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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Compositional regularities common to petroleum reservoir fluids and pyrolysates of asphaltenes and kerogens
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Compositional regularities common to petroleum reservoir fluids and pyrolysates of asphaltenes and kerogens

机译:石油储层流体和沥青质和干酪根的热解产物共有的组成规律

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Slope Factor (SF), based on the concept of Kissin, specifies the rate of decrease in concentration with increasing carbon number in the exponential distribution of n-alkanes in reservoir fluids and pyrolysates. Two exponential series occur. SF(C-2-n-C-5) is invariably steeper than SF(n-C-6+), reflecting stabilities and cracking mechanism. The break in slope occurs at n-C-6. Pseudo-components (P-n), representing the total composition subdivided by carbon number, also decrease in concentration exponentially beyond C-10, facilitating the measurement of SF(P-10+). In asphaltene pyrolysates, in the C-10+ range, SF(P-10+) and SF(n-C-10+) exhibit significant correlation, suggesting a communality of an as yet uncertain nature in generative processes. At conversion levels within the oil window, asphaltene pyrolysis yields values of SF(C-2-n-C-5) between 1.32 and 1.55, and values of SF(n-C-10+) between 1.07 and 1.24. Reservoir fluids (oils) from the Western Canada Basin exhibit closely similar ranges and associations of values. Pyrolysates of kerogen concentrates containing pyrite yield SF values which are higher than those of both asphaltene pyrolysates and normal oils, possibly due to pyrite-induced catalysis. Migration-depleti on, operating by way of exsolution due to pressure and temperature decrease, is recognized in both oils (fluids which exhibit a bubble point) and gas-condensates (which exhibit a dew point). Oils exsolve gases and light hydrocarbons, while gas-condensates exhibit preferential loss of their heavier solutes with attendant, dominant, control of their fundamental properties. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 40]
机译:斜率因子(SF)基于基辛(Kissin)的概念,它指定了储层流体和热解产物中正构烷烃指数分布中浓度随碳数增加而降低的速率。发生两个指数级数。 SF(C-2-n-C-5)总是比SF(n-C-6 +)陡,反映了稳定性和开裂机理。斜率的折断发生在n-C-6。假组分(P-n)代表被碳原子数细分的总成分,其浓度也以指数形式下降至C-10以上,从而有助于测量SF(P-10 +)。在C-10 +范围内的沥青质热解物中,SF(P-10 +)和SF(n-C-10 +)表现出显着的相关性,这表明在生成过程中社区尚不确定。在油窗内的转化水平下,沥青质热解的SF(C-2-n-C-5)值介于1.32和1.55之间,SF(n-C-10 +)的值介于1.07和1.24之间。来自加拿大西部盆地的储层流体(油)显示出相似的范围和相关值。含黄铁矿的干酪根浓缩物的热解产物产生的SF值高于沥青质热解产物和普通油的SF值,这可能是由于黄铁矿诱导的催化作用所致。由于油和压力下降(温度低,流体)和凝析油(温度高),由于压力和温度的降低,通过迁移的方式耗尽了油。石油可以溶解气体和轻质烃,而凝析油优先显示出其较重的溶质流失,并伴随着对其基本性能的控制。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:40]

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