部分亚硝化-厌氧氨氧化耦合工艺处理污泥脱水液

在缺氧滤床+好氧悬浮填料生物膜工艺中实现部分亚硝化,然后进行厌氧氨氧化(ANAMMOX),考察其对高含氮、低C/N污泥脱水液的处理能力.结果表明,亚硝化反应器在15~29℃、DO 6~9mg/L条件下,通过综合调控进水氨氮负荷(ALR)、进水碱度/氨氮、水力停留时间(HRT)等运行参数,可以调节出水(NO2--N)/(NH4+-N)的比率,能够较好地实现部分亚硝化反应以完成厌氧氨氧化.当进水ALR为1.16kg/(m3·d),进水碱度/氨氮为5.1时,出水(NO2--N)/(NH4+-N)在1.2左右,(NO2--N)/(NOx--N)大于90%,进入ANAMMOX反应器的氮物质去除率达到83.8%.     

A 60-year sedimentary record of natural and anthropogenic impacts on Lake Chenghai, China

Recent sediments from Lake Chenghai, China, were investigated at high temporal resolution to trace both natural and anthropogenic effects on the lake using total organic carbon (TOC), total nitrogen (TN), total phosphorus (TP), organic phosphorus (P_o), inorganic phosphorus (P_i) and organic carbon and nitrogen stable isotopes (δ¹³C_org and δ¹⁵N) in a ¹³⁷Cs-dated sediment core. The results indicated that the sedimentary record covers the last 60 years, during which the lake had undergone apparent changes in nutrient sources and productivity in response to nutrient loading. Prior to the late 1980s, the nutrient contents in sediments mainly originated from algae and lake productivity was relatively stable. Since the late 1980s, increasing TOC, TN and TP concentrations together with the change of δ¹³C_org and δ¹⁵N suggested anthropogenic perturbations in nutrient loading and lake productivity. Endogenic nutrients derived from algae and anthropogenic inputs were two important sources of sedimentary nutrients. The anthropogenic nutrients mainly originated from the discharge of industrial wastewater and artificial cultivation of Spirulina after the middle 1980s, and domestic wastewater discharged from Yongsheng County since 1993.     

Size distribution of black (BC) and total carbon (TC) in Vienna and Ljubljana

During two campaigns in winter 2004, size segregated impactor samples (0.1-10 microm) and filter samples were taken in two Central European cities (Vienna, Austria and Ljubljana, Slovenia). The impactor samples were analyzed for major inorganic ions and short-chain organic acids, total carbon (TC) and black carbon (BC). Maximum concentrations of total mass were 71.6 microg m(-3) in Vienna and 73.1 microg m(-3) in Ljubljana. Minimum concentrations in Vienna were only half those in Ljubljana. The BC content of the aerosol was similar (ca. 8%), but the BC/TC ratio was higher in Vienna than in Ljubljana (0.39 vs. 0.29), reflecting the different contribution of diesel traffic emissions. The mass median diameters of the submicron size distributions of all major fractions (total mass, TC, BC and SO(4)(2-)) were smaller in Vienna (0.43 microm, 0.41 microm, 0.38 microm and 0.48 microm, respectively) than in Ljubljana (0.55 microm, 0.44 microm, 0.42 microm and 0.60 microm, respectively). Impactor/filter ratios for total mass were 0.79 in Vienna and 0.82 in Ljubljana, while the ratios for BC were 0.56 in Vienna and 0.49 in Ljubljana. An estimation of the mixing state of accumulation mode BC indicated that 33% and 37% of BC, respectively, are mixed externally to the aerosol in the accumulation size range in Vienna and Ljubljana.     

长江下游地区新近沉积土动剪切模量比和阻尼比的试验研究

通过对长江下游地区南京、苏州、常州、徐州、泰州、盐城、扬州、无锡、镇江、张家港、连云港、启东、常熟、江阴、宿迁等15个城市的淤泥质粉质粘土、粘土、粉质粘土、粉质粘土与粉砂互层土、粉土、粉细砂和粗砂等七类新近沉积土共计275个原装土样历时3年的自振柱试验研究,给出了长江下游地区七类新近沉积土的动剪切模量比 G/Gmax和阻尼比λ与剪应变幅值γ变化的平均曲线的拟合曲线、包络线及其参数的推荐值。由于未见报道其他研究者对长江下游地区新近沉积土动力参数的系统研究,该研究成果有利于加深对该长江下游地区各类新近沉积土动力特性的认识,并对该地区各类工程建设的工程场地地震安全性评价工作具有一定的借鉴和参考价值,且有利于推动长江下游地区工程场地地震安全性评价工作的开展。     

生态足迹分析法在生态持续发展定量研究中的应用--以南京市1998年的生态足迹计算为例

利用生态足迹分析方法计算了南京市1998年的生态足迹和生态承载力.认为南京市生态足迹需求对本地生态系统持续发展不构成威胁,但对全国或全球可持续发展造成负面影响.     

