反硝化细菌、硝酸钙和锆改性沸石联用对底泥中氮磷迁移转化的影响及硝态氮释放风险评估

本文考察了基于反硝化细菌、硝酸钙和锆改性沸石的组合技术（CN+DB+ZZ）对底泥中氮磷迁移转化的影响,并探讨了该技术的硝态氮释放风险.结果发现,单一的硝酸钙处理（CN）虽然可以有效地抑制底泥中磷的释放,但是会造成上覆水体的氨氮和硝态氮污染.硝酸钙和反硝化细菌联合处理（CN+DB）尽管可以有效地抑制底泥中磷的释放,并降低上覆水体的硝态氮二次污染风险,可是却无法有效地控制底泥中氨氮的释放.硝酸钙和锆改性沸石联合处理（CN+ZZ）虽然可以有效地抑制底泥中磷和氨氮向上覆水体的释放,但却会造成上覆水体硝态氮的二次污染.CN+DB+ZZ组合处理技术不仅可以有效地控制底泥中磷的释放,而且可有效降低底泥中氨氮的释放速率,并且与CN和CN+ZZ技术相比还可降低上覆水的硝态氮二次污染风险.CN+DB+ZZ组合技术对底泥中磷与铁同步释放的抑制、对底泥中氧化还原敏感态磷的削减、以及对底泥吸附磷酸盐和氨氮能力的增强,对于其控制底泥中磷和氨氮的释放是至关重要的.以上结果说明,CN+DB+ZZ组合技术是一种非常有希望的用于控制水体底泥中磷和氨氮释放的方法.     

渔业复垦塌陷地抗生素抗性基因与微生物群落

水产养殖行业抗生素的广泛使用引起了抗生素抗性基因（antibiotic resistance genes,ARGs）污染问题.为探究渔业复垦塌陷地ARGs污染特征,利用宏基因组学技术检测分析了渔业复垦塌陷地ARGs的相对丰度和微生物群落结构.研究区域共检测出29种ARGs,bacA在所有样品中相对丰度最高,达1.96×10^-5~1.19×10^-4.沉积物中磺胺类和四环素类ARGs相对丰度较高,井水中多药类ARGs相对丰度较高.微生物群落结构表明变形菌门（Proteobacteria）在所有样品中为最优势细菌门,沉积物中绿弯菌门（Chloroflexi）和广古菌门（Euryarchaeota）较为优势.属水平上,硫杆菌属（Thiobacillus）为沉积物中最优势细菌属,不动杆菌属（Acinetobacter）和假单胞菌属（Pseudomonas）为井水中优势细菌属.ARGs与微生物相关性分析表明,菌属与ARGs间主要呈中度相关,多种菌属与ARGs显著正相关,ARGs的分布受微生物群落结构的重要影响.渔业复垦塌陷地沉积物与井水均受到ARGs污染,应加强相应控制措施保护区域环境.     

秦岭山地丹江流域土地利用变化的土壤侵蚀效应评价

论文采用ArcGIS 10.0及InVEST土壤保持模型,分析2000—2010年秦岭山地丹江流域土地利用类型变化特征,模拟流域不同时期不同土地利用类型土壤侵蚀及土壤保持量的变化规律,并着重探讨土地利用类型方式转变对流域土壤侵蚀的影响。结果表明：1）2000—2010年间,流域裸地大比例减少90.18%（831.06 hm²）,主要转移至水域,耕地大面积减少5 197.24 hm²（4.11%）,主要流向灌丛和城镇;坡耕地还林还草初见成效,湿地的保护与恢复成效显著。2）2000—2010年间,流域土壤侵蚀状况较为严重,整体处于中度侵蚀至强度侵蚀级别,但10 a间侵蚀状况有减缓趋势;在该研究时段内,耕地大面积转为灌丛是该流域由土地利用类型变化引起的土壤侵蚀减缓的主要原因;另外,耕地转为林地以及裸地面积的减少也起到了减轻土壤侵蚀的作用;以自然生态系统为主的林地、灌丛及草地转为耕地时,土壤侵蚀强度则会明显增加。3）生态系统土壤保持功能受多方因素共同影响;2000、2010年研究区实际土壤保持量分别为5.35×10⁸、5.47×10⁸ t;占全区面积一半以上的林地和灌丛单位面积土壤保持量较为稳定,全区土壤保持功能有所提高。保证一定面积的林地、在人工干预下合理安排坡耕地还林还草区域的空间分布是秦岭山地丹江流域减少土壤侵蚀的必要措施,同时应注重对可利用耕地的保护。     

