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surface velocity造句

"surface velocity"是什么意思   

例句與造句

  1. The maximum surface velocity near the center is somewhere between one and two feet per day .
    靠近中心的最大表面流速為每天大約12英尺。
  2. Distribution and calculation of surface velocity field in ship wakes of sar image
    合成孔徑雷達圖像中艦船航跡表面速度場的分布與計算
  3. Rebuilding near - surface velocity field is very important for calculating statics
    摘要近地表速度場的重建是獲得準確靜校正量的關鍵。
  4. The maximum surface velocity near the center is somewhere between one and two feet per day
    靠近中心的最大表面流速為每天大約1 2英尺。
  5. Based on the acoustic radiation mode analysis , the transfer matrix relating the pressure at every field point to normal component of surface velocity is formed
    摘要基于聲輻射模態(tài)分析,建立了外部場壓和結構表面振動速度之間關系的傳遞矩陣。
  6. It's difficult to find surface velocity in a sentence. 用surface velocity造句挺難的
  7. The paper proposed the methods of multi - azimuth inverse vsp tomography to calculate near - surface velocity aimed replacing micro - log method at complex surface places
    本文首先就復雜地表常規(guī)微測井技術求取表層速度存在的問題,提出了多方位角逆vsp層析成像方法。
  8. Real - time surface velocity field measurement system and three - dimensional particle velocity measurement system are developed . systematic experimental research on the movement of coarse sediment particles in open - channel flows was carried out using developed system
    本文研制開發(fā)了表面流場實時測量系統(tǒng)和顆粒三維運動測量系統(tǒng),并采用顆粒三維運動測量系統(tǒng)對明槽水流中粗顆粒的運動進行了系統(tǒng)的試驗研究。
  9. The inversion results of the theory model and actual data show that the method can reconstruct near - surface velocity field of complex structure stably , quickly and accurately , thus , can calculate the statics and ensure structural imaging in complex area
    理論模型和實際資料的反演結果表明,該方法能穩(wěn)定、快速、準確地重建復雜地區(qū)的近地表速度場,建立準確的近地表速度場,從而可計算準確的靜校正量,保證復雜地區(qū)的構造成像。
  10. Then , the development of the tomography is reviewed in brief , while the status in quo of this technique is investigated . and analyzing two key facts in using the method , first , yield data gather ; second , solve near - surface velocity after tomographic inversion
    然后回顧了層析成像方法的發(fā)展歷程,并調(diào)查了層析成像方法的研究現(xiàn)狀,分析實際應用中存在的兩個關鍵問題,一、野外數(shù)據(jù)采集;二、用層析成像方法反演求解表層速度,從而確立了本文的研究方向。
  11. As we know , inverse techniques make blade ' s profile well compatible with its surface velocity distribution , however , they give designers big challenges that the ideal velocity distribution is hard to obtained and sometimes the non - physical solution , such as double covering of flow field or unclosed profiles , would come out . the proposed design procedure in the paper has avoided the disadvantage mentioned above . in this paper , a quasi - irrotational equation is used to describe the flow in cascade instead of the generally used irrotational equation
    眾所周知,一般的反問題和混合問題的最大特點,是在給定的壓力面和吸力面上的壓力分布或速度分布條件下,直接得到葉片的幾何形狀,它可以使葉型型面與表面氣流參數(shù)有機結起來;其不足之處在于,對設計者而言,很難給定理想的葉片表面壓力分布或速度分布,并且有時會得到一個非物理解,如:得出的初始葉型可能會出現(xiàn)前緣、尾緣不封閉的現(xiàn)象。
  12. This thesis mainly studies the method of how to realize the scientific information visualization in the field of geophysics and its application , and develops a software system which displays related data information by 3 _ d pictures , combining the research project on 3 _ d surface velocity model tomography inversion
    本論文針對物探應用的實際需要,結合三維表層速度模型層析反演的研究課題,對地震數(shù)據(jù)可視化顯示方法進行研究,開發(fā)了三維表層速度模型可視化顯示軟件,對三維反演的有關數(shù)據(jù)進行可視化顯示。
  13. The authors established an initial velocity model based on the first break time of the actual data , then realized the forward calculation with the improved shortest path ray tracing algorithm , and applied the improved constrained damped simultaneous iterative reconstruction technique ( cdsirt ) to solve large - scale and sparse equations for inversing the near - surface velocity field
    根據(jù)實際地震數(shù)據(jù)的初至波時間建立初始速度模型;采用改進的最短路徑射線追蹤算法進行正演;利用改進的約束帶阻尼聯(lián)合迭代重建技術( cdsirt )求解大型、稀疏的方程組來反演近地表的速度場。
  14. We can analyze and observe directly the reasonability of processed data , that is helpful to improve the quality of tomography inversion and the reliability of velocity model tomography inversion , then provide reasonable surface velocity model for tomography static correction by some means , such as rotating , scale graphics , meanwhile combining with relating sectional drawing and clipping drawing
    通過對三維立體進行全方位旋轉(zhuǎn)、縮放顯示,并結合與三維體一致的剖面和平截面的綜合考察,便于直觀地分析、監(jiān)控地震數(shù)據(jù)處理結果的合理性,有助于提高模型層析反演的質(zhì)量和表層速度模型層析反演的可靠性,并可為層析靜校正提供合理的表層速度模型。
  15. On the other hand , it is indicated that the velocity field consists of a depth - independent inertial oscillation and a time - mean shear flow , which can be obtained by subtracting the inertial oscillations time mean in one inertial period . the hodograph of the velocity vector of time - mean flow at the different depths consists of a ekman spiral , and the surface velocity is 30 . 3 ? to the right of the wind
    一維模式的流場結果表明,混合層中的流場是由慣性波動與時間平均流兩部分疊加而成,且通過時間平均消去慣性波動后得到平均流,其不同深度的流速矢量構成一ekman螺旋,表層流速矢量相對風向右偏了30 . 3 ’ 。

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