無機碳 的英文怎麼說

中文拼音 [wújītàn]
無機碳 英文
dic
  • 無 : 無Ⅰ動詞（沒有） not have; there is not; be without Ⅱ名詞1 （沒有） nothing; nil 2 （姓氏） a surn...
  • 機 : machineengine
  • 碳 : 名詞[化學] （非金屬元素） carbon （c）
  • 無機 : [化學] inorganic無機氮肥 inorganic nitrogenous fertilizer; 無機肥料 inorganic fertilizer; 無機化...
  1. The beef extract, a beef derivative, is a source of organic carbon, nitrogen, vitamins, and inorganic salts

    牛肉萃取物是一種牛肉衍生製品，可以作為有機碳、氮、維生素與無機鹽類的一個來源。
  2. The acidtreated packing causes release of co2 from inorganic carbonates.

    酸化處理過的填料會使co2從無機碳中釋放出來。
  3. The remaining 5 percent of the ingredients are non - organic or synthetic, and include baking powder, pectin to make yogurt thicker, or carbon dioxide to keep products, like cottage cheese, fresher longer

    其餘5 %的成分為無機物質或人工合成物，包括用來製作高濃度酸乳酪的發酵粉，膠質，或可使像松軟乾酪一類產品保持持久新鮮的二氧化碳。
  4. Caco3 not only affects soil physical and chemical characteristics but also causes co2 change in the air, because caco3 is main components among the total pool of inorganic carbon of soil. this paper systematically summarized and analyzed general development characteristics of soil profile caco3 in loess hill gully area including source, content, forming - condition, distribution and illuviation - depth of caco3, which will have the most important significance for the further studies on global soil and climate change

    碳酸鈣在土壤剖面中淀積的深度和類型是黃土高原土壤發育的重要標志，鈣積層是黃土高原土壤發育環境的歷史信息庫，同時土壤碳酸鈣作為土壤無機碳庫重要組成，它通過溶蝕后再結晶與大氣co _ 2之間進行物質交流來影響全球氣候變化。
  5. The main conclusions are as follows : the hco3 - ion content of zhujiang river changes notably in one hydrological year, especially in wet season and dry season. as for the content of inorganic carbon, that of the xijiang river is the highest, then the beijiang river, and then the dongjiang river. the xijiang river ' s inorganic carbon source was major from karst process in the drainage basin

    得出如下的結論：珠江水體hco _ 3 ~ -離子含量在一個水文年中發生顯著變化，特別是豐水期與枯水期之間波動幅度較大；無機碳含量西江含量最高，其次是北江，東江最低；西江無機碳主要來源於巖溶作用，由於受河流沖刷效應影響，豐水期hco _ 3 ~ -離子含量升高；東江流域無機碳主要來源於硅酸鹽巖的碳酸鹽風化過程，豐水期hco _ 3 ~ -離子含量無顯著變化；北江無機碳來源於巖溶作用和硅酸鹽巖的碳酸鹽風化過程，受稀釋效應影響，無機碳含量隨水量增加而降低。
  6. Inorganic carbon transport was a major factor in facilitating quenching during the initial stage and the initial rate of fluorescence quenching in the presence of iodoacetamide, an inhibitor of co2 fixation, was 87. 9 % of control

    初始階段的熒光淬滅主要是由於無機碳轉運所致，加入co _ 2固定的抑制劑iodoacetamide ，熒光淬滅的初始速率為對照的87 . 9 。
  7. The distribution and ecology of ge - xian - mi in rice fields of hefeng county in china were investigated. furthermore, the co2 concentrating mechanism ( ccm ) in cyanobacterium was reviewed and the utilization of inorganic carbon in ge - xian - mi in addition to its role in alleviating the photoinhibition were studied in the present paper

    本文對葛仙米在中國鶴峰縣水稻田的分佈與生態學進行研究，綜述了藍藻的二氧化碳濃縮機制，並在此基礎上對葛仙米無機碳利用及其在減輕光抑制方面的作用進行了探討。
  8. As there are less such materials in loess as fossil, plants, slag, etc, which could be used for dating, luminescence dating, especially optically stimulated luminescence dating, was extensively applied to aeolian deposits, for its dating materials were minerals, such as quartz and feldspar

    由於黃土中所含的化石、木質、炭屑等適于其它方法測年的物質很少，同時，全新世黃土受年輕有機碳和無機碳的影響較大，致使全新世黃土類沉積物的測年迄今仍缺少理想方法。
  9. Standard test method for on - line monitoring of total carbon, inorganic carbon in water by ultraviolet, persulfate oxidation, and membrane conductivity detection

