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191.
Hyo Jin Lee Chang Joon Kim Gi Hoon Hong Sang Hee Hong Won Joon Shim Gi Beum Kim 《Environmental science and pollution research international》2014,21(12):7480-7488
Industrial, domestic wastewater, and livestock sludge samples were collected from 23 wastewater treatment plants in Korea and analyzed for polybrominated diphenyl ethers (PBDEs). The concentrations of Σ19PBDE ranged from 4.01 to 10,400 ng/g dry weight. The average Σ19PBDE concentrations in industrial, domestic wastewater, and livestock sludge were 1,560?±?3,610, 402?±?148, and 27.6?±?50.4 ng/g dry weight, respectively. The composition of PBDEs differed according to the type of sludge. Among the PBDE congeners, BDE 209 was dominant in all sludge samples. After BDE 209, relatively high levels were found for BDE 28 and 47 from industrial sludge, BDE 47 and 99 from domestic wastewater sludge, and BDE 206, 207, and 208 from livestock sludge. Using hierarchical cluster analysis, sludges were divided into three groups according to PBDE congener composition. A risk assessment of PBDEs in sludge used for soil amendment was carried out. Preliminary results indicated that the potential risk of soil exposed to PBDEs in sludge was relatively low. 相似文献
192.
好氧颗粒污泥自生动态膜生物反应器处理碱减量印染废水 总被引:1,自引:0,他引:1
自生动态膜生物反应器(SFDMBR)接种颗粒污泥启动,研究溶解氧浓度和水力停留时间对该反应器处理碱减量印染废水的影响。自生动态膜生物反应器形成稳定的动态膜后,出水浊度小于10 NTU,系统对浊度的去除率在90%以上,溶解氧和水力停留时间对反应器出水浊度基本无影响。系统对废水色度的去除率随着溶解氧浓度的提高和水力停留时间的延长而增加,但是系统对色度的去除效率一般不超过40%。溶解氧浓度由0.3 mg/L逐渐增大至2.4 mg/L,COD的去除率由40%提升至80%,而当溶解氧浓度大于1.0 mg/L后,UV254的去除率达到95%。水力停留时间在8~48 h时,COD去除效率由65%逐渐上升至85%左右;水力停留时间在8~32 h,UV254去除效率为68%~93%,超过32 h后水力停留时间对UV254去除效率的影响已不明显。 相似文献
193.
应用自主研制的强化循环厌氧反应器(SCAR)中试规模处理实际印染废水,研究反应器的启动特性。反应器接种厌氧颗粒污泥后启动运行83 d,形成连续内循环并实现了对印染废水处理的高效稳定运行。在进水COD浓度1 000~3 650 mg/L、系统容积负荷0.7~6.4 kg/(m3·d)条件下,废水COD和色度平均去除率分别达到55%和73%。反应器内较高浓度的NH+4-N保证了系统pH的稳定性,350~600 mg/L的NH+4-N浓度没有对强化循环厌氧反应器产生抑制作用,系统内也没有出现VFA(以乙酸计)积累。启动过程中,厌氧颗粒污泥的粒径增大、沉降性能变好。启动实验完成时,反应器内微生物的脱氢酶活性(以TF计)和辅酶F420浓度分别为3.4973 mg/(g·h)和0.1872μmol/g。 相似文献
194.
Jacob Carstensen Daniel J. Conley Erik Bonsdorff Bo G. Gustafsson Susanna Hietanen Urzsula Janas Tom Jilbert Alexey Maximov Alf Norkko Joanna Norkko Daniel C. Reed Caroline P. Slomp Karen Timmermann Maren Voss 《Ambio》2014,43(1):26-36
Hypoxia has occurred intermittently over the Holocene in the Baltic Sea, but the recent expansion from less than 10 000 km2 before 1950 to >60 000 km2 since 2000 is mainly caused by enhanced nutrient inputs from land and atmosphere. With worsening hypoxia, the role of sediments changes from nitrogen removal to nitrogen release as ammonium. At present, denitrification in the water column and sediments is equally important. Phosphorus is currently buried in sediments mainly in organic form, with an additional contribution of reduced Fe-phosphate minerals in the deep anoxic basins. Upon the transition to oxic conditions, a significant proportion of the organic phosphorus will be remineralized, with the phosphorus then being bound to iron oxides. This iron-oxide bound phosphorus is readily released to the water column upon the onset of hypoxia again. Important ecosystems services carried out by the benthic fauna, including biogeochemical feedback-loops and biomass production, are also lost with hypoxia. The results provide quantitative knowledge of nutrient release and recycling processes under various environmental conditions in support of decision support tools underlying the Baltic Sea Action Plan. 相似文献
195.
