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英語人>網(wǎng)絡(luò)例句>heterogeneity 相關(guān)的網(wǎng)絡(luò)例句
heterogeneity相關(guān)的網(wǎng)絡(luò)例句

查詢詞典 heterogeneity

與 heterogeneity 相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò),僅供參考]

The results from principle components analysis showed that density of grasses, heterogeneity of ground environments and cover of grasses were the main factors for rock partridge and heterogeneity of ground environments, cover of grasses for Alecto...

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The heterogeneity idiosyncracy of education level has inapparently passVe influence,and the heterogeneity idiosyncracy of age has same result.

4首次構(gòu)建了獨(dú)立董事的異質(zhì)性模型男人的天堂精品视频网站,包括學(xué)歷的異質(zhì)性、職業(yè)背景的異質(zhì)性久草欧美性爱、年齡的異質(zhì)性及任期的異質(zhì)性91中文字幕永久在线看。

The paper has first analyzed the heterogeneity asynchronous machine mathematical model harmonious wave analysis, and has carried on the analysis to the heterogeneity asynchronous machine invertor power supply situation's space and time overtone, has established under six asynchronous machine static coordinate system's simulation model and has given the concrete step which Matlab/Simulink realizes, has conducted the analytical study to six asynchronous machine's characteristic.

論文首先分析了多相感應(yīng)電機(jī)數(shù)學(xué)模型和諧波分析乱伦视频无码一级,并對多相感應(yīng)電機(jī)逆變器供電情況下的時(shí)空諧波進(jìn)行了分析,建立了六相感應(yīng)電機(jī)靜止坐標(biāo)系下的仿真模型并給出了Matlab/Simulink實(shí)現(xiàn)的具體步驟av福利资源福利,對六相感應(yīng)電機(jī)的特性進(jìn)行了分析研究啪无码高请不卡在线观看。

Based on grid pattern sampling, by the analysis of lacunarity indices in Huairou and Mentougou District, it is found that: In different scales, the higher lacunarity indices are, the greater heterogeneity of spatial distribution for forest landscape elements is. This performance can be considered as macroheterogeneity characteristics. Oppositely, the lower lacunarity indices values are, the smaller heterogeneity of spatial distribution for forest landscape elements are.

4通過對懷柔和門頭溝試驗(yàn)區(qū)進(jìn)行網(wǎng)格局抽樣及孔隙度指數(shù)分析發(fā)現(xiàn):在不同尺度下,孔隙度指數(shù)值越高全国精品第一区黄片,森林景觀組分空間分布的不均勻程度越高蛋蛋福利导航,表現(xiàn)為宏觀異質(zhì)性特征;孔隙度指數(shù)值越低黄黄黄黄aaaa片,其景觀組分在其研究范圍內(nèi)空間分布均勻日韩欧美女自拍图片视频网站在线观看,表現(xiàn)為微觀異質(zhì)性特征。

In this method, we make use of xml mapping to eliminate name heterogeneity,utilize transformation expression to eliminate unit heterogeneity, make use of transformation function and mapping tables to eliminate precision heterogeneity, data type heterogeneity and the heterogeneity of data expression method.

在該方法中国产成人麻豆tv在线看,利用xml映射來消除命名異構(gòu)国产第一视频毛片;利用轉(zhuǎn)換表達(dá)式來消除單位異構(gòu);利用轉(zhuǎn)換函數(shù)日韩超刺激黄片,映射表來消除精度的異構(gòu)欧美视频二区网站,數(shù)據(jù)類型異構(gòu)以及數(shù)據(jù)表示方法的異構(gòu)。

Inner layer heterogeneity, plane heterogeneity and microfacies heterogeneity are studied by using heterogeneity parameters: permeability variance coefficient, permeability tantivy coefficient and permeability differential.

應(yīng)用滲透率的變異系數(shù)欧美喷水大屁股、突進(jìn)系數(shù)和級差來分析儲層層內(nèi)18禁止黄片、平面非均質(zhì)性與各微相的非均質(zhì)性。

In this paper, the characteristics of reservoir of reservoir of delta frontal sub-faces of PI Formation in the south of Xingshugang are studied with the data of dense well pattern and rock-mineral identification. The delta frontal sub-faces can be divided into lobate delta frontal sub-faces, branched delta frontal sub- faces and sheeted delta frontal sub-faces. The genetic types of sand bodies in different sedimentary envivonments are analyzed in detail, and the distribution and space-matching relationship of different sand bodies are studied. The micro-pore structure type is studied on the base of the thin section analysis, so the reservoir heterogeneity is studied including plane heterogeneity, interlayer heterogeneity, in-layer heterogeneity and microcosmic characteristic.

