Evolution on qualities of leachate and landfill gas in the semi-aerobic landfill

To study the characteristics of stabilization in semi-aerobic landfill, large-scale simulated landfill was constructed based on the semiaerobic landfill theory. Consequently, the concentrations of chemical oxygen demand (COD), ammonia nitrogen, and nitrite nitrogen, and the pH value in leachate, as well as the component contents of landfill gas composition (methane, carbon dioxide, and oxygen) in landfill were regularly monitored for 52 weeks. The results showed that COD and ammonia concentrations declined rapidly and did not show the accumulating rule like anaerobic landfill, and remained at about 300 and 100 mg/L, respectively, after 48 weeks. Meanwhile, the descending rate reached 98.9% and 96.9%, respectively. Nitrate concentration increased rapidly after 24 weeks and fluctuated between 220–280 mg/L after 43 weeks. The pH values were below 7 during the first 8 weeks and after that leachates appeared to be alkaline. Carbon dioxide was the main composition in landfill gas and its concentration remained at a high level through the whole stabilization process. The average contents of carbon dioxide, oxygen, and methane varied between 19 vol.%–28 vol.%, 2 vol.%–8 vol.%, and 5 vol.%–13 vol.%, respectively. A relative equilibrium was reached after 48 weeks. The highest temperature in the landfill chamber could amount to 75.8 degrees centigrade.     

Geological emission of methane from the Yakela condensed oil/gas field in Talimu Basin, Xinjiang, China

A static flux chamber method was applied to study natural emissions of methane into the atmosphere in the Yakela condensed oil/gas field in Talimu Basin, Xinjiang, China. Using an online method, which couples a gas chromatography/high-temperature conversion/isotope ratio mass spectrometry (GC/C/MS) together, the 13C/12C ratios of methane in the flux chambers were measured. The results demonstrated that methane gases were liable to migrate from deep oil/gas reservoir to the surface through microseepage and p...     

模糊控制在湿法脱硫烟气系统中的应用

介绍了石灰石-石膏湿法脱硫装置烟气系统的设计情况,重点讲述了增压风机动叶的控制,针对增压风机动叶系统时滞、非线性等特点,常规PID控制效果并不理想,设计出模糊控制器,仿真后证明了理论的正确性。     

活性碳为载体的生物反应器填埋场模拟实验研究

生物反应器填埋场是一种新型的垃圾卫生填埋场,可以加速填埋场的稳定及甲烷的产生。通过模拟试验探讨了加装了活性炭载体的生物反应器填埋场在不同操作条件下的产气情况及COD,pH值、挥发性脂肪酸的变化趋势。试验证明添加活性炭做载体的反应器不仅有助于垃圾降解及渗滤液中COD。浓度的降低,而且填埋气中甲烷含量也较高;但是简单的两相型反应器却不利于甲烷气体的产生和CODCr的降解,这是由于其水解速度慢,水解反应时间长引起的。     

高炉煤气干法布袋除尘技术的应用

高炉煤气干法布袋除尘技术是钢铁行业重要的综合节能环保技术之一,以其煤气净化质量高、节水、节电、投资省、运行费用低、环境污染小等优点,优于传统的湿法洗涤除尘工艺,是国家大力推广的清洁生产技术。本文以承德钢厂1260米3高炉干法布袋除尘技术为例,介绍了该技术的工艺流程及主要参数,对设计过程中要注意的几个问题进行了分析论述,同时对该技术进一步的发展方向提出了见解,并建议国家相关部门应大力推广和使用这一技术,使其在节约能源和环境保护的建设中发挥更大作用。     

油气储运设施事故的人为因素分析与预防

结合心理学知识从人为因素的角度分析和归纳了油气储运设施事故的原因,提出了应对人为因素负面影响的措施和对策。     

川气东送管道工程建设水土流失成因与防治措施

分析了川气东送管道工程建设过程中水土流失的特点,对工程区地形地貌进行了区域划分。针对不同防治分区采取相应的防治措施即采用分层开挖、设排水沟、护坡、种树、修建拦渣墙等方式防治水土流失。同时坚持水土保持三同时制度,有效减少因本工程建设所引起的水土流失。     

