丙二酸二(2-(2,3-二羟基苯甲酰胺)乙基)酯的合成与螯合性能研究

用2,3-二羟基苯甲酸经羟基保护、酰胺化、酯化和去保护4步反应,生成一种新型的四齿丙二酸二(2-(2,3-二羟基苯甲酰胺)乙基)酯配体.采用傅里叶变换红外光谱(FT-IR)、紫外-可见光谱(UV-Vis)、核磁共振氢谱(1H NMR)、核磁共振碳谱(13C NMR)和质谱(MS)对其结构进行了表征.在中性pH值条件下,研究了这种配体对铀酰离子的络合能力.结果表明,丙二酸二(2-(2,3-二羟基苯甲酰胺)乙基)酯配体与铀酰离子的螯合常数为23.2.     

长株潭城市环境空气中PM2.5和O3质量浓度的相关性研究

PM2.5与O3均为导致城市环境空气质量恶化的主要污染物,采用自动设备监测湖南省长沙、株洲、湘潭3市商业区和郊区空气中的PM2.5和O3质量浓度,并对数据进行相关性分析.结果表明:PM2.5和O3质量浓度的季节性变化大,其中O3质量浓度夏、秋2季高,春、冬2季低;PM2.5则秋、冬2季高,春、夏2季低;O3质量浓度峰值一般出现在当天午后,PM2.5质量浓度峰值一般出现在上午;空间分布上,O3质量浓度在郊区站点相对较高,而PM2.5质量浓度在商业区站点较高.PM2.5与O3质量浓度变化以负相关为主,即PM2.5质量浓度高时,O3质量浓度则低,反之亦然,二者一般不产生叠加污染.总体上,夏、秋季节应主要防O3污染,春、冬季节则主要防PM25污染.     

北京夏季典型PM2.5与O3相继重污染事件分析

根据北京市环境保护监测中心发布的PM2.5和O3小时质量浓度及气象、卫星遥感数据,分析了2013年7月2日至10日北京典型PM2.5及O3重污染过程的质量浓度特征及在大气边界层过程各个阶段的质量浓度演变.结果表明,北京夏季O3质量浓度先于PM2.5达到峰值,而天气型演变是导致这一现象的主要原因.具体过程为:1)重污染初始阶段,高压天气型利于前体物积累,PM2.5及O3质量浓度升高;2)在反气旋中部,由于各种污染物质量浓度较低,对大气紫外波段辐射的吸收较弱,导致该阶段紫外辐射强,因而加快了O3生成的光化学反应,O3质量浓度最先达到峰值;3)在反气旋后部,随PM2.5质量浓度增加,辐射变弱,因此O3质量浓度增加速度下降,而受高压后部影响,区域内PM2.5经东南风输送通道进入北京,导致北京PM2.5质量浓度相继达到峰值;4)在重污染清除阶段,在北方反气旋前部的冷锋清除作用下,PM2.5及O3质量浓度同时降低至谷值.     

三维点云基础上排土场垮塌影响范围研究

高台阶排土场下游常分布有居民区、厂房等,一旦垮塌,后果严重,因此完善的防治与应急准备工作十分关键,而排土场垮塌影响范围的预测是这些工作的重要前提依据。为提升高台阶排土场垮塌影响范围的预测准确性,需要获取准确的地形边界基础数据。通过利用三维激光扫描仪对新建排土场及其下游地形精细扫描,对获取的三维点云数据去噪、拼接、建模等处理,生成精度更高的数字高程模型与三维实体模型。在此基础上,结合新建高台阶排土场地质勘查与设计资料,建立颗粒离散元数值模型,利用PFC3D计算高台阶排土场垮塌影响范围,并与经验公式法计算结果对比分析,结果表明排土场颗粒离散元数值模型精度符合要求,可快速、准确地计算影响范围,从而为相关部门提供科学决策依据。     

小麦-玉米轮作体系农田氮素淋失特征及氮素表观平衡

连续6年采用渗漏计法研究了不同施氮处理下陕西关中小麦-玉米轮作区农田土壤90 cm深度处氮素(N)淋失特征和土壤-作物体系氮素表观平衡状况.结果表明:该地区农田氮素淋溶主要发生在降雨量较多的玉米季,且集中在8月和9月.监测期内,TN和NO-3-N年平均流失量分别为2.72~23.07 kg·hm-2和1.53~18.72 kg·hm-2,年流失率分别为0.65%~3.44%和0.82%~3.32%,且年总氮、硝态氮流失量均随年施氮量增加呈指数增加.氮素淋失形态中,NO-3-N比例较高,可占总氮淋失量的56.00%~81.00%,且随着氮肥用量的降低,其占总氮淋失量的比例也随之减小.可见,施氮量的大小在一定程度上会影响淋失液中各形态氮的比例.氮素表观平衡结果显示,随着施氮量提高,氮素在土壤中的残留和表观氮盈余均呈现指数增加趋势.长期施氮条件下,土壤-作物体系氮素表观损失率的幅度为32.60%~55.20%,土壤表观残留率为-0.17%~8.20%.多年监测结果表明,优化施氮模式下,作物不仅可以获得较高的产量和氮肥利用率,农田氮素淋失量也大幅降低,在节约肥料资源的同时减轻了潜在的环境风险.     