Biologic risk and source diagnose of 16 PAHs from Haihe River Basin,China

Surface sediments of rivers can exhibit spatial and temporal variations in contaminant concentrations that may significantly affect risk evaluations. As to pollution control and remediation of watershed, large-scale and further background data on PAHs in China were required urgently. Spatial distribution and compositional characteristics of 16 polycyclic aromatic hydrocarbons (PAHs) in surface sediments from Haihe River Basin were investigated. A method based on effects range (ER) was used to assess ecosystem risk of ∑PAHs (the total of 16 PAH) sensitively and accurately. The results indicated that ∑PAHs content levels ranged from 257 to 16901 μg·kg⁻¹ dry weight. The lower rings predominated in the samples, and 2-, 3-, 4-, 5- and 6-ring PAHs accounted for 12%, 21%, 30%, 30%, and 7% respectively in total PAHs. The ratio of Fl / (Fl+ Py) uniformly distributed in the interval 0.20–0.80, indicating that it may be affected by petroleum origin, oil combustion, biomass and coal combustion jointly. ∑PAHs in Cetian (S6), Dongwushi (S19), Handan (S20), Aixinzhuang (S21) and Tianjin (S37) exceeded effects range low (ERL), in which biologic effects were in a medium level with an adverse effect on biologic organisms. Thus, it is necessary to strengthen the PAHs monitoring and research of the Haihe River Basin.     

Multiphase redistribution differences of polycyclic aromatic hydrocarbons (PAHs) between two successive sediment suspensions

Successive sediment suspensions often happen in estuary, yet little research has probed into the difference in the release behaviors of organic compounds among different suspensions. This study took polycyclic aromatic hydrocarbons (PAHs) as typical organic contaminants and investigated the release behaviors between two successive suspensions with a particle entrainment simulator (PES). Results showed that successive sediment suspensions lowered the concentration of dissolved PAHs in the overlying water via facilitating the re-adsorption of dissolved PAHs onto the suspended particles. Fast-release and slow-release periods of PAHs were successively observed in the both suspensions. The concentration changes of dissolved PAHs in the second suspension were generally similar with but hysteretic to those in the first suspension. More vigorous desorption and re-absorption of PAHs were induced in the second suspension. Successive sediment suspensions obviously decreased the concentrations of mineral composition and organic matters in the overlying water, which significantly affects multiphase distribution of PAHs.     

巢湖表层沉积物重金属生物有效性与生态风险评价

以巢湖表层沉积物为对象,对重金属(Cd、Cr、Cu、Zn、Ni和Pb)总量及形态进行分析并运用潜在风险指数法和风险评价编码两种方法对巢湖表层沉积物重金属的生态风险进行了评价.结果表明,巢湖表层沉积物中的重金属含量表现为西部湖区高,东部湖区低的特征,其中南淝河入湖区重金属含量是全湖的1.09~1.21倍.BCR形态分析表明,巢湖表层沉积物中Cr、Ni和Cu以残渣态为主(分别占总量82.99%、63.63%和54.25%),Cd和Zn以弱酸提取态为主(分别占总量55.96%和35.84%),Pb以可还原态和可氧化态为主(分别占总量39.66%和24.56%).潜在生态风险危害指数(RI)表明,南淝河入湖河口区域具有较大生态风险(RI值范围为351.54~381.17).风险评价编码方法(RAC) 的结果显示,Cd处于极高风险水平,Zn基本处于高风险水平,Cu 和Ni处于中低风险,Pb处于低风险水平,Cr各采样点均处于无风险.因此, 对需着重考虑对南淝河入湖湖区的Cd和Zn元素的重点治理.     

细微泥沙对活性污泥系统的影响及其恢复特征

不同地区、排水体制和季节下,我国城市污水厂进水中细微泥沙含量〔以ρ(ISS)/ρ(COD_Cr)表征,ISS为无机悬浮固体〕差异较大,细微泥沙进入生化处理单元将会对活性污泥系统的正常运行产生一定影响. 考察在不同进水细微泥沙浓度下,活性污泥系统各运行参数的变化及系统恢复情况,结果表明:①随着进水中细微泥沙浓度的增大,活性污泥系统ρ(MLVSS)/ρ(MLSS)、SOUR′(单位质量污泥活性)、CST(污泥毛细吸水时间)和SVI(污泥容积指数)降低;在影响期,ρ(MLVSS)/ρ(MLSS)最小值、SOUR′平均值、CST平均值与细微泥沙浓度均呈良好的线性关系,R2(相关系数)分别为0.963 7、0.979 9和0.786 5;系统恢复所需时间与进水细微泥沙浓度呈正相关. ②污泥中细微泥沙浓度的增加导致SOUR′下降,使得ρ(MLSS)和剩余污泥量增加,不利于污水厂的节能减排. 可见进水中细微泥沙浓度的增大不利于污水厂的稳定高效运行.      

