物候演替 的英文怎麼說

中文拼音 [hòuyǎn]
物候演替 英文
phenological succession
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • : 動詞1 (演變; 演化) develop; evolve 2 (發揮) deduce; elaborate 3 (依照程式練習或計算) drill;...
  • : Ⅰ動詞1 (代替) replace; substitute for; supply [take] the place of 2 [書面語] (衰敗) decline Ⅱ...
  1. ( 2 ) there is stage of soil formation from the evolution of pedogenic environment in the weihe valley during holocene. soil formation shows the law of evolving from warm and wet strong soil formation period to cold and dry dust deposition period ( weak soil formation period ) and to warm and wet strong soil formation period again. the loess - soil sequence is a compound soil sectional system of different kinds of soil evolution under different bio - environment and pedogenic processes

    ( 2 )通過對全新世渭河流域成壤環境變問題的討論,揭示了全新世渭河流域土壤的發育具有階段性,表現為由溫濕的強成壤期向冷乾的沉積期(弱成壤期)變、再向溫濕的強成壤期變的規律;黃土一古土壤序列是不同生環境下、不同成壤過程發育的不同土壤類型而形成的復合型土壤剖面體系;而且由於冬夏季風環流及其環境效應在空間上的差異,使得復合型土壤剖面體系也存在著南北差異。
  2. The quaternary environmental evolution of the beijing plain region mainly depends upon the neotectonics and palaeoclimatic changes, which controlled and influenced the distribution, evolution of depositional areas and uplifting erosional areas and changes of sedimentary types, and also the scale and scope of quaternary transgressions

    冷暖交的軟體動組合,反映了本區第四紀時古氣的變動特點。北京?通縣平原地區的第四紀環境變,主要取決于氣變化和新構造運動。
  3. ( 2 ) the analysis by characteristic section planes can draw that the ancient climate in deposit period of the characteristic section plane one sediments ( about seventeen thousand years before present ) is warm - dry and has relative humid and dry evolution rule, from fifteen to thirty years as its evolution period, that the ancient climate in deposit period of the characteristic section plane two sediments ( about fourteen thousand years before present ) is humid and has relative alternate very humid and humid evolution rule, from two to fourteen years as its evolution rule

    ( 2 )通過對兩個典型剖面的綜合分析得出,典型剖面沉積沉積時期(距今約17kab . p . )的古氣特徵總體上為暖干,並具有以15 30年為化周期,相對的濕潤-乾燥-濕潤的變規律。典型剖面沉積沉積時期(距今約14kab . p . )的古氣總體特徵為濕潤,並具有以2 14年為變周期,相對的很濕潤-濕潤交化規律。
  4. Climatic climax a plant community that is in equilibrium with a stable climate. it represents the of a succession

    頂級群落:與穩定的氣平衡的植群落,它代表的頂級。
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