共查询到20条相似文献，搜索用时 46 毫秒
1.
水平井分段多簇压裂是非常规油气藏开发的关键技术,在合理利用压裂诱导应力增大储层改造体积的同时,避免井间干扰所导致的裂缝砂堵和压裂窜扰,是压裂工艺优化中的关键科学问题。文章针对超临界CO2分段多簇压裂的缝间干扰和井间干扰问题,采用流固耦合的扩展有限元方法研究单井及多井裂缝诱导应力演化特征,充分考虑裂缝内超临界CO2流动和滤失,从非常规油气储层岩性特征、地应力场分布及施工工艺等多方面对压裂扰动应力进行系统研究,揭示单井分段多簇压裂缝扩展机制及应力扰动特征,在此基础上研究多井井间压裂缝干扰规律。结果表明：高水平应力差、高弹性模量的储层中压裂干扰界限较大,低水平应力差、低弹性模量地层需适度增大簇间距,减小簇间干扰;老井压裂后,其邻井压裂缝非对称系数随井间距呈先增大、后减小的趋势;当井间距等于压裂干扰界限时,非对称系数λ达到最大,且井周改造范围最大,但裂缝两翼的非对称性可能导致储层动用不充分。本研究为水平井细分切割压裂和立体式井网设计优化提供理论基础,在“双碳”战略背景下对非常规油气资源高效开发具有重要意义。 相似文献
2.
福山凹陷流沙港组致密砂岩是海南福山油田勘探开发的重要目标之一。受复杂构造演化影响,该区致密砂岩具有砂泥薄互层明显、低孔低渗、高温等特征,为了解决以往储层改造中经常出现的施工压力高、缝高失控、砂堵、单井产量低、压裂后产量下降快等问题。借鉴非常规体积压裂技术,采用变排量、人工隔层控缝高、暂堵转向等工艺,同时进一步优化压裂液,应用纳米增效洗油剂,在福山油田致密砂岩开展了4口井次试验。研究结果表明：非常规体积压裂技术可有效降低砂堵风险,提高福山油田致密砂岩储层的改造效果。变排量、人工隔层控缝高、暂堵转向压裂等储层改造工艺的实施,有效控制了缝高,提高了储层的压开程度。纳米增效洗油剂的应用,最大限度地降低了液体对地层和裂缝的伤害,发挥了纳米液滴渗吸洗油作用,增加了油气井的稳产期。 相似文献
3.
在干热岩的开发和改造阶段,需要对储层进行水力压裂改造,储层改造体积(stimulated reservoir volume, SRV)是评价压裂效果的主要标准。微地震监测作为水力压裂的技术环节之一,可以对储层改造体积进行有效估算。本文探讨了基于微地震连续裂缝网络模型的SRV计算方法,以指导干热岩的水力压裂工作。首先,基于微震事件时空分布特征与多项震源参数进行连续裂缝网络建模;其次,提取裂缝网格长度,并选取适当的裂缝高度与裂缝宽度以计算储层改造体积;最后,选取某双井型干热岩微地震监测数据对该方法进行实际应用。实例应用结果表明,该方法可有效估算储层改造体积,为干热岩后续开发与改造提供依据。 相似文献
4.
多段多簇水平井压裂技术作为页岩油藏的重要开发手段已经得到了广泛认同,压后关井能充分发挥渗吸的作用,提高单井压后产量,但目前压裂液渗吸作用区域一直是困扰油藏工程师的重要难题。本文以陇东页岩油藏多段压裂井为研究对象,基于物质平衡原理,利用渗流力学和岩石力学理论,建立了压裂施工过程中和压后关井过程中流体压力扩散数学模型,研究了压力扩散和压裂液波及体积随时间的变化关系。结果表明：压裂液波及体积随关井时间的增加逐渐增加,但增加的幅度会逐渐降低。储层渗透率越小,孔隙度越大,压裂施工时间越长,关井阶段井底压力越高,地层能量越高。该结果可为页岩油藏最佳关井时间的确定提供理论支持。 相似文献
5.
页岩气的工业化开发要求对致密储层进行体积压裂改造,水平井多级分段压裂技术是成功开发页岩气藏的关键技术之一。页岩储层在地应力与致裂压力联合作用下突破页岩基质,沟通天然裂隙等弱结构面,形成高导流能力缝网系统,页岩储层中赋存的游离气和吸附气得以释放,提高了页岩气井的初始产量和最终采收率。根据渝东地区页岩储层工程地质特征,结合渝页A-2HF井、渝页B-2HF井矿场压裂施工数据,探索适用于渝东地区的页岩储层压裂工艺技术,结果表明,采用前置盐酸处理储层保持近井带导流能力,能够保障后续大排量施工压力窗口;低砂比粉砂段塞多级降滤实现“控近扩远”,增加储层改造体积;压力异常层段胶液前置充分造缝,可为后续滑溜水携带支撑剂进入地层创造有利条件。 相似文献
6.
7.
合理的储层改造和排采工艺技术是煤层气勘探开发的关键环节。在剖析比德—三塘地区煤层气地质与储层特征基础上,总结贵州省煤层气地质特征为:煤层多、累计厚度大（20 m以上）、含气量高（一般大于15 m3/t）、资源丰度高（一般大于2亿m3/km2）、临储比高（一般0.8以上）;但断层多、煤层跨度大（300 m左右）、地应力高、渗透性低、含水性差。提出可捞式桥塞分段压裂、连续油管水力喷射射孔分段压裂、电缆射孔桥塞联作分段压裂、复配低伤害压裂液等工艺技术。采用递进排采技术,优化管柱结构,实施动态分析的精细化排采。 相似文献
8.
微地震监测技术是页岩气开采过程中对页岩气储层压裂效果评价和指导压裂过程的重要手段,可通过观察、分析压裂过程中诱发微地震事件,获取压裂裂缝参数、导流能力、裂缝展布发育方向等信息。中牟区块牟页1井具有低孔、低渗储层特征,对含气层段的三层储层,采用大排量水力压裂施工,进行地面微地震监测、井中微破裂成像技术压裂监测及微地震监测;牟页1井监测压裂结果显示为缝长251～496m,缝宽120～252m,改造体积约为237.5×104～387.7×104 m3,方位角64°～80°。压裂实施使储层裂缝开启含气层段得到改造,指导了实时压裂和压裂效果评价。 相似文献
9.
为了提高水平井分段压裂煤储层改造体积,提高煤层气的采收率,基于水平井分段压裂裂缝诱导应力场,运用数值模拟手段,对裂缝间距进行了优化。结果显示,水平井分段压裂先压裂缝产生的水平诱导应力差随着与其裂缝距离的增加呈先增加后减少的趋势,导致最大水平主应力转向乃至反转。当诱导应力场叠加后的最大水平主应力转向角为5°时对应的位置为最优压裂分段间距,以此布置分段间距,既能保证间距尽可能的小,也能使裂缝正常扩展,形成多个相互平行的有效主裂缝,实现对煤储层的体积切割,提高煤储层的压裂改造增产效果,对于煤层气水平井分段压裂裂缝参数优化具有较好的指导意义。 相似文献
10.
11.
Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
12.
Inter-regional correlation of transgressions and regressions in the Cretaceous period 总被引：1，自引：0，他引：1
T. Matsumoto 《Cretaceous Research》1980,1(4):359-373
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous. 相似文献
13.
The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism. 相似文献
14.
正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8 相似文献
15.
正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci- 相似文献
16.
正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province 相似文献
17.
正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.) 相似文献
18.
正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet 相似文献
19.
正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.) 相似文献
20.
正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3), 相似文献