slip region 中文意思是什麼

slip region 解釋
滑移區
  • slip : SLIP =Serial Line Internet [Interface]Protocol 【計算機】串線網際協議。vi (slipped 〈古語〉 sli...
  • region : n. 1. 地方,地域,地帶;地區;行政區,管轄區,區;左近,鄰近;(大氣、海水等的)層,界,境。2. 【解剖學;動物學】(身體的)局部,部位。3. (學問等的)范圍,領域。4. 〈罕用語〉天空。
  1. It is shown in the simulation that sliding mode control can guarantee the stability and robustness while vehicle is braking even if abs operates at the instability region of the adhesion coefficient and wheel slip curve or the surface condition changes, which is better than the pid control and nonlinear pid control

    模擬結果顯示,即使在附著系數和滑移率關系曲線的不穩定區域,或是路面狀況發生變化,滑模控制也能保證制動的穩定性和魯棒性,其控制效果優于pid和非線性pid控制效果。
  2. The result show, most of the medium - strong earthquakes faults are dip - slip reversed, distribution of the main stress p axis is sector from west to east ; there are large difference between kuche and baicheng region in seismic activities, but the characteristic of cluster is same in the two region ; the distribution of medium - strong earthquakes is nw direction in baicheng region, it show, there can have a concealed fault ; small earthquake clusters ' activities can reflect the effect that local medium - strong earthquakes to the secondary small structure around it

    結果表明:南天山東段中強震震源斷錯以傾滑逆斷為主,主壓應力p軸由西到東呈扇形分佈;相距較近的庫車與拜城地區地震活動存在較大差異,但均存在明顯的成叢性分佈特點;拜城地區中強地震分佈呈北西向可能預示著該區存在隱伏斷裂,小震群活動則可能反映了局部中強震對周圍次級小構造的影響。
  3. The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults

    大慶地區內發育在晚侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂,依斷層形成時期、活動特徵及切割層位可將蓋層斷層細分為四種類型,即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層;按其活動歷史可以分為五種類型:即長期活動斷層、早期活動斷層、早-中期活動斷層、中期活動斷層和晚期活動斷層。
  4. However, if we were to maintain hong kong s position as a trading, financial, and technology centre as well as a major tourist destination in this region, our community must not allow the importance of english to slip from our daily lives

    不過,如果要維持香港作為亞太區貿易金融及科技中心和主要旅遊勝地的地位,我們便不能讓英語在日常生活中的地位下降。
  5. When impact applies on a discrete system in which one of constraints is a constant with coulomb friction, the phenomenon of slip - stick at the point can cause the change of friction and the integration for frictional force during infinitesimal impulsive interval becomes impossible according to traditional impulsive dynamics of discrete systems. by introducing a new dimensional time parameter, first - order momentum - impulse differential equations are obtained and the discussion over infinitesimal impulsive interval is transformed into a piece - wise study on the finite region of impulse

    在引入新的無量綱的時間參數后,通過建立相應的動量-沖量的一階微分方程,在趨近於零的沖擊區間的討論變為在有限區間中來分段研究含滑動-黏滯的沖擊過程,得到了受到多點打擊的離散系統考慮庫侖摩擦時的動力學的求解方法,即根據沖擊前的初始狀態無需回到繁瑣的微分方程的求解便可以得到沖擊后系統的動力學響應。
  6. The results show that the squeeze viscous force decreases with the slip parameter increases, rigid region of the fluid increases with the slip parameter increases. when the slip parameter tends to infinite, the results of the squeeze viscous force reduce to the case of the squeeze flow of rigid - plastic solid between two parallel disks

    結果表明,圓盤上的擠壓力隨著滑移參數的增加而減小,當流體全部處于流動狀態時,即為圓盤擠壓牛頓流體時的情況;當流體全部處于剛性狀態時,即為圓盤擠壓理想剛塑性介質時的情況。
  7. These phenomena show that the fault has strongly activities at the same time. at that time tan - lu fault zone occurred a large - scale left - lateral displacement. the strike - slip movement on the tan - lu fault zone cau sed the zhangbaling uplifting which became source region and the hefei basin appeared strike - slip flexure at the west side of the fault

    說明了控盆斷裂?郯廬斷裂帶在該時期具有強烈活動,且以大規模走滑運動為主,郯廬斷裂帶的走滑使得東側張八嶺進一步快速隆升,仍構成沉積物源系統;在斷裂西側,合肥盆地因走滑而撓曲,形成沉積可容空間。
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