沉淀-电解氧化法处理高铁氰化废水

采用沉淀-电解氧化联合技术处理高铁氰化提金废水,重点考察了沉淀剂添加量、沉淀时间、温度、电解电压、电解时间等因素对总氰、游离氰和铁氰络合物去除率的影响。结果表明,随着CuCl₂加入量的增大,氰化废水中各主要离子的沉淀率逐步增加。常温下向100 mL含氰废水中加入3.0 g CuCl₂并搅拌40 min后,总氰(CN_T)、CN⁻、Fe离子的去除率分别可达到95.29%、98.00%与100%。以钛板为阴阳极,采用一阴两阳体系对沉淀后液进行电解氧化实验,当电压为6 V、极间距为15 mm、电解时间为5 h、初始浓度为60%的条件下,CN_T和CN⁻的去除率最高可达到99.76%和99.90%。XRD分析表明,沉淀过程中铜氰、铁氰络合离子的去除主要归因于CuCN、Cu₂Fe(CN)₆、CuSCN等沉淀的形成。电解氧化过程中随着外加电压与氯离子浓度的增大,废水中残存的游离氰与金属氰络合离子的去除率逐渐增加,这主要是阳极反应产生的Cl₂/ClO⁻等强氧化剂作用的结果。以上研究结果可为高铁氰化提金废水的综合处理提供参考。     

生石灰孔结构对高温脱硫性能的影响

喷钙脱硫工艺的炉内脱硫率 ,不仅受工艺参数的影响 ,还与石灰石分解生成的新生CaO或直接喷入的CaO的表面结构有关。本研究用同一石灰石经不同方法 (煅烧、过烧、煅烧 -水合 -脱水等 )制备了四种具有不同比表面积和孔结构的生石灰。高温脱硫研究表明 :这四种不同孔结构的生石灰 ,具有不同的脱硫率。通过对高温脱硫前后吸着剂宏观结构变化的对比 ,发现半径小于 30 的孔易被反应产物堵塞 ,因而脱硫能力有限 ,而半径大于 5 0 的孔对脱硫更有效。本研究将为提高炉内喷钙的脱硫率、研制和开发高效脱硫剂提供新的途径。     

结晶沉淀-树脂吸附组合工艺回收黄连素废水中铜试验研究

通过多批次的小试试验考察了结晶沉淀-树脂吸附组合工艺对黄连素含铜废水的处理效果,并对产生的碱式氯化铜(TBCC)结晶沉淀进行X射线衍射(XRD)成分分析。结果表明:反应pH为7.0~9.0时,废水中超过99.9%的Cu ²⁺以碱式氯化铜结晶沉淀的形式得以回收,反应生成的碱式氯化铜沉淀通过水洗后,其成分符合GB/T 21696—2008《饲料添加剂 碱式氯化铜》质量标准。剩余的废水再经过树脂吸附工艺处理后,出水Cu ²⁺浓度小于1.0 mg/L。在小试试验的基础上,开展了中试试验研究,其结果进一步验证了小试试验的运行效果及该工艺的可行性。通过该处理工艺既可综合利用废水中的铜资源,又可将废水的pH由小于1调至大于7,有利于实现制药废水综合处理和达标排放。     

采用两级物化法去除黄磷废水中的氟化物

采用向含氟废水中加入适量石灰和聚合氯化铝，然后投加适量钙盐、磷酸和聚丙烯酰胺的二级处理工艺除氟，通过控制合适的pH、钙盐和磷酸的投加量、反应时间、反应温度、搅拌强度和絮凝剂的投加量，可使黄磷废水中氟的质量浓度降至5mg/L，氟的去除率达到99％以上，出水中氟的质量浓度达到GB8978－1996一级排放标准。     

