油页岩灰渣浸取铝酸钠溶液试验研究

以油页岩废渣为原料,通过酸浸法浸取油页岩灰渣中的铝酸钠溶液.采用焙烧活化方法将废渣中含铝的低活性晶体物质活化为高活性半晶体或非晶体物质,利用酸浸法浸取焙烧后的高活性含铝废渣,得到铝液;依据试验分析了影响酸浸法浸取铝酸钠溶液的主要影响因紊为焐烧温度、焙烧时间、浸取酸浓度和浸取温度;得出酸浸法的最佳工艺参教:活化温度850℃,活化时间3 h,选用酸浓度40%,浸取温度60℃,此时油页岩废渣铝浸取率为75%.     

从硬质合金处理渣中回收氧化钴

根据硫酸钠熔炼法处理废合金所得钴渣组成特点,通过氧化焙烧、酸分解、水解除杂、沉钴和煅烧等工序制取氧化钴.焙烧最佳工艺条件为:NaNO3用量为钴渣量的0.8倍,焙烧温度750 ℃,时间2.5 h.盐酸分解、喷淋水解除铁、草酸铵沉钴和煅烧阶段钴的回收率(%)分别为97.5、96.6、99.5和99.0,使Co、Ta的回收率分别达到92.78%和85%.     

用含硫化砷废渣制备砷酸铜

以湖北省某化工企业含砷废水处理过程中产生的含硫化砷废渣为研究对象，采用氧化碱浸—沉淀工艺制备砷酸铜。考察了沉淀反应液pH、沉淀反应温度、搅拌转速对砷沉淀效果的影响。采用XRD和SEM技术对砷酸铜的物相及形貌进行了表征。实验结果表明：废渣在氧化碱浸过程的砷浸出率为96.53%；沉淀反应时间为30 min时，沉淀步骤的最佳工艺条件为沉淀反应液pH 5.0、搅拌转速500 r/min、沉淀反应温度50 ℃。验证实验结果表明，在该工艺条件下，砷沉淀率均达93.96%以上。SEM表征结果显示，砷酸铜产品为颗粒状，粒径约为500 nm。XRD表征结果显示，砷酸铜产品中主要含有Cu₃As₂O₈，Cu₄O（AsO₄）₂，Cu₄（As₂O₇）O₂。该方法工艺简单、无二次污染，为废渣的综合利用提供了一种新的技术路线。     

生态修复植物蜈蚣草中砷的回收

采用管式炉高温热解-NaOH-Na₂CO₃混合液碱浸-CuSO₄·5H₂O沉淀的方法回收生态修复植物蜈蚣草中的砷，最终得到产品砷酸铜。该方法的最佳工艺条件为：热解温度600 ℃，热解时间30 min，CaO加入量（CaO与蜈蚣草的质量比）8%； m（NaOH）∶m（Na₂CO₃）=1∶3，碱浸温度70 ℃， 碱浸时间2 h， 固液比1∶10； 沉淀反应pH 5， 沉淀反应温度70 ℃。采用该方法处理生态修复植物蜈蚣草，得到产品砷酸铜的纯度为93%，砷回收率达88%。     

氯化焙烧法回收铬渣中的铬

以CaCl2为氯化剂,碳粉为还原剂,采用氯化焙烧—盐酸浸取的方法处理铬渣,铬渣中的铬以CrCl3的形式被回收。在m(铬渣)∶m(碳粉)为10∶2.0、m(CaCl2)∶m(铬渣)为0.4、焙烧温度为1 200℃、焙烧时间为50min的条件下,Cr(Ⅲ)回收率为91.2%。采用本方法处理1g铬渣可回收CrCl3约0.033g。     

利用矾泥制备铵明矾

采用酸熔法分离矾泥中的铝与硅，不仅克服了碱浸工艺脱硅的复杂过程和铝回收率低的不足，而且解决了酸浸工艺中产品纯度低和设备材质要求高等问题，通过试验确定了酸熔最佳工艺条件为：温度200℃，时间30min，酸铝比1.18，活性铝的回收率为96.69%，铵明矾的纯度在99.5%以上。     

硫酸渣制备高纯度硫酸亚铁

以高铁硫酸渣为原料,采用酸浸一还原-除杂-结晶-重结晶-干燥工艺,合成高纯度硫酸亚铁.通过反应温度、反应时闻对硫酸渣中铁的浸出率的影响,以及结晶温度、干燥温度,干燥时间、于燥时间对硫酸亚铁产品纯度的影响做分析实验,得出最佳酸浸条件:硫酸渣与硫酸的固液比为1:3,硫酸质量分数为20%-25%,反应温度为80℃,反应时间为6 h,搅拌强度为200 r/min;最佳结晶精制条件:结晶溶液pH值1:3,温度为60℃,温度海60℃;除杂最佳条件:pH值约为4.5;冷却结晶温度控制在20℃,结晶秣过程为30℃于燥6 h.     

