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以紫外灯为光源,考察了自制纳米ZnO在光催化体系中降解海产品深加工废水中高浓度氨氮、COD的降解率。研究催化剂用量、溶液pH值、氨氮、COD初始浓度以及催化时间等因素对光催化降解影响。结果表明,纳米ZnO催化体系能有效降解海产品中的氨氮和COD。优化的光催化降解条件为:对于废水中氨氮降解来说,ZnO投加量0.9 g/L,氨氮初始浓度140 mg/L,COD初始浓度900 mg/L,pH值9,光照时间4 h,降解率达65.804%。对废水中COD来说,ZnO投加量0.9 g/L,氨氮初始浓度110 mg/L,COD初始浓度600 mg/L,pH值9,光照时间3 h,降解率达80.00%。 相似文献
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以五水合四氯化锡为原料,采用化学沉淀法制备了纳米SnO2光催化剂,采用电子显微镜和X光衍射仪对粉体的粒径、物象和形貌等进行了表征,对比分析了自制纳米SnO2对于养殖废水中氨氮的光催化降解情况。研究结果表明催化剂投加量、废水中氨氮初始质量浓度、溶液pH值和H2O2质量浓度均是影响氨氮催化氧化去除效果的重要因素。通过正交实验确定了SnO2光催化剂氧化的优化反应条件:SnO2投加量为1.2 g/L,氨氮初始质量浓度为40 mg/L,pH值为8.0,H2O2质量浓度为1.0 g/L,催化时间为2 h时,去除率可达72%。 相似文献
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Fenton试剂对久效磷的降解实验研究 总被引：9，自引：0，他引：9
初步研究了Fenton试剂对久效磷的降解,分析了H2O2浓度、温度、反应时间、pH值和Fe2 浓度这5个因素对COD去除率的影响。实验结果表明,250 mL水样中3.75×10-4mol的久效磷在Fe2 浓度为0.5 mmol/L,pH=3,H2O2浓度为0.19 mol/L,T=70℃的条件下,Fenton试剂在1 h内COD去除率为60%,3 h内COD去除率为90%,8 h内COD去除率为100%。GC-MS测试结果表明,Fenton试剂对250 mL水样中3.75×10-4mol的久效磷5 min可降解81%,30 min降解100%。根据反应速率常数拟合得出该反应符合准一级反应,反应速率常数k=0.655 6 h-1。实验还发现了Cu2 对Fenton试剂有很强的协同催化作用,体系中Cu2 浓度为1.0×10-5mol/L时,Fenton试剂在5 h内对相同水样中COD去除率为101%。 相似文献
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闭合循环水产养殖系统中生物过滤器的水处理效果研究 总被引：11，自引：0，他引：11
对闭合循环水产养殖系统中生物过滤器生物膜的培养、处理能力等方面进行了研究。试验结果表明 ,在生产性试验阶段 :(1 )系统中添加培养液培养生物膜 ,水温在 2 0～ 2 2℃时需要 1 1 d,生物膜成熟后生物过滤器具有较强的转化能力 ;(2 )系统稳定后放养暗纹东方豚 ,连续运行 5个月 ,系统中 NH4- N浓度平均值为 0 .6 8mg/L ,NO2 - N平均值为 0 .5 8mg/L。在规模化生产阶段 :(1 )不预先培养生物膜 ,而直接放养饲养对象 ,这种情况下系统中的水质波动比较明显 ,NH4- N,NO2 - N浓度最高值分别为 2 .2 2 mg/L ,1 .1 2 mg/L ,经过 2个月的运行 ,分别降为 0 .4 7mg/L ,0 .1 4 mg/L ;(2 )在系统中加入 2 .5 mg/L的五倍子和 2 0～ 30 mg/L的生石灰均不影响生物过滤器的处理能力。加入 5 0 mg/L的福尔马林和 2 mg/L的土霉素对生物过滤器的处理能力影响比较明显 ;(3)生物过滤器对流经水体的NH4- N,NO2 - N,COD1次性去除率分别为 4 4.79%,2 0 .31 %,2 0 .1 0 %。 相似文献
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利用溶胶凝胶法自制了碳纳米管和纳米二氧化钛的复合光催化剂,采用投射电子显微镜和X光衍射仪对粉体的粒径、物象、形貌和热稳定性等进行表征。通过研究光照条件、催化剂的投加量、油的初始浓度、催化剂制备的煅烧条件等因素,考察了自制碳纳米管和纳米二氧化钛的复合催化剂对降解模拟海洋柴油污染的海水去除率的影响。研究发现,在可见光照条件下,400℃煅烧2 h的复合催化剂,投加量为0.4 g/L、柴油的初始浓度为0.6 g/L、反应的光照时间为4 h时效果最好,去除率可达到67.65%。 相似文献
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本文研究碳氮(C/N)比变化对移动床生物膜反应器(MBBR)处理海水养殖废水性能的影响。结果表明,当C/N比从7∶1降至3∶1,出水COD浓度无明显变化,平均去除率保持在90%以上。C/N比的变化对脱氮过程有较大影响,当C/N比从7∶1降低至3∶1,NH+4-N去除率由89.51%±1.24%增至92.70%±1.08%,NO-2-N浓度由(4.84±0.50)mg/L降至0 mg/L,NO-3-N浓度由(0.47±0.29)mg/L升至(8.12±0.25)mg/L。C/N比的降低提高了比氨氧化速率、比亚硝酸盐氧化速率和与硝化相关的微生物酶活性,但降低了比耗氧速率、比硝酸盐还原速率、比亚硝酸盐还原速率、脱氢酶活性和与反硝化相关的微生物酶活性。松散型胞外聚合物和紧密型胞外聚合物的多糖含量随C/N比的降低而降低,说明在低COD条件下,多糖能够被微生物利用。微生物群落的丰富度和多样性随C/N比的降低而降低,硝化菌属(Nitrosomonas和Nitrospira)和反硝化菌属(Azoarcus、Comamonas、Hyphomicrobium、Paracoccus、Thauera、Devosia、Pseudomonas和Rhodanobacter)的相对丰度发生改变,从而影响MBBR脱氮性能。 相似文献
