石油实验地质
石油實驗地質
석유실험지질
Petroleum Geology and Experiment
2015年
6期
681-688
,共8页
原油稳定性%原油裂解%生烃动力学%油气相态%寒武系%塔里木盆地
原油穩定性%原油裂解%生烴動力學%油氣相態%寒武繫%塔裏木盆地
원유은정성%원유렬해%생경동역학%유기상태%한무계%탑리목분지
oil stability%oil cracking%hydrocarbon generation kinetics%hydrocarbon phase%Cambrian%Tarim Basin
塔里木盆地寒武系深层烃类相态是地球化学家和石油勘探家密切关注的科学问题。应用封闭体系黄金管热模拟方法,对塔里木盆地塔河油田稠油、正常原油、高蜡原油进行热模拟实验。在频率因子为1.78×1014s-1的前提下,塔河油田奥陶系井稠油具有最宽的C1-C5质量生成的活化能分布,分布范围为56~66 kcal/mol,主频活化能最低,为59 kcal/mol。根据原油转化率,使用Kinetic软件计算表明原油作为油相可以存在于178~205℃的储层中。依据塔里木盆地塔北、塔中、塔东、巴楚4个古隆起典型钻井寒武系古地温演化,建立了4个古隆起寒武系古油藏裂解动力学模型。模型表明塔北隆起塔深1井寒武系建隆Ⅰ顶部的古油藏至今可以保持独立油相状态,建隆Ⅰ底部的古油藏能保持凝析油状态。巴楚、塔中、塔东地区典型寒武系钻井模拟表明,寒武系中的烃类可能以天然气、凝析油为主要相态类型。
塔裏木盆地寒武繫深層烴類相態是地毬化學傢和石油勘探傢密切關註的科學問題。應用封閉體繫黃金管熱模擬方法,對塔裏木盆地塔河油田稠油、正常原油、高蠟原油進行熱模擬實驗。在頻率因子為1.78×1014s-1的前提下,塔河油田奧陶繫井稠油具有最寬的C1-C5質量生成的活化能分佈,分佈範圍為56~66 kcal/mol,主頻活化能最低,為59 kcal/mol。根據原油轉化率,使用Kinetic軟件計算錶明原油作為油相可以存在于178~205℃的儲層中。依據塔裏木盆地塔北、塔中、塔東、巴楚4箇古隆起典型鑽井寒武繫古地溫縯化,建立瞭4箇古隆起寒武繫古油藏裂解動力學模型。模型錶明塔北隆起塔深1井寒武繫建隆Ⅰ頂部的古油藏至今可以保持獨立油相狀態,建隆Ⅰ底部的古油藏能保持凝析油狀態。巴楚、塔中、塔東地區典型寒武繫鑽井模擬錶明,寒武繫中的烴類可能以天然氣、凝析油為主要相態類型。
탑리목분지한무계심층경류상태시지구화학가화석유감탐가밀절관주적과학문제。응용봉폐체계황금관열모의방법,대탑리목분지탑하유전주유、정상원유、고사원유진행열모의실험。재빈솔인자위1.78×1014s-1적전제하,탑하유전오도계정주유구유최관적C1-C5질량생성적활화능분포,분포범위위56~66 kcal/mol,주빈활화능최저,위59 kcal/mol。근거원유전화솔,사용Kinetic연건계산표명원유작위유상가이존재우178~205℃적저층중。의거탑리목분지탑북、탑중、탑동、파초4개고륭기전형찬정한무계고지온연화,건립료4개고륭기한무계고유장렬해동역학모형。모형표명탑북륭기탑심1정한무계건륭Ⅰ정부적고유장지금가이보지독립유상상태,건륭Ⅰ저부적고유장능보지응석유상태。파초、탑중、탑동지구전형한무계찬정모의표명,한무계중적경류가능이천연기、응석유위주요상태류형。
The hydrocarbon phase of the deep Cambrian in the Tarim Basin is a scientific focus of geochemists and explorationists. Thermal simulations of heavy oil, normal oil and waxy?oil from the Tahe Oilfield in the Tarim Basin were carried out using a gold?tube confined system. For a frequency factor ( A) of 1. 78 × 1014 s-1, the activation energy range of C1-C5 gas yield of heavy oil is the widest, ranging from 56 to 66 kcal/mol, and the dominant potential is at 59 kcal/mol. In view of the ratio of oil conversion to gas, oil can be a separate phase at temperatures of 178-205 ℃. According to the paleo?temperatures of the Cambrian wells from the Tabei, Tazhong, Tadong and Machu uplifts, four dynamic models of the Cambrian reservoir cracking were established. The paleo?oil reservoir of well Tashen1 in the Tabei Uplift can be as a separate oil phase above BuiltupⅠin the Cam?brian at present, whereas only condensate oil phase existsat the bottom of the UpliftⅠ. The models of the Cam?brian paleo?oil reservoirs of typical wells from the Bachu Uplift, Tazhong Uplift and Tadong Uplift suggest that the hydrocarbon phase of the above areas may be dominated by gas and condensate phases.