營力 的英文怎麼說

中文拼音 [yínglì]
營力 英文
agency
  • 營 : Ⅰ動詞1 （謀求） seek 2 （經營; 管理） operate; run; manage Ⅱ名詞1 （軍隊駐扎的地方） camp; barrac...
  • 力 : Ⅰ名1 （力量; 能力） power; strength; ability; capacity 2 [物理學] （改變物體運動狀態的作用） forc...
  1. In forced convection the movement of the fluid or gas is caused by an external agent which gives rise to pressure differences.

    在強制對流中，液體或氣體的運動是產生壓力差的某種外營力造成的。
  2. And the rock mass as the main object of most engineering practice is developed by all kinds of geotechnical action and force in the long geology history to the complex characteristic of continuous medium, crannied medium and granular medium, to the anisotropic and heterogeneous entity with elasticity, plasticity, viscidity, creepocity and rheology

    作為主要工程對象的巖體是在漫長的地質歷史發展過程中經受各種地質營力作用而形成的成因和構造復雜，巖性多樣且包含了連續介質，裂隙介質和散體介質特徵的，兼有彈性、塑性、粘性、流變性的各向異性的非均質地質體。
  3. Furthermore, the dq value ranges of profile multifarctal spectra in different landform types and in different directions of the same sections perform different properties and anisotrpies. it can be concluded that the landscape fractal properties depends closely on the int ensity, manner and inhomogenity of exogenic and inogenic processess, and with the properties, we can study quantatively the dynamic geomorphic process. by using the same methods just above, local fractal dimensions d, crossover length tc and the multifractal spectra dq - q of two large - scale landform profiles ( across and along tianshan mountain ranges respectively ) are calculated. the results show that in the studied scaling range the two profiles perform different scaling properties, and both of them can be divided to three evident different linear scaling subsections

    不同類型地貌區二維地貌表面也表現出多度域分形特徵，而且隨著觀測尺度的增加，每個區間的分維值均表現為依次減小，表明外營力作用的影響逐漸被內營力作用所取代：不同類型地貌區在相應區間的分維值表現為高山區中低山區盆地區，體現了不同類型地貌表面粗糙性或復雜性的差異，因此分維值大小可作為地貌表面外營力侵蝕作用強度的重要指標：利用標度區的間斷點和各種地貌類型表面分維值或宏觀效應趨於一致，提出5 - 6km左右可作為地貌的宏觀臨界點，並且與利用地貌剖線研究所得到的5km這一數值是基本吻合的。
  4. In addition, the dq - q curves behave in different shapes. it can be concluded that the scaling properties depend colsely on the way, intensity. acting scale and distribution in space of inogenic and exogenic processes. according to the scaling natures of the two landform profiles, it is proposed that the 5km scale is the low limit of the inogenic process effects which begin to dominate landscape patterns in landform systems

    該結果對理論地貌研究具有重要意義：不同地貌類型表面的多重分形譜值域表現為高山區中低山區盆地區的總體特徵，地貌表面多重分形譜特徵表明了內外營力地貌作用類型和強度在空間上分佈的不均勻程度。
  5. Dongying linuo glasswork co., ltd. it lies in shengli oil field with an area of173000 square metres

    東營力諾玻璃製品有限公司，位於渤海灣畔勝利油田腹地， ?地260畝。
  6. Most men live only for the gratification of it.

    許多人正是終生營營，力求填充自己的欲壑。
  7. The mechanical genesis of the complicated rock mass is because several times of tectonism in pro - period made the structure of rock mass in the right dam foundation damaged seriously and rock mass alteration made its mechanical character more anisotropy. after that the fractures in the right dam foundation slope were stretched at the beginning of the quaternary period because in the period yakouhoushan mountain quaquaversal dome was blowups quickly. at the same time, the valley trenching of lancang river reach to 800 - 1000 meter in altitude at the right bank in nuozadu dam site

    導致右岸巖體復雜化的成因是，右岸巖體在早期遭受了多期構造作用和巖體蝕變的基礎上，第四紀早期丫口後山穹隆的快速隆起與當時河谷下切至800m 1000m高程這一特殊因素組合引起了右岸巖體沿原有的斷裂（裂隙）張開，使地下水等風化營力能夠到達坡體較深部位，經過長期的風化卸荷作用，形成了右岸復雜巖體。
  8. The surface wind is the principal agent controlling nontidal currents' surface waves.

