N，N－二甲基甲酰胺在血液中代谢物S－（N－甲基氨基甲酰）谷胱甘肽的气质联用方法

根据先将ＳＭＧ转化为乙基、Ｎ－甲基氨基酸盐（ＥＭＣ），然后以气相色谱－质谱联用手段测定所产生的ＥＭＣ的原理，发展出一种定量检测大鼠血清中ＳＭＧ及其他Ｎ－甲基氨基甲酸硫酯类物质的分析方法．方法采用人工合成的ＳＭＧ和ＥＭＣ进行标定，每次测定需要样品量为０．５ｍＬ，方法的合理检出极限为ｃ（ＳＭＧ）＝１０μｍｏｌ／Ｌ．     

N,N—二甲基甲酰胺在血液中代谢物S—（N—甲基氨基甲酰）谷胱…

根据先将ＳＧＭ转化为乙基、Ｎ－甲基氨基酸盐（ＥＭＣ），然后以气相色谱－质谱联用手段测定所产生的ＥＭＣ的原理，发展出生种定量检测大鼠血清中ＳＭＧ及其他Ｎ－甲基氨基甲酸硫酯类物质的分析方法。方法采用人工合成的ＭＳＧ和ＥＭＣ进行标定，每次测定需要样品量为０．５ｍＬ，方法的合理检出极限为ｃ（ＳＭＧ）＝１０μｍｏｌ／Ｌ。     

单甲脒农药对土壤微生物种群和土壤酶活性的影响

研究了单甲脒（Ｎ＇－２，４－二甲苯基－Ｎ－甲基甲脒，简称ＤＭＡ）对土壤微生物种群和土壤酶活性的影响．田间试验表明，喷洒单甲脒盐酸盐（ＤＭＡＨ）于棉花植株对土壤微生物种群和土壤酶活性无明显影响．实验室试验表明，投加ＤＭＡＨ于土壤对土壤微生物种群有不同的抑制作用；当ＤＭＡＨ在土壤中的浓度为２０ｍｇ／ｇ时，好氧异养菌总量开始降低，硝化细菌和放线菌、真菌的土壤ＤＭＡＨ抑制浓度分别为０．５ｍｇ／ｇ和０．１ｍｇ／ｇ．ＤＭＡＨ对土壤酶活性的影响亦不相同，脱氢酶对土壤中ＤＭＡＨ含量为１０ｍｇ／ｇ时其活性即有明显的减弱，而过氧化氨酶对ＤＭＡ的耐受性相当高，其活性的抑制浓度达５００ｍｇ／ｇ．试验还证明了土壤中ＤＭＡ的微生物降解作用．当ＤＭＡ在土壤中的浓度为５０～５００ｇ／ｇ时，其消解速率可从８．７５ｍｍ·ｋｇ－１·ｄ－１提高到４８ｍｇ·ｋｇ－１·ｄ－１．     

土壤中水溶性有机碳与铜的相互影响

通过向土壤溶液中加入Ｃｕ２＋和可溶性有机碳(ＤＯＣ),研究它们之间的相互作用．结果发现,加入铜可以显著改变土壤水溶性有机碳(ＷＳＯＣ)的吸着平衡,并降低了其水溶性．影响程度在０．８ｍｍｏｌ·ｌ－１Ｃｕ以下随铜浓度的增加而增加．加入０．５ｍｍｏｌ·ｌ－１铜的土壤中 ＷＳＯＳ含量从 ０．２７ｍｇ Ｃ·ｇ－１降至０．０４７ｍｇ Ｃ·ｇ－１,吸着系数从６．６×１０－３ｌ·ｇ－１降至３．３×１０－３ｌ·ｇ－１．另一方面,用Ｆｒｅｕｎｄｌｉｃｈ方程描述铜离子在土壤中的吸附行为(液相浓度单位取ｍｍｏｌ·ｌ－１,固相浓度取ｍｍｏｌ·ｇ－１土),ｋ＝９．ｌ×１０－３;ｎ＝３．４０． 加入ＤＯＣ后,ｋ＝９．２×１０－３;ｎ＝３．６６,没有明显改变土壤对铜的吸附性能．加入小同浓度的ＤＯＣ,结果仍说明该浓度范围内ＤＯＣ(＜８ｍｇ Ｃ·ｌ－１)的加入没有明显改变土壤对铜的吸附性能．     

