Effect of nutrient level on phytoplankton community structure in di erent water bodies

Increasing levels of pollution within water bodies can cause eutrophication and an associated rapid growth in and reproduction of phytoplankton. Although most frequently occurring in bodies of water such as lakes and dams, in recent years an increasing number of river systems in China have suffered serious algal blooms. The community structure of phytoplankton may differ, however, dependent on the hydrodynamic conditions and nutrient levels within the water body. The field investigation results obtained fro...     

Effects of metal lead on growth and mycorrhizae of an invasive plant species （Solidago canadensis L.）

It is less known whether and how soil metal lead (Pb) impacts the invasion of exotic plants.A greenhouse experiment was conducted to estimate the effects of lead on the growth and mycorrhizae of an invasive species(Solidago canadensis L.)in a microcosm system. Each microcosm unit was separated into HOST and TEST compartments by a replaceable mesh screen that allowed arbuscular mycorrhizal (AM) fungal hyphae rather than plant roots to grow into the TEST compartments.Three Pb levels(control,300,and 600 mg/kg soil)were used in this study to simulate ambient soil and two pollution sites where S. canadensis grows.Mycorrhizal inoculum comprised five indigenous arbuscular mycorrhizal fungal species (Glomus mosseae,Glomus versiform,Glomus diaphanum,Glomus geosporum,and Glomus etunicatum).The 15N isotope tracer was used to quantify the mycorrhizally mediated nitrogen acquisition of plants.The results showed that S. canadensis was highly dependent on mvcOrrhizae.The Pb additions significantly decreased biomass and arbuscular mycorrhizal colonization(root length colonized,RLC%) but did not affect spore numbers,N(including total N and 15N) and P uptake.The facilitating efficiency of mycorrhizae on nutrient acquisition was promoted by Pb treatments.The Pb was mostly sequestered in belowground of plant (root and rhizome).The results suggest that the high efficiency of mycorrhizae on nutrient uptake mightgive S. canadensis a great advantage over native species in Pb polluted softs.     

Nitrous oxide fluxes from upland soils in central Hokkaido, Japan

Nitrous oxide (N2O) fluxes from soils were measured using the closed chamber method during the snow-free seasons (middle April to early November),for three years,in a total of 11 upland crop fields in central Hokkaido,Japan.The annual mean N2O fluxes ranged from 2.95 to 164.17 μgN/(m2·h),with the lowest observed in a grassland and the highest in an onion field.The instantaneous N2O fluxes showed a large temporal variation with peak emissions generally occurring following fertilization and heavy rainfall eve...     

高效吸收氧化法处理炼油工业恶臭气体研究

以碳酸钠溶液为吸收液,对苯二酚为催化荆,研究了对炼油企业硫化氢恶臭气体的吸收氧化效果,考察了吸收氧化的影响因素、再生方法及再生效果。结果表明：高效氧化吸收法处理硫化氢恶臭气体效果很好,吸收液可循环使用。     

Spatial and temporal variation of below-ground N transfer from a leguminous tree to an associated grass in an agroforestry system

Nitrogen (N) transfer from leguminous trees can be a major N source for the associated crop in low-input agroforestry systems. The aim of this study was to identify the main climatic and soil factors controlling N transfer from the leguminous tree Gliricidia sepium (Jacq.) Walp to the associated grass Dichanthium aristatum (Poir.) C.E. Hubb, in a 16-year-old tropical agroforestry system. Nitrogen transfer was estimated using the natural ¹⁵N abundance method. Before tree pruning, total N transfer represented 57% of the N uptake of the grass, including 31% coming from N₂ fixation. The spatial variation induced by the tree was well described by soil organic N content (ON). In this system, ON is an index of soil available N as well as of tree root density. Rainfall (R) and evapotranspiration (ETP) were the main climatic factors controlling N transfer. Multiple regression analysis indicated that R, ETP and ON explained 79% of the temporal and spatial variation of N transfer. Transferred N cannot be estimated after pruning because of the change in the isotopic signature of the soil N source. This was related to N release from root turnover. The results suggest that grass showed a preferential uptake of N coming from the tree, which could be due to a lower energy cost compared to obtaining absorbed N from the clayey soil used in this work.     

