SRT对UCT-MBR反硝化除磷性能与膜污染行为的影响

采用脱氮除磷膜生物反应器(UCT-MBR)工艺处理冀南地区城市污水,考察了SRT对UCT-MBR工艺反硝化除磷性能与膜污染行为的影响.结果表明:较短(15d)与较长(40d)SRT均不利于反硝化聚磷菌(DPAOs)的富集;SRT控制在25d时系统的反硝化除磷性能得到最大程度强化,反硝化聚磷菌(DPAOs)占聚磷菌(PAOs)的数量比例及缺氧除磷率达到最大值,分别稳定在50.9%和88%,并且此时系统总磷(TP)、总氮(TN)去除率也达到最大值91.7%、73.6%,出水浓度分别稳定在0.48, 13.3mg/L左右;SRT对系统COD、氨氮(NH₄⁺-N)的去除效能影响不大,COD、NH₄⁺-N平均去除率分别为89.8%、99.7%,出水浓度分别稳定在30.8, 0.15mg/L;随着SRT的延长,膜池混合液固体(MLSS)浓度升高,分子量大于100kDa、小于1kDa的溶解性微生物代谢产物(SMP)浓度和胞外聚合物(EPS)比污泥浓度升高及污泥粒径(PSD)减小,是导致膜池污泥可滤性变差的主要原因,从而致使系统膜渗透性加速降低、持续运行周期缩短,而红外光谱(FT-IR)分析表明SRT对膜污染物质的组成无显著影响,光谱折射率与SMP、EPS含量呈现一致性.     

基于TASCC的典型农田溪流氨氮滞留及吸收动力学模拟

为揭示农田溪流氨氮滞留的动态变化性,选择NaCl为保守示踪剂、NH4Cl为添加营养盐开展野外瞬时投加示踪实验.在此基础上,采用TASCC方法和养分螺旋指标定量刻画 滞留动态,并以Michaelis-Menten模型(M-M方程)模拟 吸收动力学特性.结果表明:背景浓度的 吸收长度Sw-amb变化范围为93.94~295.54m,平均值为177.41m;质量传输系数Vf-amb变化范围为0.16~0.38mm/s,平均值为0.26mm/s;吸收速率Uamb变化范围为0.16~0.38mg/(m2×s),平均值为0.26mg/(m2×s).由M-M方程模拟得到的 最大吸收速率Umax为0.59~1.38mg/(m2×s),半饱和常数Km为1.10~5.03mg/L. 在从背景浓度到饱和浓度区间范围内展现出的Sw-add-dyn、Utot-dyn和Vf-tot-dyn动态变化性,验证了TASCC解析 滞留动态和吸收动力学特征的可行性和有效性.     

Modeling forest floor contribution to phosphorus supply to maritime pine seedlings in two-layered forest soils

The quantitative contribution of the forest floor to P nutrition of maritime pine seedlings was experimentally determined by Jonard et al. (2009) in a greenhouse experiment using the radio-isotopic labeling. To extend the results of the experiment on a known mineral soil, a modeling approach was developed to predict P uptake of maritime pine seedlings growing in a mineral soil covered with a forest floor layer. The classical nutrient uptake model based on the diffusion/mass-flow theory was extended to take into account mineralization of P in dead organic matter, microbial P immobilization and re-mineralization and P leaching. In addition, the buffer power characterizing the P retention properties of the mineral soil was allowed to vary with time and with the P-ion concentration in solution. To account for increasing root competition with time, a moving boundary approach was implemented. According to the model, the forest floor contributed most of the P supply to the seedlings (99.3% after 130 days). Predicted P uptake was consistent with observed P uptake and modeling efficiency was 0.97. The uptake model was then used to evaluate the impact of the P retention properties of the mineral soil on the contribution of the forest floor to P uptake. Simulations showed that the contribution of the forest floor was much lower in the quasi non-reactive soil (45.7%) but rapidly increased with soil P reactivity.     

镉胁迫对龙葵幼苗氮代谢及其相关酶活性的影响

采用营养液培养方法,研究了系列镉浓度处理对龙葵（Solanum nigrumL）幼苗氮代谢的影响。结果表明：龙葵根系可溶性蛋白质较叶片受Cd影响更大。龙葵植株叶片和根系NO3--N含量、硝酸还原酶（NR）、谷氨酰胺合成酶（GS）活性均随镉浓度提高而先增后降,且随处理时间的延长而逐渐下降。叶片NO3--N含量和NR活性均在25μm镉处理8d后达到峰值,而根系NO3--N则在50μm镉处理8d后最高。叶片NO3--N含量受镉处理影响较根系稍大。然而,龙葵叶片中NH4＋-N含量随镉浓度升高和时间延长逐渐升高,100μm镉处理16d后最高,表明镉胁迫下龙葵叶片铵态氮富集效应明显。龙葵叶片和根系中谷氨酸脱氢酶（GDH）活性随镉处理浓度提高和处理时间延长而逐渐升高,100μm镉处理16d后达到峰值。     