垃圾填埋场渗滤液处理工艺研究

通过对垃圾填埋处理场渗滤液的处理工艺研究,并根据渗滤液的特性建立一套适合我国实际的 Ａ— Ｏ— Ｃ— Ｃ Ｌ 处理工艺．试验研究结果表明,出水ρ（ Ｃ Ｏ Ｄ Ｃｒ） ＝ ２０５ ．６ ｍｇ Ｌ－ １ 、ρ（ Ｂ Ｏ Ｄ５） ＝ １８ ．２ ｍｇ Ｌ－ １ 、ρ（ Ｎ Ｈ３ － Ｎ） ≈０ｍｇ Ｌ－ １ 、色度＝ ４０（ 倍） 、ｎ（ 大肠菌群数） ＝ ２００ 个 Ｌ－ １ ．达到 Ｇ Ｂ１６８８９ － １９９７《生活垃圾填埋污染控制标准》中对垃圾渗滤液排放要求的二级标准     

微生物制剂EM控制鸡粪堆制过程恶臭的研究

以上海阿妮优美容保健品有限公司提供的微生物制剂──环境有用微生物群（简称ＥＭ）作为添加剂进行鸡粪堆肥腐熟对比试验，结果差异明显。ＥＭ处理的堆肥中ＮＨ－Ｎ含量比对照下降４１．８６％（１０ｄ）～５６．７１％（２０ｄ），ＮＨ－Ｎ散发量明显减少，且在后期有较强酿酒芳香味逸出，除臭效果显著。ＥＭ处理能加速堆肥腐熟，减少氮的气态损失，并可将无害化处理时间缩短到２０ｄ。这些作用是由ＥＭ引入的外源微生物所引起的。     

原生质体转化构建有机磷农药降解工程菌

降解有机磷农药甲胺磷、敌敌畏和对硫磷的菌株地衣芽孢杆菌 Ｐ１２（ Ｂａｃｉｌｌｕｓｌｉｃｈｅｎｉｆｏｒｍｉｓ） 经溶菌酶处理获得原生质体,加入降解乐果的供体菌 Ｇ１ Ｄ Ｎ Ａ,经ρ（ Ｐ Ｅ Ｇ６ ０００） ＝ ３００ ｇ Ｌ－ １ 诱导,在液体再生培养基中振荡培养ｔ＝ ２０ ｈ ,使其恢复细胞壁后,离心收集菌体,涂布于含乐果的基础培养基上,经筛选得一转化子 Ｊ Ｐ Ｚ．其菌落形态明显不同于出发菌株,乐果平板连续传代１０ 次,性状保持稳定．在θ＝ ３０ ℃,１００ ｒ／ｍｉｎ 的培养条件下,３ ｄ 内对ρ（ 甲胺磷） ＝ ０ ．５ ｇ Ｌ－ １ ,ρ（ 敌敌畏） ＝ ０ ．２ ｇ Ｌ－ １ ,ρ（ 对硫磷） ＝ ０ ．１ ｇ Ｌ－ １ ,ρ（ 乐果） ＝ ０ ．３ ｇ Ｌ－ １ 的降解率分别为 Ｒｄ ＝ ７９ ．１ ％ ,４６ ．７ ％ ,２９ ．４ ％ 和４６ ．４ ％ ．     

流动注射荧光分析法用于土壤及水系沉积物中铈（Ⅲ）含量的测定

研究表明Ｃｅ＾３＋在ｐＨ〈６．２ＫＣｌ介质中以２５４．０ｎｍ紫外光激发时，在３５２．０ｎｍ处发出具有恒定强度的荧光。因而可选择ｐＨ５－６作为测定酸度条件，利用Ａｌ２（ＳＯ４）３消除Ｆｅ＾３＋等离子的干扰，建立起Ｃｅ＾３＋的流动注射荧光分析法。方法的线性范围是２．０×１０＾－７—２．０×１０＾－６ｍｏｌ／ｌ，一元回归方程△Ｆ＝６６３６００Ｃ－０．０４１（ｎ＝１０，ｒ＝０．９９９７），检测限６．０×１     

