测定高氯废水CODcr的方法探讨——硫酸汞添加法

化学需氧量是评价水体中有机物污染的重要指标,通常采用CODcr来表示。在其测定过程中氯离子是影响结果准确性的重要因素。由于氯离子的干扰,高氯废水中化学需氧量测定误差较大,尤其对于高氯低化学需氧量的水样,其干扰更为严重。本文对高氯废水化学需氧量的测定方法以及原理进行了阐述,针对不同范围的化学需氧量,对应采用高浓度重铬酸钾氧化法、低浓度重铬酸钾氧化法来测定,最终确定了一种最直接、简便、准确的方法-硫酸汞添加法来测定高氯废水的CODcr。     

软锰矿改性污泥活性炭对Cu~(2+)吸附特性的研究

文章对比研究了污泥活性炭(AC)和1%软锰矿改性的污泥活性炭(ACP)对溶液中Cu2+的吸附特性,考察了时间、pH值和吸附剂投加量等因素对吸附反应的影响。结果表明:室温下,180 min后Cu2+吸附达到平衡,pH=4.8时吸附效果最优;伪二阶动力学方程和Langmuir吸附等温方程能很好地拟合两种污泥活性炭的吸附反应。通过计算,室温下,改性前后的污泥活性炭Langmuir模型的饱和吸附量Qm分别是78.13 mg/g和94.34 mg/g。在初始浓度200 mg/L,pH=5,吸附剂投加量为2g/L时,1%软锰矿改性的污泥活性炭对Cu2+的最大吸附量为90.15 mg/g,比未改性时提高了23.33%。     

微生物燃料电池利用甘薯燃料乙醇废水产电的研究

利用空气阴极微生物燃料电池(MFC)处理甘薯燃料乙醇废水,以COD为5000mg/L的废水做底物,获得的最大电功率密度为334.1mW/m2,库仑效率(CE)为10.1%,COD去除率为92.2%.实验进一步考察了磷酸缓冲液(PBS)浓度和废水浓度对MFC产电性能的影响.PBS含量从50mmol/L增加到200mmol/L,MFC输出的最大电功率密度提高了33.4%,CE增加26.0%,但PBS对废水的COD去除率影响不大.含50mmol/LPBS的废水COD从625mg/L增加到10000mg/L,COD去除率和MFC输出的最大电功率密度在废水浓度为5000mg/L处均获得最大值,但CE值有降低的趋势,从28.9%变化至10.3%.这些结果表明,MFC可以在处理甘薯燃料乙醇废水的同时获得电能;增大PBS浓度能提高MFC的产电性能;MFC输出的最大电功率密度随废水COD增加而增大,但废水浓度过高会引起酸化使MFC产电性能下降.     

甲烷氧化菌在填埋场覆盖层的工程应用 (Ⅰ):分离与筛选

选取了湖泊底泥、矿化垃圾、覆盖土和好氧污泥4种填埋场周边易得基质为分离源,采用驯化、传代培养、甲烷氧化能力及适应性等方法进行了适合于填埋场覆盖层应用的甲烷氧化菌的筛选研究.结果表明,从好氧污泥中分离得到的甲烷氧化菌较其它分离源得到的甲烷氧化菌具有更高的甲烷氧化活性(2461.29μg·h-1·g-1,以每g干污泥每小时氧化的CH4量(μg)计,下同)和甲烷氧化速率增幅(1045.56μg·h-1·g-1,以每g干污泥每小时氧化的CH4量(μg)计,下同),接种后能显著提高覆盖材料的甲烷氧化能力(p0.05),且不受CH4浓度的抑制.源自好氧污泥的甲烷氧化菌具有生长迟滞期短、生长速率高等特点,对填埋场的甲烷削减更具适应性,有利于工程扩大应用.     

广西罗城地质公园地质遗迹特征及综合评价

广西罗城国家地质公园地质遗迹资源十分丰富,以典型壮美的喀斯特地貌景观和水体景观为主,辅以地质剖面遗迹景观和地质构造遗迹景观等.介绍了罗城地质公园内的地质遗迹类型及其分布,并从科学价值、科普价值、美学价值、旅游开发价值四个方面对其进行了综合评价.     

110千伏变电站常用噪声控制方案的分析与研究

阐述了110千伏变电站噪声环境影响的现状,全面列举了变电站的主要噪声源并分析其分布规律及噪声影响特点.针对各类声源的特点,结合变电站设计、施工、运行维护三个主要阶段,全过程分析了常用的变电站噪声控制方案及其效果,重点关注了有源消声技术的应用和排风扇噪声影响的问题.对常用噪声控制方案的分析与研究,旨在寻求最经济、最有效的110千伏变电站噪声控制方案.     