浅谈N-（1-萘基）-乙二胺二盐酸盐对苯胺类测定的影响

实验就N-（1-萘基）-乙二胺二盐酸盐对苯胺类测定的影响进行探讨,结果表明,测定低浓度苯胺类样品时,N-（1-萘基）-乙二胺二盐酸盐的品质对测定产生重要影响,所以测定低浓度苯胺类样品时建议采用进口N-（1-萘基）-乙二胺二盐酸盐进行分析。     

A2N双污泥反硝化除磷系统微生物的先间歇后连续培养及快速启动

以实际生活污水为对象,研究了反硝化聚磷菌（DPB）的驯化培养以及A₂N双污泥反硝化除磷系统的快速启动.采用先独立培养反硝化聚磷菌和好氧硝化生物膜再连续运行的方式成功地快速启动了A₂N系统.采用污水处理厂除磷工艺中的活性污泥为种泥,在SBR系统中以先A/O（厌氧/好氧）后A/A（厌氧/缺氧）的方式运行,32 d成功地使反硝化聚磷菌成为优势菌属.在SBR反应器中,采用硝化效果较好的活性污泥为种泥,好氧硝化生物膜30 d挂膜成功,氨氮去除率稳定在99%以上.然后,A₂N系统连续运行,11 d后系统反硝化除磷效果进入稳定状态,出水氨氮和正磷酸盐浓度均为0,硝态氮为10.26 mg/L ,出水COD为19.56 mg/L ,COD、氨氮、总氮和磷去除率分别为91%、100%、77%和100%,说明A₂N系统具有很好的脱氮除磷效果,认为系统启动成功.     

SRT对于污水脱氮过程中N2O产生的影响

试验采用经过长期驯化,控制污泥龄分别为9d和15d的活性污泥,以实际生活污水为研究对象,考察了不同污泥龄(SRT)对污水脱氮过程中N2O的产生量和转化率的影响.结果表明N2O主要产生于污水脱氮的硝化过程中,而反硝化过程的贡献较少.较短的污泥龄有利于脱氮过程中N2O的产生,9d污泥龄的活性污泥系统产生N2O量是15d污泥龄污泥系统的1.2倍,分别为4.62mg·L-1和3.8mg·L-1.不同污泥龄条件下产生N2O的转化率也有所差别,污泥龄较短的活性污泥系统产生N2O的转化率也较高,分别为11.2%和7.8%.系统经长期在较短的污泥龄下运行,并没有影响系统的脱氮效果,两种污泥龄条件下系统的脱氮率都在96%以上.为了减少污水脱氮过程中N20的产生量,应避免污水处理系统过短的污泥龄,造成污水脱氮过程N2O的产量和转化率的大幅升高.     

氮输入对三江湿地小叶章不同生长阶段土壤产生CH_4能力的影响

在小叶章(Deyeuxia angustifolia)不同生长阶段,用室内鲜土培养法对土壤CH4的产生能力进行了研究.结果表明,氮输入后,植物各生长阶段的土壤CH4产生率均随时间的推移发生了明显的波动.从生长季(6月7日～8月24日)CH4产生率均值来看,不同氮输入水平对土壤CH4产生起促进作用;不同氮输入水平对植物不同生长阶段CH4产生率影响明显.第一(6月7日～7月2日)、第二(7月2日～7月20日)阶段适量的氮输入(6g.m-2)对CH4产生起促进作用,但过量氮输入(12g.m-2)会对CH4产生起抑制作用;而第三(7月20日～8月7日)、第四(8月7日～8月24日)阶段不同氮输入均对CH4产生起促进作用;氮输入后,土壤微生物量碳(MBC)、土壤微生物量氮(MBN)、土壤基础呼吸(BR)、土壤代谢熵(qCO2)、土壤诱导呼吸(SIR)、铵态氮(NH4+-N)、硝态氮(NO3--N)和植物地上生物量与土壤CH4产生的动态关系存在差异.土壤CH4产生与qCO2呈显著正相关(p0.01),与土壤MBN、TOC和地上生物量呈显著正相关(p0.05).     

高浓度氨氮消化污泥脱水液半短程硝化试验研究

采用A/O工艺考察了消化污泥脱水液半短程硝化及维持的影响因素和控制方法.结果表明,在温度9～20℃、平均DO浓度5.4 mg/L、SRT 30 d左右时,进水氨氮负荷（以N计,下同）0.64 kg/(m³·d)的条件下启动,经过29 d实现了短程硝化,此后的65 d内,动态控制反应器游离氨FA>4 mg/L时,70%亚硝氮累积率的短程硝化得以维持;在实现短程硝化的基础上,进而实现了半短程硝化,出水氨氮与亚硝氮浓度比维持在1∶1.32左右;当氨氮负荷降至0.19 kg/(m³·d)时(FA<1 mg/L),短程遭到破坏,在不同FA下取样做FISH分析,进一步证明了高FA是维持半短程硝化的主要因素;在进水中COD为282 mg/L, C/N仅为0.85的条件下,由于实现了短程硝化,系统TN去除量约为91 mg/L.结果分析表明,消化污泥脱水液在中低温、高DO浓度、长SRT下,通过动态控制氨氮负荷和pH值等运行参数,在系统中维持适宜的FA浓度(>4 mg/L),可以实现并维持半短程硝化,为后续的厌氧氨氧化提供进水或回流到污水厂主流区而节省反硝化碳源.