表面崩塌 的英文怎麼說

中文拼音 [biǎomiànbēng]
表面崩塌 英文
surface avalanche
  • : Ⅰ名詞1 (外面;外表) outside; surface; external 2 (中表親戚) the relationship between the child...
  • : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
  • : 動詞1 (倒塌; 崩裂) collapse 2 (破裂) crack; burst 3 (崩裂物擊中) hit 4 [口語] (槍斃) shoo...
  • 表面 : surface; superficies; boundary; face; rind; sheet; skin; outside; appearance
  • 崩塌 : (突然崩裂倒塌) slide; collapse; crumble
  1. Under pulse condition, charging and discharging of surface states between gate and drain induce gan hemt current collapse

    脈沖條件下, ganhemt電流效應主要由柵漏之間態充放電引起。
  2. The main conclusions and cognitions are as follows : ( l ) rockmass weathering should be studied from either microcosmic and macrocosmic, microcosmic contain includes of mineralogy and of lithology, and in macrocosmic, weathering action damages integrality of rockmass, so studying rockmass structure can open out weathered degree of epigenetic - surface rockmass. ( 2 ] the dissertation sums up the characteristic indexes which can token weathered and unloaded degree, simultaneously, puts forth and summerizes several methods that classifies different weathered and relaxed zones of slope rockmass. ( 3 ) river valley epigenetic - surface reformation is controlled by rockmass structure, but weathering and unloading of rockmass is the direct cause which leads to different epigenetic - surface physical geology phenomena, for example, collapse, landslide, incline, dynam - relaxed and so on

    本文主要結論與認識為: ( 1 )對于巖體風化的研究從微觀與宏觀兩方入手,微觀方重視對礦物學、巖石學的研究,宏觀方,上升到巖體結構被改造的高度進行研究; ( 2 )歸納了徵巖體風化、卸荷程度的特徵指標並提出了劃分巖體風化、卸荷程度的幾種方法; ( 3 )巖體結構控制著河谷淺改造,但導致、滑坡、傾倒、松動等生物理地質現象的直接原因乃是巖體的風化、卸荷。
  3. 4. the non - linear interaction mechanism derived from the scale of system was discussed. the paper deemed that, falling sliding face is not a rectilinear type, the non - linear coupling of falling factors sharply enhanced in large sand - pile ; the stabilization of surface layer sands are different in the time and space, especially the stating probability is higher than halting, and probability of fault in slope foot is higher than top as well ; the faulting forms will be affected by bounder situation strongly

    大尺度散粒體坡滑動,一般並非直線形,在過程中的耦合作用將增大落沙規模;理想化的沿直線坡滑動情況,坡層砂粒的穩定性也並不是在時間、空間上都均衡的,可以造成起動容易止動難,或坡角失穩概率大從而牽連整個坡的情況;長大高陡坡的失穩形式,可以受坡腳(邊界)的巨大影響。
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