粉煤灰对阴离子水溶性混合染料的吸附动力学

以燃煤废弃物粉煤灰作为吸附剂,对活性红23与活性蓝4、活性黄4、酸性黑1、酸性蓝193的混合染料溶液进行吸附性能研究.结果表明,在不同的混合体系中,活性红23的脱色率基本保持在60%~70%;体系中酸性染料的脱色率均超过90%;活性蓝4的脱色率高达85%;活性黄4的脱色率仅为50%.准二级吸附动力学能够更好地描述粉煤灰对水溶性混合染料的吸附过程.染料在溶液中的外扩散系数均为10-4cm·s-1数量级,染料在粉煤灰颗粒的内扩散系数为10-8cm2·s-1数量级.根据BN数,水溶性染料在粉煤灰上的竞争吸附是外扩散控制的吸附过程.     

疏勒河上游地表水水化学主离子特征及其控制因素

在系统收集了疏勒河流域上游河水、地下水、降水和冰雪融水水样的基础上,综合运用描述性统计、Gibbs图和Piper阴阳离子三角图等方法,对疏勒河上游地表水中主离子组成特征及其控制因素进行了分析.结果表明,流域内不同水体(大气降水、河水和地下水)之间的主离子组成以及水化学类型差异显著.河水TDS的变化范围为51.7~432.3 mg·L-1,平均值为177.7 mg·L-1;河水中阳离子Ca2+、Mg2+的百分比为45%和31%,优势阴离子为HCO-3,占阴离子总量的75%,河水的水化学类型主要为HCO-3-Ca2+-Mg2+型;河水中主离子浓度值介于大气降水和地下水之间,并且十分接近地下水浓度,说明地表水同时受大气降水和地下水补给并主要依靠地下水补给;地表水样品的水化学组成落在Gibbs分布模型的中翼偏左端,表明研究区的水化学离子组成受到岩石风化作用和蒸发结晶作用的共同影响,且岩石风化作用对水化学离子组成的影响更加显著.     

活性炭负载铁催化过硫酸盐降解酸性大红3R

采用浸渍-高温煅烧法制备负载型的Fe/活性炭催化剂,利用电镜扫描(SEM)、X射线衍射(XRD)对催化剂进行表征.并以酸性大红3R为目标污染物,用此催化剂研究了过硫酸盐在非均相催化体系的氧化性能.考察了Fe负载量、过硫酸钠用量、催化剂用量、初始污染物浓度等因素对酸性大红3R降解的影响,并对催化剂重复使用性能进行测试.结果表明,Fe负载量为6%时,催化降解效果最好;当Na2S2O8浓度为3.0 g·L-1,催化剂用量1.5 g·L-1,降解3 h时,酸性大红3R去除率达80%以上;催化剂可重复使用5次以上.同时还采用紫外可见、气相色谱-质谱分析其降解的历程.     

Differential responses of short-term soil respiration dynamics to the experimental addition of nitrogen and water in the temperate semi-arid steppe of Inner Mongolia, China

We examined the effects of simulated rainfall and increasing N supply of different levels on CO2 pulse emission from typical Inner Mongolian steppe soil using the static opaque chamber technique, respectively in a dry June and a rainy August. The treatments included NH4NO3 additions at rates of 0, 5, 10, and 20 g N/（m2.year） with or without water. Immediately after the experimental simulated rainfall events, the CO2 effluxes in the watering plots without N addition （WCK） increased greatly and reached the maximum value at 2 hr. However, the efflux level reverted to the background level within 48 hr. The cumulative CO2 effluxes in the soil ranged from 5.60 to 6.49 g C/m2 over 48 hr after a single water application, thus showing an increase of approximately 148.64% and 48.36% in the efftuxes during both observation periods. By contrast, the addition of different N levels without water addition did not result in a significant change in soil respiration in the short term. Two-way ANOVA showed that the effects of the interaction between water and N addition were insignificant in short-term soil COz efftuxes in the soil. The cumulative soil CO2 fluxes of different treatments over 48 hr accounted for approximately 5.34% to 6.91% and 2.36% to 2.93% of annual C emission in both experimental periods. These results stress the need for improving the sampling frequency after rainfall in future studies to ensure more accurate evaluation of the grassland C emission contribution.     

Effect of ozone on the performance of a hybrid ceramic membrane-biological activated carbon process

Two hybrid processes including ozonation-ceramic membrane-biological activated carbon （BAC） （Process A） and ceramic membrane-BAC （Process B） were compared to treat polluted raw water. The performance of hybrid processes was evaluated with the removal efficiencies of turbidity, ammonia and organic matter. The results indicated that more than 99% of particle count was removed by both hybrid processes and ozonation had no significant effect on its removal. BAC filtration greatly improved the removal of ammonia. Increasing the dissolved oxygen to 30.0 mg/L could lead to a removal of ammonia with concentrations as high as 7.80 mg/L and 8.69 mg/L for Processes A and B, respectively. The average removal efficiencies of total organic carbon and ultraviolet absorbance at 254 nm （UV254, a parameter indicating organic matter with aromatic structure） were 49% and 52% for Process A, 51% and 48% for Process B, respectively. Some organic matter was oxidized by ozone and this resulted in reduced membrane fouling and increased membrane flux by 25%-30%. However, pre-ozonation altered the components of the raw water and affected the microorganisms in the BAC, which may impact the removals of organic matter and nitrite negatively.     

