伊拉克南部鲁迈拉北部油田Zubair油藏上砂岩段油田水化学、物理特征及矿化度分布

Salih Muhammad Awadh
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引用次数: 3

摘要

对鲁迈拉北油田Zubair储层上砂岩段(Barriemian-Hauterivian)油田水进行了盐度解释和盐水组成地球化学演化研究。油田水与储层岩石相互作用,形成了与墨西哥湾近海/陆上中生代储层地层水成分相似的部分混合海水盐水。高TDS (207350- 230100;平均215625 mg/L)与电导率(340362-372762;平均351024μs),阴离子Cl (123679 mg/L)和阳离子Na (29200 mg/L)和Ca (14674 mg/L)分别占主导地位。阳离子的贡献(epm%)分别为Na(70.2)、Ca(18.9)、Mg(8.1)和K (1.7);阴离子为Cl(99.7)、SO4(0.25)、HCO3(0.07)、CO3(0.005)。钠(57550-60500mg/L)比海水高6倍,钙和镁高3倍,氯化物高6.5倍,但硫酸盐的消耗减少到6倍,因为硫酸盐释放出硫,并与不同的碳氢化合物结合,作为天然硫,与氢结合形成H2S。Zubair油田的水具有酸性pH值(pH=5.2- 5.77),岩石物性增强,高比重(1.228)预示着高流体压力(4866 psi)、油气饱和度(0.43%)、含水饱和度(0.57%)和孔隙度(12.7)。矿物饱和度模型表明,Zubair油田水在pH值为5.45时为不饱和水,但在模拟pH值下,水镁石在pH值为9.12时处于平衡状态,水镁石和波特兰石在pH值为11.9时处于过饱和状态。矿物的溶解度随温度、压力、pH、Eh和离子强度的变化而变化,因此地层损害是按比例发展的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Chemical, physical characterization and salinity distribution of the oilfield water in the Upper Sandstone Member of the Zubair reservoir at Rumaila North Oilfield, Southern Iraq
The oilfield water in the Upper Sandstone Member of the Zubair reservoir (Barriemian-Hauterivian) at Rumaila North Oil Field was investigated for the interpretation of salinity and geochemical evolution of brine compositions. The interaction of the oilfield water with reservoir rock resulted in a brine water derived from the marine water origin of partial mixing with meteoric water similar to the compositional ranges of formation water from Gulf of Mexico offshore/onshore Mesozoic reservoirs. The high TDS (207350- 230100; average 215625 mg/L) is consistent with the electrical conductivity (340362-372762; average 351024μs), and predominantly represented by Cl (123679 mg/L) as anions and (29200 and 14674 mg/L) for Na and Ca as cations respectively. The contribution of cation (epm%) are as Na (70.2), Ca (18.9), Mg (8.1) and K (1.7); and anion as Cl (99.7), SO4 (0.25), HCO3 (0.07) and CO3 (0.005). sodium (57550-60500mg/L) is greater than of seawater six times, calcium and magnesium three times greater, and chloride 6.5 times greater, but Sulfate is depleted to six times less due to a sulfur release from sulphates and link with different hydrocarbon species, precipices as native sulphur and link with hydrogen forming H2S. The Zubair oilfield water is characterised by acidic pH (pH=5.2- 5.77) enhanced petrophysical properties, high specific gravity (1.228) predicts a high fluid pressure (4866 psi), hydrocarbon saturation (0.43%), water saturation (0.57%) and porosity (12.7). The Mineral saturation model indicates that the Zubair oilfield water is an unsaturated water with respect to all suggested minerals at 5.45, but at simulated pH, brucite being an equilibrium at pH 9.12, but brucite and portlandite being supersaturated at pH 11.9. The mineral solubility responses to the changes in temperature, pressure, pH, Eh, and ionic strength, thereby formation damage is proportionally developed.
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