固相萃取-UPLC-MS/MS法测定环境水体中多种抗生素

采用固相萃取-超高效液相色谱串联质谱法测定环境水样中25种磺胺类和喹诺酮类抗生素,通过优化试验条件,使方法在2.00μg/L～200μg/L范围内线性良好,方法检出限为1.01ng/L～2.85ng/L,7次测定结果的RSD为2.3%～8.0%。将该方法用于自来水和地表水测定,结果均为未检出,高、低质量浓度水平的加标回收率为61.2%～102%。     

HPLC-三重四级杆质谱法测定医疗废水中抗生素残留

采用固相萃取/高效液相色谱-三重四级杆质谱法同时测定医疗废水中的20种超痕量抗生素残留,通过优化试验条件,使方法在100μg/L～100μg/L范围内线性良好,方法检出限为024ng/L～122ng/L。空白水样和实际水样3个质量浓度水平的加标回收率分别为80.2%～108%和75.8%～114%,6次测定结果的RSD分别为2.4%～8.4%和1.7%～8.1%。将该方法用于测定重庆市2家三甲医院医疗废水中的超痕量抗生素残留,结果有11种抗生素检出,其余均为未检出。     

采用接触面单元分析砼-岩系统的力学行为

考虑实际修建过程中塔基岩石开挖的施工特点和砼分期浇筑特点,通过建立三维实体模型,根据基于大变形理论的快速拉格朗日方法,运用考虑库仑屈服准则的塑性接触面单元计算了锦屏一级水电站泄洪洞进口塔基砼-岩接触系统的应力和变形,评价了塔基的稳定性,并与直接考虑材料为实体单元的计算结果进行了比较。工程算例数值计算结果表明,采用接触面单元来分析砼-岩系统的力学行为更合理、更实用。     

覆水场地地震反应分析

随着各种海洋结构物的兴建,覆水场地的地震反应逐渐成为研究热点。基于任意拉格朗日-欧拉描述,推导时变区域上的流体运动方程,给出流场、结构的接触条件和流场网格运动控制方法。对于平坦覆水场地,水平向地震动作用下,根据Couette流理论证明该类场地流体作用可以忽略;竖向地震动激励下,横向均匀场地可以通过动水压力公式准确考虑流体作用,横向非均匀场地则需要通过流固耦合方法考虑流体作用,以海底隧道为例加以说明。对于起伏场地,天然起伏场地在地震动激励下的动力反应具有明显的流固耦合特征,以三角形起伏场地为算例;结构物的兴建造成的人工起伏场地同样需要考虑流固耦合效应,以某沉管隧道在水平向地震动激励下的动力反应为算例,并根据结果初步提出该类结构物流固耦合分析的简化计算方法。     

苏-35反隐形战略大曝光

作为在俄第四代战机问世前唯一有能力对抗美制隐形战机的苏-35,其反隐形性能及战略一直被外界关注。近日有俄航空专家表示,作为三代半战机,苏-35拥有多样性的探测系统：除了X波段的Irbis—E前视雷达外,还有0LS-35光电探测仪、AFAR—L主动L波段相控测仪。未来可能还有后视X波段雷达、激光预警接收器与红外线预警接收器等。其无线电视野与预警系统视野接近球形,     

基于GIS和RS的嵩山森林生态旅游环境变化分析

考虑景区内外管理政策的不同,以1980年和2006年的遥感影像为信息源,在GIS技术的支持下获取了嵩山森林生态旅游景区和景区缓冲区的生态环境变化信息,借助压力-状态-响应模型,建立了森林生态旅游的环境评价指标体系,对景区内外生态环境的动态变化进行了分析.结果表明:1)26年来景区和景区缓冲区的容量、农业化压力、交通压力和服务压力增大,多样性指数、破碎度指数均呈上升趋势;2)26年来景区缓冲区内的建筑用地、旅游服务用地、通往景区的道路用地的面积均呈上升趋势;3)26年来该景区内部分林地的覆盖率下降,裸岩面积增加,景区缓冲区内的林地面积增加,说明人们对环境的认识得到加强.     