Characteristics of secondary inorganic aerosol and sulfate species in size-fractionated aerosol particles in Shanghai

Sulfate, nitrate and ammonium(SNA) are the dominant species in secondary inorganic aerosol, and are considered an important factor in regional haze formation. Size-fractionated aerosol particles for a whole year were collected to study the size distribution of SNA as well as their chemical species in Shanghai. SNA mainly accumulated in fine particles and the highest average ratio of SNA to particulate matter(PM) was observed to be 47% in the fine size fraction(0.49–0.95 μm). Higher sulfur oxidation ratio and nitrogen oxidation ratio values were observed in PM of fine size less than 0.95 μm. Ion balance calculations indicated that more secondary sulfate and nitrate would be generated in PM of fine size(0.49–0.95 μm). Sulfur K-edge X-ray absorption near-edge structure(XANES) spectra of typical samples were analyzed. Results revealed that sulfur mainly existed as sulfate with a proportion(atomic basis) more than 73% in all size of PM and even higher at 90% in fine particles. Sulfate mainly existed as(NH4)2SO4 and gypsum in PM of Shanghai. Compared to non-haze days, a dramatic increase of(NH4)2SO4 content was found in fine particles on haze days only, which suggested the promoting impact of(NH4)2SO4 on haze formation. According to the result of air mass backward trajectory analysis, more(NH4)2SO4 would be generated during the periods of air mass stagnation. Based on XANES, analysis of sulfate species in size-fractionated aerosol particles can be an effective way to evaluate the impact of sulfate aerosols on regional haze formation.     

贵州施秉白云岩喀斯特区水化学和溶解无机碳稳定同位素特征

对贵州施秉白云岩喀斯特世界自然遗产地49个水点进行采样,分析地表水和地下水水化学特征及控制因素,并探讨溶解无机碳(DIC)稳定同位素的分布特征和来源.结果发现,研究区地表水和地下水p H值呈中性到碱性,溶解质较低,水中阳离子以Ca2+、Mg2+为主,阴离子以HCO-3为主,水化学类型为重碳酸-钙镁型(HCO3-Ca·Mg).北部上游页岩分布区外源水水中Cl-、NO-3、SO2-4的比重相对白云岩区喀斯特水水点的高,Si的含量也明显高于白云岩地区喀斯特水;外源水的SIc和SId值为负,而流经白云岩区后均大于0.水化学数据表明研究区水化学受降水和人为活动影响很小,Gibbs图显示水中离子组成主要受岩性的控制.研究区喀斯特地表水中δ13CDIC值变化范围为-8.27‰~-11.55‰,平均为-9.45‰,地下水的δ13CDIC值范围为-10.57‰~-15.59‰,平均为-12.04‰,地表水δ13CDIC值比地下水偏重.DIC的δ13CDIC值在杉木河支流上整体表现为河流上游相对于下游偏轻,而杉木河干流上河水DIC的δ13CDIC值的变化则比较复杂.根据同位素质量平衡,利用DIC的δ13CDIC实测值,计算了喀斯特区地下水DIC来自土壤CO2和白云岩矿物溶解的比例,计算结果为51.2%来自于土壤CO2,矿物本身的贡献约为48.8%.     

邻苯二甲酸酯类化合物正辛醇-水分配系数的QSPR研究

采用PM3算法计算邻苯二甲酸酯类化合物(PAEs)的量子化学参数,应用偏最小二乘(PLS)算法建立了PAEs的正辛醇-水分配系数(K_OW)的定量结构-性质相关(QSPR)模型.模型的结果表明,用量子化学参数建立的QSPR模型相关性显著,具有较好的稳健性和预测能力,因此,利用该模型可对其他PAEs分子的lgK_OW值进行初步预测.模型的结果表明,影响lgK_OW的主要量子化学参数是分子总能量TE、相对分子质量M_r、平均分子极化率α和分子生成热ΔH_f.lgK_OW随着M_r和α的增大而增大,随着TE和ΔH_f的增大而减小.     

Removal of SO2 from O2-containing flue gas by activated carbon fiber (ACF) impregnated with NH3

Adsorption of SO(2) from the O(2)-containing flue gas by granular activated carbons (GACs) and activated carbon fibers (ACFs) impregnated with NH(3) was studied in this technical note. Experimental results showed that the ACFs were high-quality adsorbents due to their unique textural properties. In the presence of moisture, the desulphurization efficiency for the ACFs was improved significantly due to the formation of sulfuric acid. After NH(3) impregnation of ACF samples, nitrogen-containing functional groups (pyridyl C(5)H(4)N- and pyrrolyl C(4)H(4)N-) were detected on the sample surface by using an X-ray photoelectron spectrometer. These functional groups accounted for the enhanced SO(2) adsorption via chemisorption and/or catalytic oxidization.     

贸易协定对我国污染排放的影响后评价模型初步研究

当今世界全球化推进到一个新的阶段,全球双边/区域贸易协定的数量呈现不断上升的趋势,而贸易自由化在促进经济扩张的同时,也导致资源的大量消耗和污染排放。因此需要建立有关环境影响评价机制,及时跟踪反馈,有针对性地引导中国出口方向的转变和进口水平的提升,为落实后续的监督管理,以及我国在贸易协定谈判或协定升级谈判中处理贸易与环境问题提供决策建议。在国内外已普遍开展贸易协定环境影响预评价并忽略后评价的背景下,本文选取工业行业大气污染排放作为指标,通过整合现有的贸易协定对经济影响测算的因素剥离方法以及经济对环境影响测算的环境投入产出分析方法,初步构建贸易协定对我国工业污染排放的影响后评价模型。建议下一步:建立贸易协定环境影响评价制度,定期开展评估;积极跟踪并参与国际贸易谈判,适时向商务部门提出打造绿色贸易的建议;加强环境与贸易领域能力建设,提升我国应对环境与贸易问题的能力。