Assessment of spatial distribution of soil loss over the upper basin of Miyun reservoir in China based on RS and GIS techniques 总被引:2,自引:0,他引:2
Chen T Niu RQ Wang Y Li PX Zhang LP Du B 《Environmental monitoring and assessment》2011,179(1-4):605-617
Soil conservation planning often requires estimates of the spatial distribution of soil erosion at a catchment or regional scale. This paper applied the Revised Universal Soil Loss Equation (RUSLE) to investigate the spatial distribution of annual soil loss over the upper basin of Miyun reservoir in China. Among the soil erosion factors, which are rainfall erosivity (R), soil erodibility (K), slope length (L), slope steepness (S), vegetation cover (C), and support practice factor (P), the vegetative cover or C factor, which represents the effects of vegetation canopy and ground covers in reducing soil loss, has been one of the most difficult to estimate over broad geographic areas. In this paper, the C factor was estimated based on back propagation neural network and the results were compared with the values measured in the field. The correlation coefficient (r) obtained was 0.929. Then the C factor and the other factors were used as the input to RUSLE model. By integrating the six factor maps in geographical information system (GIS) through pixel-based computing, the spatial distribution of soil loss over the upper basin of Miyun reservoir was obtained. The results showed that the annual average soil loss for the upper basin of Miyun reservoir was 9.86 t ha(-1) ya(-1) in 2005, and the area of 46.61 km(2) (0.3%) experiences extremely severe erosion risk, which needs suitable conservation measures to be adopted on a priority basis. The spatial distribution of erosion risk classes was 66.9% very low, 21.89% low, 6.18% moderate, 2.89% severe, and 1.84% very severe. Thus, by using RUSLE in a GIS environment, the spatial distribution of water erosion can be obtained and the regions which susceptible to water erosion and need immediate soil conservation planning and application over the upper watershed of Miyun reservoir in China can be identified. 相似文献
196.
Harold N. Bass Joan B. Oliver Murali Srinivasan Ruth Petrucha Won Ng Jo Ellen S. Lee 《黑龙江环境通报》1986,6(1):33-35
Intrauterine fetal demise (IUFD) in one of twins at 12 weeks of gestation was accompanied by markedly elevated maternal serum alpha-fetoprotein (AFP) at 17 and 18 weeks. Amniotic fluid AFP from the healthy surviving twin's sac at 18·5 and 23 weeks was also greatly increased along with a positive acetylcholinesterase (AChE) band. Persistently elevated AFP and positive AChE so long after fetal demise–-6·5 and 11 weeks post IUFD–-has not, to our knowledge, been previously described. In similar cases, high level ultrasound and careful placental examination at birth should be utilized to search for fetal abnormalities or multiple pregnancy with IUFD. 相似文献
197.
198.
川西亚高山针叶林土壤硝化作用及其影响因素 总被引:3,自引:0,他引:3
采用BarometricProcessSeparation(BaPS)技术对川西亚高山针叶林土壤总硝化作用速率的季节动态进行了研究,并分析了各影响因素与总硝化速率的关系.通过土壤温度和水分含量的控制实验,对温度和水分含量与总硝化速率之间的关系进行了一次线性和曲线模拟.结果表明,6至10月各月份之间的总硝化速率存在显著差异(P<0.01),在7月总硝化速率达到最大值;土壤温度和水分含量与总硝化速率显著正相关(P<0.05),对总硝化速率的影响存在明显的交互作用,水分含量可能对总硝化速率的影响更大,在季节变化中温度和水分含量可能对硝化过程产生直接和间接两种作用;pH值与总硝化速率之间的相关性不明显;森林凋落量与总硝化速率间没有显著相关性,但若仅考虑6至9月,森林凋落量与总硝化速率极显著相关(P<0.01).总之,土壤温度和水分含量很可能是影响总硝化速率的两个最主要的因素.图6表2参31 相似文献
199.
川中丘陵区典型小流域地下水硝酸盐污染分析 总被引:14,自引:1,他引:14
对川中丘陵区典型小流域地下水N素含量及形态分配的监测结果表明,硝酸盐(NO3--N)是该地区地下水N素存在的主要形态。川中丘陵区54.5%的地下水NO3--N含量超过世界卫生组织(WHO)饮用水准则规定的10mg.L-1标准,另有27.3%的地下水NO3--N含量接近这一标准,表明该区地下水已经大范围地受到NO3--N污染的威胁。土地利用状况可能是影响川中丘陵区地下水NO3--N含量的主要因素。降雨量和水井深度也影响该区地下水NO3--N含量。紫色土坡耕地NO3--N随壤中流向浅层地下水迁移,可能是造成该区地下水NO3--N含量较高的最重要原因。 相似文献
200.
气态甲醛致雌性小鼠生殖细胞DNA-蛋白质交联的研究 总被引:4,自引:3,他引:4
为了研究气态甲醛对雌性小鼠生殖细胞的影响,以昆明雌性小鼠卵巢为实验材料,采取动态吸入式染毒方式,应用KCl-SDS沉淀法检测了气态甲醛染毒后所引起的小鼠卵巢生殖细胞DNA-蛋白质交联(DPC)效应.结果表明,较低浓度的甲醛(0.5mg·m-3),即可导致明显的DPC效应(与对照相比,p<0.05),并且随着染毒浓度的升高(0.5、1.0、3.0mg·m-3),DPC系数也逐渐升高.上述结果表明在实验所设浓度范围内,甲醛对小鼠卵巢生殖细胞的DNA损伤可以引起DNA-蛋白质的交联,并且DPC系数随着染毒浓度的增大而增大.DNA-蛋白质交联是DNA分子的一种严重损伤,气态甲醛对雌性小鼠生殖细胞具有一定的影响. 相似文献