山西省低碳城镇化的发展路径

低碳城镇化是新型城镇化建设的重要内容。本文从分析山西省城镇化特征入手,梳理了城镇化中的高碳问题,针对山西省的发展阶段和特征,提出发展低碳经济、实施低碳规划、推行绿色交通和建筑、倡导低碳生活等低碳城镇化的路径选择。     

Resolving the influence of nitrogen abundances on sediment organic matter in macrophyte-dominated lakes, using fluorescence spectroscopy

A controlled experiment was designed to resolve the influence of nitrogen abundance on sediment organic matters in macrophyte-dominated lakes using fluorescence analysis. Macrophyte biomass showed coincident growth trends with time, but different variation rates with nitrogen treatment. All plant growth indexes with nitrogen addition (N, NH₄Cl 100, 200, 400 mg/kg, respectively) were lower than those of the control group. Four humiclike components, two autochthonous tryptophan-like components, and one autochthonous tyrosine-like component were identified using the parallel factor analysis model. The results suggested that the relative component changes of fluorescence in the colonized sediments were in direct relation to the change of root biomass with time. In the experiment, the root formation parameters of the plants studied were significantly affected by adding N in sediments, whichmay be related to the reason that the root growthwas affected byNaddition. Adding a low concentration of N to sediments can play a part in supplying nutrients to the plants. However, the intensive uptake of NH₄⁺ may result in an increase in the intracellular concentration of ammonia, which is highly toxic to the plant cells. Hence, our experiment results manifested that organic matter cycling in the macrophyte-dominated sediment was influenced by nitrogen enrichment through influencing vegetation and relevant microbial activity.     

Sources and characteristics of fine particles over the Yellow Sea and Bohai Sea using online single particle aerosol mass spectrometer

Marine aerosols over the East China Seas are heavily polluted by continental sources. During the Chinese Comprehensive Ocean Experiment in November 2012, size and mass spectra of individual atmospheric particles in the size range from 0.2 to 2.0 μm weremeasured onboardby a single particle aerosol mass spectrometer (SPAMS). The average hourly particle number (PN) was around 4560 ± 3240 in the South Yellow Sea (SYS), 2900 ± 3970 in the North Yellow Sea (NYS), and 1700 ± 2220 in the Bohai Sea (BS). PN in NYS and BS varied greatly over 3 orders of magnitude, while that in SYS varied slightly. The size distributions were fitted with two log-normal modes. Accumulation mode dominated in NYS and BS, especially during episodic periods. Coarse mode particles played an important role in SYS. Particles were classified using an adaptive resonance theory based neural network algorithm (ART-2a). Six particle types were identified with secondary-containing, aged sea-salt, soot-like, biomass burning, fresh sea-salt, and lead-containing particles accounting for 32%, 21%, 18%, 16%, 4%, and 3% of total PN, respectively. Aerosols in BS were relatively enriched in particles from anthropogenic sources compared to SYS, probably due to emissions from more developed upwind regions and indicating stronger influence of continental outflowonmarine environment. Variation of source types dependedmainly on origins of transported air masses. This study examined rapid changes in PN, size distribution and source types of fine particles in marine atmospheres. It also demonstrated the effectiveness of high-time-resolution source apportionment by ART-2a.     

Resolving the influence of nitrogen abundances on sediment organic matter in macrophyte-dominated lakes,using fluorescence spectroscopy

A controlled experiment was designed to resolve the influence of nitrogen abundance on sediment organic matters in macrophyte-dominated lakes using fluorescence analysis.Macrophyte biomass showed coincident growth trends with time, but different variation rates with nitrogen treatment. All plant growth indexes with nitrogen addition(N, NH4Cl100, 200, 400 mg/kg, respectively) were lower than those of the control group. Four humiclike components, two autochthonous tryptophan-like components, and one autochthonous tyrosine-like component were identified using the parallel factor analysis model. The results suggested that the relative component changes of fluorescence in the colonized sediments were in direct relation to the change of root biomass with time. In the experiment, the root formation parameters of the plants studied were significantly affected by adding N in sediments, which may be related to the reason that the root growth was affected by N addition.Adding a low concentration of N to sediments can play a part in supplying nutrients to the plants. However, the intensive uptake of NH4+may result in an increase in the intracellular concentration of ammonia, which is highly toxic to the plant cells. Hence, our experiment results manifested that organic matter cycling in the macrophyte-dominated sediment was influenced by nitrogen enrichment through influencing vegetation and relevant microbial activity.