化学镀镍老化液中镍、磷的处理与回收

以 Ca(OH) 2 作为沉淀剂 ,调节溶液 p H =1 2 ,在 80℃条件下反应 1 h,使化学镀镍老化液中镍浓度降到1 / mg· L- 1 ;分离沉淀后的溶液用硫酸调节 p H=8,按 Ca(Cl O) 2 与总 P重量比为 3 .5∶ 1 .0的比例加入 Ca(Cl O) 2 ,老化液中的磷酸盐通过形成沉淀得到去除 ,从而使化学镀镍老化液中的镍、磷含量均达到国家排放标准。对于含 Ni(OH) 2 的沉淀 ,以稀硫酸溶解回收其中的镍 ,剩余沉渣建议填埋处理 ;磷酸盐沉淀可以作为磷肥资源回用于农业生产。     

化学镀镍老化液资源化处理工艺的研究

利用三步法综合处理化学镀镍老化液。以多孔性泡沫镍作为阴极、Ti RuO2 作为阳极 ,电解回收化学镀镍老化液中的金属镍离子 ,镍的回收率可以达到 97.5 % ,同时废液中总有机碳去除率达到 97.3 % ;再以 15 %石灰乳作沉淀剂 ,每克镍投加量为 6.5mL时进一步将溶液中的残余镍处理至排放标准以下 ;最后以Ca(ClO) 2 作为氧化沉淀剂 ,处理剩余溶液中的磷 ,排放水中总磷浓度达到 1.0 6mg L ,沉淀中镍的含量低于 1.4mg kg ,以P2 O5计的磷含量高达 67.3 % ,符合农用污泥污染物控制指标 ,可以作为农业肥料使用。实验结果表明 ,利用以上方法处理 ,可以有效地将老化液中的镍、磷处理至排放标准以下 ,同时溶液中的大量有机物得到去除 ,化学镀镍老化液中的有用资源得到回收利用     

国外化学镀镍老化液处理现状

介绍了国外目前应用的化学镀镍老化液处理方法，着重推荐了沉淀法、电解法、离于交换法和电渗析法     

共沉淀富集原子吸收法测定水中5种重金属元素

使用有机共沉淀剂DDTC钠盐（铜试剂）。La^3＋作载体离子富集和乙炔火焰原子吸收分光光度法测定监测井水中Cu,Ni,Zn,Pb和Cd,结果表明，该方法精密度较高、结果准确，回收率满足微量元素测定要求,适用于达标排放水，监测井水中常见污染指标元素Cu,Ni，Zn,Pb和Cd的测定。     

木屑黄原酸酯的合成及其在处理含镍废水中的应用

采用木屑黄原酸酯(SCX)对含镍(Ni)废水进行试验研究，考察了SCX酯剂对Ni^2 的吸附性能以及药剂用量、进水的浓度，pH值和反应时间等条件对其吸附效果的影响。结果发现，木屑黄原酸酯对Ni2^2 附性能较好，经其处理后的水质可达国家有关排放标准。残渣稳定，也可酸液浸取回收重金属。     

Influence of iron,nickel and cobalt on biogas production during the anaerobic fermentation of fresh residual biomass

We have investigated the dependence of the rate of the production of biogas upon the concentration of nickel, cobalt and iron at sub-toxic concentration and monitored its composition as amount of hydrogen, methane and carbon dioxide. The distribution of the added metals between the liquid and solid phase has also been monitored.

The results of our investigations show that the addition of any of the listed metals to the sludge may cause the production of a higher amount of biogas and influence the methane or carbon dioxide percentage. Conversely, the effect on the hydrogen production depends upon the metal added, the age of the active sludge used, and its adaptation to the susbtrate. As a general feature, during the acidogenesis phase, nickel reduces, while iron increases, the percentage of dihydrogen in the biogas, while cobalt has no influence.     

The effect of calcium and pH on nickel accumulation in and rhizotoxicity to pea (Pisum sativum L.) root-empirical relationships and modeling

The accumulation and rhizotoxicity of Ni to pea were investigated. Calcium, H, and Ni competed for root-binding sites with high pH and low Ca favoring more Ni accumulation. At low pH, Ca accumulation is the key factor determining root growth, while at medium to high pH, root elongation is more sensitive to Ni concentration. The tissue concentration of Ni and Ca ([Ni]t or [Ca]t, μmol g⁻¹ dry root) can be predicted from total dissolved Ni ([Ni]_T, μM), pH, and total dissolved Ca ([Ca]_T, mM) by two approaches. Approach 1 is the empirical equations [Ni]t = (0.361 pH-0.695[Ca]_T)*[Ni]_T and [Ca]t = 8.29 pH + 10.8 [Ca]_T. The second approach involves a two-step model. The surface-bound Ni and Ca are estimated from a surface adsorption model with binding constants derived from independent ion adsorption experiments. Then transfer functions are used to predict internal root Ni and Ca accumulation.     

Transfer of elements relevant to radioactive waste from soil to five boreal plant species

In long-term safety assessment models for radioactive waste disposal, uptake of radionuclides by plants is an important process with possible adverse effects in ecosystems. Cobalt-60, ^59,63Ni, ⁹³Mo, and ²¹⁰Pb are examples of long-living radionuclides present in nuclear waste. The soil-to-plant transfer of stable cobalt, nickel, molybdenum and lead and their distribution across plant parts were investigated in blueberry (Vaccinium myrtillus), May lily (Maianthemum bifolium), narrow buckler fern (Dryopteris carthusiana), rowan (Sorbus aucuparia) and Norway spruce (Picea abies) at two boreal forest sites in Eastern Finland. The concentrations of all of the studied elements were higher in roots than in above-ground plant parts showing that different concentration ratios (CR values) are needed for modelling the transfer to roots and stems/leaves. Some significant differences in CR values were found in comparisons of different plant species and of the same species grown at different sites. However, large within-species variation suggests that it is not justified to use different CR values for modelling soil-to-plant transfer of these elements in the different boreal forest plant species.     

Influence of variable chemical conditions on EDTA-enhanced transport of metal ions in mildly acidic groundwater

Adsorption of Ni and Pb on aquifer sediments from Cape Cod, Massachusetts, USA increased with increasing pH and metal-ion concentration. Adsorption could be described quantitatively using a semi-mechanistic surface complexation model (SCM), in which adsorption is described using chemical reactions between metal ions and adsorption sites. Equilibrium reactive transport simulations incorporating the SCMs, formation of metal-ion-EDTA complexes, and either Fe(III)-oxyhydroxide solubility or Zn desorption from sediments identified important factors responsible for trends observed during transport experiments conducted with EDTA complexes of Ni, Zn, and Pb in the Cape Cod aquifer. Dissociation of Pb-EDTA by Fe(III) is more favorable than Ni-EDTA because of differences in Ni- and Pb-adsorption to the sediments. Dissociation of Ni-EDTA becomes more favorable with decreasing Ni-EDTA concentration and decreasing pH. In contrast to Ni, Pb-EDTA can be dissociated by Zn desorbed from the aquifer sediments. Variability in adsorbed Zn concentrations has a large impact on Pb-EDTA dissociation.