1-9,共9页
生烃是岩石中所含的有机质产生流体有机化合物的化学反应。岩石有机质化学反应存在两种系统:封闭系统和开放系统,随着埋深加大,烃源岩越来越致密,岩石的化学反应逐渐由开放系统转变为封闭系统。目前的生烃理论仅仅是开放系统下烃源岩成... 生烃是岩石中所含的有机质产生流体有机化合物的化学反应。岩石有机质化学反应存在两种系统:封闭系统和开放系统,随着埋深加大,烃源岩越来越致密,岩石的化学反应逐渐由开放系统转变为封闭系统。目前的生烃理论仅仅是开放系统下烃源岩成熟与生烃理论,烃源岩成熟与生烃是不匹配的。封闭系统下烃源岩成熟与生烃是不匹配的,烃源岩成熟但不生烃,而是形成另外一种成熟的固体有机质。大多数情况是烃源岩为半封闭系统,烃源岩处于欠生烃状态。构造运动形成的断层和裂隙将烃源岩与疏导层沟通,烃源岩迅速由封闭、半封闭系统转变为开放系统。这种生烃系统的转变形成短时间内过量生烃,笔者将这种生烃作用命名为构造生烃,意味着构造运动期即为主生烃期,伴随着多次构造运动可以形成多个幕式生烃高峰。构造生烃理论开拓两个极其重要的勘探领域:第一,新构造勘探。以往认为已经过了生、排烃期的构造得以解放,如渤海湾郯庐断裂带第四纪圈闭不是过了主生烃期,而是正处于构造生烃的过生烃高峰期。以PL19-3为代表的油气运聚强度只有构造生烃能够解释;第二,超深勘探,特别是天然气勘探。深层勘探的下限将大大延伸,生烃门限,特别是生气门限将大大加深,仅生烃而言万米都不是天然气勘探的极限。 展开更多
关键词 开放系统 封闭系统 过生烃 构造 新构造勘探 超深勘探
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Fractal Evolving Theory and Growing Model of Olefin Polymerization Process 被引量:1
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作者 霍超 孟濬 +2 位作者 任晓红 阳永荣 戎顺熙 《Chinese Journal of Chemical Engineering》 SCIE EI CAS CSCD 2003年第1期33-37,共5页
The surface morphology of Ti-Mg supported catalyst and the polyethyleneparticles are studied using scanning electron microscope(SEM) technology. The results show thateithen the catalyst's surface or polymer partic... The surface morphology of Ti-Mg supported catalyst and the polyethyleneparticles are studied using scanning electron microscope(SEM) technology. The results show thateithen the catalyst's surface or polymer particle's surface is irregular and has fractalcharacteristics, which can be described by fractal parameter. The more interesting discovery is thatthe surface fractal dimension values of the polymer particles vary periodically with thepolymerization time. We call this phenomenon fractal evolution, which can be divided into the'revolution' stage and the 'evolution' stage. And then we present polymerization fractal growingmodel (PFGM), and successfully describe and/or predict the whole evolving process of thepolyethylene particle morphology under the different slurry polymerization (includingpre-polymerization) conditions without H_2. 展开更多
关键词 polyethylene catalyst fractal evolution theory surface morphology polymerization fractal growing model
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Potential of the White-Rot Fungus Pleurotus pulmonarius F043 for Degradation and Transformation of Fluoranthene 被引量:5
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作者 Riry WIRASNITA 《Pedosphere》 SCIE CAS CSCD 2016年第1期49-54,共6页
Fluoranthene, a four-ring polycyclic aromatic hydrocarbon that is possible genotoxic in nature, has been used as an indicator for assessing polycyclic aromatic hydrocarbon (PAH)-containing pollutants. Microbial degr... Fluoranthene, a four-ring polycyclic aromatic hydrocarbon that is possible genotoxic in nature, has been used as an indicator for assessing polycyclic aromatic hydrocarbon (PAH)-containing pollutants. Microbial degradation is one of the promising methods in removing up PAH-contaminated environments. White-rot fungi have showed the ability to degrade a wide range of PAHs. This study aimed to investigate enzyme production, fungal biomass, and glucose utilization during the biodegradation process of fiuoranthene by a white-rot fungus Pleurotus pulmonarius F043 and to identify the metabolites produced in the degradation process. The extracellular ligninolytic enzyme system of the fungi, producing laccases and peroxidases, was directly linked to the biodegradation of fiuoranthene. The production of ligninolytic enzymes during fluoranthene degradation was related to an increase in the biomass of Pleurotus pulmonarius F043. Fluoranthene removal decreased with an increase in fluoranthene concentrations. The highest biomass production of Pleurotus pulmonarius F043 (〉 4 400 mg L-1) was found in the 10 mg L-1 fluoranthene culture after 30 d of incubation. Two fluoranthene metabolites, naphthalene-l,8-dicarboxylic acid and phthalic acid, were found in the process of fluoranthene degradation. Laccase was revealed as the major enzyme that played an important role in degradation process. Suitable conditions must be found to promote a successful fungal biotransformation augmentation in liquid culture. 展开更多
关键词 gas chromatography-mass spectrometer ligninolytic enzymes METABOLITES naphthalene-l 8-dicarboxylic acid phthalicacid
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Geobiological processes of the formation of lacustrine source rock in Paleogene 被引量:12
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作者 LI GuoShan WANG YongBiao +4 位作者 LU ZongSheng LIAO Wei SONG GuoQi WANG XueJun XU XingYou 《Science China Earth Sciences》 SCIE EI CAS 2014年第5期976-987,共12页
Gypsum-salt rocks and coccolith calcareous shale are widely deposited in the lower part of the Paleogene Shahejie Formation in the Dongying Sag, Sbandong Province. The gypsum-salt rock is believed to be formed during ... Gypsum-salt rocks and coccolith calcareous shale are widely deposited in the lower part of the Paleogene Shahejie Formation in the Dongying Sag, Sbandong Province. The gypsum-salt rock is believed to be formed during the earlier deposition in salt lake, while the overlying coccolith shale in saline lake with relatively low salinity. By comparing the lake environment and la- custrine microbial communities between ancient and recent lakes, cyanobacteria are regarded as the main representative of productivity during the formation of gypsum-salt strata series, with the annual productivity of 1500-2000 gC m-2 yr1. Based on the research of ultramicrofossils in the calcareous shale, coccolith is considered as the main contributor to the productivity during the formation of calcareous shale. On the basis of statistic data of sedimentary rates, shale laminations, and coccolith fossils in each lamination, the quantitative value of productivity is calculated, with the annual productivity of 2250 3810 gC m 2 yr-1 (averagely 3120 gC m-2 yr-1). Statistic data of large amount of pyrite framboids indicate that the lower water col- umn was persistently in sulfidic or anoxic conditions during the deposition of gypsum-salt strata series, but it changed to be dysoxic when the coccolith calcareous shale was deposited. Both of these water conditions are favorable for the preservation of organic matter. It is estimated that the organic carbon burial efficiency of the Lower Paleogene salt lakes and saline lakes of Dongying Depression is about 10%-15%, which is calculated and analyzed using the multi-parameter geobiological model. 展开更多
关键词 source rock GEOBIOLOGY paleo-oxygenation facies PALEOGENE Dongying Sag
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