N—N—二（1—甲基—庚基）乙酰胺萃取苯酚的动力学研究

用恒界面池法研究了Ｎ,Ｎ－二（１－甲基－庚基）乙酰胺（ＤＭＨＡＡ,Ｎ５０３）萃取苯酚的动力学,试验表明,萃取速率随水相苯酚浓度,有机相Ｎ５０３浓度的提高而增加,当水相ｐＨ值≥１０．５时,萃取速度明显下降,萃取反应的表观活化能为１４．３ｋＪ·ｍｏｌ＾－１,萃取过程属扩散控制,水相中萃酚向两相界面的扩散是萃取速度的控制步骤。     

吸水链霉菌井冈变种JG5008转化系统的初建

吸水链霉菌井冈变种ＪＧ５００８的最佳转化条件是：ＪＧ５００８在添加ＭｇＣｌ２（ｃｆ＝０．００５ｍｏｌ／Ｌ）和甘氨酸（ρｆ＝０．５ｇ／Ｌ）的含１０％蔗糖的ＹＥＭＥ培养基中接种浓度ｎ≈１０＾８ｍＬ＾－１的ＪＧ５００８孢子悬液，３７℃摇床培养１２ｈ，收获菌丝体。在３２℃、溶菌酶浓度ρ＝２ｍｇ／ｍＬ的条件下溶菌１ｈ后制备原生质体，用Ｔ缓冲液在Ｒ２ＹＥ培养基上进行转化。本文初步建立了ＪＧ５００８的质粒载体系     

N fertilization effects on denitrification and N cycling in an aggrading forest.

We investigated N cycling and denitrification rates following five years of N and dolomite amendments to whole-tree harvested forest plots at the long-term soil productivity experiment in the Fernow Experimental Forest in West Virginia, USA. We hypothesized that changes in soil chemistry and nutrient cycling induced by N fertilization would increase denitrification rates and the N2O:N2 ratio. Soils from the fertilized plots had a lower pH (2.96) than control plots (3.22) and plots that received fertilizer and dolomite (3.41). There were no significant differences in soil %C or %N between treatments. Chloroform-labile microbial biomass carbon was lower in fertilized plots compared to control plots, though this trend was not significant. Extractable soil NO3- was elevated in fertilized plots on each sample date. Soil-extractable NH4+, NO3-, pH, microbial biomass carbon, and %C varied significantly by sample date suggesting important seasonal patterns in soil chemistry and N cycling. In particular, the steep decline in extractable NH4+ during the growing season is consistent with the high N demands of a regenerating forest. Net N mineralization and nitrification also varied by date but were not affected by the fertilization and dolomite treatments. In a laboratory experiment, denitrification was stimulated by NO3- additions in soils collected from all field plots, but this effect was stronger in soils from the unfertilized control plots, suggesting that chronic N fertilization has partially alleviated a NO3- limitation on denitrification rates. Dextrose stimulated denitrification only in the whole-tree-harvest soils. Denitrification enzyme activity varied by sample date and was elevated in fertilized plots for soil collected in July 2000 and June 2001. There were no detectable treatment effects on N2O or N2 flux from soils under anaerobic conditions, though there was strong temporal variation. These results suggest that whole-tree harvesting has altered the N status of these soils so they are less prone to N saturation than more mature forests. It is likely that N losses associated with the initial harvest and high N demand by aggrading vegetation is minimizing, at least temporarily, the amount of inorganic N available for nitrification and denitrification, even in the fertilized plots in this experiment.     

Green synthesis of symmetrical N, N′-disubstituted thiourea derivatives in water using solar energy

Thioureas are of importance in medicinal chemistry due to their biological activities such as antituberculosis, anti-HIV, analgesic, anti-inflammatory, antimicrobial, antiarrhythmic, fungicide, herbicides, rodenticides and as phenoloxidase enzymatic inhibitors. Treatment of primary and secondary amines with thiophosgene is the common method of making symmetrical disubstituted thioureas. However, this method is hazardous due to the toxic properties of thiophosgene. Here, we report a green, operationally simple approach for the synthesis of 1, 3-disubstituted thiourea derivatives in moderate to excellent yields of 57–99 %. We use primary amines and CS₂ in water without any catalyst and solar thermal energy. This method is more environmentally benign and energy-saving compared with previously reported methods.     