碱性氧化焙烧回收含铬污泥中的铬

采用碱性氧化焙烧工艺回收含铬污泥中的铬，以浸出渣作为焙烧填料，最佳工艺条件为：含铬污泥加入量10g，浸出渣加入量8g，焙烧温度700℃，焙烧时间40min，n（Cr2O3）：n（NaNO3）：n（Na2CO3）：n（NaOH）=1：2：3．5：10。在此条件下，碱性氧化焙烧工艺铬浸出率高达98％以上。     

废无汞碱性电池极性材料制备锰锌铁氧体磁性纳米颗粒

以硝酸浸取废无汞碱性电池极性材料,再加入硝酸铁及蔗糖生成前驱体,最后通过焙烧制得锰锌铁氧体磁性纳米颗粒。优化了酸浸和焙烧条件,采用FTIR和DTA-TG技术研究了前驱体的形成和热解过程,采用XRD、FTIR、TEM技术和振动样品磁强计对锰锌铁氧体进行了表征。结果表明:废无汞碱性电池极性材料酸浸的最佳条件为H_2O_2加入量3%(w)、液固比10 mL/g、稀硝酸浓度4 mol/L、浸取温度40℃,该条件下浸取10 min锰和锌的浸出率均可达100%;所得前驱体为葡萄糖酸盐,其最佳焙烧条件为焙烧温度450℃、焙烧时间2 h;最佳条件下所得锰锌铁氧体为尖晶石型Mn_(0.5)Zn_(0.5)Fe_2O_4,其颗粒为球形、大小均匀,且磁性能优良。     

粉煤灰制备聚硅酸铝铁及条件选择

研究了以粉煤灰为原料制取聚硅酸铝铁的方法和合成的最佳条件.焙烧粉煤灰应以钙基盐作为活化剂方能达到最佳效果;粉煤灰的适宜活化温度应为900～1000℃;酸浸粉煤灰的适宜温度为70～80℃;反应时间为1.0～1.5h,盐酸的质量分数为30%;合成聚硅酸铝铁的各成分最佳质量比为Al/Fe为1.8;Si/(Al+Fe)为1.5.     

干式还原法处理铬渣的机理及应用

采用干式还原法处理铬渣。在多级还原焙烧炉中于高温条件下，将过量的煤粉和铬渣混合后与O₂反应，经冷却、擦磨、磁分离后可得到铁精砂和处理后铬渣。介绍了干式还原法处理铬渣的机理和工艺参数。以3种铬渣试样进行应用试验，经多级还原焙烧—磁分离后，铬渣中的Cr（Ⅵ）质量浓度为0.05~0.18 mg/L，低于HJ/T301—2007标准中的要求（0.50 mg/L），可作为建材原料加以利用。磁分离得到的铁精砂产品中铁的质量分数大于50%，铁回收率大于70%。目前设计的多级还原焙烧炉单炉处理铬渣能力为150 kt/a，标煤消耗为35 kg/t，处理成本约为60元/t。     

Transformation of phosphorus during drying and roasting of sewage sludge

Sewage sludge (SS), a by-product of wastewater treatment, consists of highly concentrated organic and inorganic pollutants, including phosphorus (P). In this study, P with different chemical fractions in SS under different drying and roasting temperatures was investigated with the use of appropriate standards, measurements, and testing protocol. The drying and roasting treatment of SS was conducted in a laboratory-scale furnace. Two types of SS samples under different treatment temperatures were analyzed by ³¹P NMR spectroscopy. These samples were dried by a vacuum freeze dryer at ?50 °C and a thermoelectric thermostat drying box at 105 °C. Results show that the inorganic P (IP) content increased as the organic P content decreased, and the bio-availability of P increased because IP is a form of phosphorous that can be directly absorbed by plants. ³¹P NMR analysis results indicate the change in P fractions at different temperatures. Non-apatite P was the dominant form of P under low-temperature drying and roasting, whereas apatite P was the major one under high-temperature drying and roasting. Results indicate that temperature affects the transformation of P.     

