一种油田原油含水率的近红外光谱检测与分析方法

石油作为重要战略资源,对其组分进行实时分析检测在石油化工领域有着重要意义。随着石油资源的不断开发,在已长时间开采油井的生产过程中以及新油井开采前,需要对井下原油组分进行分析检测,以判定开采的必要性。原油组分实时检测,在原油开采、生产、储运以及销售过程中都起着关键的作用,针对传统检测方法存在精度低、效率低等问题,近年来在原油组分检测技术的研究方法上引入了在测量领域得到广泛、有效应用的近红外光谱测量技术。以井下原油作为研究对象,利用从大庆油田获得的提纯原油与水按体积比配制了原油占比分别为1%~20%共39个组分的实验样品来模拟井下原油。研究了近红外光谱透射法测量原油组分的基本原理,并利用SW2520型近红外光谱仪与卤素光源以及配套组件集成了原油样品近红外光谱数据测量系统,完成了系统的标准化实验并利用此标准化后的系统采集了39个组分原油样品的近红外吸收光谱数据。利用移动窗口平滑法、Savitzky-Golay卷积平滑法以及Savitzky-Golay卷积求导法对原油近红外光谱数据进行预处理以消除噪声,利用偏最小二乘法和支持向量机回归方法SVR两种分析方法对预处理后的原油样品近红外光谱进行建模,分别建立了原油组分分析预测模型。研究结果表明,利用偏最小二乘法模型预测均方根误差为0.003 755 14,决定系数R2为0.999 999,预测精度优于0.1%,预测效果十分理想。利用近红外光谱技术对配制的不同比例的井下原油模拟测试样品进行测试建模和分析,为井下原油组份检测提供了一种新的思路,该方法可以有效的解决原油含水率的检测问题,为开发油田现场实时原油检测分析装备提供技术支撑。     

Supported Nickel-Cobalt Oxide Catalysts for the Isotopic Exchange of Deuterium between Hydrogen and Water Vapour

The specific catalytic activity of supported nickel-cobalt (II) oxide catalysts for the isotopic exchange of deuterium between hydrogen and water in the vapour phase was tested. The specific surface area of the catalysts was evaluated by nitrogen adsorption at ?195.8 °C and application of the BET-equation. The specific metallic surface area for these catalysts was carried out at liquid nitrogen temperature by hydrogen adsorption. Comparison between the specific activity of the catalysts and the specific surface area and specific metallic surface area teas made. The results of this study indicated that nickel catalysis supported with 15 – 20 mole% CoO exhibit a relatively high catalytic activity for the isotopic exchange reaction between hydrogen and water vapour, high specific surface area and high specific metallic surface area.     

A dynamic method for the study of H/D exchange on Ni catalysts

An experimental method and an adequate theoretical model for the study of H/D exchange on Ni supported catalysts are proposed. A satisfactory agreement between experimental measurements and theoretically calculated data is obtained. The method can be applied to determine parameters of a process such as the hydrogen content on metal, the hydrogen content on support, the equilibrium isotopic effects and the rate coefficients of the H/D exchange between the involved phases.     

NMR properties of petroleum reservoir fluids

NMR well logging of petroleum reservoir require the measurement of the NMR response of water, oil, and gas in the pore space of rocks at elevated temperatures and pressures. The viscosity of the oil may range from less than 1 cp to greater than 10,000 cp. Also, the oil and gas are not a single component but rather a broad distribution of components. The log mean T1 and T2 relaxation time of dead (gas free) crude oils are correlated with viscosity/temperature and Larmor frequency. The relaxation time of live oils deviate from the correlation for dead crude oils. This deviation can be correlated with the methane content of the oil. Natural gas in the reservoir has components other than methane. Mixing rules are developed to accommodate components such as ethane, propane, carbon dioxide, and nitrogen. Interpretation of NMR logs uses both relaxation and diffusion to distinguish the different fluids present in the formation. Crude oils have a broad spectrum of components but the relaxation time distribution and diffusion coefficient distribution are correlated. This correlation is used to distinguish crude oil from the response of water in the pores of the rock. This correlation can also be used to estimate viscosity of the crude oil.     

Nickel/Chromium oxide/Zirconium oxide Catalysts for Hydrogen/Deuterium Isotopic Exchange

Catalysts composed of nickel and promoted with different metal oxides proved to be suitable for H/D isotropic exchange between hydrogen and water vapour. They loss their activity due to water condensation on their surfaces. Several nickel/chromium oxide/zirconium oxide catalysts of different composition were prepared by the coprecipitation technique. The liquid phase activity of these catalysts were followed using the hydrogen peroxide decomposition on their surfaces at different temperatures. The surface characteristics of the examined catalysts were followed by applying the BET method. The results were discussed and lead to the required catalyst composition which resists the water condensation on its surface during operation and has relatively high activity in the vapour phase H/D isotopic exchange reaction between hydrogen and water.     

