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Temperature models for nitrification and denitrification in lake sediments

机译:湖泊沉积物中硝化和反硝化的温度模型

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During this century the Intergovernmental Panel on Climate Change (IPCC) predicts the global climate to change significantly with temperature increases of 3 to 5 ℃ in the Danish region, with highest increases in winter (Houghton et al. 2001). Changes in wind climate and hydrology and their effects on temperature and mixing regimes must be modelled to present a complete picture of consequences of climate changes. We focused on the direct effects of temperature on key process rates. In general, the rates of physical, chemical, and biological processes increase with temperature. Chemical equilibrium studies describe temperature influence on process rates as: Q_(10) = (μ_1/μ_2)~(10/(Θ_2-Θ_1)) (Van't Hoff 1884), where μ_1 and μ_2 are process rates at 2 temperatures Θ_1 and Θ_2, respectively; or by a more theoretically founded expression and introduction of an activation energy: k_T = Ae~(-E_a/RT) (Arrhenius 1889), where k_T is a rate constant at the absolute temperature T, A is a frequency factor, E_a is an activation energy, and R is the gas constant. These equations, however, are only valid over small temperature intervals. Strong deviations occur at low temperatures and especially at high temperatures, where the proteins of enzymes are denaturised. In many studies these exponential equations have been routinely applied, although careful inspections have shown a temperature dependence not statistically different from a simple linear response (Coussins & Bowler 1987, Montaignes et al. 2003).rnTo study the effect of climate changes on the nutrient metabolism in lakes we measured nitrification and denitrifi-cation rates over the temperature range 0-60 ℃ in sediment samples from Frederiksborg Castle Lake and applied a number of temperature models to the data. The most predictive model was used to describe the acclimatisation of the processes, and the model was calibrated and verified on sediments from a series of mesocosms run with various climate scenarios.
机译:在本世纪中,政府间气候变化专门委员会(IPCC)预测,随着丹麦地区温度升高3至5℃,全球气候将发生显着变化,冬季升高幅度最大(Houghton等,2001)。必须模拟风能气候和水文学的变化及其对温度和混合方式的影响,以完整呈现气候变化后果的全貌。我们关注温度对关键工艺速率的直接影响。通常,物理,化学和生物过程的速率随温度而增加。化学平衡研究将温度对工艺速率的影响描述为:Q_(10)=(μ_1/μ_2)〜(10 /(Θ_2-Θ_1))(Van't Hoff 1884),其中μ_1和μ_2是2个温度下的工艺速率Θ_1和Θ_2;或通过更理论上建立的表达式并引入活化能:k_T = Ae〜(-E_a / RT)(Arrhenius 1889),其中k_T是绝对温度T的速率常数,A是频率因子,E_a是活化能,R为气体常数。但是,这些方程式仅在较小的温度间隔内有效。在低温下,尤其是在高温下,酶的蛋白质被变性,会产生强烈的偏差。在许多研究中,这些指数方程式已被常规应用,尽管仔细检查已显示出温度依赖性与简单线性响应在统计上并无不同(Coussins&Bowler 1987,Montaignes等人,2003)。■研究气候变化对养分的影响在湖泊的新陈代谢过程中,我们测量了腓特烈堡城堡湖沉积物样品在0-60℃温度范围内的硝化和反硝化速率,并将多个温度模型应用于数据。使用最具预测性的模型来描述过程的适应性,并对该模型进行校准和验证,该模型是针对来自各种气候情景的一系列中观的沉积物进行的。

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