Plant diversity, CO2, and N influence inorganic and organic N leaching in grasslands

In nitrogen (N)-limited systems, the potential to sequester carbon depends on the balance between N inputs and losses as well as on how efficiently N is used, yet little is known about responses of these processes to changes in plant species richness, atmospheric CO2 concentration ([CO2]), and N deposition. We examined how plant species richness (1 or 16 species), elevated [CO2] (ambient or 560 ppm), and inorganic N addition (0 or 4 g x m(-2) x yr(-1)) affected ecosystem N losses, specifically leaching of dissolved inorganic N (DIN) and organic N (DON) in a grassland field experiment in Minnesota, USA. We observed greater DIN leaching below 60 cm soil depth in the monoculture plots (on average 1.8 and 3.1 g N x m(-2) x yr(-1) for ambient N and N-fertilized plots respectively) than in the 16-species plots (0.2 g N x m(-2) x yr(-1) for both ambient N and N-fertilized plots), particularly when inorganic N was added. Most likely, loss of complementary resource use and reduced biological N demand in the monoculture plots caused the increase in DIN leaching relative to the high-diversity plots. Elevated [CO2] reduced DIN concentrations under conditions when DIN concentrations were high (i.e., in N-fertilized and monoculture plots). Contrary to the results for DIN, DON leaching was greater in the 16-species plots than in the monoculture plots (on average 0.4 g N x m(-2) x yr(-1) in 16-species plots and 0.2 g N x m(-2) x yr(-1) in monoculture plots). In fact, DON dominated N leaching in the 16-species plots (64% of total N leaching as DON), suggesting that, even with high biological demand for N, substantial amounts of N can be lost as DON. We found no significant main effects of elevated [CO2] on DIN or DON leaching; however, elevated [CO2] reduced the positive effect of inorganic N addition on DON leaching, especially during the second year of observation. Our results suggest that plant species richness, elevated [CO2], and N deposition alter DIN loss primarily through changes in biological N demand. DON losses can be as large as DIN loss but are more sensitive to organic matter production and turnover.     

N2O emission from a sequencing batch reactor for biological N and P removal from wastewater

Nitrous oxide （N2O） is a greenhouse gas that can be released during biological nitrogen removal from wastewater. N2O emission from a sequencing batch reactor （SBR） for biological nitrogen and phosphorus removal from wastewater was investigated, and the aims were to examine which process, nitrification or denitrification, would contribute more to N2Oemission and to study the effects of heterotrophic activities on N2O emission during nitrification. The results showed that N2O emission was mainly attributed to nitrification rather than to denitrification. N2O emission during denitrification mainly occurred with stored organic carbon as the electron donor. During nitrification, NaO emission was increased with increasing initial ammonium or nitrite concentrations. The ratio of N2O emission to the removed ammonium nitrogen （N2O- N/NH4-N） was 2.5% in the SBR system with high heterotrophic activities, while this ratio was in the range from 0.14% to 1.06% in batch nitrification experiments with limited heterotrophic activities.     

Recovery of plant diversity following N cessation: effects of recruitment, litter, and elevated N cycling

