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971.
长江口表层沉积物中半挥发性有机物的分布 总被引:4,自引:1,他引:3
采用GC-FID方法对2005年11月采集于长江河口区表层沉积物中的64种半挥发性有机物(SVOCs)进行分析测定,并对影响该类污染物分布的主要因素进行了讨论. 结果表明:该区域表层沉积物中共检出半挥发性有机物35种,包括多环芳烃类11种,取代苯类7种,酚类5种,酯类3种,醚类2种和其他类7种. 其中,属于我国优先控制污染物的有7种,属于美国优先控制污染物的有22种. 沉积物中SVOCs的分布未呈现出明显的规律,其分布主要受采样点所处的水利条件、与排污口的相对位置、沉积物颗粒粒径、有机质含量和洪枯季等因素的影响;采样点的水动力条件越弱,与排污口的距离越近,沉积物颗粒粒径越小,导致沉积物中污染物的种类和数量就越多. 相似文献
972.
紫外光降解高浓度氯苯气体的研究 总被引:2,自引:0,他引:2
为评价紫外光降解作为高浓度挥发性有机物生物预处理的可行性,系统考察了其对高浓度氯苯气体的去除性能及其影响因素.所考察的影响因素包括紫外光波长、进口ρ(氯苯)、空塔停留时间和气体相对湿度等.结果表明:复合254和185 nm波长紫外光照射对氯苯的去除效果优于单一254 nm波长;紫外光降解反应器的进口ρ(氯苯)在2 300~2600 mg/m3,空塔停留时间为27 s时,对氯苯气体的去除率可达40%,继续延长空塔停留时间对氯苯去除率的提高作用有限;进口ρ(氯苯)在150~3 000 mg/m3时,氯苯去除速率随进口浓度单调增加,当高于3 000 mg/m3时,氯苯去除速率基本保持不变;增加气体相对湿度可以提高紫外光降解反应器对氯苯的去除效果. 相似文献
973.
以20种微量有机污染物为目标物,针对北京市2个再生水厂的不同工艺,系统地考察了污水再生水中目标化合物的去除效果,并采用重组酵母雌激素活性筛检法(YES法)对再生水中雌激素活性进行评价.结果表明,超滤(UF)+臭氧(O3)氧化处理工艺可有效地去除微量有机污染物,出水中雌二醇当量浓度(EEQ)低于YES法检出范围.A2/O+膜生物反应器(MBR)+反渗透(RO)处理工艺对微量有机污染物有很高的去除能力,出水中可检测出的目标化合物较少.2种工艺均可降低再生水的环境风险,保障其使用安全. 相似文献
974.
975.
Global emissions trading allows for agricultural measures to be accounted for the carbon sequestration in soils. The Environmental Policy Integrated Climate (EPIC) model was tested for central European site conditions by means of agricultural extensification scenarios. Results of soil and management analyses of different management systems (cultivation with mouldboard plough, reduced tillage, and grassland/fallow establishment) on 13 representative sites in the German State Baden-Württemberg were used to calibrate the EPIC model. Calibration results were compared to those of the Intergovernmental Panel on Climate Change (IPCC) prognosis tool. The first calibration step included adjustments in (a) N depositions, (b) N2-fixation by bacteria during fallow, and (c) nutrient content of organic fertilisers according to regional values. The mixing efficiency of implements used for reduced tillage and four crop parameters were adapted to site conditions as a second step of the iterative calibration process, which should optimise the agreement between measured and simulated humus changes. Thus, general rules were obtained for the calibration of EPIC for different criteria and regions. EPIC simulated an average increase of +0.341 Mg humus-C ha−1 a−1 for on average 11.3 years of reduced tillage compared to land cultivated with mouldboard plough during the same time scale. Field measurements revealed an average increase of +0.343 Mg C ha−1 a−1 and the IPCC prognosis tool +0.345 Mg C ha−1 a−1. EPIC simulated an average increase of +1.253 Mg C ha−1 a−1 for on average 10.6 years of grassland/fallow establishment compared to an average increase of +1.342 Mg humus-C ha−1 a−1 measured by field measurements and +1.254 Mg C ha−1 a−1 according to the IPCC prognosis tool. The comparison of simulated and measured humus C stocks was r2 ≥ 0.825 for all treatments. However, on some sites deviations between simulated and measured results were considerable. The result for the simulation of yields was similar. In 49% of the cases the simulated yields differed from the surveyed ones by more than 20%. Some explanations could be found by qualitative cause analyses. Yet, for quantitative analyses the available information from farmers was not sufficient. Altogether EPIC is able to represent the expected changes by reduced tillage or grassland/fallow establishment acceptably under central European site conditions of south-western Germany. 相似文献
976.
