污泥处理处置技术的现状与探讨

污泥的处理处置是一项关系民生的社会化工程,由于前些年对污泥处理的忽视,导致污泥引起的环境问题愈来愈严重。对现阶段污泥常用处理处置的各种工艺与方法进行梳理和总结,同时对各种工艺及处理措施技术的优劣进行了探讨。     

Sources of nitrous and nitric oxides in paddy soils：Nitrification and denitrification

Rice-paddies are regarded as one of the main agricultural sources of N 2O and NO emissions. To date, however, specific N2O and NO production pathways are poorly understood in paddy soils. ^15N-tracing experiments were carded out to investigate the processes responsible for N2O and NO production in two paddy soils with substantially different soil properties. Laboratory incubation experiments were carried out under aerobic conditions at moisture contents corresponding to 60% of water holding capacity. The relative importance of nitrification and denitrification to the flux of NaO was quantified by periodically measuring and comparing the enrichments of the N2O, NH~-N and NO3-N pools. The results showed that both N2O and NO emission rates in an alkaline paddy soil with clayey texture were substantially higher than those in a neutral paddy soil with silty loamy texture. In accordance with most published results, the ammonium N pool was the main source of N2O emission across the soil profiles of the two paddy soils, being responsible for 59.7% to 97.7% of total N2O emissions. The NO3-N pool of N2O emission was relatively less important under the given aerobic conditions. The rates of N2O emission from nitrification （N2On） among different soil layers were significantly different, which could be attributed to both the differences in gross N nitrification rates and to the ratios of nitrified N emitted as NzO among soil layers. Furthermore, NO fluxes were positively correlated with the changes in gross nitrification rates and the ratios of NO/N2O in the two paddy soils were always greater than one （from 1.26 to 6.47）. We therefore deduce that, similar to N2O, nitrification was also the dominant source of NO in the tested paddy soils at water contents below 60% water holding capacity.     

Dry deposition of PM10 over the Yellow Sea during Asian dust events from 2001 to 2007

Dry deposition velocities and fluxes of PM10during Asian dust events over the Yellow Sea from 2001 to 2007 were investigated using observation data in Qingdao, China and Jeju, Korea. The dry deposition velocities of PM10 during dust events over the Yellow Sea ranged from 0.19 to 8.17 cm/sec, with an average of 3.38 cm/sec. Dry deposition fluxes of PM10during dust events over the Yellow Sea were in the range of 68.5–2647.1 mg/(m2·day), with an average of 545.4 mg/(m2·day), which is 2–10 times higher than those reported by other studies for both dust and non-dust periods. It was estimated that 2.6 × 1011–48.7 × 1011g dust particles deposit to the Yellow Sea during dust events through dry deposition every year. Compared with the results in previous studies, it was found that the dry deposition of PM10over the Yellow Sea during dust events in the years with high frequency of dust could account for a large or overwhelming fraction of the annual total dry deposition. Backward air mass trajectory analysis showed that dust events influenced Jeju mainly originated from the desert regions located in Mongolia and Inner Mongolia, China. There were 119 backward trajectories influenced both Qingdao and Jeju during 15 dust events from 2001 to 2007, accounting for 61.3% of the total trajectories of 194, indicating that Qingdao and Jeju were usually on the same pathway of dust transport downwind from source areas.     

岩溶区地下水补给型水库表层无机碳时空变化特征及影响因素

为更深入地认识岩溶区地下水补给型水库表层无机碳的循环过程,于2014-07-12~2014-07-20期间,以广西上林县大龙洞岩溶水库表层水体为研究体系,对无机碳循环研究的重要指标进行定点观测和高密度的昼夜监测.结果发现:1从上游到下游DIC含量和水体p CO2值逐渐增加[DIC(平均):122.88 mg·L-1增至172.02 mg·L-1,p CO2(平均):637.91×10-6增至1 399.97×10-6],δ13CDIC值逐渐偏负[δ13CDIC(平均):-4.34‰降至-6.97‰].2库区均为大气CO2的源,CO2交换通量在7.11~335.54 mg·(m2·h)-1之间,平均125.03 mg·(m2·h)-1,上游和下游地区CO2交换通量较大[平均131.73 mg·(m2·h)-1、170.25 mg·(m2·h)-1],中游狭窄地区CO2交换通量较小[平均116.05 mg·(m2·h)-1].3表层水体p CO2值和水-气界面CO2交换通量存在晚上升高,白天降低的昼夜变化规律,且与叶绿素a(Chla)呈负相关关系.分析认为:1大龙洞水库表层水体DIC含量、δ13CDIC值和水体p CO2的空间分布主要受浮游植物浓度、浊度、电导率、水深、透明度等的影响,而水-气界面CO2交换通量除了受浮游植物浓度空间变化的影响外还受风速的影响.2浮游植物昼夜垂向运动及光合作用和呼吸作用昼夜变化控制着水库表层水体溶解性无机碳的昼夜循环过程.     

