腐殖的 的英文怎麼說

中文拼音 [zhíde]
腐殖的 英文
humic
  • : Ⅰ名詞(豆腐) bean curdⅡ動詞(腐爛; 變壞) decay Ⅲ形容詞(腐爛) rotten; corroded; putrid
  • : 殖Ⅰ動詞(生息; 孳生) breed; grow; multiply Ⅱ名詞(姓氏) a surname
  • : 4次方是 The fourth power of 2 is direction
  1. Humic acids are usually regarded as polymers of aromatic compounds.

    酸通常被看作是芳烴化合物聚合物。
  2. The black earth is a kind of alfisol, with a thick layer of humus, loose texture, high fertility, high porosity ratio, poor permeability and a high content of clay, which is suitable for cultivation

    摘要黑土是一種質層厚,質地鬆散,肥力很高,孔隙比較大而透水性差,粘粒含量高,適于耕作淋溶土。
  3. Sand - fixing effects of caragana microphylla shrub in keerqin sandy land

    不同土壤酸對辛硫磷水解影響
  4. The final process in organic matter decomposition is known as humification.

    有機物分解最後程序稱為質化。
  5. An improved method for extraction of soil humic acid was used to isolated dissociative humic acid ( ha - i ) and enwrapped humic acid ( ha - ii ) from paddy soil and pohakee peat. quantified and characterized ha - i and ha - ii with 13c nmr, py - gc - ms, optical and elemental analysis. the results indicate that two humic acids are highly different in structure, and ha - ii is more condensed

    採用一種改進酸萃取方法從珠江三角洲稻田土壤和pahokee泥炭中分離出了游離酸( ha - )和包裹酸( ha - ) ,並採用元素分析、 ~ ( 13 ) cnmr 、 py - gc - ms和有機巖石學方法對ha -和ha -進行了定量和定性研究,結果表明兩種酸在性質和結構上是有區別
  6. Humic substances are known to coat membrane filters.

    質是已知能夠覆蓋濾膜物質。
  7. Determination of humus fractionation in forest soil

    森林土壤質組成測定
  8. A hole about 1. 25 cm deep should be made into a soil of friable loam soil with a high humus content

    一個大約1 . 25厘米深洞、應該做成一易碎肥土土壤或者高土壤。
  9. Gley ( glei ) a waterlogged soil lacking in oxyen, in which raw humus accumulates as a result of lack of decomposition by bacteria

    潛育土:是一種氧含量低而水含量很高土壤,由於缺少分解性細菌而在其內積累了大量質。
  10. The defining feature is the gley horizon below the humus - blue - grey clay whowe color is due to ferrous iron compounds that have been reduced by microorganisms, flecked with localized areas of rust - colored oxidized ferric compounds

    潛育土一個重要特點是位於土壤質層之下,其土層呈灰藍色是由於含有被微生物還原亞鐵離子,而且常有部分鐵被氧化生成紅棕色銹斑。
  11. Ultimate analysis provides an useful inventory of the distribution of the major elements in humic substances.

    元素分析提供物質中主要元素分佈有用資料。
  12. Remediation of oily soil in gas station using humic acid as surfactant

    酸做表面活性劑對加油站油污土壤修復
  13. Studies on increasing n utilizing efficiency in maize by applying humic acid

    施用酸對提高玉米氮肥利用率研究
  14. The influences of reinforcing cement soil on soil humus

    土體質對水泥土固化影響
  15. Characteristics of humus in maturing salt - affected soil

    鹽漬土熟化過程中質特性研究
  16. Relative colour degree of humus acid

    相對色度
  17. Habitat and ecology : in forests, on mossy rocks and stony ground with rich humus soil ; alt. 300 m. flowering : oct. to jan. of the following year

    生境與生態:生於低海拔700米以下林下質豐富多石之地或溪旁生苔蘚巖石上。花期: 10月至翌年1月。
  18. The earth surface of the region across it is mostly thicker humus soil or leaf falling covering layer, and has good heat reserving property, it is mostly weathering shingle, soil - aggregate mixture, and clay - gravel 0. 5m - 4. 0m under it, and weathering rock

    所經地區地表多為較厚土或落葉覆蓋層,其保溫性良好,下層0 . 5 ? 4 . 0米多為風化沙礫、碎石土和礫石土, , 4 . 0米以下為風化巖石。
  19. Besides humic acid and kerogen, four soms consist of a special organic fraction black carbon ( bc ), it accounts for the least 18. 36 % of toc in marine sediment. and different fractions of som have different origin

    四種土壤和沉積物有機質中除了酸和乾酪根,都含有相當數量碳黑,最少海洋沉積物有機質中碳黑含量也達到18 . 36 。
  20. 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比值能很好指示生物風化成壤作用和淋溶作用;總有機碳( toc )含量高低,在一定程度上反應了土壤發育過程中氣候和植被狀況變化,指示著成壤過程中質化程度; caco3含量變化,可以反映了黃土古土壤形成時風化成壤作用強弱程度,指示成壤過程中淋溶作用和次生碳酸鹽化作用;並且各指標所指示成壤環境和成壤強度存在明顯區域差異,即渭河流域土壤生物風化成壤作用、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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