緩慢消失 的英文怎麼說

中文拼音 [huǎnmànxiāoshī]
緩慢消失 英文
linger on
  • 緩 : Ⅰ形容詞1 （遲; 慢） slow; unhurried 2 （緩和; 不緊張） not tense; relaxed Ⅱ動詞1 （延緩; 推遲） d...
  • 慢 : Ⅰ形容詞1. （速度低; 走路、做事等費的時間長） slow 2. （態度冷淡, 沒有禮貌） supercilious; rude Ⅱ動詞（從緩） postpone; defer
  • 消 : 動詞1 （消失） disappear; vanish 2 （使消失; 消除） eliminate; dispel; remove 3 （度過; 消遣） pa...
  • 緩慢 : slow
  • 消失 : disappear; vanish; dissolve; die away; fade away
  1. Have disease slow, the ache of the area that damage nerve place controls, brief hypersensitive, the feeling is unusual, serious sao is urticant, afterwards has a feeling to disappear, have show " glove - sock " model distributing, also have distributing by section

    起病緩慢，受損神經所支配的區域的疼痛，短暫的感覺過敏，感覺異常，嚴重瘙癢，繼有感覺消失，有呈「手套襪子」型分佈，也有按節段分佈。
  2. Social stratification is not very clear in the village, and memory of community is disappearing gradually

    石村社區結構的典型特點就是社區分層不明顯以及社區記憶正在緩慢消失。
  3. And when you eradicate that core it starts its degradation process

    當這個核心被清除掉時相應的記憶會緩慢消失
  4. Instead of the atlantic disappearing, they say, the pacific might slowly vanish, sending north and south america careering into asia

    他們並指稱，緩慢消失的可能不是大西洋而是太平洋，從而促成南北美洲和亞洲結合。
  5. Then, by the comprehensive analysis of essential conditions for stone forest development, and the quantitative study on the evolution phases of bajiang karst catchment and the spacial coupling analysis of its hydro - geomorphological system, the paper studies the relationship between the evolution of bajiang karst drainage area and the development of stone forest, and, combined with the evolution history of the catchment, puts forward a model concerning the relationship between the evolution of bajiang karst catchment and stone forest development, in the mechanism of " tri - level erosion ", if a < s < c, the visible and actual height of stone pillars will keep on increasing, meanwhile, soil layer among stone pillars will become thicker and thicker, so the the height of stone pillars " root will become higher and higher, too

    在「三重剝蝕」機制中，若a s c ，石柱的可見高度和實際高度會不斷增高，同時，石柱的根部的土層會增厚，其土下部分的高度也會不斷增大。若a c s ，說明石柱的實際高度在增加的同時，其可見高度也在增加，但土層會變得越來越薄，最終當底土被完全剝蝕掉后，氣下溶蝕和土下溶蝕的差異消失，此時a接近於c ，石柱的實際高度將停止拔高或極緩慢增長，並在各種物理、化學風化的作用下而變得日益矮小。若s a c ，石柱的可見高度將趨于變矮，但驅動石林發育的土層厚度將會增大。
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