石油与天然气地质
石油與天然氣地質
석유여천연기지질
OIL & GAS GEOLOGY
2014年
3期
317-325
,共9页
国朋飞%何生%朱书奎%柴德蓉%张万峰%代威%张君立
國朋飛%何生%硃書奎%柴德蓉%張萬峰%代威%張君立
국붕비%하생%주서규%시덕용%장만봉%대위%장군립
基线鼓包%未知复杂混合物%全二维气相色谱-飞行时间质谱%生物降解油%泌阳凹陷
基線鼓包%未知複雜混閤物%全二維氣相色譜-飛行時間質譜%生物降解油%泌暘凹陷
기선고포%미지복잡혼합물%전이유기상색보-비행시간질보%생물강해유%비양요함
baseline hump%unresolved complex mixture%total two-dimensional gas chromatography/time-of-flight mass spectrometry%biodegraded oil%Biyang Depression
选择泌阳凹陷北部斜坡带的5个生物降解油,利用全二维气相色谱-飞行时间质谱(GC ×GC/TOFMS),结合气相色谱(GC)和气-质谱( GC/MS)等方法研究了生物降解油中“基线鼓包”的成因及其化合物组成。所选油样的原始化学组成相似、成熟度相近、降解等级分别为2,3,5,6,8级。随着降解等级增加,原油中的正构烷烃、异构烷烃、低分子量芳烃、甾萜类、多环芳烃等化合物依次被降解,化合物的种类显著减少;生物降解作用导致抗降解能力强,极性差别小的环烷烃同系物逐渐成为原油的主要组成,这些化合物在GC谱图中共流出,形成“基线鼓包”,其中的化合物被称为“未知复杂混合物( UCMs)”。全二维结构化谱图及标准样品验证分析表明,UCMs主要由环烷烃及其同系物组成,其碳环以六元环为基本组成单元,且可被区分为6类(Ⅰ-Ⅵ)化合物;其中Ⅰ和Ⅱ类UCMs分别由C16-C26长侧链烷基环己烷和C11-C16烷基十氢化萘等一环和二环环烷烃及其同系物组成,它们可能是微生物降解原油产生的新化合物;Ⅲ-Ⅵ类分别由倍半萜烷、三环萜烷、低分子量甾烷及重排甾烷、降藿烷等二环-五环环烷烃及其同系物组成,这些化合物主要由原油中抗降解能力较强的烃类富集而来。
選擇泌暘凹陷北部斜坡帶的5箇生物降解油,利用全二維氣相色譜-飛行時間質譜(GC ×GC/TOFMS),結閤氣相色譜(GC)和氣-質譜( GC/MS)等方法研究瞭生物降解油中“基線鼓包”的成因及其化閤物組成。所選油樣的原始化學組成相似、成熟度相近、降解等級分彆為2,3,5,6,8級。隨著降解等級增加,原油中的正構烷烴、異構烷烴、低分子量芳烴、甾萜類、多環芳烴等化閤物依次被降解,化閤物的種類顯著減少;生物降解作用導緻抗降解能力彊,極性差彆小的環烷烴同繫物逐漸成為原油的主要組成,這些化閤物在GC譜圖中共流齣,形成“基線鼓包”,其中的化閤物被稱為“未知複雜混閤物( UCMs)”。全二維結構化譜圖及標準樣品驗證分析錶明,UCMs主要由環烷烴及其同繫物組成,其碳環以六元環為基本組成單元,且可被區分為6類(Ⅰ-Ⅵ)化閤物;其中Ⅰ和Ⅱ類UCMs分彆由C16-C26長側鏈烷基環己烷和C11-C16烷基十氫化萘等一環和二環環烷烴及其同繫物組成,它們可能是微生物降解原油產生的新化閤物;Ⅲ-Ⅵ類分彆由倍半萜烷、三環萜烷、低分子量甾烷及重排甾烷、降藿烷等二環-五環環烷烴及其同繫物組成,這些化閤物主要由原油中抗降解能力較彊的烴類富集而來。
선택비양요함북부사파대적5개생물강해유,이용전이유기상색보-비행시간질보(GC ×GC/TOFMS),결합기상색보(GC)화기-질보( GC/MS)등방법연구료생물강해유중“기선고포”적성인급기화합물조성。소선유양적원시화학조성상사、성숙도상근、강해등급분별위2,3,5,6,8급。수착강해등급증가,원유중적정구완경、이구완경、저분자량방경、치첩류、다배방경등화합물의차피강해,화합물적충류현저감소;생물강해작용도치항강해능력강,겁성차별소적배완경동계물축점성위원유적주요조성,저사화합물재GC보도중공류출,형성“기선고포”,기중적화합물피칭위“미지복잡혼합물( UCMs)”。전이유결구화보도급표준양품험증분석표명,UCMs주요유배완경급기동계물조성,기탄배이륙원배위기본조성단원,차가피구분위6류(Ⅰ-Ⅵ)화합물;기중Ⅰ화Ⅱ류UCMs분별유C16-C26장측련완기배기완화C11-C16완기십경화내등일배화이배배완경급기동계물조성,타문가능시미생물강해원유산생적신화합물;Ⅲ-Ⅵ류분별유배반첩완、삼배첩완、저분자량치완급중배치완、강곽완등이배-오배배완경급기동계물조성,저사화합물주요유원유중항강해능력교강적경류부집이래。
Five biodegrade d oil samples from the north slope of Biyang Depression were analyzed by integrating the two -dimensional gas chromatography/time-of-flight mass spectrometry(GC ×GC/TOFMS),gas chromatography(GC)and gas chromatography-mass spectrometry ( GC-MS) to reveal the composition and genesis of ‘baseline hump ’ .All the oil sam-ples analyzed are of similar original compositions and thermal maturities ,but different degradation levels at 2,3,5,6 and 8,respectively.With the increasing of oil degradation level ,n-alkanes,iso-alkanes,aromatic hydrocarbons with low molec-ular weight,steranes,terpanes and polycyclic aromatic hydrocarbons are degraded successively ,resulting in the significant decrease of the number of compound types .The cyclic alkanes and isomers with similar polarities and strong resistance to biodegradation are enriched relatively in the biodegraded oil ,and their co-elution in GC chromatograms results in ‘base-line hump’ or so-called ‘unresolved complex mixtures (UCMs)’.Total 2D characteristic mass spectrums and standard compound tests show that cyclic alkanes and their homologues are the major components of the UCMs ,with a basic frame-work of cyclohexane .Additionally ,the UCMs can be divided into six types ( typeⅠto typeⅥ) .The typeⅠandⅡare com-posed of C16 -C26 long chain alkyl-cyclohexanes,C11 -C16 alkyl-decalins and their isomers.These cyclic alkanes with one or two rings might be the new compounds from the microbial transformation of normal oils .TypeⅢ-Ⅵare composed of sesquiterpenoids ,tricyclic terpanes , low molecular weight steranes , diasteranes and norhopanes , originated from the en-richment of hydrocarbons having relatively strong resistantance to degradation in the normal oils .