棕色化 的英文怎麼說

中文拼音 [zōngshǎihuà]
棕色化 英文
browning
  • : 名詞1. [植物學] (棕櫚樹) palm2. (棕毛) palm fibre; coir
  • : 色名詞[口語] (顏色) colour
  • 棕色 : brown棕色土 umber; 棕色顏料 brown
  1. B substance function the pure product is achromaticity oil liquid. if it contained impurity then showed yellow and palm in industry

    B物性質:本產品純品為無油狀液體,工業中如果含有雜質,則呈黃
  2. By using the similar separation and purification methods, a nifh and a nife mofe protein were obtained from azotobacter vinelandii mutants dj54 and dj35. the results of the complement activity experiments showed that a nifh mofe could be activated by femoco

    固氮菌突變種dj _ ( 54 )中得到了nifhmofe蛋白;並參與了固氮菌突變種dj _ ( 35 )的nifemofe蛋白的分離純,所用方法與nifb ~ - mofe蛋白的分離純相似。
  3. Polished on one side, this unique piece from madagascar is a glorious, organically - patterned combination of ivory, gold, beige, rust, and brown stone, with a few small scattered veins of druzy quartz

    石片一面已經打磨,馬達加斯加的木石花紋顏是象牙、金、米黃(淺褐) 、銹,有少數晶體紋理。
  4. In vegetation, acute injury by often results in an ivory coloration, but sometimes the coloration is reddish brown.

    在植物方面,因二氧硫嚴重損傷經常導致象牙,但有時為紅
  5. H3fe ( cn ) 6 ), a brown unstable acid formed from ferricyanide

    一種的不穩定酸,由鐵氰物形成。
  6. 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

    潛育土的一個重要特點是位於土壤腐殖質層之下,其土層呈灰藍是由於含有被微生物還原的亞鐵離子,而且常有部分鐵被氧生成紅的銹斑。
  7. Abstract : soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and erman ' s birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in erman ' s birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in erman ' s birch forest. because the forests of broad - leaved / korean pine, dark coniferous and erman ' s birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil

    文摘:為了研究土壤溫度和土壤含水量對闊葉紅松林(山地暗壤) 、雲冷杉暗針葉林(山地針葉林土壤)和岳樺林(生草森林土)的土壤呼吸的影響,於2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量,將土壤含水量分為9 , 、 21 、 30 、 37和43 5個等級,土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 ( 35范圍內,土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土壤呼吸隨含水量的增加而升高,當含水量超出該范圍,土壤呼吸速率則隨含水量的變而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ,含水量37 ;雲冷杉暗針葉林下的山地針葉土壤呼吸作用的最佳條件是25 , 21 ;岳樺林土壤呼吸作用的最佳條件是35 ,含水量37 .但是,由於長白山闊葉紅松林,雲冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土壤溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地針葉林土呼吸速率應低於暗森林土呼吸速率,山地生草森林土呼吸速率應高於山地針葉林土的呼吸速率.圖2表1參25
  8. Soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and ermans birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in ermans birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in ermans birch forest. because the forests of broad - leaved / korean pine, dark coniferous and ermans birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil

    為了研究土壤溫度和土壤含水量對闊葉紅松林(山地暗壤) 、雲冷杉暗針葉林(山地針葉林土壤)和岳樺林(生草森林土)的土壤呼吸的影響,於2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量,將土壤含水量分為9 , 、 21 、 30 、 37和43 5個等級,土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 ( 35范圍內,土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內( 21 ( 37 ) ,土壤呼吸隨含水量的增加而升高,當含水量超出該范圍,土壤呼吸速率則隨含水量的變而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異,大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ,含水量37 ;雲冷杉暗針葉林下的山地針葉土壤呼吸作用的最佳條件是25 , 21 ;岳樺林土壤呼吸作用的最佳條件是35 ,含水量37 .但是,由於長白山闊葉紅松林,雲冷杉林和岳樺林處在不同的海拔帶上,同期不同森林類型土壤溫度各不相同,相差4 ~ 5 ,所以野外所測的同期的山地針葉林土呼吸速率應低於暗森林土呼吸速率,山地生草森林土呼吸速率應高於山地針葉林土的呼吸速率.圖2表1參25
  9. The light penetrated to it from two deep - set openings high up in the wall, but at that hour of the night the dressing room was lit by flaring gas. it was papered with a paper at seven sous a roll with a pattern of roses twining over green trelliswork

    在夜晚這樣的時刻,煤氣燈的光焰照亮了妝室,妝室的墻上貼著每卷值七個蘇的紙,上面印著爬在架子上的玫瑰花。
  10. By the mixing of sodium sulfide and sodium molybdate within a suitable ph range, molybdenum trisulfide particles were obtained as precipitation substance

    在一定酸性的條件下將硫鈉和鉬酸鈉的水溶液進行混合與反應,生成三硫鉬膏狀沉澱。
  11. " its about the natural nude face - - thats what i call it, " says makeup artist bobbi brown. " its not all beiges, its about finding the colors that are right for you

    妝大師鮑比?布朗說: 「 『自然真臉龐才是最美,這是我的叫法。並不是說淡就最好,關鍵是要找到適合你自己的顏。 」
  12. Brown podzolic soil

  13. The result shows that the greater positive influence is from the dissolutions of carotene and browning reaction, next come the cembratriendid compounds and hypoglycemia compounds, while the negative influence is from indoles, toluene and some aldehydes, and the negative influence from the dissolutions of carotene and browning reaction is less

    結果表明,對評吸結果影響較大的是胡蘿卜素降解產物類和棕色化反應產物類;類西柏烷類和苯丙氨酸類中性致香物質的貢獻較小;負面影響較大的成分主要集中在吲哚、甲苯及一些醛類上,類胡蘿卜素降解產物類和棕色化反應產物類中的個別成分也有一定的負面影響。
  14. In their place we found intriguing alternations of turquoise - blue, gray and green clays, brown sandstone and fossilized plant matter called lignite

    我們發現取而代之的巖層組成十分有趣,其中包括了藍綠、灰、綠的黏土、的沙巖,以及稱做褐煤的植物石。
  15. The rock varies in color: white, buff, brown, black, and green varieties occurring.

    巖石在顏上有多種變,有白、淡黃、黑及多種綠變種。
  16. Yellow - brown powder. it is insoluble in water. it is soluble in sodium sulfide solution with a yellow - orange colour, slightly soluble in concentrated sulfuric acid

    均勻粉末,不溶於水,溶於硫鈉溶液中呈黃光橙,微溶於濃硫酸。
  17. Carbohydrate metabolism of the brown cotton yield organs

    彩棉產量器官的碳水合物代謝
  18. Remove foil ; bake until top is browned and sauce is bubbling, 12 to 15 minutes

    去掉箔片;烤12 - 15分鐘,直至通心粉頂部變成,番茄沙司融
  19. Compared with the common cultivation, the contents of carotenoid, phenylalanine, products of browing reaction and neophytadiene were greatly increased in every treatment

    並使煙葉中性致香物質總量增加,類胡蘿卜素類、苯丙氨酸類、棕色化產物、新植二烯等致香物質含量均較對照有很大提高。
  20. Spring sees a return to whites, browns and other muted tones

    系、系以及其它柔系將在春季回歸。
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