鸭绿江口的溶解无机氮

本文讨论了１９９６年５月鸭绿江溶解无机氮的含量和分布变化特征，并同其他一些河口作了比较，鸭绿江口ＮＯ３－Ｎ，ＮＯ２－Ｎ，ＮＨ４－Ｎ的平均含量分别为５０．３．０．４５和３．０５μｍｏｌ／Ｌ，而丹东上游鸭绿江支流瑗河下降的溶解无机氮浓度很高，达２０３．４μｍｏｌ／Ｌ，主要由农业施用氮肥大量从耕用地中流失所致。     

外源稀土微肥对土壤氮磷养分的影响

通过小区试验和盆栽试验，研究了施加不同的浓度稀土微肥对土壤中有效氮、有效磷浓度以及土壤脲酶活性的影响。结果表明，施加高浓度稀土微肥将会影响土壤中有效氮和有效磷的浓度。在分析与之相关的土壤酶活性时发现，施加低浓度的稀土微肥（≤１ｍｇ／ｋｇ）促进土壤脲酶活性并增加土壤有效氮浓度，而施加高浓度稀土微肥（≥５ｍｇ／ｋｇ）则明显的抑制土壤脲酶活性并减少土壤有效氮浓度；施加稀土元素浓度与土壤有效磷浓度之间有较     

碳源循环单级生物脱氮技术研究

开发了一种列管式固定化细胞生物反应器，其特征在于硝化菌和反硝化菌被混合固定于中空的PVA凝胶管的管壁之中，PVA凝胶管平行置于圆柱形筒体内，构成一个类似于列管式换热器的生物脱氮反应器。需要处理的氨氮废水在固定化细胞管的外侧与圆柱形壳体的内侧间流动，而反硝化所需的碳源（乙醇水溶液）则在PVA凝胶管内循环。研究了列管式固定化细胞生物反应器进行单级生物脱氮的可行性和连续运行的效果，并证明了在非纯菌种的固定化细胞单级生物脱氮过程化细胞生物反应器进行单级生物脱氮的可行性和连续运行的效果，并证明了在非纯菌种的固定化细胞单级生物脱氮过程中，存在着NH^ 4→NO^-2→N2的短积生物脱氮。     

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。     

杭州城市及其边缘区湿地磷化学特征的研究

对杭州城市及其边缘区湿地土壤的磷形态组成、固磷能力和释放潜力等方面进行了初步的研究。结果表明,杭州城市及边缘地区的湿地由于受人类影响的不同及所处环境的差异,性质已有很大的分异。城区的西湖、水塘和河流底泥中磷的积累、磷的饱和度和零吸附磷平衡浓度均明显高于城市边缘地区的湿地;湿地土壤中的磷主要呈不稳定、或亚稳定态,可提取态磷约占总磷的80%,62%的湿地土壤磷饱和度在25%以上。最大磷吸附量的大小主要与湿地中无定形氧化铁、铝含量有关。零吸附时磷的浓度(EPC)较高,在0.10~2.48mg·L-1之间,具有较强的释放潜力。半透膜渗析法测得的磷释放量与磷积累呈正相关,但当磷饱和度超过25%时,其磷释放量显著增加。研究表明杭州市及其边缘区湿地土壤磷已普遍达到较高水平,这在一定程度上影响磷净化功能的正常发挥。     

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。     

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).