    通過紫外線，過硫酸鹽氧化作用，膜導電位檢測對水中總碳，無機碳在線監測的標準試驗方法
  10. Standard test method for total carbon, inorganic carbon, and organic carbon in water by ultraviolet, persulfate oxidation, and membrane conductivity detection

    用紫外線過硫酸鹽氧化物和薄膜導電率檢測法測定水中總含碳量有機碳和無機碳的標準試驗方法
  11. The spatial variability at all of soil layers was contributed to the influencing of the correlation rather than of the random

    進一步分析表明，各層次土壤無機碳和有機碳的空間變異主要是由空間自相關部分引起的，由隨機因素引起的空間變異小。
  12. As regionalized variables, the contents of sic and of soc had the characteristic of structure as well as random

    土壤無機碳和有機碳作為區域化變量，既有隨機性又有結構性。
  13. The study about carbon stored in inorganic form. especially carbonate carbon, should be highly valued in the loess plateau

    因此，在黃土高原地區必須重視對土壤碳酸鹽無機碳庫的研究。
  14. Co2 water quality - evaluation of ultimate aerobic biodegradability of organic compounds in aqueous medium - method by analysis of inorganic carbon in sealed vessels co2 headspace test

    水質水介質中有機化合物最大需氧生物降解能力的評價.密封容器中無機碳分析法
  15. Standard test method for low level determination of total carbon, inorganic carbon and organic carbon in water by ultraviolet, persulfate oxidation, and membrane conductivity detection

    通過紫外線，過硫酸鹽氧化，和膜導檢測對水中總碳，有機碳，無機碳低水平測定的標準試驗方法
  16. Spatial variability of soil inorganic carbonate carbon ( sic ) content and of soil organic carbon ( soc ) content were analyzed by geostatistics approach. the complex factors affected spatial variability of soil carbon content were preliminarily discussed the storages of sic and soc c pool were estimated in the whole watershed based on the two years located research, the storage of co2 c pool in same watershed was estimated too

    本文以磚窯溝流域為研究區域，通過對該流域62個點的取樣分析，運用地統計學方法研究了該流域土壤無機碳酸鹽碳和有機碳的空間變異性特徵，探討了影響空間變異的復雜因素，估算了流域土壤無機碳酸鹽碳庫和有機碳碳庫儲量。
  17. Co2 water quality - biological methods - evaluation of ultimate aerobic biodegradability of organic compounds in aqueous medium - method by analysis of released inorganic carbon in sealed vessels co2 headspace test - evaluation of ultimate aerobic biodegradability of organic compounds in aqueous medium - method by analysis of released inorganic carbon in sealed vessels

    水質.生物法.水介質中有機化合物最終有氧生物降解能力的評價.密封容器中釋放無機碳的分析方法
  18. Spatial structure analysis indicated that the semivanograms of sic and of soc content at different soil layer were simulated by different theoretical models and had same obvious spatial structure. their correlated distances were 1 km or so. the sic content at the layer of 20 - 40cm had the smallest correlated distance of 0. 9474km and the soc content at the layer of 10 - 20cm had the biggest correlated distance of 1. 4113km

    結構分析表明，不同層次土壤無機碳和有機碳含量可用不同的理論模型來擬合，各層次土壤無機碳和有機碳在所設計的研究尺度上均具有良好的結構性，它們的空間自相關距離大約都在1km左右， 20 - 40cm層土壤無機碳的獨立間距最小（ 0 . 9474km ） ， 10 - 20層土壤有機碳的獨立間距最大（ 1 . 4113km ） 。
  19. At the same soil layer, the sic contents on the tops of the hills were higher than those in the gullies, however, the soc contents on the tops of the hills were lower than those in the valleys. the possible factors of influence on the distribution of soil carbon were soil water content and human activities

    Kriging插值結果顯示，在同一土壤層次的不同地貌部位，土壤碳含量存在明顯差異，土壤無機碳含量是梁峁地高、溝川地低，土壤有機碳含量是溝川地高、梁峁地低。
  20. On the contrary, the valley soils had the minimum change for the profile sic content and the maximum change for the profile soc content the diversity of the soil profile carbon content change were related to their sources, movements and inversions in the soils

    在不同地貌部位的不同層次之間，無機碳含量在地勢高的梁峁地的土壤剖面上變化幅度大，有機碳含量在地勢低的溝川地的土壤剖面上變化幅度大，二者的差異主要由各自的來源、在土壤中的遷移、轉化等的不同所引起。
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