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total organic carbon (toc) in Chinese

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How to pronounce "total organic carbon (toc)""total organic carbon (toc)" in a sentence

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  • 總有機(jī)碳

Examples

  • Soil labile organic carbon is involved in all biological and biochemical processes in soil , the minor change of loc can be detected before the content of total organic carbon ( toc ) in soil has changed , although it accounts for small fraction of toc
    土壤活性碳直接參與了土壤生物化學(xué)轉(zhuǎn)化過程,雖然只占土壤全碳的較小部分,但它們可以在土壤全碳變化之前反映土壤微小的變化。
  • However , although prechlorination efficiently removed algae , its effect was directly related to the quantity of algae and was more obvious in the period of algae bloom . with regard to yellow river water in winter with low temperature and low turbidity , it was discovered that preozonation did not result in a substantial removal of total organic carbon ( toc ) , but a remarkable uv254 . it was further revealed that preozonation changed the characteristics and structure of organic matters and then enhanced removal efficiencie s of them by subsequent processes
    對于夏季高藻期水質(zhì),高錳酸鉀預(yù)氧化對有機(jī)物有一定的去除能力,并能提高后續(xù)工藝出水水質(zhì);預(yù)氯化能顯著去除藻類,但后續(xù)工藝出水水質(zhì)受藻類數(shù)量影響明顯,預(yù)氯化只有在高藻期才能提高后續(xù)常規(guī)處理工藝出水水質(zhì);對于冬季低溫低濁水,預(yù)臭氧化雖不能降低水中有機(jī)物濃度,但能顯著提高后續(xù)常規(guī)處理單元出水水質(zhì)。
  • 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(shí)驗(yàn)結(jié)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(fēng)化成壤作用; sr和rb sr比值能很好的指示生物風(fēng)化成壤作用和淋溶作用;總有機(jī)碳( toc )含量的高低,在一定程度上反應(yīng)了土壤發(fā)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(zhì)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(fēng)化成壤作用的強(qiáng)弱程度,指示成壤過程中的淋溶作用和次生碳酸鹽化作用;并且各指標(biāo)所指示的成壤環(huán)境和成壤強(qiáng)度存在明顯的區(qū)域差異,即渭河流域土壤的生物風(fēng)化成壤作用、次生粘化作用和淋溶作用均表現(xiàn)出南部強(qiáng)于北部。

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