碳氮比对悬浮填料生物反应器氮去除效果的影响

文章研究了C/N对悬浮填料生物反应器脱氮效果的影响。出水中NH4+-N、NO2--N和NO3--N浓度以及pH值变化均受C/N的影响,实验得到的最佳C/N质量比为12∶1,TN去除率平均在85%。     

Assessing and Monitoring the Health of Western Rangeland Watersheds

The most important function of watersheds in the western U.S. is the capacity to retain soil and water, thereby providing stability in hydrologic head and minimizing stream sediment loads. Long-term soil and water retention varies directly with vegetation cover. Data on ground cover and plant species composition were collected from 129 sites in the Rio Grande drainage of south-central New Mexico. This area was previously assessed by classification of Advanced Very High Resolution Radiometry (AVHRR) imagery. The classification of irreversibly degraded sites failed to identify most of the severely degraded sites based on size of bare patches and 35% of the sites classified as degraded were healthy based on mean bare patch size and vegetation cover. Previous research showed that an index of unvegetated soil (bare patch size and percent of ground without vegetative cover) was the most robust indicator of the soil and water retention function. Although the regression of mean bare patch size on percent bare ground was significant (p < 0.001), percent bare ground accounted for only 11% of the variability in bare patch size. Therefore bare patch size cannot be estimated from data on percent bare ground derived from remote sensing. At sites with less than 25% grass cover, and on sites with more than 15% shrub cover, there were significant relationships between percent bare soil and mean bare patch size (p < 0.05). Several other indicators of ecosystem health were related to mean bare patch size: perennial plant species richness (r = 0.6, p < 0.0001), percent cover of increaser species (r = 0.5, p < 0.0001) and percent cover of forage useable by livestock (r = 0.62, p < 0.0001). There was no relationship between bare patch size and cover of species that are toxic to livestock. In order to assess the ability of western rangeland watersheds to retain soil and water using remote sensing, it will be necessary to detect and estimate sizes of bare patches ranging between at least 0.5 m in diameter to several meters in diameter.     

福建泉州市东、西湖水体中氮的空间分布研究

初步探讨了东湖和西湖水体中氯的空间分布特征以及3种不同形态的氮与溶解氧的相关性.结果表明,(1)泉州东湖、西湖水体中总氮的平均含量分别为3.396、3.929mg/L,氨氮的平均含量分别为1.927、2.182mg/L,硝酸盐氮的平均含量分别为1.061、1.236mg/L,亚硝酸盐氮的平均含量分别为0.084、0.059 mg/L,东湖和西湖水体的主要氮素形式均是氨氮.(2)东湖出水口和位于动物园附近的采样点总氮、氨氮和亚硝酸盐氮浓度较其它采样点高,入水口、湖区北部及湖心区采样点的氨氤和硝酸盐氮的分布趋势基本一致.西湖东南部采样点总氮、氨氯、硝酸盐氯和亚硝酸盐氮的含量都较其它采样点高.(3)东湖水体的DO浓度与氨氛、硝酸盐氮和亚硝酸盐氯的含量都不具有相关性,而西湖水体的DO浓度与这3种形态氮显著相关.     

Testing differences in methods of preparing moss samples

The main objective of this research was to estimate the total mass of nitrogen discharged from various sources in Korea using the mass balance approach. Three different nitrogen mass balances were presented: (1) agricultural activities including raising crops and animal husbandry; (2) domestic activities, and (3) activities in forest and urban areas. These nitrogen balances were combined to estimate riverine discharge of nitrogen to the ocean in national scale. Nitrogen inputs include atmospheric deposition, biological nitrogen fixation, application of inorganic fertilizers/manures, animal feed/imported foodstuffs, and meat/fish. Nitrogen outputs include ammonia volatilization, denitrification, human/animal waste generation, crop/meat production, and riverine discharge to the ocean. The estimated total nitrogen input in Korea was 1,194.5 × 10³ tons N/year. Nitrogen discharged into rivers was estimated as 408–422 × 10³ tons N/year, of which 66–71% was diffuse in origin. The estimated diffuse discharges for land uses were estimated as 82 × 10³ tons N/year from agricultural areas, 7 × 10³ tons N/year from forestry and 75 × 10³ tons N/year from urban and industrial areas.     

氮氧化物的污染控制对策

详细地介绍了日本针对不同的排放源－－固定源和流动源－－所采取的氮氧化物污染控制对策。对固定源,在实施全国统一的排放标准的基础上,对于一些工厂相对集中、污染问题严重的地区实施总量控制,同时积极促进技术革新以及降低氮氧化物的排放;对流动源所采取的措施有,确定不同车型汽车排放尾气递减的短期目标和长期目标,实施汽车氮氧化物法,积极推进低公害车的普及。通过采取上述措施,在日本,固定源排放的氮氧化物得到了较好