四海龙湾表层沉积物中有机质的组成特征及其源解析

为研究玛珥湖四海龙湾表层沉积物中有机质的组成特征及来源,采集四海龙湾表层沉积物样品,并对其中的有机质进行了分析. 结果表明,四海龙湾表层沉积物中w(TOC)(TOC为总有机碳)为6.7%、w(TN)为0.6%、δ13C_org(TOC同位素丰度)为-28.0‰、δ15N_total(TN同位素丰度)为2.2‰. 可溶性有机质主要包括脂肪烃、脂肪醇、脂肪酸和GDGTs(甘油二烷基甘油四醚脂)等,其中脂肪酸是可溶性有机质的主要组分,约占可溶性有机质总量的68.8%,主要来源于内源性的藻类和厌氧菌; 脂肪烃主要来源于陆源的C3木本植物;结合态脂肪醇具有明显的内源来源特征,而游离态脂肪醇却呈现陆源来源特征. 四海龙湾沉积物中含有丰富的GDGTs,主要来源于陆源土壤,包括支链类GDGTs和类异戊二烯类GDGTs,其中类异戊二烯类GDGTs以GDGTⅣ和GDGTⅤ为主,但其在四海龙湾沉积物中的含量相对较小. 研究显示,四海龙湾流域陆源是沉积物中可溶性有机质的主要来源,陆源有机质的大量流入改变了四海龙湾的营养水平;不同种类可溶性有机质表现出不同的来源特征,这主要是由于微生物对不同种类有机质降解速率的不同所致,并且导致降解所产生的二次有机质数量也不同.      

Microbial communities biostimulated by ethanol during uranium (VI) bioremediation in contaminated sediment as shown by stable isotope probing

Stable isotope probing (SIP) was used to identify microbes stimulated by ethanol addition in microcosms containing two sediments collected from the bioremediation test zone at the US Department of Energy Oak Ridge site, TN, USA. One sample was highly bioreduced with ethanol while another was less reduced. Microcosms with the respective sediments were amended with ¹³C labeled ethanol and incubated for 7 days for SIP. Ethanol was rapidly converted to acetate within 24 h accompanied with the reduction of nitrate and sulfate. The accumulation of acetate persisted beyond the 7 d period. Aqueous U did not decline in the microcosm with the reduced sediment due to desorption of U but continuously declined in the less reduced sample. Microbial growth and concomitant ¹³C-DNA production was detected when ethanol was exhausted and abundant acetate had accumulated in both microcosms. This coincided with U(VI) reduction in the less reduced sample. ¹³C originating from ethanol was ultimately utilized for growth, either directly or indirectly, by the dominant microbial community members within 7 days of incubation. The microbial community was comprised predominantly of known denitrifiers, sulfate-reducing bacteria and iron (III) reducing bacteria including Desulfovibrio, Sphingomonas, Ferribacterium, Rhodanobacter, Geothrix, Thiobacillus and others, including the known U(VI)-reducing bacteria Acidovorax, Anaeromyxobacter, Desulfovibrio, Geobacter and Desulfosporosinus. The findings suggest that ethanol biostimulates the U(VI)-reducing microbial community by first serving as an electron donor for nitrate, sulfate, iron (III) and U(VI) reduction, and acetate which then functions as electron donor for U(VI) reduction and carbon source for microbial growth.     

巢湖重污染汇流湾区沉积物重金属污染特征及风险评价

对巢湖重污染汇流湾区沉积物中主要重金属分布和累积特征及生态风险进行了分析评价.结果表明:受底泥分布影响,湾区沉积物重金属主要累积于距岸边约700m以上的低洼区,且表层沉积物(0~2cm)重金属含量大致随泥深增加而增大.基于地积累指数法和潜在生态风险指数法的评价结果表明,除Hg(Eri=325.5)和Cd(Eri=240.28)外,大多数重金属处于低风险状态,各金属元素污染顺序为Hg>Cd>Zn>Pb>Cu>As>Cr>Ni.其中,富集倍数最高的Hg和Cd具有同源性,污染等级均为3级.垂向分析表明,受Hg和Cd的影响,0~14cm沉积物已达严重生态风险程度(RI>525),14~34cm沉积物中Hg具有中度生态风险.建议亟须从流域角度对该汇流湾区重金属特别是Hg和Cd进行控制.