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Trần Trung Đức

@lonhoc0812
  • Việt Nam
  • Theo dõi 0
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  • 05/11/15 08:25:59
    Dịch đúng nghĩa kỹ thuật là sao ạ
    the role of soil microbial biomass must be taken into consideration in any attempt to assess nutrient and energy transfer within soil system.
  • Ai dịch đoạn này cho em với , em dịch mãi mà cũng không hay được
    The importance of organic carbon estimation lies inthe fact that it gives an indication of the organic matter content of the soil which is an important index of soil fertility. The organic carbon content of soil, is reported directly as percentage of C or calculated as organic matter by multiplication with a factor of 1.724 assuming that soil organic matter contains on an average 58 percent carbon, so that 100/58 = 1.724. There...
    Ai dịch đoạn này cho em với , em dịch mãi mà cũng không hay được
    The importance of organic carbon estimation lies inthe fact that it gives an indication of the organic matter content of the soil which is an important index of soil fertility. The organic carbon content of soil, is reported directly as percentage of C or calculated as organic matter by multiplication with a factor of 1.724 assuming that soil organic matter contains on an average 58 percent carbon, so that 100/58 = 1.724. There is also a close relationship between organic carbon and nitrogen content of the soil (C : N ratio). For organic carbon determination dry combustion and wet digestion methods are used. The former is useful for very accurate purposes since absolute values are obtained, while for routine work Walkley-Black rapid titration method (wet combustion) is extremely useful. Soil organic carbon is oxidized to C02 in presence of an excess of oxidizing agent such as a mixture of potassium dichromate and sulphuric acid. It is actually the chromic acid formed by the action of potassium dichromate and sulphuric acid which oxidizes the carbon. The excess of dichromate is determined by blank titration with ferrous ammonium sulphate (redox titration). The Walkley Black procedure uses the heat of dilution of sulphuric acid to provide the temperature required. However, this does not enable the dichromate to oxidize all the organically bound carbon. An empirical recovery factor of 0.77 was used by the original authors

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    • Banycol
      1 · 05/11/15 10:46:42
    • Trần Trung Đức
      0 · 05/11/15 07:15:34
  • ai dịch giùm em đoạn này với ạ
    Standard certified buffer tablets are available for a whole range of pH-values and these are most convenient. One tablet dissolved in a specified amount of water, usually 100cc provides a solution of known pH to within about 0.02 of a unit. Buffer tablets of pH 4.0, 7.0 and 9.2 are mostly used now a days for instrument calibration. For 1(N) KCl :Analytical Grade salt is used.
    • Sáu que Tre
      0 · 04/11/15 08:20:06
    • Trần Trung Đức
      0 · 04/11/15 05:50:43
  • giúp mình dịch đoạn này với
    The soil is extracted with a normal ammonium acetate, atljusted to pH = 4.8. Extractable AI in the extract is treated with colour developing aluminon reagent (dilute solution of aurine tri-carboxylic acid) in presence of thioglycollic acid to eliminate the interference of Fe. The intensity of the coloured complex, formed a high temperature is measured colorimetrically at a wavelength of 535 nm. The estimation of extractable acidity or more precisely, extractable AI...
    giúp mình dịch đoạn này với
    The soil is extracted with a normal ammonium acetate, atljusted to pH = 4.8. Extractable AI in the extract is treated with colour developing aluminon reagent (dilute solution of aurine tri-carboxylic acid) in presence of thioglycollic acid to eliminate the interference of Fe. The intensity of the coloured complex, formed a high temperature is measured colorimetrically at a wavelength of 535 nm. The estimation of extractable acidity or more precisely, extractable AI is an useful index of weathering status of soils and minerals. Extractable aluminium includes exchangeable aluminium plus soluble aluminium hydroxide and probably some hydroxy al­ monomers and polymers which perhaps remain strongly adsorbed in the colloidal complex or trapped between the expansible silicate layers of the clay (non-exchangeable AI).
    Reagents
    • Normal ammonium acetate adjusted to pH 8.2 ; Add 58 ml of glacial acetic acid to about 400ml of water in one litre volumetric flask. To it add 70ml of concentrated NH40H through a funnel that extends into the acid and dilute the contents to volume with distilled water. Mix the solution and transfer it to a 2 litre beaker. Adjust the
    solution pH at 4.8 with 1(N) CH3COOH (approximately 1litre CH3COOH will be required). Mix the contents and keep the solution into a storage flask.

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