烴裂解 的英文怎麼說
中文拼音 [tīnglièjiě]
烴裂解
英文
hydrocarbon purolysis-
The betaine will collapse to the alkene only when these two functions are eclipsed.
只有當這兩個基團移至重迭位置時碘鹽才能裂解為烯烴。After the decarboxylation process the alkane produced can be degraded or "cracked" =to lower carbon number alkanes.
脫羧基作用后，所形成的烷烴能被降解或「裂解」成低碳數烷烴。During incomplete combustion some of the hydrocarbon fuel is cracked.
在不完全的燃燒中，一些烴燃料裂解。The existing of poypropylene can raise the liquid fraction ratio, especially the light oil ratio, so it can fortify the effect of the cracking reaction of polyene to light oil
摘要在廢舊聚烯烴的裂解反應中，聚丙烯的存在，可以提高輕油餾份的收率，增強反應的油化效果，本文稱之為聚烯烴裂解反應的增強效應。Study on coke inhibitor of hydrocarbon pyrolysis
烴類裂解阻焦強化劑的研究The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian, comes from carbonatite hydrocarbon rocks permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas
摘要通過對川中川南過渡帶西部的磨溪潼南地區嘉二段天然氣組成、碳同位素組成、高演化天然氣儲層瀝青生物標志化合物的系統分析測試和混合成因氣的定量估算，闡明了該區嘉二段天然氣主要屬於二疊系腐泥型有機質成因氣，來源於二疊系過成熟為主的碳酸鹽巖烴源，主力氣源與嘉陵江組自身的碳酸鹽巖烴源無關，並具有油型裂解氣的地球化學特徵。The gas generation of low mature source rocks has been simulated in the open system and close system respectively. the models of primary cracking gas ( gas from kerogen ) and secondary cracking gas ( gas from oil ) have been established. the ro value of primary cracking gas generation peak is ranged from 1. 0 % to 1. 5 %. the ro value of secondary gas generation peak is ranged from 1. 5 % to 2. 5 %
對低成熟（部分為成熟）的烴源巖在開放和密閉體系下的生氣熱模擬實驗研究建立了熱解氣和油裂解氣的生氣模式，熱解氣的生氣高峰在ro = 1 . 0 ? 1 . 5 ，油裂解氣生氣高峰是在ro = 1 . 5 ? 2 . 5之間，從熱解氣和油裂解氣的相對含量來看熱解氣占總生氣量的21 ，油裂解氣可能佔79 ，油裂解氣產率為620m ~ 3噸Cleavage of paraffin
石蠟烴裂解The late permian coal from southern china are unique in high content of barkinite and element hydrogen, as well as significant hydrocarbon - generation potential. in this paper, rock - eval, py - gc and mpv - 3 were used to study the hydrocarbon - generation potential, the hydrocarbon composition, hydrocarbon - generation mechanism and thermoevlutional characteristics of barkinite in open system simulation. the results indicate that barkinite has higher hydrocarbon - generation potential, the values of hydrocarbon - generation potential s
為1 . 55 %左右烴類組成以輕質烴凝析油或輕質油占絕對優勢，濕氣次之，並且烯烴含量較高此現象與開放體系熱模擬有關氣態烴與液態烴演化規律相似，據此可以認為，氣態烴很大一部分是由液態烴進一步裂解來的。Study kinetics behavior of oil generation, gas generation from organic matter in carbonate rock and oil to gas. and calibrate kinetic models using experimental data. make it possible to calculate quantity of oil generation, gas generation from carbonate source rocks quantificationally and dynamically
考察了碳酸鹽巖有機質成油、成氣及油裂解成氣動力學行為，並根據實驗結果對動力學模型進行了標定，使得定量、動態的計算碳酸鹽巖烴源巖的生氣量成為可能。On the basis of above experiments, the chemical kinetic model inwhich organic matter of source rock of deep - formation in the north of songliao basin primarily crack into oil or gas is established, which set up a basis for evaluating oil - generating amount, gas - generating amount of source rock of deep formation in different periods ; set up the chemical kinetic model inwhich different qualities of oil and family constituents in oil secondarily cracked into gas, which provide theoretical foundation and practical methods for dynamic evaluation of gas - generating amount and oil - consuming amount in process of oil cracking. the geochemical features of source rocks in deep - formation of basins are systematically evaluated
在上述實驗基礎上，建立了松遼盆地北部深層源巖有機質初次裂解成油、成氣的化學動力學模型，為評價深層源巖于不同時期的生油量、生氣量奠定了基礎；建立了不同性質原油及原油中各族組分二次裂解成氣的化學動力學模型，為動態評價油裂解過程的成氣量和耗油量提供了理論依據和實用方法；對盆地深層源巖的地化特徵進行了系統評價；考慮到深層源巖的成熟度較高，實測地化指標（殘余有機碳、氫指數等）不能客觀反映源巖有機質的原始豐度和原始生烴潛力。This work include : in order to demarcate chemical kinetic model inwhich organic matter generate oil and gas, constant velocity, rising temperature thermal modeling experiment is designed ; in order to demarcate chemical kinetic model inwhich oil crack into gas, isothermic thermal modeling experiment inwhich oil crack into gas is designed ; in order to establish chemical kinetic model inwhich family constituents in oil ( saturated hydrocarbon, arene, non - hydrocarbon, bitumen ) change into gas, isothermic or constant velocity jsothermal modeling experiment is designed
這一工作包括：為標定有機質成油、成氣的化學動力學模型，設計進行了恆速升溫熱模擬實驗；為標定油成氣的化學動力學模型，設計進行了等溫的油裂解成氣的熱模擬實驗；為建立油中各族組分（飽和烴、芳烴、非烴、瀝青質）成氣的化學動力學模型，進行了恆溫或恆速升溫模擬實驗。And the reduced chemical reaction mechanism of supersonic hc propellant is confirmed. as the production of splitting reaction, ethane is plentiful in the hydrocarbon
確定超高音速飛行器碳氫類推進劑的簡化化學反應機理，乙烯作為裂解產物在小分子烴中含量居多。On the basis of current situation on the investigation, the paper brings forward several suggestions and prospects of the research : strengthen the high resolution research on the characteristics of the hydrocarbon - expulsion in the section of source rocks, set up the hydrocarbon - expulsion model including three phases ( compaction, uncompaction and cracking ), evaluate hydrocarbon - expulsion on classification of the anisotropic source rocks, and discuss the relation between hydrocarbon - expulsion and hydrocarbon accumulation
在針對研究現狀分析的基礎上，提出了幾點研究方向及展望：加強對烴源巖剖面排烴特徵的高解析度研究，建立壓實欠壓實壓裂三端元排烴模型，對存在嚴重非均質性的烴源巖進行烴源巖排烴分級評價，深入探討排烴與油氣成藏的關系。In this paper, the author will take the qibei area ad the example and from the point of to describe the oil generation, migration and accurmulation characteristics in superpressure condition
壓力對烴源巖中乾酪根的熱降解有阻滯作用，壓力升高不僅使乾酪根的化學鍵更穩定且不宜斷裂，還使乾酪根分子與烴源巖礦物結合更加牢固。Forming of hydrocarbon and fission of oil which increase the bulk of fluid will lead the increase of formation compression in the stratum enclosed well
生烴和原油裂解使流體體積增大，但只有在地層的封閉性較好時，才會導致地層壓力增加。分享友人