硫氧同位素示踪南京北郊大气PM2.5中硫酸盐来源

采用EA-IRMS联用技术对2014年1月南京北郊大气细粒子(PM2.5)中硫酸盐的硫和氧同位素组成进行了分析,结合大气颗粒物化学组成,追溯南京北郊大气PM2.5中硫酸盐的来源,并评估了各污染源的贡献率.结果表明,2014年1月南京北郊硫酸盐气溶胶的硫同位素组成(δ34S)范围为2.7‰~6.4‰,平均值为5.0‰±0.9‰(n=16);氧同位素组成(δ18O)值范围为10.6‰~16.1‰,平均值为12.5‰±1.37‰(n=16).通过气溶胶与可能污染源的δ34S值对比和后向轨迹分析,得出结论:研究区域大气中硫同位素组成主要受当地燃煤中硫的影响,其次是远距离传输硫.此外,有低δ34S值硫源存在,但贡献比较小,可能来自生物成因硫.绝对主因子分析结果显示:人为成因硫和远距离传输硫贡献率分别为46.74%和31.54%.     

硫氮沉降下西北荒漠煤矿区周边土壤性质的变化特点

近年来中国大部分区域大气硫、氮沉降速率趋于平稳甚至下降,但西北地区煤炭行业的快速发展使得硫、氮沉降速率加快.燃煤电厂作为酸前体物的主要排放源之一,在其周围开展硫、氮沉降效应研究,可为合理评价煤矿区大气污染物控制措施的实施效果提供数据支撑.该文以宁东能源化工基地3个燃煤电厂为采样点,研究了电厂周围土壤化学和生物学性质的变...     

新农药硫肟醚在土壤中降解的影响因子研究

在实验室条件下对新农药硫肟醚(O(3苯氧苄基)2甲硫基1(4氯苯基)丙基酮肟醚)在土壤中降解的影响因子进行了研究.结果表明,在20 d的培养时间内,随着土壤含水量的增加,硫肟醚的降解速率加快.当土壤含水量增加到80%(质量分数)时,其降解率达到最大(46.73%),然后随土壤含水量增加反而下降.随着土壤温度的升高,硫肟醚在土壤中的降解速率增加.30 ℃时降解速率达到最大(47.83%),以后温度继续升高,其降解速率呈现出下降趋势.在5～100 mg/kg的质量比范围内硫肟醚在土壤中的降解速率随其质量比的增加而提高;但当质量比继续增加时,硫肟醚的降解速率表现出下降趋势.硫肟醚在土壤中的降解遵循一级动力学方程,其在非灭菌与灭菌土壤中的降解速率常数k分别为8.106×10-3和1.63×10-3;半衰期分别为85.5 d和425.2 d.微生物对硫肟醚在土壤中的降解具有显著的影响.     

高硫酸盐难降解废水高温厌氧处理中限量曝气的应用及影响

由于硫酸盐还原的影响,普通高温UASB反应器处理亚硫酸盐纸浆厂排出的高硫酸盐难降解废水过程中甲烷菌活性受到了严重抑制.考虑到空气对硫化氢的吹脱和对硫化物的氧化作用可能减轻硫化物对甲烷菌的抑制,本研究在厌氧反应器中引入限量曝气措施.试验结果表明,反应器的运行稳定性和处理能力均得到大幅提高.在有机负荷提高到原来2倍的情况下,曝气后COD去除率仍有提高,从40%～50%提高到60%～70%.试验证明部分甲烷菌可以耐氧,而某些种类的水解酸化细菌则对不完全厌氧环境比较敏感.     

赴兰州炼油厂、克拉玛依炼油厂进行高硫高酸原油加工管理情况的考察

2004年10月16-24日,齐鲁石化公司炼油厂组织了考察组,赴兰州炼油厂、克拉玛依炼油厂进行了高硫高酸原油腐蚀防护及管理控制情况的考察.考察期间,分别与两厂的技术、机动、安全环保、防腐研究所、生产车间等各部门进行了技术交流,并参观了装置现场.两厂整洁有序的现场管理面貌和以员工为本的管理风格给我们留下深刻的印象.     

气态硫闪爆事故原因分析及对策

对处理硫磺回收装置高温掺合阀故障时发生的硫闪爆事故进行了分析,提出了相应的对策.