黄河三角洲风暴潮灾害及其对滨海湿地的影响

黄河三角洲是中国重要的滨海湿地分布区，也是中国风暴潮易发区。该区的风暴潮有温带气旋型与热带台风型两种，以温带风暴潮为主。近年来，重大风暴潮的发生有频率增加、危害加重的趋势。风暴潮对滨海湿地的影响是广泛而深远的，主要表现为淹没滨海低地、加速海岸蚀退、破坏地表结构、毁坏湿地植被、加剧海水入侵等，使滨海湿地不断损失退化，生态环境恶化。     

西藏湿地的现状和保护

本研究对西藏全区湿地的概况、类型、现状、重要湿地和现有湿地保护区进行系统描述,提出了湿地保护方面存在的问题与对策;并对西藏湿地标准、功能、特点、类型等,进行了科学的论证。     

人工湿地基质再生技术的研究进展

人工湿地中基质对污染物的吸附是一个有限的过程,对其进行再生可减缓净化效果的下降趋势,降低周期性更换基质的材料消耗和购置成本,回用营养物质于农业。基质可以通过物理、化学或生物的方法原位或异位再生。其中生物再生成本低廉,生态友好且具有可持续性,是基质脱氮再生的最有效途径,可以通过优化离子浓度和交换速率,碳源、溶解氧、微生物群落结构等提高再生效果和速率。基质除磷物理再生效果受基质类型、磷浓度负荷、落干休作开始时机和持续时间等的影响,其操作简便,可在人工湿地的日常运行管理中原位实施。化学再生效果受基质种类、再生试剂的成分和浓度、环境条件如温度、pH值、Eh值和DO值等的影响,可在基质吸附饱和后作为应急措施使用。     

电解强化人工湿地对农村生活污水中氮磷的去除性能

采用电解强化-三级串联潜流人工湿地的组合工艺,深化处理农村生活污水中的氮、磷营养盐.探究了系统对农村生活污水中氮、磷的净化效果,测定了填料对磷的吸附贡献及其磷的形态,采用高通量测序的方法分析了基质微生物的群落结构.结果 表明:当水力负荷为0.30 m3·(m2·d)-1时,电解系统对TN、NH4+-N和TP去除率分别为...     

人工湿地在污水处理中的应用及其展望

作为污水处理的有效途径，人工湿地具有众多的优点。本文分析了人工湿地的构造及去污机理，总结了人工湿地在污水处理中应用的历史及现状，并对其未来的应用前景做出了展望。     

ENVIRONMENTAL IMPACT ASSESSMENT OF TAILINGS DISPERSAL FROM A URANIUM MINE USING TOXICITY TESTING PROTOCOLS1

ABSTRACT: Toxicity testing is a means of establishing the environmental risk of a uranium tailings release. It is valuable in designing tailings containment structures because it assists in setting acceptable levels of risk for the design. This paper presents details of toxicity tests of the tailings from Ranger Uranium Mine, Northern Territory, Australia. The results suggest that the non-radiological toxicity of the tailings is low. The environmental risk of a tailings release is more likely to be related to the physical impacts of the tailings, including infilling of billabongs and changes in the sedimentology of riparian ecosystems rather than their biogeochemical impact. Two major results were: (1) water from treatment with washed tailing fines were not toxic to Hydra viridissima, and (2) mixtures of washed tailings fines and natural floodplain sediment (overlying water or elutriates) were not toxic to Hydra viridissima or Moinodaphnia macleayi.     

不同基质垂直流人工湿地对猪场污水季节性处理效果的研究

研究了3套不同基质垂直流人工湿地小试装置在不同季节处理猪场污水的运行效果.结果表明,垂直流人工湿地对有机污染物的去除效果随季节变化差异不明显,对有机物降解情况可用一级降解模型模拟;传统型湿地系统NH4 -N去除率在各季节稳定在52%,而沸石和沸石-煤渣型系统冬季NH4 -N去除效率分别从秋季的89.8%和93.4%下降至冬季的64.2%和73.5%,春、夏季回升至80%左右.冬季湿地系统中生物硝化与反硝化作用的减弱影响了垂直流人工湿地系统TN的去除;3套不同基质系统中,沸石-煤渣型系统各高度层硝化强度均为最高,沸石型和沸石-煤渣型系统的反硝化强度明显高于传统型系统,与实际运行过程TN去除率变化相吻合.采用沸石作为基质有利于系统的反硝化进程和TN的去除.垂直流系统对TP去除率随季节性变化波动不显著,但随着垂直流人工湿地系统的运行,基质层对TP的吸附逐渐饱和,去除效率明显下降.     

