sedimentous中文是什么意思

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中文翻譯
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[網(wǎng)絡(luò)] 沉積的

sediments,geologic 《英文msh詞典》Sediments,Geologic ; [同義詞] Sediments,Geologic ; [主題詞] Geologic Sediments ; [中文釋義] 沉積,地質(zhì) ; [英文釋義] A mass of organic or inorganic solid fragmented material,or the solid fragment itself,that comes from the weathering of rock and is carried by,suspended in,or dropped by air,water,or ice. It refers also to a mass that is accumulated by any other natural agent and that forms in layers on the earth's surface,such as sand,gravel,silt,mud,fill,or loess. (McGraw-Hill Dictionary of Scientific and Technical Terms,4th ed,p1689)
sedimentormeter 紅血球沉降速度測定器
sediments,marine 《英文msh詞典》Sediments,Marine ; [同義詞] Sediments,Marine ; [主題詞] Geologic Sediments ; [中文釋義] 沉積,海洋 ; [英文釋義] A mass of organic or inorganic solid fragmented material,or the solid fragment itself,that comes from the weathering of rock and is carried by,suspended in,or dropped by air,water,or ice. It refers also to a mass that is accumulated by any other natural agent and that forms in layers on the earth's surface,such as sand,gravel,silt,mud,fill,or loess. (McGraw-Hill Dictionary of Scientific and Technical Terms,4th ed,p1689)
sedimentometric analysis 沈降體積分析
sedimenttrap 沉降池;除垢閥
sedimentologists (sedimentologist 的復(fù)數(shù)) n. 沉淀學(xué)者, 沉積學(xué)家
sedimentum [醫(yī)] 沉淀, 沉積物
sedimentologies [網(wǎng)絡(luò)] 沉積物
sedimentum lateritium [醫(yī)] 紅磚灰狀沉淀，磚末狀沉淀
sedimentologically adv. sedimentological的變形

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例句與用法

By using of the data of sedimentous microfacies, logging and cores, the text studies in-layer heterogeneity, between-layer heterogeneity and plane heterogeneity of the sand layers in the south part of n2 " reservoir in gasikule oil field of qinghai province
本文綜合運(yùn)用沉積微相、測井以及巖心分析等資料，對青海尕斯庫勒油田n21油藏南區(qū)儲層層內(nèi)非均質(zhì)性、層間非均質(zhì)性以及平面非均質(zhì)特征進(jìn)行研究。
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(nèi)非均質(zhì)性研究，通過計(jì)算不同沉積微相砂體滲透率的變異系數(shù)、突進(jìn)系數(shù)以及級差來說明主要儲集微相的非均質(zhì)特征；據(jù)巖性及電性特征，將層內(nèi)夾層分為兩類，統(tǒng)計(jì)單砂層段內(nèi)夾層的個(gè)數(shù)、累積夾層厚度、夾層頻率及夾層密度，并且根據(jù)夾層頻率及密度平面分布圖統(tǒng)計(jì)出每層的頻率相對高值區(qū)和低值區(qū)，總結(jié)夾層分布特征；根據(jù)物性參數(shù)隨深度的變化趨勢建立了五種儲層層內(nèi)物性非均質(zhì)模式，指出研究區(qū)內(nèi)以a型和c型模式為主。
The studies of plane heterogeneity are as follows : the text counts the parameters of the sandlayers " geometric shape of different sedimentous microfacies; speculates the conditions of lateral communication by sandstone density according to the method brought forward by j . r . l . allen; gets a group of parameters including the reservoir thickness, porosity and coefficient of permeability by using kriging method according to the data of logging results; makes certain the direction of coefficient of permeability with variation function by modeling globosity function; divides the sandlayers into five types by using the method of flowing cell based on three parameters, that is x h, kxh and h / h, and accounts the favorable region . on the base of above-mentioned studies, the text evaluates the heterogeneity of sandlayers and gives the resolutions to these problems to serve the development of the field
allen)等人提出的統(tǒng)計(jì)方法，用垂向上砂體密度的界限來推測砂體側(cè)向連通情況；根據(jù)每口井的測井解釋資料，利用克里金插值法對外間進(jìn)行插值，得到了一組反映儲層特征在平面上變化的參數(shù)，包括儲層厚度分布、孔隙度以及滲透率，并且成圖；利用變差函數(shù)法，通過球狀函數(shù)模擬，確定儲層優(yōu)勢滲透率方向：根據(jù)流動單元法，以儲能系數(shù)、容積系數(shù)以及凈毛厚度比三個(gè)參數(shù)為依據(jù)，通過聚類分析方法進(jìn)行流動單元劃分，并且按照參數(shù)特征將其分為五類，統(tǒng)計(jì)各砂層有利流動單元區(qū)塊。

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