The effects of temperature and resource availability on denitrification and relative N2O production in boreal lake sediments

Anthropogenic environmental stressors(like atmospheric deposition,land use change,and climate warming) are predicted to increase inorganic nitrogen and organic carbon loading to northern boreal lakes,with potential consequences for denitrification in lakes.However,our ability to predict effects of these changes is currently limited as northern boreal lakes have been largely neglected in denitrification studies.The aim of this study was therefore to assess how maximum potential denitrification and N_2O production rates,and the relationship between the two(relative N_2O production),is controlled by availability of nitrate(NO_3~-),carbon(C),phosphorus(P),and temperature.Experiments were performed using the acetylene inhibition technique on sediments from a small,nutrient poor boreal lake in northern Sweden in 2014.Maximum potential denitrification and N_2O production rates at 4°C were reached already at NO_3~-additions of 106–120 μg NO_3~-–N/L,and remained unchanged with higher NO_3 amendments.Higher incubation temperatures increased maximum potential denitrification and N_2O production rates,and Q10 was somewhat higher for N_2O production(1.77) than for denitrification(1.69).The relative N_2O production ranged between 13% and 64%,and was not related to NO_3~-concentration,but the ratio increased when incubations were amended with C and P(from a median of 16% to 27%).Combined,our results suggests that unproductive northern boreal lakes currently have low potential for denitrification but are susceptible to small changes in NO_3 loading especially if these are accompanied by enhanced C and P availability,likely promoting higher N_2O production relative to N_2.     

射流曝气的气液两相流的数值模拟

射流曝气在活性污泥处理方法中起着重要的作用.采用数值模拟的方法研究自吸式单级单喷射流器中的气液两相流动状况,通过对不同长径比和喷嘴面积比的射流曝气器模型的气液两相流的计算,定量分析长径比和喷嘴面积比对射流曝气器流场和空气与工作介质流量比的影响,为进一步设计开发新型高效的射流曝气器提供参考.     

接种量对餐厨垃圾中温厌氧产甲烷潜能的影响

以接种量作为餐厨垃圾厌氧消化进料负荷的衡量参数,研究不同接种量对餐厨垃圾中温产甲烷潜能的影响,确定餐厨垃圾中温厌氧消化最适接种量。实验设置10%、15%、20%、25%、30%和35%等6种不同的接种量,分析不同接种量之间产气量、甲烷含量、发酵前后总固体（TS）和挥发性固体（VS）、发酵过程中总挥发酸（VFAs）的变化情况。实验结果表明,发酵6 d后,所有发酵瓶罐均无气体产生,35%接种量导致系统酸化;30%和25%接种量时,发酵液维持较高的VFA浓度,在发酵结束后仍有较高浓度的VFA残留,这说明虽然该接种量下系统可以运行,但酸化产生的VFA并未充分转化为甲烷;10%、15%和20%接种量的发酵罐则能够将产生的VFAs利用掉,相比之下,接种量为20%时产气量最大,甲烷含量达到52.88%,TS和VS的去除率也能达到32.11%和38.24%,因此,20%接种量可作为后续实验的最适接种量。     

The Behaviour of Selenium in Geological Processes

Selenium contents were analyzed from a total of 244 soil samples collected over different rock types at a sampling density of one sample per 4km² around Geita gold mining areas, Northwestern Tanzania. Comparisons using literature survey contents of selenium in geological materials and some implications on the selenium in soils are compiled and discussed. Most selenium occurs as simple selenides in small quantities in low temperature hydrothermal deposits devoid of sulphur. It has been observed that to a large extent selenium content is increased more than most trace elements in the upper parts of the Earth perhaps through extraterrestrial deposition. In deep-seated rocks selenium is associated with sulphur but being volatile selenium and sulphur do not behave according to the crystallochemical law. Due to the higher stability of S⁶⁺, Se⁴⁺ and Se⁰ separate during migration. Thus, selenium is especially found in deep-seated plutonic rocks where large magma bodies cooled slowly and sulphur is available to precipitate sulphides. Selenium, which occurs with sulphides, is inhomogeneously deposited into continental margins. It is increased during magmatic differentiation and is highest in basic rocks. In magmatic and metamorphic conditions, selenium is found in the crystal structures of sulphides while in pneumatolytic and hydrothermal processes, it is relatively enriched into the late differentiates compared to sulphur. In metamorphic rocks selenium is more widely distributed. Selenium content in soils in the investigated area varies from (0.3–0.5gg^–1) in laterite and in black cotton soil 0.4gg^–1. Of all volcanic rocks selenium is highest in volcanogenic rocks especially the basalts. Surface waters are enriched in selenium, which they leach from volcanic materials. Selenium in sediments containing clay and organic matter is elevated but the content decreases with increased metamorphism. Selenium in volcanic areas can be used as a pathfinder in prospecting for volcanogenic ore deposits. S/Se ratios are distinct in different rock types and can thus be used to elucidate the origin of rocks, ores, and sediments.     

Seasonal variation of soil carbon and nitrogen under five typical Pinus massoniana forests

Five different typical Pinus massoniana forests were sampled in the Guizhou Province to evaluate the effects of seasons on soil organic carbon (SOC), total nitrogen (STN), and inorganic nitrogen (SIN) in these forests. More seasonal variation occurred in the topsoil than in lower layers. The SOC and STN contents varied the least amongst the soil layers, but the SIN contents had the largest values and ranges during autumn. Carbon-to-nitrogen ratio (C/N) exhibited neither a vertical change nor a seasonal trend. C/N was either maximal or minimal depending upon the sites during autumn, indicating that ecological process during summer soils would strongly change this. More gravel content resulted in higher litter stock, SOC, and STN level in low-productivity forests. A low phosphorus level might result in low SOC and STN contents in clay-rich soils. Low litter stock and clay content will result in low SOC and STN levels in coniferous and broad-leaved mixed forests in contrast to pure forests. The SOC and soil N contents in P. massoniana forests are apparently affected by different sampling seasons, particularly in topsoil. This should be taken into account when evaluating C and N contents and their respective storages in other forest types.