巖層滲透性 的英文怎麼說
中文拼音 [yáncéngshèntòuxìng]
巖層滲透性
英文
formation permeability- 巖 : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
- 層 : 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...
- 滲 : 動詞(液體慢慢地透過或漏出) ooze; seep
- 透 : Ⅰ動詞1 (滲透; 穿透) penetrate; pass [seep] through 2 (暗地裡告訴) tell secretly; let out; lea...
- 性 : Ⅰ名詞1 (性格) nature; character; disposition 2 (性能; 性質) property; quality 3 (性別) sex ...
- 滲透性 : permeability滲透性防腐劑 osmose preservative
- 滲透 : 1 [物理學] [生理學] osmosis2 (液體從細小空隙中透過) permeate; seep; permeation; seepage; inflow...
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Oil is usually found in porous rock under a layer of impermeable rock which prevents it from escaping.
石油通常存在於多孔性的巖石中,上面覆蓋著不可滲透的巖層,使石油不致散失。The principal direction of small-scale movement is from a shale or clay to a sandstone or other permeable bed.
小范圍運動主要從頁巖或粘土巖向砂巖或其他滲透性地層中運動。The paper divided turbidite fan in deep water from long source into braided channel microfacies, inter - braided channel microfacies, medium fan over - belt microfacies, and external fan subfacies, and divided slump turbidite which related with delta into medium fan subfacies and external fan subfacies, and summed up 15 kinds of marking of subfacies and microfacies classification. at the same time, it formed a series of effective technology of analyzing turbidite source at the base of studying region geological which combined with analyzing the content change of terrigenous debris, with the found of logging facies, and with the ancient terrestrial magnetism test and other technology means under the guidance of three - dimensional model of turbidite which has been founded already and the flat surface feature of microfacies
將遠源深水濁積扇劃分為辮狀水道微相、辮狀水道間微相、中扇過渡帶微相和外扇亞相;將與三角洲有關的滑塌濁積扇劃分為中扇和外扇兩個亞相,並總結了濁積巖沉積劃分各種亞相、微相類型的十四種標志,分別為:巖石類型、層理類型、砂巖單層厚度、粒度結構特徵(粒度中值、分選性、概率曲線) 、生物化石、儲層物性(孔隙度、滲透率) 、泥巖隔層特徵(泥巖單層厚度、層數、顏色) 、鮑瑪層序組合和自然電位曲線特徵。Experimental research on permeability of rocks of coal - bearing strata
煤系地層巖石滲透特性試驗研究Based on cores analyses of coring well, studied are the " four properties " ( i. e., lithology, physical property, conductivity and oil bearing ) relationships between conglomerate and glutenite formation ; set up are the logging interpretation models of porosity, permeability and oil saturation in conglomerate and glutenite reservoirs with different lithologies
以取心井巖心分析為基礎,分別研究礫巖、砂礫巖儲層巖石的巖性、物性、電性及含油性兩兩之間的關系,建立了分巖性的礫巖和砂礫巖孔隙度、滲透率、含油飽和度測井解釋模型。Divisional method and characteristic analysis of impermeable barrier layers in carbonate rock formation
碳酸鹽巖儲層中非滲透性隔層的識別及分類評價The studies of in - layer heterogeneity are as follows : the text depicts the characteristics of heterogeneity by calculating the coefficient of variability, kmax / k and k. max / k. min of sand layers of different sedimentous microfacies ; divides interlayer into two types, and counts their numbers, thickness, frequency and density of a single sand layer according to the characteristics of lithology and logging, finally summarizes the characteristics of interlayer distributing ; sets up five in - layer heterogeneity models and points out that the primary models are model a and c. the studies of between - layer heterogeneity are as follows : the text depicts sand layers " growth and distributing conditions by calculating the lamination factor, sandstone density and overlap coefficient ; makes certain the lithology and thickness of interlayer by the method of contrasting the typical curves