Contribution of the Kodama and 4S pathways to the dibenzothiophene biodegradation in different coastal wetlands under different C/N ratios

Dibenzothiophene (DBT) degradation mechanisms and the transformation of pathways during the incubation of three types of coastal sediments with C/N ratios ranging from 1 to 9 were investigated. The DBT degradation efficiencies were clearly improved with increasing C/N ratio in reed wetland sediments, tidal wetlands sediments and estuary wetland sediments. The quantitative response relationships between DBT degradation rates and related functional genes demonstrate that the Kodama pathway-related gene groups were dominant factors at low C/N ratios, while the 4S-related gene groups mainly determined the degradation rate when the C/N ratio was up to 5. Network analysis also shows that the pathway shifts from the Kodama pathway to the 4S pathway occurred through changes in the connections between functional genomes and rates. Furthermore, there were competition and collaboration between the Kodama and 4S pathways. The 4S pathway-related bacteria were more active in estuary wetland sediments compared with reed wetland sediments and tidal wetland sediments. The higher degradation efficiency in estuary wetland sediments may indicate the greater participation of the 4S pathway in the DBT biodegradation reaction. And the effects of ring cleavage of Kodama pathway caused more complete metabolizing of DBT.     

崇明东滩湿地干湿交替过程脲酶活性变化初探

以典型滨海湿地——崇明东滩为原型区域,采集湿地沉积物及海水样品,通过土柱模拟方法(30、35、40℃),研究了半月潮(15d左右为周期的"大潮")与日潮(一个太阴日内出现的涨潮和落潮)水分生态过程沉积物脲酶(Urease)活性及溶解性有机氮(DON)与铵态氮(NH+4-N)含量等的变化,计算了Urease活性的表观温度敏感性系数(Q’10),旨为揭示典型滨海湿地潮汐驱动下周期性干湿交替过程沉积物Urease活性的变化规律.半月潮过程,干燥沉积物(1%~3%)淹水后,Urease活性迅速增加.随着沉积物变干,酶活性逐渐下降.Urease活性对沉积物水分变化的敏感性随干湿交替频次的增加而下降.日潮过程对Urease活性的影响较小.30、35、40℃下,酶活性分别为(0.067±0.018)、(0.143±0.027)、(0.028±0.011)g·(10 g·h)-1.相比较而言,半月潮过程Urease活性明显低于日潮过程.这表明,干湿交替显著降低了沉积物Urease活性(30、35℃).半月潮过程中,沉积物Urease活性Q’10的最高值出现在35~40℃,而日潮过程中出现在30~35℃.因此,干湿交替可能增高了Urease活性Q’10的温度响应范围.此外,半月潮过程中,Urease活性主导着沉积物NH+4-N含量的变化(30、35℃),但其与DON含量之间并无显著相关性.日潮过程Urease活性与NH+4-N和DON含量之间均不显著相关.     

互花米草入侵对长江口湿地土壤碳动态的影响

为了评价互花米草入侵对长江河口湿地土壤碳动态的影响,利用配对的试验设计在长江口崇明东滩湿地的高潮滩和低潮滩各设置1条入侵种互花米草与土著种的配对样线.结果表明,与土著植物相比,互花米草入侵显著增加了长江口湿地的植物碳库、土壤微生物碳、土壤总碳库和有机碳库,而对占土壤总碳库60%以上的无机碳库无显著影响,意味着互花米草入侵导致的土壤总碳库改变主要是通过增加土壤有机碳库来实现的.高潮滩互花米草和芦苇群落的年均土壤呼吸强度分别为（210.02±4.90）,（157.79±6.39）mg/（m²·h）;低潮滩互花米草和海三棱藨草群落年均土壤CO₂排放速率分别为（157.41±5.27）,（110.90±5.16）mg/（m²·h）,表明互花米草入侵显著增加长江口湿地的土壤呼吸.上述结果意味着互花米草入侵同时增加土壤碳输入和碳输出,但入侵也显著增加了土壤碳库表明入侵增加的土壤碳输入显著高于增加的土壤碳输出.本研究表明互花米草入侵可能会增强了长江河口湿地的土壤碳汇强度和固碳能力.但仍然需要长期系统的监测研究,以便全面定量评估互花米草入侵我国滨海湿地的综合生态影响.