非飽和方式的英文怎麼說

中文拼音 [fēibǎofāngshì]
非飽和方式英文
nonsaturated mode

  • : Ⅰ名詞1 (錯誤) mistake; wrong; errors 2 (指非洲) short for africa 3 (姓氏) a surname Ⅱ動詞1 ...
  • : Ⅰ形容詞1 (吃足) have eaten one s fill; be full 2 (充實; 飽滿) full; plump Ⅱ副詞(充足; 充分)...
  • : 和動詞(在粉狀物中加液體攪拌或揉弄使有黏性) mix (powder) with water, etc. : 和點兒灰泥 prepare some plaster
  • : Ⅰ名詞1 (方形; 方體) square 2 [數學] (乘方) involution; power 3 (方向) direction 4 (方面) ...
  • : 名詞1 (樣式) type; style 2 (格式) pattern; form 3 (儀式; 典禮) ceremony; ritual 4 (自然科...
  • 飽和: (在一定溫度壓力下, 溶液可含溶質的量達到最大限度, 不能再溶解, 泛指事物達到最高限度) saturation; saturated
  • 方式: way; fashion; pattern

※中文詞彙非飽和方式在字典百科國語字典中的解釋。

  1. It is mainly a faith or ideology with which some actor ( an individual, a group or a nation ), for the purpose of realizing some political, economic, cultural interests suppressed, driven by hatred and retaliative motivation, takes by specific and secret individual or small group unconventional extreme measures which are abrupt and unpredictable, and utilizes every means which is as harmful as possible to the opposite, and often violent enough to endanger the innocent or to massacre with malice aforethought the innocent and lead to huge social panic, to attack the opposite

    它主要是指一定的行為體(個人、團體或國家)為使受到壓制的一定政治、經濟、文化等利益能夠實現,在仇恨報復性動機的驅使下,通過特定的個人或小集團採用突然的、難以預料的常規,利用一切可能危害對的、常常是暴力殃及無辜或蓄意濫殺無辜等足以產生巨大社會恐慌效果的手段打擊對的一種信仰或意識形態。
  2. By direct shear for and normal triaxial shear tests of non - saturated desert sand, the parper studied the effect of water content and dry density on the strength of the non - saturated desert sand, and set up the code of this sand. based on the plane strain test of non - saturated desert sand slope, the paper analysed the destruction way of the excavaion side during the construction by means of adding water, and brough forward a formule that calculates the allowable of excavation and pile hole

    通過沙漠砂直剪試驗常規三軸剪切試驗,研究了含水量干密度對砂強度的影響,建立了這種砂的強度準則。通過沙漠砂邊坡室內平面應變試驗,分析了沙漠井場浸法施工中就基坑壁的破壞,推導出了基坑樁孔容許開挖深度的計算公
  3. Abstract : using the convective - dispersive equation and based on labo ratory exp eriment, the hydrodynamic dispersion coefficient of unsaturated soil is determi n ed under different inial soil water content, different manner of water infiltra t ion and fertilizer supply

    文摘:用土壤水動力彌散程及其解析解,在室內試驗的基礎上,研究了土壤在不同初始含水量、不同入滲及不同加肥下的水動力彌散系數。
  4. Traditionally, the saturated zone is modeled as a simple lumped continuity equation :, dsitqsdt where t is time, s is the total storage in the reservoir, i is the spatially integrated volume of incoming wa - ter, and q is the discharge subsurface runoff which only depends on the total storage s. this kind of subsurface runoff model has many different parame - terizations 10 12, however it has a very common char - acteristic that the subsurface runoff is just a sin - gle - valued storage - discharge function

    對于大尺度水文模型而言,目前常常採用的是集總的地下徑流機制,其連續性程一般可表示為d , dsitqst ? 1這里t是時間, s表示整個流域潛水面土壤層的區域總的水分儲存量, i t表示t時刻土壤的區域向整個潛水面的水分補充量, q s表示僅依賴於水分儲存量s的地下徑流量量
  5. The results indicate that the inial soil water conten t and the manner of water supply affect the dispersion - coefficient deeply, but the manner of fertilizer supply does not affect it

    研究結果表明:土壤初始含水量、灌水土壤水動力彌散系數影響大,而加肥對土壤水動力彌散系數影響小。
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