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渤海某气田采取间歇式注气开采的方式,当停止注气后管道内高压气体需要泄放以保证海管安全。一种泄放方式是将高压气体泄放到另外一条低压输气海底管道,另一种泄放方式是在平台上通过火炬放空。利用OLGA动态模拟软件进行方案比选,结果表明:将高压气体泄放到另外一条低压输气海底管道,冬季泄压会造成高压海底管道温度低于其设计温度,因此推荐在夏季进行泄放;当泄放阀开度达到10%时,泄放最大流量与开度100%时接近,而低压海管入口流体温度升高到-12.9℃,有效降低了泄放时产生的低温对下游低压海底管道输气的影响。至于泄压至平台火炬系统,因泄压阀上下游压差过大,造成火炬管网需要超低温设计。因此最终推荐采取泄压至低压输气海底管道的方案。 相似文献
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针对未设置隔热层的轻质油品管道是否需要设置热膨胀安全泄压阀问题,通过对封闭油品箭道内温度和压力变化过程进行分析,推导出两者之间的变化关系,给出了管道是否需要设置热膨胀安全泄压阀的判断和计算方法,并以实例分析证明油品符道设置热膨胀安全泄压阀的必要性。 相似文献
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用Flarenet软件对某新建乙醇合成项目的整个火炬排放系统的安全阀及火炬管网进行建模,按照不同泄放工况分别计算。根据排放支管和火炬总管的马赫数计算结果,对管道尺寸进行调整并校核计算,使所有排放管道的马赫数满足规范的要求。在计算过程中,设定安全阀尺寸(经验值),使额定泄放量满足实际泄放量的需求,并按安全阀后总背压与设定压力的比值选择合适的安全阀型式。Flarenet软件可以高效率的对管道尺寸进行优化,使排放管的马赫数符合要求;准确计算安全阀的总背压,有良好的实际应用价值。 相似文献
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通过对衰减方程进行求导,然后再积分的方法,推导得到了衰减方程参数之间的关系:6=dc。由此提出了一种求解方程参数的新方法。该方法克服了传统采用近似法确定衰减方程参数的不足,具有简单、方便、快速、精确的特点。经实际算例验证表明,方法是有效、可靠的,易于被油气藏工作者掌握和使用。 相似文献
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利用酯化反应和聚合反应合成各种不同化学结构的PMA降凝剂小样,考察了在各种基础油中的降凝效果,重点探讨了PMA降凝剂的分子量和酯基侧链碳数分布等化学结构对降凝效果的影响,对提高我国PMA降凝剂的技术水平具有一定现实意义。 相似文献
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南京地区金子运动与黄马青群底部石灰岩质角砾岩的成因 总被引:3,自引:0,他引:3
1935年朱森[1]等研究宁镇山脉地质时,首先提出中三叠世末期这里发生过重要的地壳运动,称金子运动,上三叠统黄马青群底部有石灰岩质角砾岩不整合在下中三叠统青龙群之上。1945年喻德渊[2]研究了安庆地区的同一地壳运动,黄马青群底部角砾岩同样不整合在青龙群之上,称淮阳运动,并强调淮阳运动结束了古生代以来下扬子地区长期海侵的历史,在地质发展中具有重要的变革作用。李四光[3]从区域的角度肯定了金子运动(淮阳运动)在华南和东南亚地区的地质意义。1962年以来,不少单位和个人[4,5,6]对此期运动作了研究,并肯定了它的存在。 相似文献
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THE CONFIGURATION OF THE BASEMENT BENEATH THE ZAGROS BASIN 总被引:4,自引:0,他引:4
It has long been recognised that the deposition and deformation of the Phanerozoic cover in the Zagros Basin (mountains plus foreland) was strongly influenced by the reactivation of old tectonic fabrics in its basement. Facies boundaries and structures trending north-south and NW-SE can be attributed to the reactivation of Pan-African sutures and Najd faults which are exposed in the Nubian-Arabian Shield. However, to the east of a projection of the Oman line SWwards into the Rhub Al Khali Basin, cover structures have a NE-SW trend which is not seen in Arabia. This boundary may overlie a Pan-African suture between Arabia and India (Somalia or Pakistan).