结合有效介质理论的乳状液太赫兹光谱分析

原油乳状液对原油的长距离输运具有重要影响,乳状液的油、水状态及相互作用机制还需新理论和新方法获得新认识,基于有效介质理论,本文研究了原油乳状液太赫兹光谱响应特征.通过太赫兹时域光谱系统测试得到了含水率为0～28％的原油乳状液的太赫兹时域光谱,结合傅里叶变换计算了吸收系数和介电常数等光学参数,同一频率下吸收系数等光学参数...     

用分子动力学模拟甲烷水合物热激法分解

用分子动力学模拟方法研究甲烷水合物热激法分解，系统地研究注入340 K液态水的结构Ⅰ型甲烷水合物的分解机理.模拟显示水合物表层水分子与高温液态水分子接触获得热能，分子运动激烈，摆脱水分子间的氢键束缚，笼状结构被破坏.甲烷分子获得热能从笼中挣脱，向外体系扩散.热能通过分子碰撞从外层传递给内层水分子，水合物逐层分解.对比注入277K液态水体系模拟结果，得出热激法促进水合物分解. 关键词： 甲烷水合物 分子动力学模拟 热激法     

金刚石压腔结合拉曼光谱技术进行氢同位素分馏的实验研究

应用水热金刚石压腔结合拉曼光谱技术来进行石膏和重水间稳定同位素分馏的实验研究.氢同位素 D 与 H 的质量差百分比是所有稳定同位素里最大的,由质量引起的分馏更容易发生,更容易在实验中观测;石膏是浅部地壳重要的含水矿物,它与重水之间的同位素分馏效应对矿物-水体系的同位素平衡分馏研究具有重要意义.常用分馏系数是指两矿物或两...     

SPA-PLS的高含水原油近红外光谱含水率分析

准确及时的检测原油含水率对注水策略调整、原油开采能力评估、油井开发寿命预测等均具有重要意义。然而,当前我国大多数油田均已进入高含水的开发中晚期,含水率测量难度大且准确率不高。在此背景下,开展了高含水情况下利用近红外光谱进行原油含水率测量的研究。 首先介绍了目前原油含水率检测的常用方法,分析了它们的优劣。理论上,由于水的近红外光吸收带与原油中C-H键的吸收带有明显区别,根据Lambert-Beer吸收定律和吸光度线性叠加定律可知,不同含水率高含水原油近红外光谱会存在较强响应差异。为此,对高含水原油进行近红外光谱检测,建立原油含水率与近红外光谱响应间的非线性映射模型,可实现高含水原油含水率的精确测量。为了验证该方法的有效性,搭建了近红外光谱数据采集实验装置：采用白炽灯作为光源,经过光路调节成平行光后垂直射入样品池,用近红外光谱仪（海洋光学NIR512）采集光谱用于分析。其中,接收光谱仪带宽为900～1 700 nm,平均分成512个波段。光谱数据利用光谱仪配套软件储存在电脑中。样本采用相同厚度不同比例的油水混合物,样本含水率范围为70%～99%,共采集数据60组,每组重复3次取平均值。得到原始数据后,先进行原始数据预处理,以减少数据采集时来自高频随机噪音及温度不稳定、样本不均匀、基线漂移、光散射等不利因素的影响。分别选用了S-G滤波、一阶导数和S-G滤波+一阶导数作为数据预处理的方法,利用连续投影算法(SPA)对光谱数据进行降维,并利用偏最小二乘法（PLS）和多元线性回归（MLR）进行建模,模型精度通过计算均方根误差值（RMSE）和相关系数（r）来验证。对比发现,使用S-G滤波+一阶导数建立的模型RMSE值最小（RMSE=0.007 0,r=0.998 3）。使用SPA降维后的模型要优于全波段PLS模型（RMSE=0.083 3,r=0.920 6）与MLR模型（RMSE=0.099 9,r=0.967 1）。利用SPA提取出的31个特征波长建立的模型仅占全波段的6.05%,并获得了较好的精度。证明了利用光谱检测高含水原油含水率可行性,并且得到了满意的精度,为高含水原油的含水率检测提供了新的方法, 为进一步利用近红外光进行高含水原油的快速检测与在线监测提供参考。     

