Directional Radial Drilling Increases Reservoir Coverage with Precise Wellbore Placement Resulting in a Significant Production Increase from a Thin Reservoir

A. Bashirov, I. Galas, M. Nazyrov, D. Kuznetsov, A.A. Akkuzhin
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Abstract

In many oil and gas provinces not only in Russia, but throughout the world, carbonate strata make up a significant portion of the sedimentary cover, and large accumulations of hydrocarbons are associated with them. However, the purposeful study of them as reservoirs for hydrocarbons in our country practically began only in the post-war years. In the special petrography laboratory carbonate rocks composing various stratigraphic complexes of almost all oil and gas provinces of the Soviet Union were studied, and in particular, Paleozoic carbonate strata of the Timan-Pechora province, Ural-Volga region, Belarus, Kazakhstan, ancient Riphean-Cambrian formations of Yakutia and relatively young strata of the Late Cretaceous of the northeastern Ciscaucasia. Carbonates are widespread sedimentary rocks. A very significant part of them was formed in the conditions of vast shallow-water marine epicontinental basins. A large number of works are devoted to the study of such deposits. However, issues related to the conditions of formation of carbonate sediments and their postsedimentary changes cannot be considered resolved, as well as the classification of the rocks themselves. The analyzed field is the Osvanyurskoye one. It was discovered in 2007. The field is located in the north-east of the European part of the Russian Federation, 2 km from Usinsk in the Komi Republic. The field is a part of the Timano-Pechora oil and gas province and it is a mature field (fig. 1). The objective was a 2.5m thick layer of the Serpukhov horizon.
定向径向钻井通过精确的井筒定位增加了储层的覆盖范围,从而使薄储层的产量显著提高
不仅在俄罗斯,而且在世界各地的许多石油和天然气省,碳酸盐岩地层构成了沉积盖层的很大一部分,并且与之相关的是大量的碳氢化合物聚集。然而,我国对它们作为油气储集层的有目的研究实际上是在战后才开始的。在专门的岩石学实验室中,对苏联几乎所有油气区的各种地层复合体的碳酸盐岩进行了研究,特别是对梯曼-佩霍拉省、乌拉尔-伏尔加地区、白俄罗斯、哈萨克斯坦的古生代碳酸盐岩地层、雅库特的古里芬-寒武纪地层和东北高加索晚白垩世相对年轻的地层进行了研究。碳酸盐岩是广泛分布的沉积岩。其中很大一部分是在广阔的浅水海相陆表盆地条件下形成的。大量的著作致力于研究这种矿床。然而,与碳酸盐沉积物形成条件及其沉积后变化有关的问题,以及岩石本身的分类问题,都不能被认为得到解决。分析的场是Osvanyurskoye场。它于2007年被发现。该油田位于俄罗斯联邦欧洲部分的东北部,距离科米共和国的乌辛斯克2公里。该油田是Timano-Pechora油气省的一部分,是一个成熟的油田(图1)。目标是Serpukhov地平线上2.5米厚的层。
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