典型进口含铜原料熔炼烟气中重金属的释放特性

为了解我国进口含铜原料熔炼烟气中重金属的释放特性,以近年进口申报的铜精矿、铜锍、铜转炉渣和含铜污泥4种典型含铜原料为研究对象,通过高温管式炉模拟研究不同含铜物料、熔炼温度、熔剂添加比例等条件下,熔炼烟气中重金属的释放特性。结果表明,4种进口含铜原料熔炼烟气中As、Pb质量分数较高,进口铜精矿和含铜污泥熔炼烟气重金属质量分数高于进口铜锍和铜转炉渣;熔炼温度从1 000 ℃升至1 300 ℃时,铜精矿和铜锍熔炼烟气中Zn、Cu、As、Pb等重金属的质量分数随着温度的升高而增加,Mn的质量分数随温度升高变化不大;熔剂添加比例由0增至18%时,铜精矿熔炼烟气中Zn、As的质量分数分别降低了28%、44%,Mn、Cu和Pb质量分数变化不大,进口铜锍熔炼烟气中Zn质量分数减少了85.2%,As的质量分数则随熔剂添加比例的增加而增加。本研究结果可为进口含铜原料熔炼烟气中重金属减排提供参考。     

沼气增温与控制系统的设计与仿真

冬季北方寒冷地区温度偏低,难以满足大中型沼气厌氧发酵系统对于温度的要求。为了解决该问题,针对天津地区某奶牛场沼气工程,设计了一套回收发电机余热并辅助电加热为发酵罐体供热的沼气增温控制系统,且实验确定最佳控制温度为35℃。在该系统中,罐体内部均匀布置竖直型循环加热管路,从而使料液温度分布更加均匀,热响应更加迅速,6 d左右即可将发酵罐内发酵料液提升到所需最佳温度;另外,采用罐内部温度及循环水流量的反馈调节,使料液的温度波动维持在±1℃范围内,解决了在冬季由于温度过低而导致沼气产气率偏低、甚至停滞的问题;同时,采用MATLAB软件对基于F-PID及传统PID的温度控制系统进行了仿真。对比结果表明,F-PID控制器较传统PID控制器超调量减小3℃,响应时间缩短60%,表明F-PID系统具有更高的效率、稳定性及实用价值。     

海水微絮凝预处理对超滤膜通量的影响

以聚合氯化铁为絮凝剂,研究了海水微絮凝预处理过程的絮凝特征以及对超滤膜通量的影响。考察了微絮凝对海水中有机物的去除作用,并采用体系稳定动力学参数、絮凝指数评价不同絮凝剂投加量在海水中的絮凝效果,探讨了微絮凝对超滤膜污染的改善作用。实验结果表明,微絮凝预处理能强化超滤膜对海水UV254的去除效果,与超滤相比提高了27.5%,可有效去除海水中的蛋白类有机物。超滤膜直接过滤海水可造成膜通量严重下降,采用微絮凝作为预处理能有效减缓超滤膜污染,且减缓效果与絮凝剂的投加量密切相关,当PFC的投加量为40 mg·L-1时,膜比通量J/J0值大于0.9。     

北方地区农村清洁取暖技术适用性评价—以北京为例

为了切实改善区域大气环境质量,中国在北方地区大规模开展以煤改电、煤改气为主的农村清洁取暖改造工程,如何选择技术可行、经济上可接受的清洁取暖技术路径是清洁取暖改造可持续的关键问题。基于北京农村地区实地调研数据,从经济性和舒适性2个维度对4种农村清洁取暖技术进行适用性评价,总结出各种技术的适用条件,提出农村清洁取暖技术路径选择建议。结果表明：空气源热泵运行费用较低,舒适性较好,适合冬季温度不低于−20 ℃的各类区域;燃气壁挂炉运行费用略高于空气源热泵,舒适性较好,适合距离燃气管线或燃气站较近的平原、半山区地区,不同气候温度范围均适用;蓄能式电暖器运行费用较高,舒适性较差,适合冬季温度接近于城区的农村或城乡接合部、农宅面积较小的区域;地源热泵取暖最好结合政府资金支持项目实施,运行费用较低,舒适性较好,适合地质结构适宜建井,有足够空间进行地埋管的区域。建议农村清洁取暖工作立足长远,因地制宜地选择清洁取暖技术,着力降低农户清洁取暖运行成本,同时提高农村清洁取暖电力和天然气供应的可靠性。

     

The Water Fluxes of the Yellow River to the Sea in the Past 50 Years, in Response to Climate Change and Human Activities

Since the 1970s, the water fluxes to the sea of the Yellow River have declined significantly. Based on data of precipitation, air temperature, the measured and “natural” river flow, the water diversion and consumption, and the areas of erosion and sediment control measures over the drainage basin, water fluxes to the sea of the Yellow River are studied in relation with the influences of changing climate and human activities. The Yellow River basin can be divided into different water source areas; multiple regression indicates that the variation in precipitation over different water source areas has different effect on water fluxes to the sea. In the period between 1970 and 1997, averaged air temperature over the whole Yellow River increased by about 1.0°C, from 16.5°C to 17.5°C, a factor that is negatively correlated with the water yield of the Yellow River. Water diversion and consumption has sharply increased and resulted in a significant decline in the water fluxes to the sea. Since the 1960s, erosion and sediment control measures have been practiced over the drainage basin. This factor, to a lesser degree, is also responsible for the decrease in water fluxes to the sea. A multiple regression equation has been established to estimate the change in water fluxes to the sea caused by the changes in precipitation, air temperature, water diversion and consumption, erosion, and sediment control measures, indicating that the contribution of water diversion and consumption to the variation in annual water flux to the sea is 41.3%, that of precipitation is 40.8%, that of temperature is 11.4%, and that of erosion and sediment control measures is 6.5%.     