铵水间质子交换的再研究:不受扩散约束的化学交换

对铵盐水溶液中铵离子与水分子间的质子交换进行了再研究. 以核磁共振(NMR) 波谱学方法测定了不同pH值, 不同温度和含不同共存盐浓度的氯化铵水溶液中质子交换速率, 组分自扩散系数及NMR自旋晶格弛豫时间. 结果显示铵水间的质子交换并不受交换主体分子或离子自扩散的约束. 交换机理包括化学键和氢键的交换. 在溶液中, 水分子以氢键为桥 梁连接铵和其因水解而产生的碱性部分--氨. 在氢交换的过程中, 氨从水分子接受一个氢 成为铵, 同时另外一端的铵提供一个氢给水分子而变成氨, 或者一个氢从水分子转移到氨而同 时另外一个氢从铵转移到水. 在铵水质子交换的过程中没有净的电荷转移. 在低pH条件下, 由水解产生的氨的浓度降低, 亦即铵-水-氨复合物减少, 结果氢交换的可能性降低. 这解释了生物氢交换体系中的一种常见的在低pH值条件下氢交换变慢的现象.     

Methane steam reforming in an annular microchannel with Rh/Al2O3 catalyst

Regularities of methane conversion in the presence of water steam were obtained experimentally while activating chemical conversions on the inner convex wall of an annular microchannel. The steam methane reforming was done on the Rh/Al₂O₃ nanocatalyst with the heat applied through the microchannel gap from the outer wall. Concentrations of the products of chemical reactions in the outlet gas mixture are measured at different temperatures of the outer microchannel wall. The range of channel wall temperatures at which the ratio of hydrogen and carbon oxide in the outlet mixture grows substantially is determined. Data on the composition of methane conversion products for the ratio H₂O/CH₄ = 1.77 and the activation energy of methane steam reforming at reactor outer wall temperatures of up to 880°C are obtained. The effect of the radiation heat exchange and the external diffuse limitation on the rate of chemical conversions in methane steam reforming in an annular microchannel with external heat supply is determined.     

Using stable isotopes and major ions to identify hydrological processes and geochemical characteristics in a typical karstic basin,Guizhou, southwest China

The investigation of hydrological processes is very important for water resource development in karst basins. In order to understand these processes associated with complex hydrogeochemical evolution, a typical basin was chosen in Houzai, southwest China. The basin was hydrogeologically classified into three zones based on hydrogen and oxygen isotopes as well as the field surveys. Isotopic values were found to be enriched in zone 2 where paddy fields were prevailing with well-developed underground flow systems, and heavier than those in zone 1. Zone 3 was considered as the mixture of zones 1 and 2 with isotopic values falling in the range between the two zones. A conceptual hydrological model was thus proposed to reveal the probable hydrological cycle in the basin. In addition, major processes of long-term chemical weathering in the karstic basin were discussed, and reactions between water and carbonate rocks proved to be the main geochemical processes in karst aquifers.     

Reactivation of Promoted Nickel Catalysts for Deuterium Exchange between Hydrogen and Water in the Vapour Phase

Binary promoted nickel – chromium oxide and ternary promoted nickel – chromium oxide – aluminium oxide mixed catalysts were prepared for use in the present study. The catalysts were prepared by co-precipitation of the corresponding metal nitrates as carbonates followed by calcination in nitrogen atmosphere at 350 °C and reduction in hydrogen atmosphere at 320 °C. To prevent spontaneous oxidation of the catalysts, bidistilled water was added followed by heating of the catalyst mixtures at about 110 °C in hydrogen atmosphere for few hours. Deactivation of catalysts was studied by measurements of the variation of their activities with the time of contact of the reacting gas mixtures with the catalyst surface in the reaction chamber. It was found that while the catalytic activity of ternary catalysts for the isotopic exchange of deuterium between hydrogen and water vapour was higher than that of the binary one, the loss in activity of the former teas faster than the latter. Reactivation of the catalysts were carried out at different temperatures between 110–160°C in hydrogen atmosphere. Catalytic activity measurements indicated that higher temperatures are better for the reactivation process.     

分子动力学模拟研究方解石表面润湿性反转机理

利用分子动力学模拟技术从分子尺度探究方解石表面润湿性反转机理.首先,研究方解石表面润湿性反转过程;而后,从原油分子-方解石表面与原油分子-原油分子/水分子相互作用两个方面系统揭示方解石表面润湿性反转机理.结果:(1)水分子能够驱离方解石表面弱吸附的非极性分子造成润湿性的改变,但不能驱离强吸附的极性分子使润湿性反转难以实现;(2)原油分子极性越强与方解石表面相互作用越强,极性分子与方解石表面之间主要为静电力,非极性分子与方解石表面之间主要为范德华力;(3)原油分子极性越相近分子之间的相互作用越强,分子极性相差越大分子之间的相互作用越弱.非极性分子之间主要是范德华力,极性分子之间主要是静电力;(4)原油分子在方解石表面和水分子的共同作用下形成乙酸-吡啶-水-甲苯-己烷的稳定吸附序列.本研究为靶向提高采收率技术的设计与应用提供理论基础.     