    表面風是控制非潮汐的海流表面浪的基本營力。
  9. Ii ) runoff erosivity reflects relationship of water erosion forces and sediment yield more directly than rainfall erosivity. it intergrated ability of runoff volume and flood peak on detaching soil and transporting sediment and is more reasonable than single runoff depth or flood peak volume

    （ 2 ）以徑流侵蝕力代替降雨侵蝕力來反映水蝕營力與產沙量的關系更加直接，而且綜合了徑流量與洪峰在剝蝕土壤和搬運泥沙能力，比單獨運用徑流深或洪峰流量更加合理。
  10. After that, the multifractal spectra dq - q are computed by fixed - mass method. the results show that in the studied scaling range different types of landscapes and profiles in different directions perform different fractal properties, that is, the d value and crossover length ^ decrease in turns with the landform type from high - moutain, mid - low mountain to basin, and the profile parallel to wear grooves often has lower d values ( < 1. 5 ) than those perpendicular to wear grooves do ( 1. 5 ) in the same section

    提出以地貌分形特點和渡越長度為依據的地貌層次界定方案，研究指出了5km左右應為宏觀臨界點：不同構造地貌區、不同取向的剖線的多重分形譜值域范圍寬窄表現出中低山區高山區盆地區，垂直構造地貌斜坡方向斜交方向平行方向的特點，表明了內外營力作用的不均勻性和方向性。
  11. In riverbed, rqd is an appropriate index of rock mass structure classification. because the weathering agent causes the change of integrity and structure of rock mass, the relationship between rock mass structure indexes and weathering zoning is discussed through wave velocity ratio

    風化營力的作用使巖體中次生裂隙增多從而導致巖體完整性、巖體結構的變化，本文以波速比為紐帶，研究了兩岸壩肩部位巖體結構量化指標與風化分帶的關系。
  12. Agents of erosion

    侵蝕營力
  13. This means that additional climate forcing should not exceed about one watt per square meter

    這表示增加的氣候營力每平方公尺不能大於一瓦特。
  14. From these data we know that the change of climate forcing between the ice age and today was about 6. 5 watts per square meter

    根據這些資料，我們知道從冰期到今天，氣候營力的改變約為每平方公尺6 . 5瓦特。
  15. More fundamentally, the observed heat gain by the world ocean in the past 50 years is consistent with the estimated net climate forcing

    更重要的是，觀察過去50年間全球海洋吸收的熱，與氣候營力的凈估計值也是一致的。
  16. But evidence of a small solar brightening over the past 150 years implies a climate forcing of a few tenths of a watt per square meter

    不過證據顯示，過去150年間，太陽亮度小幅提升，造成的氣候營力每平方公尺不到0 . 1瓦特。
  17. Natural forcings, such as volcanic eruptions and fluctuations of the sun ' s brightness, probably have little trend on a timescale of 1, 000 years

    自然的氣候營力如火山噴發與太陽亮度的變動，在1000年的時間尺度上恐怕沒有什麼變化。
  18. Permafrost fracture and ice fracture are both the result of freezing expansion without evident relation to tectonic deformation and regional structures

    凍土裂縫和冰裂縫屬外營力成因地裂縫，是凍土與冰層不均勻融凍變形的重要表現形式。
  19. One additional watt per square meter of forcing, over and above that today, will take global temperature approximately to the maximum level of the eemian

    今後的氣候營力每平方公尺只要增加一瓦特，就會使全球氣溫達到艾姆間冰期的最高水準。
  20. Specifically, radiative forcings ? volcanic eruptions and solar changes, for instance ? do in fact alter el ni ? o, turning it into more of a la ni ? a state, with colder sea - surface temperatures

    明確來說：火山爆發、太陽變化等輻射營力，確實會影響聖嬰現象，並將它轉為反聖嬰狀態，此時海洋表面溫度較冷。
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