响应面法优化铝灰中氮化铝脱除工艺

为了优化二次铝灰中AlN氧化焙烧脱除工艺,基于响应面法建立了焙烧温度、焙烧时间、铝灰粒径等工艺参数与AlN脱除率之间的数学模型,并进行了方差分析,对铝灰中AlN的脱除工艺参数进行了优化设计。结果表明,所建立的回归模型能够准确预测AlN脱除率,预测值与实验值误差为0.93%。经优化设计得到铝灰中AlN的最佳脱除工艺参数为：焙烧温度1 026 ℃,焙烧时间36 min,铝灰粒径110目（铝灰粒径指其所对应目数的筛下料）。     

Programs assessing implementation and effectiveness of state forest practice rules and BMPs in the West

The major forest nonpoint source control programs in the West are largely regulatory, either under forest practices acts (California, Idaho, New Mexico, Nevada, Oregon, and Washington) or a streamside management act (Montana). These programs and the specific rules they enforce continue to undergo intensive scrutiny. Still, the questions are the same for these regulatory programs as for states that base nonpoint source control on voluntary BMPs (Arizona, Colorado, Utah, Wyoming). Are the rules or BMPs being applied, and are they effective in reducing nonpoint source pollution to levels that protect beneficial uses of water? The level of debate about forestry in the West has resulted in detailed monitoring and research to answer these questions. In the past, state agencies have assumed levels of BMP compliance based on the percent of operations without enforcement actions. These estimates are being replaced by statistically valid and reproducible monitoring of forest practices rules and BMP compliance levels. BMP effectiveness is being assessed using both qualitative and quantitative methods. This can involve field assessments, process-based research, and control watershed studies. Some trend monitoring is also beginning. With the regional implementation rate for forestry BMPs at about 94% and rising, it is likely that effectiveness testing will continue to be a priority and consume the majority of assessment resources for this region.     

Hysteresis in Reversal of Central European Mountain Lakes from Atmospheric Acidification

Extremely high emissions of S and N compounds in Central Europe (both 280 mmol m^-2 yr^-1) declined by 70and 35%, respectively, during the last decade. Decreaseddeposition rates of SO₄ ^-2, NO₃ ^-, and NH₄ ⁺ in the region paralleled emission declines. The reduction in atmospheric inputs of S and N to mountain ecosystemshas resulted in a pronounced reversal of acidification in the Tatra Mountains and Bohemian Forest lakes. Between the 1987–1990and 1997–1999 periods, concentrations of SO₄ ^-2 and NO₃ ^- decreased (average ± standard deviation) by 22±7 and 12±7 mol L^-1, respectively, in theTatra Mountains, and by 19±7 and 15±10 mol L^-1, respectively, in the Bohemian Forest. Their decrease was compensated in part (1) by a decrease in Ca²⁺ + Mg²⁺ (17±7 mol L^-1) and H⁺ (4±6 mol L^-1), and an increase in HCO₃ ^-(10±10 mol L^-1) in the Tatra Mountains lakes, and (2) by a decrease in Al (7±4 mol L^-1), Ca²⁺ + Mg²⁺ (9±6 mol L^-1), and H⁺ (6±5 mol L^-1), in Bohemian Forest lakes. Despite the rapid decline in lake water concentrations of SO₄ ^-2 and NO₃ ^- in response to reduced S and N emissions, their present concentrations in some lakes are higher than predictionsbased on observed concentrations at comparable emission rates during development of acidification. This hysteresis in chemical reversal from acidification has delayed biological recovery of the lakes. The only unequivocal sign of biological recovery hasbeen observed in erné Lake (Bohemian Forest) where a cladoceran species Ceriodaphnia quadrangular has recentlyreached its pre-acidification abundance.     