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采用序批式实验,分别以活性污泥和颗粒污泥为吸附材料,考察接触时间、pH等因素对废水中Pb2+生物吸附效果的影响.结果表明,活性污泥和颗粒污泥对低浓度Pb2+(0～20 mg/L)能在30 min内达到吸附平衡,当Pb2+浓度在20～100 mg/L时,浓度越低,达到平衡时间越快,以被动吸附为主.在Pb2+低浓度条件下(0～20 mg/L),初始pH为4～5时,Pb2+的去除率达99%以上,且初始pH值是影响活性污泥和颗粒污泥生物吸附Pb2+的重要因素.活性污泥和颗粒污泥对Pb2+的生物吸附符合朗缪尔(Langmuir)方程,在pH为4及25 ℃下,活性污泥饱和吸附量为59.88 mg/g,颗粒污泥饱和吸附量为80.65 mg/g.因此,活性污泥和颗粒污泥可作为有效的生物吸附剂处理低浓度(0～20 mg/L)含铅废水,且颗粒污泥比活性污泥的生物吸附效果好. 相似文献
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利用序批式反应器(SBR)对活性污泥进行培养和驯化,分别取未经驯化和经盐驯化后的活性污泥,通过批量实验研究了两种污泥中微生物对苯胺的降解效果。SBR运行结果表明,活性污泥经过驯化适应了10gNaCl/L后,取得较高的COD、NH_4~+-N和TN的去除率,分别为86.5%、97.6%和96.4%。批量实验结果表明,苯胺降解速率随初始苯胺浓度的升高逐渐增加,且苯胺降解速率在未驯化污泥无盐条件下高于盐驯化污泥加盐条件,分别为2.63~21.31和2.06~12.08mg/(gVSS×h);未投加苯胺时,COD和NH_4~+-N的降解速率是投加苯胺时的5.2~19.3和2.5~4.2倍,且未驯化污泥无盐条件下COD和NH_4~+-N的降解速率是盐驯化污泥加盐条件的2.4和1.5倍;投加苯胺后,COD的降解速率随苯胺浓度的升高逐渐增加;实验结束时,未驯化污泥无盐条件下只存在NO-3-N,而盐驯化污泥加盐条件下同时存在NO-2-N和NO-3-N。 相似文献
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应用缺氧/好氧—移动床生物膜反应器(Anoxic/Aerobic-Moving Bed Biofilm Reactor,A/O-MBBR)系统,通过固定进水COD与无机氮之比C/N为12,将COD依次设置为150、300、350和450mg·L~(-1)时,探讨反应器对海水养殖废水中氨氮、硝氮、亚硝氮及COD的去除效果,并分析微生物群落变化及响应。结果表明,在进水COD为150mg·L~(-1)、无机氮12.5mg·L~(-1)时,反应器运行效果最佳,此时氨氮、硝氮、COD和亚硝氮的去除率分别为93.7%(出水0.3 mg·L~(-1)),87.5%(出水0.7mg·L~(-1)),98.2%(出水3mg·L~(-1)),86.9%(出水0.1mg·L~(-1))。当COD提高至450mg·L~(-1)时,氨氮去除率逐渐降低到40.7%,亚硝氮在COD为350mg·L~(-1)时去除率降低至22.5%。在整个系统运行过程中,变形菌门(Proteobacteria)和拟杆菌门(Bacteroidetes)是反应器中的绝对优势类群。当COD由150mg·L~(-1)上升到350mg·L~(-1)时,变形菌门的相对丰度却由63.9%~75.2%提高到88.1%~92.4%;拟杆菌门的相对丰度则由11.9%~13.0%降低到4.5%~5.4%;引起污泥膨胀的发硫菌属(Thiothrix)的相对丰度由6.24%~7.08%增加到58.16%~76.74%,表明反应器污泥膨胀趋势加剧。应用A/O-MBBR工艺处理海水养殖废水时,在COD为150mg·L~(-1)时效果较好,随着COD浓度提高,引起污泥膨胀的微生物开始大量滋生。 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone. 相似文献
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The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 相似文献
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《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology, 相似文献
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The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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Rahul Sharma 《Marine Georesources & Geotechnology》2000,18(3):237-250
Observations on seafloor features from subbottom profiling and seabed photography data show that the undisturbed and natural conditions before the benthic disturbance undergo a substantial change after operation of the disturber. The effects can be seen in the form of deep trenches and grooves, formed by the action of the sleds and the pumping of the sediment along its path, as well as sediment piles on either side of the track. Biological traces such as fecal coils, casts, tubes, burrows, and trails get obliterated in the areas of disturbance and resedimentation. The smooth, uniform nature of the seafloor observed in predisturbance phase shows microtopographic changes in and around the disturbed area as a result of sediment excavation and resettlement. Vertical mixing as well as lateral transport of sediment alter the geological, biological, physical, and chemical conditions on the seafloor, which need to be monitored over time to assess the process and the time taken for restoration of environmental conditions. 相似文献