Plant species richness has declined and composition shifted in response to elevated atmospheric deposition of biologically active nitrogen over much of the industrialized world. Litter thickness, litter nitrogen (N) content, and soil N mineralization rates often remain elevated long after inputs cease, clouding the prospects that plant community diversity and composition would recover should N inputs be reduced. Here we determined how N cycling, litter accumulation, and recruitment limitation influenced community recovery following cessation of long-term N inputs to prairie-like grasslands. We alleviated each of these potential inhibitors through a two-year full-factorial experiment involving organic carbon addition, litter removal, and seed addition. Seed addition had the largest effect on increasing seedling and species numbers and may be necessary to overcome long-term burial of seeds of target perennial grassland species. Litter removal increased light availability and bare sites for colonization, though it had little effect on reducing the biomass of competing neighbors or altering extractable soil N. Nonetheless, these positive influences were enough to lead to small increases in species richness within one year. We found that, although C addition quickly altered many factors assumed favorable for the target community (decreased N availability and biomass of nearby competitors, increased light and site availability), these changes were insufficient to positively impact species richness or seedling numbers over the experimental duration. However, only carbon addition had species-specific effects on the existing plant community, suggesting that its apparent limited utility may be more a result of slow recovery under ambient recruitment rather than from a lack of a restorative effect. There were dramatic interactions among treatments, with the positive effects of litter removal largely negated by carbon addition, and the positive effects of seed addition generally amplified by litter removal. It remains unclear whether each mechanism explored here will induce community recovery, but over different temporal scales. Long-term monitoring will help resolve these remaining questions. Regardless, our results suggest that reversal of species loss and compositional shifts from N deposition in prairies may be more inhibited by habitat fragmentation, recruitment limitation, and long-term suppression of fire than from continued effects of elevated N.     

河套灌区地下水氮污染状况

河套灌区浅层地下水氮浓度和地下水埋深的季节变化规律调查结果表明:3月地下水NO3--N和TN浓度显著高于5、7和9月,地下水埋深也比5月和7月深。不同类型的井水N浓度差异较大:农田与庭院的井水NO3--N浓度显著高于村庄附近的井水,而NH4+-N和TN则表现为庭院井水浓度显著高于农田和村庄。地下水氮形态以NO3--N为主,全年17.1%的水井地下水NO3--N浓度高于10 mg.L-1,最高达184.4 mg.L-1。在灌溉量和其他生产条件相同的情况下,沙壕渠试验站农场内施肥区井水NO3--N浓度[(17.55±15.02)mg.L-1]明显高于未施肥区[(7.67±4.48)mg.L-1],且65.5%的水样NO3--N浓度超过WHO规定的生活饮用水NO3--N浓度上限值(10 mg.L-1),而未施肥区仅有27.6%的水样超标。井水NO3--N的来源主要为农田氮肥与动物粪肥,当地地下水NO3--N污染已不容忽视。     

农田N2O排放研究进展

农田土壤是大气中N2O的重要来源，与1990年相比，2000年我国氮肥用量升高了40％，因此，迫切需要对我国农田土壤N2O的排放通量作出新的估算。土壤理化性状的空间变异和不同生态条件下进行长期的、多点的农田N2O原位监测数据的匮乏成为提高N2O排放测定精度的制约因素。目前，航空采样法-驰豫涡动技术(微气象学方法)能够成功克服空间变异，且已经被成功应用在农业生态系统N2O排放的定量化观测上；另外Century-NGAS和DNDC模型是目前应用较广泛的机理模型，但应用不同模型所获得的N2O排放量相差较大。因此，今后农业土壤N2O排放的工作重点应集中在如何提高N2O原位观测精度，寻找合适的机理模型和提出相应的减排措施。     

湖滨带温室气体氧化亚氮(N2O)排放研究

利用不锈钢气体采集箱,在太湖梅梁湾湖区,沿水体至陆地方向对植被型和裸露型湖滨带进行温室气体N2O的原位排放观测。结果发现两种类型湖滨带N2O排放均显著高于临近的开阔水体,可以达到10~100倍,水位变幅区是湖滨带温室气体N2O排放的峰值区,是陆向和水向辐射区的5~10倍。在观测期间,N2O排放通量的范围为-159.2～1565.6μg·m-2·h-1,具有明显的时空梯度变化,时间上,9月份最高,随着气温的下降和芦苇的衰亡而逐渐减少,在1月份最低;空间上,自水向辐射区至陆向辐射区,先逐渐升高,在水位变幅区达到峰值,然后再降低。该结果初步说明了湖滨带是温室气体N2O的一个极其重要的排放源,而目前IPCC对水体N2O排放的估算可能存在很大的疏漏;同时也从一定程度上反映了湖滨带是湖泊脱氮的重要区域,其对缓解湖泊氮污染起到了举足轻重的作用。