層內非均質性研究,通過計算不同沉積微相砂體滲透率的變異系數、突進系數以及級差來說明主要儲集微相的非均質特徵;據巖性及電性特徵,將層內夾層分為兩類,統計單砂層段內夾層的個數、累積夾層厚度、夾層頻率及夾層密度,並且根據夾層頻率及密度平面分布圖統計出每層的頻率相對高值區和低值區,總結夾層分佈特徵;根據物性參數隨深度的變化趨勢建立了五種儲層層內物性非均質模式,指出研究區內以a型和c型模式為主。Main content in simulation is the spatio - temporal evolution of the set of descriptive variables characterizing tectonic mineralization state under coupling of various processes as following : ( 1 ) variables related to forming and property of ore - forming fluid, such as dissolution rate of minerals ( include metal minerals ) in rock, concentration and saturation of aqueous species in fluid, temperature, pressure, and ionic strength etc. ; ( 2 ) variables related to structural deformation and fluid flow, such as stress, deformation rate, fracture network, porosity, fracture permeability ; ( 3 ) variables related to precipitation and mineralization, such as nucleation rate of gangue and metal minerals, accumulation precipitation of various minerals, etc. ; ( 4 ) spatio - temporal coupling relation of various variables above, such as the coupling relationship between spatio - temporal evolution of fracture permeability and flow and focus of fluid and ore - forming
模擬的主要內容是在各種過程耦合作用下,以下描述構造成礦體系的主要變量的時空演化:與成礦流體的形成和性質有關的變量,如地層中礦物(包括成礦物質)的溶解速率、流體中各組分的濃度與飽和度、流體溫度、壓力、離子強度等;與構造變形和流體運移有關的各變量,如應力與變形速率、巖石孔隙度、構造(斷裂)滲透率等;與沉澱成礦有關的變量,如礦物(金屬礦物和脈石礦物)的成核速率、各礦物的沉澱量等;上述各有關變量間的時空耦合關系,如斷裂滲透率時空演化與流體流動、匯聚和成礦的耦合關系等。Test study indicates that, stress sensitivity of low permeability gas reservoirs exists objectively not only for dry rocks, but also rocks with irreducible water, and harm of stress sensitivity to permeability cannot he ignored
實驗研究表明,不管是乾燥巖石還是含束縛水巖石,低滲透砂巖氣藏儲層的應力敏感性是客觀存在的,而且這種應力敏感性對儲層滲透率造成的傷害不可忽視。A lot of results are made from calculating of case for geothermal reservoir property of earth energy within 200 2000 ( m. ) , it is helpful to analysis influence of permeability coefficient, kinematic viscosity and thermal diffusion coefficient of soils and rocks on heat transfer performance
在地表熱能熱儲物性為200 - 2000 ( m . )的范圍內進行的理論計算,得到了許多重要結果,為分析巖土層滲透系數、流體運動粘度和導溫系數等對傳熱量的影響打下了良好基礎。Despite the same tpyes of soils in this region ( the majority is dry red soil ), different types of soil parent materials / rocks imposed an important influence on soil infiltration due to soil degradation such as the removal of soil material and appearance of gravels / rock fragments. as a result, plant growth is closely related to the types of rocks
盡管該區不同的母質母巖發育形成相同的土壤一簡育干潤富鐵土(過去稱燥紅土) ,但母質母巖特性卻對植被生長有明顯的影響,其主要原因是土層淺薄化、石質粗骨化使土壤受巖性特徵深刻制約,導致不同土壤?母質?母巖系統表現出顯著的滲透性差異。The petroleum migration fractionation in the south part through unconformity and permeable carriers laterally is more obvious than that in the north part through the fault systems vertically
南部油氣通過不整合面和滲透性巖層輸導系統發生的側向運移明顯比北部通過斷裂輸導系統的垂向運移分餾效應要強。The results indicate that ( 1 ) faults are predominant pathways for oil and gas migration in the dina 2 struc - ture ; ( 2 ) the pressure released zones are available for oil and gas migration ; ( 3 ) capillary and buoyancy play an important role in sandstone with similar permeability ; ( 4 ) hydrocarbon migrates always along the predominant pathways, such as faults and associated sandstone in both sides ; ( 5 ) pathways of oil and gas migration have the nature of succession, such as oil driving water and following gas driving oil
