COD负荷对MBSBBR脱氮除磷性能的影响研究

以模拟废水为处理对象,采用一套特定的MBSBBR系统,研究了COD负荷率对COD和NH4+-N去除率的影响,验证并分析了系统的SND现象。实验结果表明:COD负荷率为2.88～4.96kg/(m3·d)时,NH4+-N的去除率在70%左右,TP去除率在85%左右。系统对有机物具有良好的去除能力,可以承受较高的有机负荷率。系统中存在SND现象,反硝化菌大量存在,反硝化过程的碳源主要来自生物膜。系统的污泥产率较低,随着COD负荷率的增大而略有提高。     

类羧酸对棕壤中与氮素转化有关的生物活性的影响

类羧酸是一种带有羧基的化工副产品，其主要成分是二羧酸和三羧酸。具有较强的络合能力，可以用做螯合剂。文章通过室内培养实验，研究了类羧酸对棕壤中与氮素转化有关的生物活性的影响。结果表明类羧酸能显著抑制土壤脲酶活性，有效减少尿素水解产物氨的挥发损失；能促进土壤中含氮有机物的分解，并能抑制土壤中氨态氮向硝态氮的转化。另外施用类羧酸还能改善土壤中氮素的有效性，提高土壤的供氮能力。     

部分氮杂环类化合物的遗传毒性及其QSAR研究

本文利用蚕豆细胞微核试验评价了１０种氮杂环类化合物的遗传毒性，一化合物的最低未占据轨道能Ｅｌｕｍｏ、分子的量负的原子净电荷ｑ建立了较好的相关方程：ＭＮ＝－２．９６（１．１４）＋４．９３（０．４８）Ｅｌｕｍｏ＋１３．６８（２．７２）ｑ＾－Ｒ＾２＝０．９４ ＳＥ＝０．７１ Ｆ＝５３．９２ Ｐ〈０．０００５推测此类化合物的至于致毒机制可能是它们作为电荷给予体和氢键予体作用于生物受体而引起的突变。     

Optimum Nitrogen Use and Reduced Nitrogen Loss for Production of Rice and Wheat in the Yangtse Delta Region

A long-term field and lysimeter experiment under different amount of fertilizer-N application was conducted to explore the optimal N application rates for a high productive rice–wheat system and less N leaching loss in the Yangtse Delta region. In this region excessive applications of N fertilizer for the rice–wheat production has resulted in reduced N recovery rates and environment pollution. Initial results of the field experiments showed that the optimal N application rate increased with the yield. On the two major paddy soils (Hydromorphic paddy soil and Gleyed paddy soil) of the region, the optimal N application rate was 225–270 kg N hm^–2 for rice and 180–225 kg N hm^–2 for wheat, separately. This has resulted in the highest number of effective ears and Spikelets per unit area, and hence high yield. Nitrogen leaching in the form of NO ₃ ^– -N occurs mainly in the wheat-growing season and in the ponding and seedling periods of the paddy field. Its concentration in the leachate increased with the N application rate in the lysimeter experiment. When the application rate reached 225 kg N hm^–2, the concentration rose to 5.4–21.3 mgN l^–1 in the leachate during the wheat-growing season. About 60% of the leachate samples determined contained NO ₃ ^– -N beyond the criterion (NO ₃ ^– -N 10 mg l^–1) for N pollution. In the field experiment, when the N application rate was in the range of 270–315 kg hm^–2, the NO ₃ ^– -N concentration in the leachate during the wheat-growing season ranged from 1.9 to 11.0 mg l^–1. About 20% of the leachate samples reached close to, and 10% exceeded, the criterion for N pollution. Long-term accumulation of NO ₃ ^– -N from leaching will no doubt constitute a potential risk of N contamination of the groundwater in the Yangtse Delta Region.     

不同氮浓度下三角褐指藻生长特性和化学组成

三角褐指藻是一类海洋单细胞硅藻,富含多不饱和脂肪酸,可以作为鱼、虾、贝等理想的饵料。而近年该藻曾多次在我国沿海海域发生暴发性增殖,给当地生态环境带来了一定的影响。为了探讨不同氮浓度对三角褐指藻生长特性和化学组成的影响,设置了低氮(44 μ mol.L-1)、中氮(880 μmol.L-1)和高氮(4 400 μmol.L-1)浓度三种处理,着重测定三角褐指藻的细胞密度、比生长率、生物量、可溶性糖、蛋白质含量和叶绿素含量等指标。结果表明,高氮浓度明显地促进了藻细胞的生长繁殖。高氮浓度下的藻细胞密度、比生长率和生物量分别比低氮浓度下的提高了 5.38 倍、0.81 倍和 2.86 倍。藻生长前期,高氮浓度和中氮浓度下的生长曲线相似,呈现一个"S"型的曲线。另外,高氮浓度下的藻细胞可溶性糖、蛋白质和叶绿素a含量分别是低氮浓度下的 2.5 倍、1.5 倍和 15 倍,说明高氮浓度促进了藻细胞化学组成的转化和积累。结果揭示,氮浓度可能是导致三角褐指藻近年在我国沿海海域发生暴发性增殖的重要因素。     

