儲油層大小 的英文怎麼說

中文拼音 [chǔyóucéngxiǎo]
儲油層大小 英文
bulk of reservoir rock
  • : Ⅰ動詞(儲藏; 存放) store up; save; keep [have] in reserve Ⅱ名詞1. (繼承人) heir 2. (姓氏) a surname
  • : Ⅰ名詞1 (脂肪; 油脂) oil; fat; grease 2 (姓氏) a surname Ⅱ動詞1 (用桐油、油漆等塗抹) apply t...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • : Ⅰ形容詞1 (體積、面積、數量、強度等不大) small; little; petty; minor 2 (年紀小的; 年幼的) youn...
  • 儲油 : oil storage
  1. The favorable reservoir spaces in the carbonate rock could be divided into five types according to their origin, configuration and size, i. e., solution fissure, solution hole, cave, erosional fissure and structural fissure, which form five different reservoirs including cave - type reservoir, erosional fracture reservoir, structural fissure reservoir, and solution pore marginal beach grainstone reservoir

    而下奧陶統灰巖段集和生產氣的有效滲空間按成因、形態及可劃分為溶蝕孔隙、溶蝕孔洞、型洞穴、風化裂隙、構造裂隙等5類,構成5種性質有別的,即洞穴型、風化裂隙型、構造裂隙型、臺緣灘相顆粒灰巖溶蝕孔隙型和地表殘積物裂隙孔隙(洞)型
  2. In order to improve oil displacement efficiency of infusing agents and precisely to predict the three dimensional distribution about residual oil, taking the sand body of p 2 individual meandering river - channel in putaohuareservior of daqing oilfield as an example, by analyzing the thin interbeds and vertical permeability discrepancy, this paper brings forward the space configuration of the thin interbeds in single sand body, the vertical permeability distribution and gravitational differentiation which control the distribution of residual oil and the vertical multisection model of displacement efficiency in the condition of excluding exploitation factors and identical single sand - body,

    摘要為了進一步提高注入劑驅效率以及準確預測中剩餘在三維空間的分佈,以田葡萄花組p 2曲流河道砂體為例,通過對曲流河道砂體內部薄夾構形及滲透率垂向分佈的差異性分析,在排除開發因素差異的同井單砂體分析條件下,提出了單砂體內部薄夾空間構形、滲透率垂向序列與重力因素共同控制剩餘分佈、驅效率多段垂向序列模式。
  3. 3 ) the sandbody distribution, physical properties, pore structure and heterogeneities are affected by the microfacies. at the center part of underwater distributive river course, the petrophysics and physical properties are both better than that at the edge of the microface. 4 ) the chang 61 2 - 3 substrata and the substrata of chang 62 " member which show the better porosity, permeability, and better pore structure ; display lower permeability variation coefficient, dart - coefficient and contrast - coefficient and good connecting sandbody so the horizontal heterogeneities is weaker ; whereas manifest stronger inner - heterogeneities due to the numerous intermediates ; present stronger inter - heterogeneities caused by the greater frequency of sandbody

    長6中長6 _ 2 ~ ( 1 - 3 )和長6 _ 2 ~ 1砂中的各個的孔隙度、滲透率值、含性較好;平面非均質性較弱,表現為級差、突進系數、變異系數較低且砂體的連片程度高,鉆遇率和連通系數較高;與此同時,內非均質性較強,表現為垂向上夾的數目較多,厚度較間非均質性也較強表現為分系數較高。
  4. This increases the accuracy for interpretation greatly. due to 5 / 6 wells are slant holes in developing cluster wellgroup, environmental corrections are made to acoustic logging data of deflecting wells. through synthesis seismic records, quasi - velocity is calculated and seismic calibration of deflecting data is carried out

    對埕島田館上段微觀非均質從主要孔隙類型、孔喉分佈、孔隙與滲透率分佈、孔隙半徑的、孔喉比、孔喉配位數和面孔率等方面進行了定量評價。
  5. By the analysis of mercury injection data and physical property data of 650 sandstone and carbonate samples collected from tuha, liaohe, shengli, eerduosi, sichuan oil gas field of china and canadian oilfield, it is found that for porosity rocks, no matter they are sandstone or carbonate, their porosity and permeability ( especially for permeability ) are closely related to pore volume distribution with different throat size

    本文通過對來自我國吐哈、遼河、勝利、鄂爾多斯、四川和加拿等地區氣田的650個砂巖和碳酸鹽巖樣品壓汞測試資料及物性數據的分析研究,成功發現了對于孔隙性巖石(無論是砂巖還是碳酸鹽巖) ,巖石孔隙度和滲透率(特別是滲透率)與巖樣不同孔喉的體積分佈有密切的相關性,並首次建立了孔喉體積分佈反演預測模型。
  6. Pi formation is combination of thick sand body, because the sediment mode of reservoir in changyuan of daqing is mainly combined of great leaf delta and partly fluvial facies, about 500m thick, combined of 130 little sand or mud layers, which is typical heterogeneity reservoir, the reservoir ' s character is greatly distribute, high permeate and serious heterogeneity

    Pi組是厚組合,由於慶長垣的沉積模式以型葉狀三角洲及部分河流相為主,總厚度500多米,由130多個和泥巖交互而成,是一套典型的非均質砂巖,該具有分佈廣、厚度、滲透率高和內非均質性嚴重等特點。
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