通過模擬實驗,揭示: ( 1 )斷層是迪那2構造中油氣運移的主要通道; ( 2 )泄壓區是油氣運移的有利指向區; ( 3 )毛管力及浮力在滲透性相近的砂巖中起重要作用; ( 4 )油氣咩是選擇優勢通道運移,在沿斷層運移的同時,也向兩側砂體中擴散; ( 5 )油驅水之後的氣驅油運移通道具有繼承性的特點。Controlled by the fouth sequence boundary, with chronostratigraphic modeling research with gridstat pro software, some models such as depositional facies model, lithology distribution and reservoir quality model ( include porosity, permeability and productivity ratio ) have been built
應用四級層序界面進行控制,利用gridstatpro軟體開展了等時性相控建模研究,建立了沉積相模型、巖性分佈模型及儲層物性模型(包括孔隙度、滲透率及產能系數模型) 。The study of the relationship between permeability and apparent resistivity is empirically significant for determining the permeability parameter and understanding the effect of permeability and groundwater on permeable formations
研究巖石的滲透能力與視電阻率的關系,對確定巖石的滲透系數,了解巖石滲透能力、地下水對滲透性巖層的作用,都有一定的實際意義。In practice, core calibration logging technology is used to establish the logging interpretation model of low resistance reservoir, to quantitatively measure some geological parameters of the reservoir, such as porosity, saturation and permeability, and to combine the core physical experiment, geological composite logging, production test data with multiple well logging data, with the qualitative logging interpretation and the quantitative logging interpretation, so as to deepen the geological understanding on the low resistance reservoir and improve the logging interpretation accuracy
在實踐中,可用巖心刻度測井技術建立低阻儲層測井解釋模型,定量測定儲層孔隙度、飽和度、滲透率等地質參數,並把巖心物理實驗、地質綜合錄井、試油資料與多井測井資料結合起來,把定性測井解釋與定量測井解釋結合起來,以便加深對低阻儲層的地質認識,提高測井解釋精度。The study shows that rock stress sensitivity has the following characteristics : rock property has little sensitivity to stress, of which porosity has the least, permeability less, and compression coefficient most ; the rock property decreases with formation pressure decrease ; in the same formation pressure drop, decrease amplitude of the rock property is not a continuous function of permeability but related to distribution scope of permeability
研究得出,巖石的應力敏感性特徵主要有:巖石物性對應力的敏感性總體上不大,其中以孔隙度最小,滲透率次之,壓縮系數最大;巖石物性隨地層壓力的下降而下降;在同一地層壓降下,巖石物性下降幅度不是滲透率的連續函數,而是與滲透率分佈范圍有關,高滲透率范圍,巖石物性下降幅度小,低滲透率范圍,巖石物性下降幅度大。The results from the core displacement test show that the adaptability of reservoir with different permeabilities for the polymer - bearing sewage with different polymer concentrations is different
由巖心驅替實驗結果證明,聚合物濃度不同的污水對具不同滲透率油層的適應性是不同的。This paper states on the problems in water preventing and draining of highway tunnel of loess in gansu province and near area. firstly, it discusses the method to analyze and calculate the affect of groundwater characteristic, estiniate of tunnel water quantity and the varying of water contained in loess to the stability of surrounding rock mass according to the principle of groundwater leaking, hydraulic penetrating principle, groundwater dynamic law, groundwater flowing modulus low and so on
本文針對甘肅省內外部分黃土公路隧道防排水方面存在的問題,首先根據黃土層地下水運規律,按水力學滲流原理並應用地下水動力學法和地下水徑流模數法等方法,探討了黃土層地下水情特性、隧道滲透涌水量估算和水對圍巖穩定性影響的分析計算方法。On the basis of comprehensive analyses on hydrocarbon accumulation conditions in the four representative foreland basins, kuqa basin, southern junggar basin, western sichuan basin and northern margin of qaidam basin, some conclusions are made as follows ; the foreland basins in central and western regions of china are characterized by multi - set source rocks dominated by coal measure ; heterogeneous reservoirs ; multiple and sealing cap nick ; anticline traps ; unblocked transport system composed of fault, unconformity and highly permeable sand body ; anti poor conservative conditions. etc
在綜合分析和對比庫車、準南、柴北緣和川西等具有代表性的前陸盆地的油氣成藏條件的基礎上指出,中西部前陸盆地具有以煤系為主的多套源巖,發育非均質儲集層,多套多封閉性的蓋層,以背料為主要圈閉;斷裂、不整合和高滲透砂體組成良好輸導體系,保存條件較差等特點。分享友人