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Base on core observation and grain size analysis, and under associated consideration of logging trace characteristics, Chang8 reservoir in study area is classified into three sedimentatal microfacies, subsea river, mouth bar and river flank.3.The mian diagenesis in study area are: mechanical compaction, cementation, metasomasis and denudation in late diagenetic phase.4. In allocation of reservoir macroscopic heterogeneity, more heterogeneticer reservoir, class 1 and class 2, mainly locate in the center of subsea river or crook and divaricate of the river; class 3 and class 4 mainly locate in river flank, and the physical property of these locality are better.5. Diagenesis of reservoir have influence on the pore structure which influences the reservoir microscopic heterogeneity. The better the pore structure is, the slighter the reservoir microscopic heterogeneity is; on the contrary, the reservoir microscopic heterogeneity is serious.

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The reservoir rock types in the region of interest are grain limestone, algal limestone, cryptite, siltstone, muddy limestone and mudstone. The thesis identified as a result of changes in the deposition causing the heterogeneity in plane, and then the geological oil reserves have been calculated in accordance with the areal heterogeneity.3、Based on the data of core analysis, bore logging, array induction imaging log and FMI, porosity and permeability model were built using regression analysis. Through testing 45 rock samples, a, b, m, n value were obtained and used to calculate single-layer oil saturation value using the Archie formula. According to the theory of laterolog and inductolog, resistivity ratio and cross plot were used to identification effective thickness. Effective thickness was identified delicately in 103 wells. Based on the over work, active porosity and oil saturation was calculated accurately.4性生活片一线天、According to observation of 100 pieces of the thin slices, cast thin slices and 383m core in three wells, the chief diagenesis in this area were compaction, cementation, denudation and cataclasis. Cementation and denudation were universally influenced active porosity this area. The intergranular pores, residual pores and secondary pores were formed in thin carbonated reservoir of lacustrine facies.5亚洲黄色在线视频观看网站、The influence of reservoir heterogeneity to reservoir calculation was analyzed systematically using actual data. And the conclusions were as follows:①The principal reason leading to oil distribution unequal is interior structural feature of reservoir in structural hydrocarbon reservoir.

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Using maximum flooding surface and local explosure erosion surface as the correlation framework surface in the 4-th hierarchical base-level cycles, sand-body in the 3-th hierarchical base-level cycles formed in the 4-th hierarchical base-level cycles may be correlated layer by layer. The law of the sand-body and the characters of reservoir heterogeneity formed in the 4-th hierarchical base-level cycles are discussed. The study shows:①During early period of the 4-th hierarchical base-level cycle rising, subaqueous distributary channel formed, continuously stacked vertically, and migrated in limit range laterally, and channel sand-body stretches farther longitudinally, and lacks interbeds of mud rock and siltsand in sand rock, reservoir heterogeneity is relatively weak.②During mid-period of the 4-th hierarchical base-level cycle rising, subsaqueous distributary channel migrated actively, channel divided and converged strongly to form netted sand-body and sand sheet mainly, but interbeds of mud rock and siltsand increases gradually in sand-body, reservoir heterogeneity increased.③During later period of the 4-th hierarchical base-level rising and early period of the 4-th hierarchical base-level falling, reservoir sand-body was poor, and only form thin sand-body of subsaqueous distributary channel, subsaqeuous creveas and distal mouth bar, sand-bodys are surrounded by mud and silt rock.

進(jìn)一步采用以第4層次基準(zhǔn)面旋回中相當(dāng)最大湖泛面的相轉(zhuǎn)換面和具有區(qū)域性暴露侵蝕作用的層序邊界面為等時(shí)地層對比框架的邊界日本爱爱高清视频,對發(fā)育于MSC2—MSC4三個(gè)第4層次基準(zhǔn)面旋回的第3層次基準(zhǔn)面旋回內(nèi)砂體進(jìn)行了逐層等時(shí)對比欧美黄色电影网址,探討第4層次等時(shí)地層對比格架內(nèi)儲集砂體發(fā)育分布規(guī)律,及儲集砂體的非均質(zhì)性特點(diǎn)蝌蚪久久,研究發(fā)現(xiàn):①第4層次基準(zhǔn)面上升初期發(fā)育的水下分流河道日韩精品理论片在线观看,砂體呈連續(xù)疊置、側(cè)向遷移受限超碰免费一欧美精品,縱向上呈長距離延伸的帶狀產(chǎn)出18水女人一级黄色,砂體間泥、粉砂巖夾層少自拍偷拍日韩欧美,儲層非均質(zhì)性相對較弱欧美精品-a;②在第4層次基準(zhǔn)面上升中期發(fā)育的水下分流河道側(cè)向遷移活躍,縱向延伸過程中分流匯合作用強(qiáng)烈,以形成網(wǎng)狀或席狀連片砂體為主黄色视频黄久久,但砂體間泥2020亚洲精品极品色在线、粉砂巖夾層逐漸增多人人射人人摸人人干,儲層非均質(zhì)性增強(qiáng)欧美黄片lv在线播放;③第4層次基準(zhǔn)面上升晚期和下降早期,不利于儲集砂體發(fā)育操淫荡美女视频,僅出現(xiàn)少量薄的水下分流河道美日韩在线A片视频、水下決口扇、遠(yuǎn)—河口砂壩砂體美女屄操出淫水视频在线观看。

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