Reconstruction of Long-Term Changes in Lake water Chemistry,Zooplankton and Benthos of a Small,Acidified High-Mountain Lake: Magic Modelling and Palaeolimnogical Analysis

Starolesnianske pleso is a small and shallow acid lake in the High Tatra Mountains, situated at 2000 m above sea level, on granitic bedrock, with sparse and thin soil cover. When detailed measurements began in the 1980s Starolesnianske pleso had pH below 5 and only one species of cladoceran zooplankton, the ubiquitous Chydorus sphaericusPalaeolimnological investigations show changes in cladoceran zooplankton and chironomid zoobenthic assemblages since about 1920 and a major change in 1970–1980. The dynamic acidification model MAGIC was used to reconstruct changes in water chemistry over the past 150 years. The results from MAGIC agree well with the sediment record; pH levels gradually decreased from 6.5 in the mid-1800s to about 5.6 in 1920 (first response in biota) to below 5.0 by 1970, and concentrations of inorganic aluminium rose dramatically beginning about 1960. In the 1990s the lake water chemistry showed clear signs of reversal in acidification brought about by a major decline in S deposition.     

Heavy Metals Removal by Biosorption and Flotation

The removal of a mixture of heavy (toxic) metal cations (copper, nickeland zinc) from liquid effluents was investigated in this study at pilotscale, using counter-current contact mode. The innovative processinvolved the abstraction of metal ions onto fungal biosorbents, followedby the application of flotation for the subsequent solid/liquid separationof biomass particles. The ability of microorganisms to remove metal ionsfrom aqueous solutions is a well-known phenomenon. Nevertheless,engineering considerations are very important in decisions, concerningthe commercial future of biosorption and practical solutions are neededfor certain problems, such as the efficient post-separation ofmetal-loaded biomass. The two processes (flotation and biosorption) caneffectively operate in combination, in what it was termed biosorptiveflotation process. The sorbents may be recycled, after appropriate elutionof metals, as well as the treated (clean) water.     

Selection of Autochthonous Plant Species from SE Spain for Soil Lead Phytoremediation Purposes

Mining activity in SE of Spain, in the west Mediterranean coast, originated more than two millenniums ago. It has generated huge areas affected by heavy metals contamination, especially of lead, which is possibly one of the most important. Investigations related to the selection of autochthonous plant taxa from a typical Spanish Mediterranean area, useful for phytoextraction and phytostabilization purposes in these polluted areas are shown. Under these edaphoclimatic conditions 12 interesting species were considered, from them six taxa were chosen for further studies. Some plant species have been proposed either for phytoextraction or phytostabilization purposes. Recommendations for further research have been discussed.     

Concentrations and Pools of Heavy Metals in Urban Soils in Stockholm,Sweden

The concentrations of heavy metals (Cd, Cr, Cu, Hg, Ni, Pb andZn) and arsenic (As) were surveyed and the metal pools estimatedin soils in Stockholm Municipality. The sampling sites were distributed all over the entire municipality with a higher sampling density in the city centre. Soils were sampled to a maximum depth of 25 to 60 cm. Soil texture, total-C content, electrical conductivity and pH were analysed. Heavy metal concentrations were determined after wet digestion with boiling7 M HNO₃.The results showed a wide range in heavy metal concentrations, as well as in other soil properties. The city centre soils constituted a rather homogeneous group whereas outside this areano geographical zones could be distinguished. These soils were grouped based on present land use, i.e. undisturbed soils, public parks, wasteland (mainly former industrial areas), and roadside soils. The city centre and wasteland soils generally hadenhanced heavy metal concentrations to at least 30 cm depth compared to park soils outside the city centre and rural (arable)soils in the region, which were used to estimate background levels. For example, the mean Hg concentration was 0.9 (max 3.3)mg kg^-1 soil at 0–5 cm and 1.0 (max 2.9) at 30 cm depth in the city centre soils, while the background level was 0,04 mg kg^-1. Corresponding values for Pb were 104 (max 444) and135 (max 339) mg kg^-1, at 0–5 and 30 cm, respectively, while the background level was 17 mg kg^-1.The average soil pools (0–30 cm depth) of Cu, Pb and Zn were 21,38 and 58 g m^-2 respectively, which for Pb was 3–4 timeshigher and for Cu and Zn 1.5–2 times higher than the backgroundlevel. The total amount of accumulated metals (down to 30 cm)in the city centre soils (4.5^*10 ⁶ m² public gardens and green areas) was estimated at 80, 1.1, 120 and 40 t for Cu, Hg, Pb and Zn, respectively. The study showed (1) thatfrom a metal contamination point of view, more homogeneous soilgroups were obtained based on present land use than on geographicdistance to the city centre, (2) the importance of establishing a background level in order to quantify the degree of contamination, and (3) soil samples has to be taken below the surface layer (and deeper than 30 cm) in order to quantify theaccumulated metal pools in urban soils.