碳酸飽充作用的英文怎麼說

中文拼音 [tànsuānbǎochōngzuòyòng]
碳酸飽充作用英文
carbonatization

  • : 名詞[化學] (非金屬元素) carbon (c)
  • : 酸構詞成分。
  • : 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)...
  • : Ⅰ形容詞(滿; 充足) sufficient; full; ample Ⅱ動詞1 (裝滿; 塞住) fill; charge; stuff 2 (擔任; ...
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  • 碳酸: carbonic acid碳酸氣 carbonic acid gas; 碳酸泉 [水文] carbonate spring; 碳酸泉水 apollinaris

※中文詞彙碳酸飽充作用在字典百科國語字典中的解釋。

  1. The activation energies of crystal growth were calculated to be 15. 9kj mol " 1 and 148. 7kj mol " 1 respectively. cerous nitrate as originating material, ammonium hydrogen carbonate as precipitator, nanocrystalline cec > 2 powders were prepared by precipitation process. during the experiment, reacting solution was heated by microwave energy

    氫銨為沉澱劑,聚乙二醇等表面活性劑為保護劑,採逐滴加入沉澱劑,微波加熱代替傳統加熱的均相沉澱法,制備出了粒度小、分散性好的ceo _ 2納米粉體。
  2. The main results are following : ( 1 ) the variation of clay / silt ratio can indicate the secondary clay action of dust depositions ; the variations of magnetic susceptibility and total fe content are inferred to be records of the changeable intensity of bio - pedogenesis ; the variations of sr content and rb / sr ratio can indicate bio - pedogenesis, dissolving and leaching action ; the content of total organic carbon ( toc ) can reflect variation of climate and vegetation during soil formation, it indicates the intensity of weathering and bio - pedogenesis ; the content variation of caco3 can show the intensity of dissolving - leaching action and secondary deposit, which was noted as pseudomycilia in pores and fissures in the sediment, so it can indicate the intensity bio - pedogenesis quite well. these proxy indexes also reflect obvious regional difference of pedogenic environment and the intensity bio - pedogenesis ; namely, secondary clay action, dissolving - leaching action and bio - pedogenesis are all much stronger in south than that in north

    實驗結果表明:粘粒粉沙比值能很好地指示粉塵堆積物的次生粘化;磁化率和全鐵很好地指示生物風化成壤; sr和rb sr比值能很好的指示生物風化成壤和淋溶;總有機( toc )含量的高低,在一定程度上反應了土壤發育過程中氣候和植被狀況的變化,指示著成壤過程中腐殖質化的程度; caco3含量的變化,可以反映了黃土古土壤形成時的風化成壤的強弱程度,指示成壤過程中的淋溶和次生鹽化;並且各指標所指示的成壤環境和成壤強度存在明顯的區域差異,即渭河流域土壤的生物風化成壤、次生粘化和淋溶均表現出南部強于北部。
  3. This paper gives a brief review of four stabilization mechanisms of soc : ( 1 ) recalcitrance of organic carbon compounds, ( 2 ) interactions with metal oxides and soil mineral surfaces, ( 3 ) spatial inaccessibility against decomposers because of micro - aggregate ' s physical protection, and ( 4 ) biological mechanisms, mainly the direct contributions of soil organisms themselves

    土壤有機的穩定機制主要包括: ( 1 )有機的難降解性; ( 2 )金屬氧化物和粘土礦物與有機的相互; ( 3 )土壤團聚體的物理保護導致的生物與有機空間隔離; ( 4 )土壤生物學機制,主要指土壤生物自身對有機穩定性的直接貢獻。
  4. Water quality - digestion for the determination of selected elements in water - part 2 : nitric acid digestion

    水質.測定水中所選元素的消化.第2部分:硝消化
  5. Application for some novel methods to produce the stable sodium percarbonate

    鈉的應和穩定技術進展
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