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水产品中甲氰菊酯残留的ELISA快速检测 总被引:3,自引:0,他引:3
为快速检测水产品中甲氰菊酯的残留,应用水溶性碳化二亚胺(EDC)法将甲氰菊酸与牛血清白蛋白(BSA)和卵清蛋白(OVA)偶联,合成了甲氰菊酯的人工免疫抗原和包被抗原.免疫抗原经紫外扫描和聚丙烯酰胺电泳验证构建成功,用此抗原免疫试验兔子,获得了甲氰菊酯的多克隆抗体.经检测,抗体对甲氰菊酯具有较好的特异性和灵敏性.在此基础上建立了水产品中甲氰菊酯残留的间接ELISA检测法.理想的甲氰菊酯-OVA包被抗原质量浓度为1.6 mg/L,酶标二抗(羊抗兔IgG-HRP)的稀释度为1∶1000,多抗的稀释度为1∶3 200,最适检测范围为20~200 μg/kg,在实际样品检测时的最低检出限为20 μg/kg,接近或达到气相色谱法的测定水平,但检测速度大大提高,可在3 h内完成近百个样品的分析,适合甲氰菊酯的快速检测. 相似文献
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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. 相似文献
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A restoration-promoting integrated floating bed and its experimental performance in eutrophication remediation 总被引:5,自引:0,他引:5
Yiming Guo Yunguo Liu Guangming Zeng Xinjiang Hu Xin Li Dawei Huang Yunqin Liu Yicheng Yin 《环境科学学报(英文版)》2014,26(5):1090-1098
Numerous studies on eutrophication remediation have mainly focused on purifying water first, then restoring submerged macrophytes. A restoration-promoting integrated floating bed (RPIFB) was designed to combine the processes of water purification and macrophyte restoration simultaneously. Two outdoor experiments were conducted to evaluate the ecological functions of the RP1FB. Trial 1 was conducted to compare the eutrophication purification among floating bed, gradual-submerging bed (GSB) and RPIFB technologies. The results illustrated that RPIFB has the best purification capacity. Removal efficiencies of RPIFB for TN, TP,NH4+-N, NO3-N, CODcr, Chlorophyll-a and turbidity were 74.45%, 98.31%, 74.71%, 88.81%, 71.42%, 90.17% and 85%, respectively. In trial 2, influences of depth of GSB and photic area in RPIFB on biota were investigated. When the depth of GSB decreased and the photic area of RPIFB grew, the height of Potamogeton crispus Linn. increased, but the biomass of Canna indica Linn. was reduced. The mortalities of Misgurnus anguillicaudatus and Bellamya aeruginosa in each group were all less than 7%. All results indicated that when the RPIFB was embedded into the eutrophic water, the regime shift from phytoplankton-dominated to macrophyte-dominated state could be promoted. Thus, the RPIFB is a promising remediation technology for eutrophication and submerged macrophyte restoration. 相似文献
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黄河口不同恢复阶段湿地土壤N2O产生的不同过程及贡献 总被引:3,自引:1,他引:2
采用时空替代法,选择黄河口生态恢复前后未恢复区(R0)、2007年恢复区(R2007)和2002年恢复区(R2002)的芦苇湿地为研究对象,分析了生态恢复工程对湿地土壤N2O产生不同过程与贡献的影响.结果表明,尽管不同恢复阶段湿地土壤N2O总产生量差异明显,但总体均表现为N2O释放.恢复区湿地土壤的N2O产生量大于未恢复区.N2O的产生主要以硝化作用和硝化细菌反硝化作用为主,而反硝化作用对N2O的产生有较大削弱作用,这与不同恢复阶段湿地土壤理化性质密切相关.非生物作用对N2O产生量贡献较大,这与黄河口为高活性铁区,Fe的还原作用关系密切.尽管黄河口不同恢复阶段湿地土壤N2O的产生是生物作用与非生物作用共同作用的结果,但由于非生物作用对N2O产生的影响较大,应受到特别关注.温度和水分对不同恢复阶段湿地土壤N2O产生过程的影响不尽一致,这与土壤微生物活性对温度和水分的响应差异有关.黄河口不同恢复阶段湿地土壤的N2O总产生量介于(0.37±0.08)~(9.75±7.64)nmol·(kg·h)-1,略高于闽江口互花米草湿地的N2O总产生量,但明显低于富氧森林土壤、草原土壤和闽江口短叶茳芏湿地的N2O总产生量.研究发现,黄河口生态恢复工程的长期实施明显促进了N2O的产生,因而下一步生态恢复工程应统筹考虑景观恢复与温室气体削弱这两方面因素. 相似文献