碳酸飽充作用英文怎麼說
碳酸飽充作用 的英文翻譯
碳酸飽充作用 英文 carbonatization 碳 : 名詞[化學] （非金屬元素） carbon （c） 酸 : 酸構詞成分。 飽 : 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）... 充 : Ⅰ形容詞（滿; 充足） sufficient; full; ample Ⅱ動詞1 （裝滿; 塞住） fill; charge; stuff 2 （擔任; ... 用 : 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
碳酸飽充作用 例句
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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採 用 碳 酸 氫銨 作 為沉澱劑，聚乙二醇等表面活性劑為保護劑，採 用 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。
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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 作 用 ；磁化率和全鐵很好地指示生物風化成壤 作 用 ； sr和rb sr比值能很好的指示生物風化成壤 作 用 和淋溶 作 用 ；總有機 碳 （ 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 作 用 的強弱程度，指示成壤過程中的淋溶 作 用 和次生 碳 酸 鹽化 作 用 ；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 作 用 、次生粘化 作 用 和淋溶 作 用 均表現出南部強于北部。
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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 碳 的穩定機制主要包括： （ 1 ）有機 碳 的難降解性； （ 2 ）金屬氧化物和粘土礦物與有機 碳 的相互 作 用 ； （ 3 ）土壤團聚體的物理保護導致的生物與有機 碳 空間隔離； （ 4 ）土壤生物學機制，主要指土壤生物自身對有機 碳 穩定性的直接貢獻。
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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 作 用 .第2部分:硝 酸 消化 作 用
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Application for some novel methods to produce the stable sodium percarbonate過 碳 酸 鈉的應 用 和穩定技術進展
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