Data including magnetic intensities, geothermal gradients and isopach maps are used here to distinguish old faults which were reactivated in the basement from more recent faults formed in the cover by Zagros shortening. Old faults trending NW-SE are interpreted as having reactivated episodically since the Permo-Triassic opening of Neo-Tethys; perhaps more significantly, the basement faults that reactivated in the East Arabian Block since then trend north-south. The basement configuration is clarified by extending a modified East Arabian Block across the Zagros to an "East Arabian-Zagros block" in which the NW trend of the Zagros lies between two syntaxes. This suggests a new tectonic framework for the region. The repeated reactivation of basement faults throughout the East Arabian-Zagros Block controlled source rocks, traps and seals for the supergiant and giant oil and gas reserves which are present at various stratigraphic levels in different areas. 相似文献
Data including magnetic intensities, geothermal gradients and isopach maps are used here to distinguish old faults which were reactivated in the basement from more recent faults formed in the cover by Zagros shortening. Old faults trending NW-SE are interpreted as having reactivated episodically since the Permo-Triassic opening of Neo-Tethys; perhaps more significantly, the basement faults that reactivated in the East Arabian Block since then trend north-south. The basement configuration is clarified by extending a modified East Arabian Block across the Zagros to an "East Arabian-Zagros block" in which the NW trend of the Zagros lies between two syntaxes. This suggests a new tectonic framework for the region. The repeated reactivation of basement faults throughout the East Arabian-Zagros Block controlled source rocks, traps and seals for the supergiant and giant oil and gas reserves which are present at various stratigraphic levels in different areas. 相似文献
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微构造对油水运动规律的影响 总被引:2,自引:0,他引:2
对微构造的成因和分类进行了论述,并以张天渠油田为例,就各种微构造组合方式对油水运动规律的影响进行了说明,得出结论:正向微构造为油气富集区,负向微构造为低含油气或严重水淹区。在确定加密井井别时,应尽可能地把生产井钻在正向微构造区,把注水井钻在负向微构造区。 相似文献
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本文阐明了最大熵反褶积(MEDEC)的理论根据,并证明:仅当地层脉冲响应为白噪序列和子波为最小相位时,MEDEC预测滤波器的逆为子波的最小相型,地震序列预测滤波输出的误差序列等于地层脉冲响应的估值;同时还分析了它的误差来源;模拟实例证实了以上分析.阐明克莱鲍特(Claerbout)将伯格(Burg)递推中的偏相关系数看成层反射系数的解释,只适应于Goupilau型地层中深部震源子波为白噪的模型,而不能把他的解释误解为MEDEC的理论根据.作者提出一种使褶积序列中子波最小相位化的滤波器G(z)的求法:将G(z)=S(z~(-1))/Sm(z~(-1))用升幂长除展开,即提G(z)的时间响应g(n),这是一种精确算法而非统计估计.这里定义S(n)为子波,S_m(n)为它的最小相型,S(z)=(s(n)),S_m(z)=z(S_m(n)).作者还导出一个多项式长除的快速递推公式,它不仅可以求解上述最小相位化滤波器,还可以以求有理分式型系统或信号z变换的反变换. 相似文献
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扬子地区古生代盆地基底普遍具有双层结构,下层中深变质基底由太古-下元古界麻粒岩相-角闪岩相、角闪岩相-高绿片岩相变质岩组成,同位素地质年龄为25~31亿年、20~25亿年,反映了陆核、陆块两个不同的发展阶段;上层浅变质基底由中元古界低绿片岩相变质岩组成,同位素地质年龄为10~20亿年,中元古代末的内硅铝造山作用及A型俯冲作用使全区连成不成熟的泛大陆,其西部、北部则发展为低稳定性的克拉通。 相似文献