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首页> 外文期刊>Russian journal of physical chemistry, B. >Simulation of Suppressing Gas Formation during Deactivation of Gas-Generating Soils
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Simulation of Suppressing Gas Formation during Deactivation of Gas-Generating Soils

机译:燃气发电土失活期间抑制气体形成的仿真

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Studies on simulation of suppressing gas formation during deactivation of gas-generating soils (GGS) by their chemical and biological treatment under anaerobic conditions are carried out. The chemical and gas-geochemical characteristics of GGS sampled from the wells drilled at different depths within in the construction site area (Moscow, North-Eastern Administrative Okrug) are examined. Simulation of an anaerobic gas-generating process has shown that the gas generation rate under conditions of natural occurrence (8–10°C) within the boundaries of the identified anomalous zones would be ~215 L/(t year) in the center and ~157 L/(t year) in the north of the site. The kinetics of organic matter degradation has revealed that the degradation rate constants of gas-forming substrates amount to 0.013 year–1 for the central zone and 0.009 year–1 for the northern zone. According to the prediction results, the main gas-generating phase will be complete within 55 years in the central zone and within 79 years in the northern one; the volume content of methane in gas production being equal to 9–12%. Simulation of chemical suppressing residual gas generation has shown that for the reduction of gas generation intensity by a factor of 10, it is sufficient to add a 45% calcium hypochlorite solution in the amount of 1% of the soil volume to the GGS massif lying in the central anomalous zone. Gas generation in soils varies from 1.6 to 35 L/(t year) after chemical treatment i.e., the process of gas generation in filled-in soils will in fact be suppressed almost completely. Simulation of a biological process of suppressing gas-generation in GGS of the northern zone caused by the presence of oil pollution made it possible to predict that the use of the certified preparation Rhoder at a dose of 1 × 109 CFU/mL will allow increasing sufficiently a degradation rate constant of hydrocarbons to 1.02 year–1 and reducing the time of their half-lifetime from 79 years to 0.68 years.
机译:通过其化学和生物处理在厌氧条件下造成气体产生土壤(GGS)抑制气体形成模拟的研究。检查了从施工现场区域(莫斯科,东北行政Okrug)不同深度钻井的GGS的化学和气体地球化学特征。厌氧气体产生过程的模拟表明,在所识别的异常区域的边界内的自然发生(8-10°C)的条件下的气体产生率将是中心〜215升/(吨)和〜 157 L /(T年)在网站北部。有机质降解的动力学表明,北方地区的气体形成基材的降解速率常数为0.013岁-1〜0.009年1。根据预测结果,主要的气体发电阶段将在中央区55年内完成,北方北部79年内;气体生产中甲烷的体积含量等于9-12%。化学抑制残余气体产生的模拟表明,为了减少气体产生强度10倍,加入45%次氯酸钙溶液,其中1%的土壤体积的含量为1%的土壤体积,以至于GGS Massif中央异常区。在化学处理之后,土壤中的气体产生从1.6〜35升/(吨/吨)不同,即,填充土壤中的气体生成过程实际上将近地抑制。模拟抑制由油污的存在引起的北方地区GGS中生气发电的生物过程使得可以预测使用1×109 CFU / mL剂量的经认证的制剂ρOder将允许充分增加烃的降解速率常数为1.02年-1,并将半寿命的时间从79年减少到0.68岁。

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