Ce(Ⅲ)对UV-B辐射胁迫下大豆幼苗光化学反应的影响

用水培法研究Ce(Ⅲ)对UV-B辐射胁迫下大豆幼苗光化学反应的影响.结果表明, 20 mg·L^-1 CeCl₃使大豆幼苗净光合速率(Pn)、Hill反应、Mg²⁺-ATPase活性与光合磷酸化活力4项指标较对照提高23.2%～14.3%; 有效抑制UV-B辐射(T₁=0.15 W·m^-2和T₂=0.45 W·m^-2)胁迫下4项指标下降, 4项指标降幅［Ce(Ⅲ)+T₁为36.6%～15.9%,Ce(Ⅲ)+T₂为65.6%～33.2%］小于对应的UV-B辐射组(T₁为50.9%～23.3%,T₂为77.3%～51.4%). 动态变化显示, Ce(Ⅲ)减缓了胁迫期4项指标的下降趋势,促进了恢复期4项指标上升幅度. 说明Ce(Ⅲ)通过减轻UV-B辐射对大豆幼苗光化学反应的伤害, 遏制UV-B辐射胁迫下大豆幼苗Pn下降.     

SBR反应器中有机物去除与硝化反硝化过程INT-ETS活性变化

通过检测不同进水氨氮浓度和有机物浓度下的SBR工艺系统的INT-ETS活性,研究了SBR工艺去除有机物与硝化反硝化过程中污泥生物活性的变化规律.结果表明,INT-ETS活性可以有效地表征SBR工艺系统的生化反应进程;SBR工艺一个反应周期内,有机物降解、硝化和反硝化阶段生物活性依次降低;当进水COD为300 mg/L,氨氮为40 mg/L时,系统的INT-ETS活性从232.59 mg/(g·h)下降到190.65 mg/(g·h),最终降至113.88 mg/(g·h);伴随有机物的去除和硝化反硝化的进程,INT-ETS活性一般会出现特征点,预示着不同反应阶段的开始与结束;通过不同进水氨氮浓度(14.5 mg/L 和42.0 mg/L)和有机物浓度(COD为293 mg/L 和685 mg/L)的试验,发现运行条件的变化并未明显改变SBR系统的INT-ETS活性变化规律,但会影响INT-ETS活性曲线上标志不同反应阶段的特征点出现时间.     

施工工地出口附近道路交通扬尘排放特征研究

为了量化施工工地附近社会道路因施工运输车辆带泥及遗撒造成的二次交通扬尘,对4个典型工地出口2个方向社会道路尘负荷进行了采样分析,根据AP-42交通扬尘排放模型,计算和分析了工地出口附近道路交通扬尘排放特征.结果表明,工地出口附近道路尘负荷高于正常道路,随着距离工地出口长度的增加,尘负荷逐渐减小;工地出口2个方向共400 m道路上交通扬尘PM₁₀排放因子为正常道路的2～10倍,因施工增加的排放量相当于422～3?800 m正常道路排放.根据以上结果,结合2002年北京市施工工地时空分布数据,经计算得出,2002年北京市城八区工地出口形成的二次扬尘相当于增加了道路总长度的59%.     

磁场对酪氨酸酶活性及其催化降解酚类有机物影响的研究

研究了恒磁场对酪氨酸酶(TYR)活性及其催化降解酚类有机物的影响.结果显示,不同磁场强度(10～350 mT)处理下TYR酶活性均有提高,最佳磁场强度150mT下酶活力提高了27.1%.不同磁化时间下TYR酶活都有上升,但磁化60min后酶活上升幅度有所下降.酶经磁场处理后对温度、pH值稳定性增强,在温度为20～35 ℃、pH为5.0～10.0时均能保持较高活性,最佳温度为25℃,最佳pH为7.0;磁化后TYR酶的Michaelis常数Km为3.83 mmol·L-1,未磁化的Michaelis常数Km为2.65 mmol·L-1.磁场作用可促进TYR对酚类有机物邻苯二酚、苯酚、2,4-二氯酚的转化,反应速度依次递减,磁化处理对邻苯二酚反应的促进作用尤其明显;磁化处理后的酶对不同浓度苯酚和2,4-二氯酚的去除率均明显高于未磁化处理的酶,且随着酶用量增加,酚去除率提高.荧光发射光谱分析表明,磁化酪氨酸酶的荧光强度增强,构像发生了变化.     