Effect of commercial pesticides on plant growth-promoting activities of Burkholderia sp. strain L2 isolated from rhizosphere of Lycopersicon esculentum cultivated in agricultural soil

The in vitro study was carried out to examine the toxicity of four commercially used pesticides (phorate, mancozeb, chlorpyrifos, and endosulfan) at the recommended dose (1X) and higher field doses (1.5X, 2X, 2.5X, and 3X) on plant growth-promoting activities of Burkholderia sp. strain L2, isolated from pesticide-treated rhizosphere of Lycopersicon esculentum. At the recommended dose, level of toxicity of all the pesticides to phosphate solubilization activity and indole-3-acetic acid (IAA) production was less detrimental as compared to exceeding doses. At maximum dose rate of each pesticide, the percentage decrease in phosphate solubilization and IAA production over control was found in order of chlorpyrifos < mancozeb < endosulfan < phorate. Present study proves that Burkholderia sp. strain L2 could be used as a potential microbial inoculant in the agricultural soil having persistent pesticide residues.     

管道中烟道气流动传热及酸凝结规律

针对注烟道气稠油热采中管道输送烟道气酸凝结问题,以连续性方程、能量方程和动量方程为基础建立了烟道气沿管道流动与传热计算模型,计算了烟道气沿管道的压力分布、温度分布和酸凝结点距离,分析了不同入口参数和烟道气成分对管道中烟道气的压力、温度、酸凝结点的影响。结果表明:SO3或水蒸汽含量增加时,烟道气酸凝结点温度提高,凝结点距离减小;入口烟道气压力提高,烟道气压降变小,温降不变,酸凝结点距离减小;入口烟温升高,压降和温降都增大,酸凝结点距离增大;保温层厚度增加,温降减小,酸凝结点距离增大。计算和分析结果表明:减少烟道气中SO3或水蒸汽含量可以有效地增大酸凝结点距离,减轻管道腐蚀问题。     

秸秆添加对厨余垃圾堆肥时H_2S和NH_3排放的影响

厨余垃圾堆肥过程中NH3和H2S的排放不但降低了堆肥的养分含量,而且会引发严重的恶臭。以厨余垃圾为研究对象,以玉米秸秆为膨松剂,设置5%、10%、15%、20%(质量分数)4个添加比例(湿基)的堆肥处理,研究秸秆添加量对厨余垃圾堆肥过程中H2S和NH3排放的影响。结果表明:从温度来看,仅T4处理未达到无害化和腐熟的要求。氧气不足是造成H2S排放的主要原因,4个堆肥处理的H2S主要集中在前2周排放,随着秸秆添加量的增加,H2S的排放量逐渐降低。与T1处理相比,T2、T3、T4的H2S累积排放量分别降低了35.5%、44.7%、64.2%。各处理NH3的排放趋势与H2S类似,高温期为NH3释放的关键时期,NH3累积释放量占总释放量的62.2%~72.2%,与T1处理相比,T2、T3和T4的NH3累积排放量分别降低了36.9%、45.2%、76.3%。由此可见,添加适量的玉米秸秆不但能促进厨余垃圾堆肥的进行,明显降低堆肥过程中H2S和NH3的排放,而且可以实现玉米秸秆的资源化利用。     

Acid-assisted hydrothermal synthesis of nanocrystalline TiO2 from titanate nanotubes: Influence of acids on the photodegradation of gaseous toluene

In order to efficiently remove volatile organic compounds (VOCs) from indoor air, onedimensional titanate nanotubes (TiNTs) were hydrothermally treated to prepare TiO₂ nanocrystals with different crystalline phases, shapes and sizes. The influences of various acids such as CH₃COOH, HNO₃, HCl, HF and H₂SO₄ used in the treatment were separately compared to optimize the performance of the TiO₂ nanocrystals. Comparedwith the strong and corrosive inorganic acids, CH₃COOH was not only safer andmore environmentally friendly, but also more efficient in promoting the photocatalytic activity of the obtained TiO₂. Itwasobserved that the anatase TiO₂ synthesized in 15 mol/L CH₃COOH solution exhibited the highest photodegradation rate of gaseous toluene (94%), exceeding that of P25 (44%) by a factor ofmore than two. The improved photocatalytic activity was attributed to the small crystallite size and surface modification by CH₃COOH. The influence of relative humidity (20%-80%) on the performance of TiO₂ nanocrystals was also studied. The anatase TiO₂ synthesized in 15 mol/L CH₃COOH solution was more tolerant tomoisture than the other TiO₂ nanocrystals and P25.     

Structure and function of rhizosphere and non-rhizosphere soil microbial community respond differently to elevated ozone in field-planted wheat

To assess the responses of the soil microbial community to chronic ozone (O₃), wheat seedlings (Triticum aestivum Linn.) were planted in the field and exposed to elevated O₃ (eO₃) concentration. Three treatments were employed: (1) Control treatment (CK), AOT40 = 0; (2) O₃-1, AOT40 = 1.59 ppm•h; (3) O₃-2, AOT40 = 9.17 ppm•h. Soil samples were collected for the assessment of microbial biomass C, community-level physiological profiles (CLPPs), and phospholipid fatty acids (PLFAs). EO₃ concentration significantly reduced soil microbial carbon and changed microbial CLPPs in rhizosphere soil, but not in non-rhizosphere soil. The results of the PLFAs showed that eO₃ concentrations had significant effects on soil community structure in both rhizosphere and non-rhizosphere soils. The relative abundances of fungal and actinomycetous indicator PLFAs decreased in both rhizosphere and non-rhizosphere soils, while those of bacterial PLFAs increased. Thus the results proved that eO₃ concentration significantly changed the soil microbial community function and composition, which would influence the soil nutrient supply and carbon dynamics under O₃ exposure.