嗜热菌株AT07-1的分离鉴定及其在污泥溶解预处理厌氧发酵产氢中的应用

从湖南大学花园土壤中采集样品,用稀释涂布法分离和纯化适于污泥溶解的典型嗜热菌菌株,从中选出一株高效菌进行形态观察,并对其进行生理生化鉴定.结果表明,该菌株的革兰氏染色为阳性,呈细杆状,产芽孢,为好氧或兼性需氧细菌,最适生长温度为65℃,最适生长pH值为6.8~7.5.通过16SrDNA碱基测序和对比证实,该菌株是目前尚未报道过的一株嗜热菌,GenBank中注册命名为Bacillus thermophilic bacteria AT071(注册号:FJ231108).同时,将其纯种菌用于嗜热酶溶解（solubilization by thermophilic enzyme,S-TE）污泥稳定化处理,接种该嗜热菌可促进污泥中悬浮固体的溶解,2.5d时接种试验挥发性悬浮固体 (volatile suspended solid,VSS)溶解率达到59.41%,比不接种试验同期提高了25.58%,达到了EPA规定的污泥稳定化要求.进一步对经AT071预处理的污泥厌氧产氢效果进行研究,试验结果显示,接种处理后污泥发酵产氢效果良好,高出未接种处理（65℃热处理）污泥26.4%,发酵气体中只含有H2和CO2.     

近50 a来三亚鹿回头石珊瑚物种多样性的演变特征及其环境意义

2005～2006年三亚鹿回头珊瑚礁现状调查共记录石珊瑚13科24属69种,礁坪以滨珊瑚占绝对优势(重要值百分比>50%),礁坡以鹿角珊瑚最占优势(28.33%).Pielou、Simpson和Shannon-Wiener多样性指数值均高于礁坪.对比历史资料发现近50 a来该岸段珊瑚礁呈衰退趋势:七世纪五六十年代该岸段珊瑚种类繁多、群落垂直分带,生物多样性较高;20世纪七八十年代礁坪已不见成片的活珊瑚,礁坡繁茂程度降低;20世纪90年代珊瑚种类虽仍比较丰富,但总体多样性下降;本次研究显示澄黄滨珊瑚已成为礁坪优势种,鹿角珊瑚在礁坡的优势度降低,物种多样性继续缩减.过度捕捞、大规模挖礁、海上和沿岸养殖等人类活动是造成该岸段珊瑚礁现有衰退的主要原凶,三亚河和近海上程建设带来的泥沙和污染物以及正向鹿回头扩展的潜水旅游可能是影响其发展的潜在威胁.     

石油污染土壤生物修复的中试系统构建与运行效果

构建了石油污染土壤生物修复中试系统,考察了中试规模下石油烃生物降解效率、矿化过程在生物降解中的作用.揭示生物修复过程中的系统微生物特性及其降解活性的关系,为现场污染土层生物修复工程评价和关键技术参数选择提供技术依据.结果表明,经过93d的运行,石油烃去除率达25.8%,其中典型轻质组分烷烃生物降解率最高,可达43.12%.中试系统运行稳定后,与现场调研的土壤微生物相比,其数量提高了1个数量级,活性提高了1.5倍.     

西南典型“退耕还林”区土地利用/覆被变化对土壤中硒及重金属含量的影响

人类活动（土地利用）和环境变化（土地覆被变化）对土壤中硒和重金属含量分布具有重要影响.“退耕还林”生态工程的实施改变了土地利用/覆被,为研究土地利用/覆被变化对土壤中硒和重金属影响提供了理想的实验场所.在西南典型“退耕还林”区,采集了旱地、水田和林地（天然林地和次生林地）的91件表层土壤样品.测定和分析了土壤中硒、重金属、 pH和有机质等参数.结果表明：（1）研究区表土中ω（Se）(0.42×10^-6)、ω（As）(13.0×10^-6)和ω（Sb）(1.03×10^-6)均值显著高于渝西地区的土壤背景值;（2）人工次生林地表土中Se、 Cd、 Cr、 Ni、 Pb和Zn含量都显著高于旱地,表明“退耕还林”工程的实施可能会显著影响表土中硒和重金属富集;（3）土壤有机质（SOM）含量水平是控制表土中硒和重金属含量差异的重要因子.结果发现土地利用/覆被变化通过影响土壤pH和SOM间接深刻地影响土壤中硒和重金属迁移和富集.     

Fate and transport of the β-adrenergic agonist ractopamine hydrochloride in soil–water systems

The feed additive ractopamine hydrochloride was fortified at four concentrations into batch vials containing soils that differed in both biological activity and organic matter(OM).Sampling of the liquid layer for 14 days demonstrated that ractopamine rapidly dissipated from the liquid layer. Less than 20% of the fortified dose remained in the liquid layer after 4 hr,and recoveries of dosed ractopamine ranged from 8 to 18% in the liquid layer at 336 hr. Sorption to soil was the major fate for ractopamine in soil:water systems, i.e., 42%–51% of the dose at14 days. The major portion of the sorbed fraction was comprised of non-extractables; a smaller fraction of the sorbed dose was extracted into water and acetone, portions which would be potentially mobile in the environment. Partitioning coefficients for all soils suggested strong sorption of ractopamine to soil which is governed by hydrophobic interactions and cation exchange complexes within the soil OM. Ractopamine degradation was observed, but to mostly non-polar compounds which had a higher potential than ractopamine to sorb to soil. The formation of volatiles was also suggested. Therefore, despite rapid and extensive soil sorption,these studies indicated a portion of ractopamine, present in manures used to fertilize soils,may be mobile in the environment via water-borne events.     