土壤二维蒸气抽排去污效果的影响研究

土壤蒸气抽排是一种经济、高效、安全并已被广泛应用的污染场址现场修复技术,它能经济高效地去除非饱和带土壤中的挥发性有机污染物。以土壤和油污染物为例,进行了土壤二维抽排模拟实验,研究了气体抽排流量对去污效果的影响,通过实验可知:在增加气体抽排流量的情况下,抽排气中挥发性较强的有机物质正戊烷(C5h12)浓度下降的很快,最终保存在较低的浓度水平。挥发性一般的正辛烷(C8h18)和挥发性较弱的正癸烷(C10h22)经过长时间的抽排后,污染物也得到了降低,但是最终保持在比较高的浓度水平。得出增加气体抽排流量可以使污染物去除速率大幅度提高,从而缩短了净化时间,获得很好的去污效果。同时对二维抽排模拟实验和一维抽排模拟实验结果做了比较。     

Simulation analysis of environmental risk accident and management of high-sulfur gas field development in complex terrain

Environmental risk of high sulfur gas field exploitation has become one of the hot spots of environmental management studies. Severe gas H₂S blowout accidents in recent years have shown that poor understanding and estimates of the poisonous gas movement could lead to dangerous evacuation delays. It is important to evaluate the real concentration of H₂S, especially in complex terrain. Traditional experiential models are not valid in the case of rough terrain, especially in low-lying areas where the gas accumulates. This study, using high sulfur content gas field of Sichuan “Pu Guang gas field” as study object and adopting objective diagnosis of wind field of land following coordinate three dimensions, applied Lagrangian Puff Model and breaking up technique of puffs to simulate the H₂S diffusion condition of blowout accidents produced in the high sulfur content gas field of complex terrain area. The results showed that the H₂S distribution did not occur mainly in low wind direction, and due to the obstruction of the mountain’s body, it accumulated in front of mountain on produced turn over, flowed around submitted jumping type distribution. The mountain waist near the hilltop and low hollow river valley site rapture points simulating contrast showed that the higher the rapture point, the better the diffusing condition of pollutant, the distribution of risk sensitive point decided piping rupture environmental risk size combining the H₂S diffusion result and residential area dispersing in the study area, synthetic judge located in the high rapture point environmental risk was smaller than the low hollow point, thus it was suggested to carryout laying of lining build of equal high line of higher terrain. According to simulation results, the environmental risk management measures aimed at putting down adverse effects were worked out.     

Simulating mesoscale transport and diffusion of radioactive noble gases using the Lagrangian particle dispersion model

In order to simulate the impact of mesoscale wind fields and to assess potential capability of atmospheric Lagrangian particle dispersion model (LPDM) as an emergency response model for the decision supports, two different simulations of LPDM with the mesoscale prognostic model MM5 (Mesoscale Model ver. 5) were driven. The first simulation of radioactive noble gas ((85)Kr exponent) emitted during JCO accident occurred from 30 September to 3 October 1999 at Tokai, Japan showed that the first arriving short pulse was found in Tsukuba located at 60km away from the accidental area. However, the released radioactive noble gas was transported back to the origin site about 2 days later due to the mesoscale meteorological wind circulation, enhancing the levels of (85)Kr with the secondary peak in Tsukuba. The second simulation of atmospheric dilution factors (the ratio of concentration to the emission rate, chi/Q), during the underground nuclear test (UNT) performed by North Korea showed that high chi/Q moved to the eastward and extended toward southward in accordance with the mesoscale atmospheric circulations generated by mesoscale prognostic model MM5. In comparison with the measurements, the simulated horizontal distribution patterns of (85)Kr during the JCO are well accord with that of observation in Tsukuba such as the existence of secondary peak which is associated with the mesoscale circulations. However, the simulated level of (85)Kr anomaly was found to be significantly lower than the observations, and some interpretations on these discrepancies were described. Applications of LPDM to two mesoscale emergency response dispersion cases suggest the potential capability of LPDM to be used as a decision support model provided accurate emission rate of accident in case of a large accident.