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Vance P. Vicente 《Marine Ecology》1989,10(2):179-191
Abstract. Long-term changes in the distributional patterns of commercial sponges ( Spongia spp. and Hippospongia spp.) within the West Indian Region indicates that: 1) commercial sponges had a widespread distribution throughout the whole West Indian Region and were ubiquitous in very shallow water until about the first half of the present century; 2) they were fished commercially not only in the traditional northern Caribbean sites (Florida, Gulf of Mexico, Bahamas) but also in the Greater ( e. g. , Hispaniola, Jamaica) and Lesser Antilles; and 3) they became extinct throughout most of the Lesser Antilles ( e. g. , Puerto Rico, Vieques, St. Thomas) sometime during the first half of this century. Mortalities of spongiids within the Antilles were found to differ from other marine mortalities in that: 1) species disappeared from a large region; 2) species vanished from different habitats and depths; and 3) natural populations never recovered. Species richness patterns suggest that commercial sponge genera ( Spongia and Hippospongia ) evolved under slightly cooler elimatic conditions than those found at present, and that these extinctions occurred as a direct or indirect effect of positive thermal anomalies in sea surface and atmospheric temperatures between 1900–1950. The concept that species diversity is stable on a regional scale is questioned. 相似文献
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The behaviour of an axially pre-loaded cylindrical member of an offshore structure, hit by a supply ship, has been investigated. The effects of axial pre-loading on the dynamic properties of members, the extent of damage and propagation of dynamic instability in the tubular members have also been investigated. Numerical models have been validated using available experimental data from the literature although these are mostly static with no pre-loading. Axial pre-loading was found to change the dynamic characteristics of some cylindrical members quite dramatically while it had no significant effect on others. The study examined whether there was any change in the behaviour between local and global modes when the loading was dynamic rather than static. The effect of damping on the dynamic instability of axially pre-loaded tubes under lateral dynamic loads was also studied. It was observed that for some geometries the quasi-static response can be used to define the boundary between bounded and unbounded dynamic responses. The main contribution of this study, compared with previous investigations reported in the literature, is that both pre-loading and dynamic effects have been included. 相似文献