能量積累因子 的英文怎麼說

中文拼音 [néngliánglěiyīnzi]
能量積累因子 英文
energy build-up factor
  • : 能名詞(姓氏) a surname
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : 累Ⅰ形容詞(疲勞) tired; fatigued; weary Ⅱ動詞1. (使疲勞; 使勞累) tire out; wear out 2. (操勞) work hard; toil
  • : Ⅰ動詞[書面語] (沿襲) follow; carry on Ⅱ介詞1 [書面語] (憑借; 根據) on the basis of; in accord...
  • : 子Ⅰ名詞1 (兒子) son 2 (人的通稱) person 3 (古代特指有學問的男人) ancient title of respect f...
  • 能量 : 1 [物理學] energy; amount of energy 2 (能力) capabilities; capacity; 能量不滅 conservation of e...
  • 積累 : 1. (逐漸聚集) accumulation; accumulate 2. [核子] build-up; 積累基金 accumulation fund
  1. Energy build up factor

  2. Energy fluence build up factor

  3. The work on seasonal dynamics of litter input and decomposition and the relationship between them and environmental factors was studied through the method of harvest and weight loss. soil respiration rate was measured by alkali - absorption method and the contribution from soil microorganism respiration and from root respiration was determined through trendline method of linear regression between soil respiration rate and belowground biomass. mathematical models were established between the seasonal dynamics of main components of soil total respiration including soil respiration, root respiration, soil microorganism respiration, litter respiration and environmental factors

    應用收獲法和重損失法對枯枝落葉輸入與分解的季節動態及其與環境的關系進行了研究;應用靜態氣室法測定了土壤總呼吸和凋落物呼吸,應用土壤呼吸與地下生物線性回歸趨勢線法測定了土壤微生物呼吸及根呼吸的貢獻,運用相關分析法建立了土壤總呼吸、根呼吸、土壤微生物呼吸及其凋落物呼吸季節動態與環境之間的數學模型;應用灰色分析比較了兩群落土壤呼吸季節動態產生差異的原;應用干重換演算法對土壤微生物的季節動態進行了測定,建立了土壤微生物與環境的數學模型;應用系統分析方法,利用分室模型,對兩群落枯枝落葉與微生物之間的流動進行了定測定和穩定性分析。
  4. After a careful comparison we found : ( 1 ) rotating the coordinate system around the z - axis for each event is necessary for the relaxation of the correlation between thrust ( or sphericity ) major - minor frame and the direction of the first hard gluon emission. ( 2 ) the horizontal factorial moments ( hfm ) are equivalent to the vertical ones ( vfm ) only after cumulant - variable transformation. therefore, in the study of nonlinear phenomena in high energy collisions the hfm can be used only in combination with the cumulant variables

    工jlnfy4ww ; 6標系與發射第一個硬膠之間的關聯效應,從而觀察到全部強度的動力學起伏;證明了:只有在引入以後,橫向矩才等於縱向矩,從而也才等效于幾率矩,困而只有在這時,橫向矩才被使用;論證了:對eb對撞末態粒系統動力學起伏的研究只在全相空間進行,而不用限定的相空間,而只採用丟掉最初的一個或幾個點的方法消除動守恆對相空間標度特性的影響。
  5. Water cement ratio and mixing fly ash or slag into concrete effect on ability of resisting chloride penetrating that are considered in the model. the effect of environment that include temperature, relative humidity and cumulating of surface chloride concentration of concrete are also considered. moreover, chloride diffusion changing with time is included in this model as well as

    模型中考慮水灰比和混凝土配合比(摻入不同的粉煤灰和礦渣)變化對混凝土抵抗氯離侵蝕力的影響,同時考慮溫度、相對濕度和表面氯離濃度變化等環境素對氯離侵入混凝土過程的影響,以及氯離擴散系數隨時間的變化。
  6. But on the later condition the trend of accumulation turned to be stable in the w3 treatment ( vseawater / v pure water = 1 ) - in root zone soil, variation of sar value accorded with total salt accumulations and sometimes decreased at the treatment where the v seawater / v pure water > 1. contents of cl - and na + which were the main ions and leached obviously in 0 - 60cm soil were greatly influenced by rainfall, but the rainfall did not affected the contents of ca2 +, mg2 + and k + whose ability of leaching is worse than that of cl - and na + in the root zone soil obviously. the vertical distribution of salt ions in the 0 - 60cm soil were mainly affected by the ratio of v seawater / v pure water in the irrigation water on the condition of not enough rainfall, but on the cont

    海水灌溉下,耕層土壤中鹽分含受降雨影響很大,足夠的降雨條件下,鹽分不會,降雨較低時,鹽分明顯,但在50海水處理下趨于平衡狀態;耕層土壤sar值的變化情況和鹽分含變化情況相一致,在灌溉水中海水濃度大於50時有所下降;土壤中主要鹽離為cl ~ -和na ~ + , 0 - 60cm土層內, na ~ + 、 cl ~ -明顯的向土壤底層遷移,其在土壤中的含受降雨影響顯著,而ca ~ ( 2 + ) 、 mg ~ ( 2 + )和k ~ +在土壤中遷移力較低,其含受降雨影響較小; 0 - 60cm層次土壤鹽分的縱向分佈在降雨較低的條件下主要受灌溉水中海水濃度的影響,而在降雨充分的條件下,地面覆蓋程度成為重要的影響鹽分和水分脅迫下菊芋的生理響應及其海水灌溉研究之一。
  7. Energy absorption build up factor

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