聚丙烯酰胺助凝处理VAE乳液废水效能研究

为了获得醋酸乙烯-乙烯共聚乳液(VAE乳液)废水的有效处理方法,通过混凝试验比较了不同类型聚丙烯酰胺对FeCl3混凝-气浮工艺的助凝效果,重点研究了阳离子型聚丙烯酰胺CZ4060,确定了其最佳的投加时间、pH值及与FeCl3的复配投量.结果表明,CZ4060对FeCl3具有明显的助凝作用,其最佳的投加点是紧随FeCl3之后投加,最佳的pH值范围为7～9,最佳絮凝时间为8 min,与FeCl3的最佳复配投量为1.5 mg/L和100 mg/L.最佳实验条件下,原水COD为3 085 mg/L时,出水COD降为55.28 mg/L,达到<污水综合排放标准>(GB 8978-1996)要求的一级排放标准.     

电-多相催化氧化法处理桉木CTMP模拟废水

提出一种基于复极性固定床反应器的有机废水处理新技术--电-多相催化氧化技术,用于桉木CTMP模拟废水的处理.以γ-Al2O3为载体,采用等体积浸渍法制备活性组分为氧化铜的催化剂,用于实验废水的处理.结果表明,在一定的操作条件下,E-HCR(电-多相催化体系)对鞣酸的降解效果明显好于传统的BPBC(复极性固定床电解槽).在外加电压20V、支持电解质质量浓度1000mg/L、pH值为5.35的条件下.降解初始质量浓度为100 mg/L的鞣酸,去除率大于90%.鞣酸降解前后的紫外和红外光普分析表明:鞣酸经电-多相催化氧化处理后,分于中的酚羟基显著减少,分子中的大部分苯环结构开环降解成小分子物质.研究表明所研制的催化剂对鞣酸的电化学降解有很好的催化效果.     

Vertical and temporal distribution of nitrogen and phosphorus and relationship with their influencing factors in aquatic-terrestrial ecotone： a case study in Taihu Lake, China

Vertical and temporal distributions of N and P in soil solution in aquatic-terrestrial ecotone （ATE） of Taihu Lake were investigated, and the relations among N, P, ORP （oxidation reduction potential）, TOC, root system biomass and microorganism were studied. As a whole, significant declines in TN, NO3^--N, DON （dissolved organic nitrogen） and TP concentration in soil solution have occurred with increase of the depth, and reached their minima at 60 cm depth, except for NH4^＋-N, which increased with depth. The concentration of TP increased gradually from spring to winter in the topsoil, the maximum 0.08 mg/L presented in the winter while the minimum 0.03 mg/L in spring. In the deeper layer, the concentration value of TP fluctuated little. As for the NO3^--N, its seasonal variation was significant at 20 cm depth, its concentration increased gradually from spring to autumn, and decreased markedly in winter. Vertical and temporal distribution of DON is contrary to that of NO3^--N. The results also show that the variation of N and P in the percolate between adjacent layers is obviously different. The vertical variation ofTN, TP, NO3^--N, NH4^＋-N and DON is significant, of which the variation coefficient of NO3^--N along the depth reaches 100.23%, the highest; while the variation coefficient of DON is 41.14%, the smallest. The results of correlation analysis show that the concentration of nitrogen and phosphorus correlate significantly with TOC, ORP, root biomass and counts of nitrifying bacteria. Most nutrients altered much from 20 to 40 cm along the depth. However, DON changed more between 60 and 80 cm. Results show that soil of 0-60 cm depth is active rhizoplane, with strong capability to remove the nitrogen and phosphorus in ATE. It may suggest that there exists the optimum ecological efficiency in the depth of above 60 cm in reed wetland. This will be very significant for ecological restoration and reestablishment.     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.