的英文怎麼說

中文拼音 []
英文
名詞(黃土丘陵) loess hills
  1. Keep your business to yourself. don ' t share all your problems. even if you resolve them you ' ll have left the impression that you ' re indecisive or unable to cope with pressure

    自己的事情自己做,不要事無巨細都向同事請教。因為即使你已經餼雋宋侍猓?慊故腔岣?擻湃訊匣蛭薹?娑匝沽牟渙加蟆
  2. There is a evolutional phenomenon to have been recognized in shaanbei loess plateau from south to north. that is luochuan district with the loess yuan ( platform land ) in south. yan ' an - an ' sai district with the loess liang ( ridges ) mainly in middle and shunde - mizhi district with the loess mao ( rounded knolls ) mainly in north. this frame and tendency is got and thought to coincide with the styles of their bedrock traditionalh ? called conformability

    在長期的研究和調查過程中,發現陜北黃土高原在南北縱向上存在明顯的黃土地貌分異現象,即由南向北,大致依次為洛川黃土塬(廣義)地貌、延安?安塞黃土梁狀(為主)丘陵溝壑地貌、綏德?子洲黃土狀(為主)溝壑地貌。
  3. But the conflict between them was appeared during our research in field and the discussion with others. it is followed that the former with the rolling bedrock, the mid with mild bedrock and the latter with the stable bedrock relatively. the conflict between two conclusion above arise, what relationship between loess landforms and their bedrock exist

    但在野外調查及同其他學者交流中發現兩者並非總體對應一致,顯示出陜北黃土高原南部黃土塬基底起伏相對較大,北部黃土梁狀(為主)丘陵溝壑區及黃土狀(為主)丘陵溝壑區基底相對平坦的特徵。
  4. At the same soil layer, the sic contents on the tops of the hills were higher than those in the gullies, however, the soc contents on the tops of the hills were lower than those in the valleys. the possible factors of influence on the distribution of soil carbon were soil water content and human activities

    Kriging插值結果顯示,在同一土壤層次的不同地貌部位,土壤碳含量存在明顯差異,土壤無機碳含量是梁地高、溝川地低,土壤有機碳含量是溝川地高、梁地低。
  5. On the contrary, the valley soils had the minimum change for the profile sic content and the maximum change for the profile soc content the diversity of the soil profile carbon content change were related to their sources, movements and inversions in the soils

    在不同地貌部位的不同層次之間,無機碳含量在地勢高的梁地的土壤剖面上變化幅度大,有機碳含量在地勢低的溝川地的土壤剖面上變化幅度大,二者的差異主要由各自的來源、在土壤中的遷移、轉化等的不同所引起。
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