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asymmetrical distribution中文是什么意思

  • 不對(duì)稱分布
  • 不對(duì)稱分配
  • 不平衡分布
  • 非對(duì)稱分布
  • 非對(duì)稱分配
  • 非對(duì)稱性分布
  • 漸近分布

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  • 例句與用法
  • Asymmetrical distribution of cortactin appeared when gastrulation starts , with higher staining in the dorsal part of the embryo , while much lower in the ventral part
    在胚盾附近區(qū)域,即未來的胚胎背側(cè),染色信號(hào)較強(qiáng),皮層蛋白標(biāo)志了正在發(fā)生匯聚遷移的細(xì)胞。
  • The strike - slip faulting was caused by asymmetrical distribution of barriers on the subducting plate . the nne - ssw distributed aftershocks occurred on , or near , the fault plane of the main shock ; while the nw - se distributed aftershocks , on , or near , the mentawai fault
    北北東?南南西向分布的余震發(fā)生在主震的斷層面上(或其附近) ;而西北?東南向分布的余震則發(fā)生在明打威斷層上(或其附近) 。
  • The theoretical analysis and simulation show that the ssnr and the sksnr are equal to or greater than the original signal - to - noise ratio ( snr ) , and that employing third order cumulant slices can effectively extract the mot - radiated quadratic phase dynamic coupling signals from asymmetrical distribution noise
    理論分析與仿真表明:切片信噪比、歪度信噪比總是大于相關(guān)信噪比;用該算法十分有效地實(shí)現(xiàn)了二次相位耦合信號(hào)與非對(duì)稱分布色噪聲的分離。
  • But in the reality credit trade activity , information is the asymmetrical distribution between credit contract parties - bank and loan enterprise . the non walrasian equilibrium is appeared in the credit contract market . the loan rate of interest can not make both sides that capital supply and demand realize the equilibrium under this kind of circumstances , and the credit market can not reach voluntarily cleaning , namely credit c
    但是在現(xiàn)實(shí)的信貸交易活動(dòng)中,交易信息在合約當(dāng)事人雙方之間的分布是非對(duì)稱的,在這種情況下,信貸市場(chǎng)呈現(xiàn)出一種非瓦爾拉斯均衡狀態(tài),貸款利率不能使得資金供求雙方實(shí)現(xiàn)均衡,市場(chǎng)不能夠自動(dòng)出清,即信貸市場(chǎng)處于一種數(shù)量配額的短邊均衡? ? “信貸配給”狀態(tài)。
  • The vibrations of ru - terminal ligands q - mode and intra - bridged ligand 6a mode as well as their combination in the mixed valence taube ion are studied by using density functional theory method under the borh - oppenheimer approximation . it is found that these three vibrations all are harmonic vibrations . and q - vibration causes the charges on ru1 and ru2 atoms to be asymmetrical distribution . the charge transfer between ru and terminal nh
    在borh - oppenheimer近似下,應(yīng)用量子化學(xué)的密度泛函理論方法研究了混合價(jià)taube離子中金屬與配體之間的振動(dòng)q -振動(dòng)模式橋配體內(nèi)的振動(dòng)6a振動(dòng)模式以及這兩種振動(dòng)的組合。發(fā)現(xiàn)這三種振動(dòng)模式都可以看成簡諧振動(dòng)。
  • Through studing the plane and vertical hydromechanical characteristics in the radial sandbanks area , the mechanisms of the formation , maintenance and asymmetrical distribution of the radial sandbanks are understood . it ' s well known that the directional to - and - fro movement and strong tidal current are the necessary dynamic conditions for the formation of tidal current sandbanks
    通過對(duì)輻射沙脊群海域平面及立面動(dòng)力特征的研究,基本探明了南黃海輻射沙脊群形成發(fā)育和維持的水動(dòng)力機(jī)制,以及其不對(duì)稱分布格局與動(dòng)力因素的內(nèi)在聯(lián)系。
  • It has been proven that the differences of magnitude and distribution of tidal currents , wave energy rate , suspended sediment concentration and the stokes number result in a asymmetrical distribution of sandbanks between the north and south . the sandbank surface area and length in the north are lager than those in the south , but its cross section area is less than that in the north
    各種動(dòng)力特征平面分布規(guī)律研究表明,輻射沙脊群南北沙脊不對(duì)稱分布的格局是潮流沙脊對(duì)潮流往復(fù)流性質(zhì)的強(qiáng)弱分布、潮波能流率大小分布、含沙量的平面分布規(guī)律及斯托克斯數(shù)的大小分布的動(dòng)力響應(yīng)。
  • Using the hulscher model of the formation of sand waves and sandbanks , under the ancient bathymetry , or under the modern bathymetry , the stokes number of the tidal flow and resistance parameter in the radial sandbanks satisfy the conditions for the formation of sandbanks . the research demonstrates that the dynamic flow conditions result in the development of tidal current sandbank . the radial sandbanks and it ' s asymmetrical distributions will still maintain in the future
    應(yīng)用hulscher沙波及沙脊增長模式,通過對(duì)該海域斯托克斯數(shù)及底部阻力參數(shù)的計(jì)算首次發(fā)現(xiàn),南黃海輻射沙脊群海域在概化古地形和現(xiàn)代輻射狀沙脊群水下地形情況下,其斯托克斯數(shù)及底部阻力參數(shù)均滿足形成潮流沙脊的條件。
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