交通干道沿线土壤重金属监测与评估综述

公路运营所带来的铅、镉、锌等重金属污染物对人体健康安全存在着潜在和长期的影响。近年来,开展交通干道沿线重金属污染监测与评估工作已经成为环境监测工作的重要内容。从监测技术、评估方法、可能影响因素等几个方面对该领域的研究进展及成果进行了综述。采样段面的选取、点位的布设与样品的收集应该同时遵循全面性和代表性的原则。在同一交通干道内,均匀布置采样段面的同时可以尽量包含高车流量、中车流量与低车流量3种类型。考虑到重金属在横向距离上的分布规律,可以在0~100 m处设置密集采样点位,在100~300 m处设置适量采样点位。评估方法一般同时采用Kriging空间插值分析、污染指数分析、多元统计分析,生态风险评价与健康风险评价等多种分析方法。     

成都平原农用土壤重金属污染现状及防治对策

随着工业化进程的加快和农业生产中化肥和农药不合理施用使得农用土壤重金属污染风险逐渐增大。本文对成都平原农用土壤和农作物重金属污染现状进行了综述,发现农用土壤和蔬菜中重金属污染均以Pb、Cd和Hg三种元素为主。分析了重金属离子在土壤一植物系统中迁移的一般规律及其影响因子,分析了农用土壤重金属污染的主要原因,为预防和防治污染提供了一些建议。     

Combined toxicity of copper and cadmium to six rice genotypes （Oryza sativa L.）

Accumulation of copper (Cu) and cadmium (Cd) in six rice cultivars (94D-22, 94D-54, 94D-64, Gui630, YY-1 and KY1360) was evaluated through exposure to heavy metal contamination (100 mg/kg Cu, 1.0 mg/kg Cd, and 100 mg/kg Cu + 1.0 mg/kg Cd) in a greenhouse. The dry weight of shoot and root, concentrations of Cu and Cd in plant tissues and the Cu, Cd, P, Fe concentrations in the root surface iron plaques were analyzed eight weeks later after treatment. The results indicated that the plant biomass was mainly determined by rice genotypes, not Cu and Cd content in soil. Separated treatment with Cu/Cd increased each metal level in shoot, root and iron plaques. Soil Cu enhanced Cd accumulation in tissues. In contrast, Cu concentrations in shoot and root was unaffected by soil Cd. Compared to single metal contamination, combined treatment increased Cd content by 110.6%, 77.0% and 45.2% in shoot, and by 112.7%, 51.2% and 18.4% in root for Gui630, YY-1 and KY1360, respectively. The content level of Cu or Cd in root surface iron plaques was not affected by their soil content. Cu promoted Fe accumulation in iron plaques, while Cd has no effect on P and Fe accumulation in it. The translocation of Cu and Cd from iron plaques to root and shoot was also discussed. These results might be beneficial in selecting cultivars with low heavy metal accumulation and designing strategies for soil bioremediation.     

Removal of heavy metals from a contaminated soil using tartaric acid

This study reports the feasibility of remediation of a heavy metal （HM） contaminated soil using tartaric acid, an environmentally-friendly extractant. Batch experiments were performed to test the factors influencing remediation of the HM contaminated soil. An empirical model was employed to describe the kinetics of riM dissolution/desorption and to predict equilibrium concentrations of HMs in soil leachate. The changes of HMs in different fractions before and after tartaric acid treatment were also investigated. Tartaric acid solution containing HMs was regenerated by chestnut shells. Results show that utilization of tartaric acid was effective for removal of riMs from the contaminated soil, attaining 50%-60% of Cd, 40%-50% of Pb, 40%-50% of Cu and 20%-30% of Zn in the pH range of 3.5-4.0 within 24 h. Mass transfer coefficients for cadmium （Cd） and lead （Pb） were much higher than those for copper （Cu） and zinc （Zn）. Sequential fractionations of treated and untreated soil samples showed that tartaric acid was effective in removing the exchangeable, carbonate fractions of Cd, Zn and Cu from the contaminated soil. The contents of Pb and Cu in Fe-Mn oxide fraciton were also significantly decreased by tartaric acid treatment. One hundred milliliters of tartaric acid solution containing HMs could be regenerated by 10 g chestnut shells in a batch reactor. Such a remediation procedure indicated that tartaric acid is a promising agent for remediation of HM contaminated soils. However, further research is needed before the method can be practically used for in situ remediation of contaminated sites.     

深圳市城市绿地土壤中重金属的含量及化学形态分布

对深圳市中心区城市绿地表层土壤(0-20cm)中Cu,Zn,Pb和Cd的含量、化学形态分布和迁移性进行研究.结果表明,土壤中Cu,Zn,Pb和Cd的含量分别为6.4-188.2(26.3)mg·kg-1,34.9-284.8(69.1)mg·kg-1,15.2-245.5(47.2)mg·kg-1和0.01-3.48(0.47)mg·kg-1.道路绿化带土壤中Cu,Zn和Pb的平均含量最高,在公园绿地土壤中Cd的平均含量最高.分别有75.6%,87.0%,98.8%和98.8%的土壤中Cu,Zn,Pb和Cd的含量超过广东省赤红壤的背景值,重金属在土壤中呈现明显的富集特征.土壤中Cu,Zn和Cd以残渣态所占比例最高,Pb以铁锰氧化物结合态最高.随着土壤中Cu,Zn,Pb和Cd含量的增加其残渣态所占比例降低,铁锰氧化物结合态或交换态所占比例增加,重金属活性增大.土壤中Cd迁移能力最强,迁移能力依次为Cd>Zn>Pb和Cu.