珍稀植物濒危机制及保育策略中的营养条件

首先简要论述了珍稀植物濒危的原因、濒危机制的各种理论和研究方法，包括就地保护和迁地保护两个方面的保育策略的制定与实践。然后着重从营养条件的角度对这些理论和现状进行了分析。认为濒危物种在其历史演化过程中存在的脆弱环节以及活植物迁地保护的评价标准均与营养条件密切相关，营养条件可能是某些物种濒危机制中的一个重要组成部分；营养条件方面的研究可以为保护区设立的大小提出指导性意见；珍稀植物迁地保护过程中应密切关注营养条件的影响；营养条件在一定程度上决定了对某些物种保育策略的制定；将分子生物学与植物营养学的研究方法相结合，将能成为珍稀植物濒危机制及保育策略研究中的一种有效手段。     

Seasonal variations of organic-carbon and nutrient transport through a tropical estuary (Tsengwen) in southwestern Taiwan

This paper reports the fluvial fluxes and estuarine transport of organic carbon and nutrients from a tropical river (Tsengwen River), southwestern Taiwan. Riverine fluxes of organic carbon and nutrients were highly variable temporally, due primarily to temporal variations in river discharge and suspended load. The sediment yield of the drainage basin during the study period (1995–1996, 616 tonne km^–2 year^–1) was ca. 15 times lower than that of the long-term (1960–1998) average (9379 tonne km² year^–1), resulting mainly from the damming effect and historically low record of river water discharge (5.02 m³ s^–1) in 1995. The flushing time of river water in the estuary varied from 5 months in the dry season to >4.5 days in the wet season and about 1 day in the flood period. Consequently, distributions of nutrients, dissolved organic carbon (DOC) and particulate organic carbon (POC) were of highly seasonal variability in the estuary. Nutrients and POC behaved nonconservatively but DOC behaved conservatively in the estuary. DOC fluxes were generally greater than POC fluxes with the exception that POC fluxes considerably exceeded DOC fluxes during the flood period. Degradation of DOC and POC within the span of flushing time was insignificant and may contribute little amount of CO₂ to the estuary during the wet season and flood period. Net estuarine fluxes of nutrients were determined by riverine fluxes and estuarine removals (or additions) of nutrients. The magnitude of estuarine removal or addition for a nutrient was also seasonally variable, and these processes must be considered for net flux estimates from the river to the sea. As a result, nonconservative fluxes of dissolved inorganic phosphorus (DIP) from the estuary are –0.002, –0.09 and –0.59 mmol m^–2 day^–1, respectively, for dry season, wet season and flood period, indicating internal sinks of DIP during all seasons. Due to high turbidity and short flushing time of estuarine water, DIP in the flood period may be derived largely from geochemical processes rather than biological removal, and this DIP should not be included in an annual estimate of carbon budget. The internal sink of phosphorus corresponds to a net organic carbon production (photosynthesis–respiration, p–r) during dry (0.21 mmol m^–2 day^–1) and wet (9.5 mmol m^–2 day^–1) seasons. The magnitude of net production (p–r) is 1.5 mol m^–2 year^–1, indicating that the estuary is autotrophic in 1995. However, there is a net nitrogen loss (nitrogen fixation–denitrification < 0) in 1995, but the magnitude is small (–0.17 mol m^–2 year^–1).     

Fe~（2＋）和Mn~（2＋）对水稻锌吸收与运转的影响

水培试验结果表明，Ｆｅ（２＋）、Ｍｎ（２＋）对水稻锌的吸收和运转有明显的影响．高浓度Ｆｅ（２＋）或Ｍｎ（２＋）（５μｇ／ｇ）显著降低水稻吸锌量、抑制锌由根向茎、叶的运转．稻株生物量与叶片Ｆｅ／Ｚｎ比值或Ｍｎ／Ｚｎ比值有明显的负相关关系，在叶片Ｆｅ／Ｚｎ＞８或Ｍｎ／Ｚｎ＞２６时，水稻生物量明显降低．造成水稻缺锌的主要原因是土壤有效锌含量低，而高浓度Ｆｅ（２＋）和Ｍｎ（２＋）是诱发和加重水稻缺锌的重要条件．因此在生产上应重视改善缺锌低洼稻田的排水通气状况．     

Geophagy in the tropics: an appraisal of three geophagical materials

Geophagy, the deliberate consumption of soil, is a common practice amongst the world's poorer or more tribally oriented people of the tropics. An appraisal of three geophagical samples suggests that Fe is a mineral nutrient which can be supplied to humans in significant amounts via ingested soil. Geophagy provides a direct link between the geochemistry of soils and human health, but as yet this association has only a limited awareness amongst research workers.     

污泥颗粒化快速启动厌氧氨氧化反应器的探讨

厌氧氨氧化工艺处理成本低,被认为是有应用前景的废水脱氮技术.但是,厌氧氨氧化菌生长缓慢,厌氧氨氧化反应器启动困难.探讨了几种快速启动厌氧氨氧化反应器的方法,包括投加颗粒污泥、惰性载体、絮凝剂及多价阳离子等,并对其作用机理进行了分析.