Carbonyl sulfide and dimethyl sulfide fluxes in an urban lawn and adjacent bare soil in Guangzhou, China

Carbonyl sulfide (COS) and dimethyl sulfide (DMS) fluxes from an urban Cynodon dactylon lawn and adjacent bare soil were measured during April–July 2005 in Guangzhou, China. Both the lawn and bare soil acted as sinks for COS and sources for DMS. The mean fluxes of COS and DMS in the lawn (–19.27 and 18.16 pmol/(m2 sec), respectively) were significantly higher than those in the bare soil (–9.89 and 9.35 pmol/(m2 sec), respectively). Fluxes of COS and DMS in mowed lawn were also higher than those in bare soils. Both COS and DMS fluxes showed diurnal variation with detectable but much lower values in the nighttime than in the daytime. COS fluxes were related significantly to temperature and the optimal temperature for COS uptake was 29°C. While positive linear correlations were found between DMS fluxes and temperature. COS fluxes increased linearly with ambient COS mixing ratios, and had a compensation point of 336 ppt.     

长白山温带森林挥发性有机物的排放通量

2010年夏季,在长白山温带森林开展了挥发性有机物(VOC)排放通量以及气象参数、PAR的综合测量.VOC排放通量采用松弛涡度积累(RelaxedEddyAccumulation)技术在森林冠层上进行测量.初步发现长白山阔叶林主要排放α-蒎烯、β-蒎烯、莰烯、香桧烯、月桂烯、蒈烯、柠檬烯、罗勒烯、松油烯、繖花烃、萜品油烯、三环烯等.研究表明,长白山阔叶混交林VOC排放有明显的日变化——早晚较低和中午前后较高.2010年夏季,单萜烯总排放通量的平均值为0.242mg·m·h-2-1,其变化范围为0.005～1.668mg·m·h-2-1;各成分排放通量的平均值(和最大值)分别为α-蒎烯0.072(0.234)、莰烯0.028(0.356)、月桂烯0.027(0.433)、蒈烯0.023(0.173)、柠檬烯0.037(0.197)、罗勒烯0.016(0.168)、萜品油烯0.053(0.320)、繖花烃0.067(0.755)mg·m·h-2-1.研究还发现VOC排放通量与气温之间存在一定的联系.     

地膜覆盖对稻-油轮作农田温室气体排放的影响

以位于西南大学农业部重庆紫色土生态环境重点野外科学观测试验站内的稻-油轮作为研究对象,采用静态箱/气相色谱法,对覆膜和对照(不覆膜)处理下稻油轮作CO2、CH4和N2O排放特征进行了为期1 a的原位观测.结果表明,稻-油轮作农田CO_2、CH_4和N_2O排放通量均呈现出明显的季节变化,且2种处理下这3种温室气体的季节变化模式相似.覆膜处理下稻-油轮作农田全年CH_4排放量为(46. 14±13. 40) kg·hm~(-2),相比于对照处理下的(18. 61±2. 05) kg·hm~(-2),提高了147. 93%(P 0. 05),但覆膜对CO_2和N_2O的排放影响并不显著,覆膜及对照处理下CO2年排放量分别是(-47. 54±2. 11) t·hm~(-2)和(-47. 60±2. 19) t·hm~(-2),N2O年排放量分别是(18. 94±4. 74) kg·hm~(-2)和(23. 14±3. 68) kg·hm~(-2).覆膜和对照处理下GWP值分别为-41. 16 t·hm~(-2)和-40. 95 t·hm~(-2),表现为大气温室气体的吸收汇,但差异并不显著.     

松散煤体渗流传热试验装置研制

为研究松散煤体低温氧化及通风供氧下的渗流传热规律,研发了渗流传热试验装置。试验装置由气体加湿系统、气体加热系统、煤样反应系统、数据采集系统和安全保护系统组成;本装置可实现自动加湿、控温、自动采集数据及处理数据。为解决装置使用和运行中的安全问题,设计了断电保护、有害气体检测等措施,保障试验装置的安全、可靠。     

基于热湿交换理论的巷道风流温、湿度影响因素研究

为了研究巷道风流参数的影响因素、预测风流温湿度的变化规律,结合热湿交换理论,建立了风流与围岩壁面之间热湿交换的数学模型,以及贴体坐标系下围岩内部温度场的导热微分方程;利用数值方法,将围岩内部的导热问题与影响风流参数变化的热湿交换问题耦合起来,并以大柳塔煤矿52505综采工作面为例进行计算,得到了与实测参数较为一致的模拟结果,验证了该数值方法的有效性。研究结果表明:风流温度受原始岩温、入风流温度、局部热源强度等因素的影响,风流相对湿度与入风流温、湿度以及井下湿源的数量和强度有关;巷道壁温作为将围岩温度场与风流参数之间关联起来的主要因素,对模拟结果影响较大,其数值取决于壁面与风流之间热湿交换以及围岩原始岩温。