Y. Liang H.T. Gollany R.W. Rickman S.L. Albrecht R.F. Follett W.W. Wilhelm J.M. Novak C.L. Douglas Jr. 《Ecological modelling》2009
Soil carbon (C) models are important tools for examining complex interactions between climate, crop and soil management practices, and to evaluate the long-term effects of management practices on C-storage potential in soils. CQESTR is a process-based carbon balance model that relates crop residue additions and crop and soil management to soil organic matter (SOM) accretion or loss. This model was developed for national use in U.S and calibrated initially in the Pacific Northwest. Our objectives were: (i) to revise the model, making it more applicable for wider geographic areas including potential international application, by modifying the thermal effect and incorporating soil texture and drainage effects, and (ii) to recalibrate and validate it for an extended range of soil properties and climate conditions. The current version of CQESTR (v. 2.0) is presented with the algorithms necessary to simulate SOM at field scale. Input data for SOM calculation include crop rotation, aboveground and belowground biomass additions, tillage, weather, and the nitrogen content of crop residues and any organic amendments. The model was validated with long-term data from across North America. Regression analysis of 306 pairs of predicted and measured SOM data under diverse climate, soil texture and drainage classes, and agronomic practices at 13 agricultural sites having a range of SOM (7.3–57.9 g SOM kg−1), resulted in a linear relationship with an r2 of 0.95 (P < 0.0001) and a 95% confidence interval of 4.3 g SOM kg−1. Using the same data the version 1.0 of CQESTR had an r2 of 0.71 with a 95% confidence interval of 5.5 g SOM kg−1. The model can be used as a tool to predict and evaluate SOM changes from various management practices and offers the potential to estimate C accretion required for C credits. 相似文献
977.
978.
镧掺杂纳米材料合成及其高氟选择性吸附特性 总被引:2,自引:0,他引:2
采用共沉淀法制备了镧渗杂的纳米镁铝层状双氢氧化物材料(LDHs),获得了一类对氟具有选择性的新型吸附材料.实验表征了LDH、其焙烧产物(LDOs)以及吸附氟后的材料(F-LDHs)的微观形态、体相组成等性质的变化,通过批处理试验和吸附柱试验对其工艺特性及影响因素进行了深入分析.实验结果表明,材料经600℃焙烧10min,在含200mg·l~(-1)SO_4~(2-),氟浓度为10mg·l~(-1)的配水中投加0.1g LDOs吸附240min,最高除氟率可达93.53%;在含200mg·l~(-1)SO_4~(2-)的氟溶液中,镁铝铜LDOs吸附氟的容量高于镁铝LDOs;吸附柱实验中,14h时出水氟含量小于国家标准(1 mg·l~(-1));共存阴离子对材料的除氟干扰强度排序为:Co_3~(2-)>PO_4~(3-)>NO_3~->Cl~-.材料吸附氟后可用0.5mg·l~(-1)的Na_2CO_3洗脱,并经600℃焙烧10min再生,再生4次后选择性除氟效果稳定. 相似文献
979.
980.
Theresa Stevens Savery George H. Belt Dale A. Higgins 《Journal of the American Water Resources Association》2001,37(3):641-654
ABSTRACT: Data collected from 121 stream reaches during 1991 to 1993 were evaluated to determine the applicability of the Rosgen Stream Classification System (RSCS) to the low relief terrain within the Chequamegon‐Nicolet National Forest (CNNF) in Wisconsin, USA. All reaches were classified to RSCS Level I and II except that 10.7 percent had sinuosities below the continuum limits and one reach had a predominantly organic substrate. Five of eight possible RSCS Level I types were observed including B, C, D, A, E, and F; 86 percent were C and E types. Seventeen of 94 possible RSCS Level II types were observed. Most reaches were slightly entrenched, had low to moderate width/depth ratios, relatively low sinuosity, low slope, and sand or gravel as the dominant channel material. Discriminant analyses were used to verify the applicability of RSCS for streams within the CNNF; discriminant functions correctly classified 92.5 and 94.7 percent of the Level I and II RSCS types, respectively. When limits for E and F types were modified slightly at Level II by adding an additional category for slopes less than 0.1 percent (a modification we recommend for low relief terrain), discriminant functions correctly classified 99.1 percent of the types. Adding another slope break at 0.3 percent produced similar results. Based on our analyses, RSCS works well within the CNNF and is probably applicable to other areas with low‐relief terrain. 相似文献