城市污水生物处理系统中微生物酶的活性及其分布

通过水解模式底物进行分光光度测定的方法,研究了城市污水生物处理系统中微生物酶的活性.选取亮氨酸氨基肽酶、β-葡萄糖苷酶、碱性磷酸酶和脂酶等胞外酶进行分析,结果发现4种胞外酶的平均活性在31.O～88.5 μmol/(L·h),其中76.9%～94.8%的酶活性分布在活性污泥中,说明绝大部分胞外酶是与细胞相连或固定在细胞外多聚絮体基质里.混合水样和出水水样中的DOC几乎相等,而各胞外酶与DOC不存在任何显著的相关关系.增加NO3-浓度可提高亮氨酸氨基肽酶和β-葡萄糖苷酶的活性,但对碱性磷酸酶和脂酶却有明显的抑制作用.     

高效降解微囊藻毒素食酸戴尔福特菌USTB-04的培养与活性研究

主要针对筛选的高效降解微囊藻毒素(microcystins,MCs)的食酸戴尔福特菌USTB-04(Delftia acidovorans,DA菌)的培养方法进行了研究.结果表明,以葡萄糖、甘油和乙醇作为惟一碳源时,与氯化铵和尿素相比,酵母粉是支持DA菌生长的较好氮源.在以酵母粉作为惟一氮源时,与甘油和乙醇相比,葡萄糖是提高DA菌生长速度的较好碳源.进一步研究显示,以葡萄糖和酵母粉作为碳源和氮源时,可以支持DA菌的快速稳定生长,但在以甘油和酵母粉作为碳源和氮源时.培养出的DA菌降解MCs的比活性最高.此研究在培养高细胞浓度DA菌作为生物催化剂用于饮用水源中的MCs去除方面具有重要意义.     

太阳活动变化与新型冠状病毒肺炎疫情的发展

已有研究表明,新型冠状病毒肺炎(以下简称"新冠肺炎")和以往的传染病大流行与太阳活动存在着密不可分的关系.但是究竟存在什么样的关系,尚未形成一致的意见.并且这些研究大多关注于大流行事件发生的年份与太阳活动周峰谷值年份之间的对应关系,却很少分析大流行的发展过程与太阳活动过程之间的关系.本文基于2020-01-01?—?2...     

铂载钴钼二元硫化物对H_2S电催化活性研究

为考察溶胶凝胶法制备的Co-Mo二元硫化物对H_2S气体的电催化活性,通过循环伏安法和Tafel曲线分析对铂载不同Co、Mo掺杂比的电催化剂进行表征.结果表明,不同阳极电催化剂交换电流密度J_0由大到小依次为,铂载n(Co):n(Mo)=2:3、铂载n(Co):n(Mo)=2:1、铂载n(Co):n(Mo)=1:1和铂,即铂载n(Co):n(Mo)=2:3阳极电催化剂具有较好的活性,这与循环伏安曲线测试结果一致.电解质溶液pH值为6～7时,随着温度的升高铂载n(co):n(Mo)=2:3阳极电催化剂活性呈现上升的趋势.优化后的Co、Mo掺杂原子比约为0.66,此类电催化剂在操作温度80℃下,交换电流密度为1.318mA/cm~2,表观活化焙值为616.6 kJ/mol .研究表明,铂载钴钼二元硫化物适合作为低温H_2S燃料电池阳极电催化剂,其中Co、Mo掺杂比对电催化活性影响较大.     

Aerobic degradation of methyl tert-butyl ether by a Proteobacteria strain in a closed culture system

The contamination of methyl ten-butyl ether （MTBE） in underground waters has become a widely concerned problem all over the world. In this study, a novel dosed culture system with oxygen supplied by H2O2 was introduced for MTBE aerobic biodegradation. After 7 d, almost all MTBE was degraded by a pure culture, a member of β-Proteobacteria named as PMI, in a closed system with oxygen supply, while only 40% MTBE was degraded in one without oxygen supply. Dissolved oxygen （DO） levels of the broth in closed systems respectively with and without H2O2 were about 5-6 and 4 mg/L. Higher DO may improve the activity of monooxygemase, which is the key enzyme of metabolic pathway from MTBE to tert-butyl alcohol and finally to CO2, and may result in the increase of the degrading activity of PM1 cell. The purge and trap GC-MS result of the broth in closed systems showed that tea-butyl alcohol, isopronol and acetone were the main intermediate products.     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.