质谱法精密测定重水中的氢同位素丰度

介绍了用高分辨气体质谱计精密测定重水中氢同位素丰度的分析方法．实验自制了一套重水分解系统,以金属铀作还原剂,在一定的温度下还原重水为氘气．采用低温活性碳作为吸收剂,将样品分解、制备成气体试样,用高分辨气体质谱计测定重水中氢同位素丰度．该方法测定高浓度（〉99％）重水的氘丰度,测量结果的相对标准偏差不大于0．02％。     

声波作用下液滴碰并沉降及其氢氧同位素特征

液滴沉降过程中会与环境水汽发生物质交换.论文通过小尺度室内实验,研究了低频声波作用下液滴碰并沉降及其与气室环境水汽氢氧同位素交换特征.研究结果证实液滴沉降过程中存在同位素交换,该过程受声波显著影响.声波作用后液滴粒径增大,液滴沉降后汇集水中重同位素出现富集.液滴与环境水汽氢氧同位素交换强度与液滴初始粒径呈正相关,声波对...     

Separation of Deuterium Isotope by Chemical Exchange between Hydrogen and Water Vapour

The separation factor of deuterium (α) for the exchange reaction between hydrogen and water vapour at 100 °C has been measured and was found to be equals to 2.52 and 2.50, depending on the used experimental technique.

An empirical equation relating the variation of the separation factor with temperature for such isotopic exchange reaction has been deduced. The values of α were calculated from 0–800 °C and indicated close agreement with those calculated from spectroscopic data.

Comparison of the deduced empirical equation with the general equation relating the separation factor with temperature for such reaction, allowed the calculation of the zero point energy, as well as the free energy as a function of temperature.     

Tribochemical investigation of DLC coating in water using stable isotopic tracers

Tribochemical reaction of DLC coating in water was investigated by using a stable isotopic tracer, ¹⁸O labeled water (H₂¹⁸O), to carry out the friction test of DLC coating and 440C ball pair, and using ToF-SIMS to analyze the worn surfaces. The result showed that DLC coating tribochemically reacted with water to form hydrophilic hydroxyl and carboxyl groups on surface, and suggested that the formed hydroxyl mainly combined with the secondary or tertiary carbons on the surface. The surface layer on the counter ball mainly consisted of C from the coating, Cr, Fe from the ball and ¹⁸O from water, and was rich in ¹⁸OH. It is thought that the hydrophilic groups formed at the interfaces play an important role in low friction and wear behaviors of DLC coating and the counter part in a water environment. Comparing with that obtained from the test in D₂O, the result also suggests that hydrogen/deuterium exchange is easy to occur between the products containing OD on the mated ball and some adsorbates in an ambient air environment.     

用分子动力学模拟甲烷水合物热激法结合化学试剂法分解

用分子动力学模拟方法研究甲烷水合物的热激法，化学试剂法，以及热激法结合化学试剂法分解，系统研究温度为277K和340K时添加液态水(WTR)和30wt％乙二醇(EG)溶液对水合物分解的影响.模拟显示WTR与水合物表面水分子形成氢键，破坏水合物原有的氢键平衡，造成笼状结构坍塌，水合物分解.EG分子中的羟基与水合物表面水分子形成氢键，从而破坏原有的稳定结构，造成水合物笼状结构被破坏，达到促进水合物分解，释放甲烷气体的效果.比较温度为277K和340K时添加WTR和30wt％EG溶液对水合物分解效果得出EG(340K)> WTR(340K)>EG(277K)>WTR(277K)，热激法结合化学试剂法能更好促进水合物分解.     

氢及其同位素宽区状态方程的核量子效应

应用大规模第一性原理分子动力学数值模拟方法,系统研究了氢及其同位素在极端条件下的分子解离规律及状态方程,并给出了参数化的解函数拟合公式。结合分子、原子流体量子振动的一阶修正,揭示了氢及其同位素的核量子效应,解析获得了氢、氘分子在温稠密区域分子解离规律的差别。由第一性原理状态方程给出了雨贡纽曲线,与气炮、化学炸药、磁驱动、高能激光等实验数据相符合,并详细讨论了由核量子效应导致的氢、氘雨贡纽曲线的同位素效应。