改进型石灰混凝法去除城市污水二级出水中有机物的研究

将石灰混凝处理后的沉淀泥渣进行回流，对石灰混凝法进行改进，研究改进后的石灰混凝法对城市污水二级出水中有机物的去除效果。结果表明，活性泥渣回流有利于提高石灰混凝法对城市污水二级出水中有机物的去除。回流位置在石灰投加前、复合絮凝剂投加后，最佳回流量为新泥渣产生量的100％～200％，活性泥渣回流的最佳pH为11．0～11．5；活性泥渣中CaCO3、Mg(OH)2、Fe(OH)3等沉淀物以及有机高分子絮体均有助于提高其对有机物的去除效果，其中Mg(OH)2沉淀物起主导作用；含循环泥渣的活性污泥回流，对有机物的去除效果无明显影响。     

Effects of Acidification and its Mitigation with Lime and Wood Ash on Forest Soil Processes: A Review

Anthropogenic acid deposition causes forest soil acidification and perturbation of the soil forming processes. The impact of soil acidification on tree growth is discussed in view of the role of mycorrhizal fungi in weathering and nutrient uptake. A review has been carried out of experiments involving treatments of forest soil by lime and wood ash, where soil properties and soil solution composition have been investigated. Results from these experiments in Europe and North America are summarized. In general, the content of C in the mor layer decreased as a result of treatment due to higher microbial activity and soil respiration as well as increased leakage of DOC. In addition, the content of N in the mor layer, in general, decreased after treatment and there are occasional peaks of high NO₃concentrations in soil solution. In nearly all reviewed investigations the pH of the deep mineral soil solution decreased and Al, SO₄and NO₃concentrations increased after treatment. These effects are probably due to the high ionic strength and increased microbial activity as a consequence of the treatments. In the soil, pH, CEC and base saturation increased in the upper horizons, but decreases in the upper mineral soil are also reported. In general, there was no increase in tree growth as a result of these treatments. The positive effects of the treatments on soil processes and tree growth are therefore questionable. In view of these conclusions, an investigation was carried out on the soil and soil solution chemistry and the role of mycorrhizal fungi in a spruce stand treated with two doses of lime and another treated with lime/ash in southern Sweden. The results of this investigation is reported in this volume.     

QUALITY OF HYDROMETEOROLOGICAL DATA IN COLD REGIONS1

ABSTRACT: Many users of hydrometeorological records are not aware of the number of inconsistencies and biases that occur in hydrometeorological records. Examples are presented illustrating how the exposures of sites for measurement of precipitation, wind, snow on the ground, and evaporation determine to a large extent how useful the records are for estimating areal conditions. For areas where precipitation in the form of snow produces a significant portion of the runoff, a smaller number of quality records may be more valuable for modeling than a much larger number of records of lower quality. Information is presented to show that the overall value of an operational hydrometeorological network is dependent upon how consistent and representative of average conditions the collected records are, especially for mountainous areas in cold regions.     

云南近百年来温度雨量的变化特征分析

用气候倾向率、Morlet小波方法,对云南10个站1901-2007年的年降水和平均温度资料分析表明:100年来云南平均增温速率为0.031℃/10a。近50年来全省平均增温速率为0.242℃/10a,略高于全国的增温,增温最大的是滇中的昆明、滇南的普洱,分别为0.442℃/10a和0.409℃/10a,并且西部明显高于东部。100年来云南年降水呈减少趋势,平均速率为7.288mm/10a,近50年来,年降水量减少平均速率为6.66mm/10a。但云南降水的区域分异非常明显,云南的东部、中部降水减少;而滇西北和滇东南地区降水增加。云南气温明显的年代际变化是32年,发生了3次突变。年降水呈明显的年代际及年际振荡,具有16～32年、4～8年周期。     

Effects of long-term nitrogen addition and precipitation changes on CH4 flux in an alpine steppe北大核心CSCD

土壤是甲烷(CH4)重要的源和汇.氮沉降和降水格局变化正在急剧改变土壤碳循环,进而可能对土壤CH4通量造成深刻影响.高寒生态系统是巨大的碳库,对氮沉降和降水变化十分敏感.然而,目前多数研究集中在短期实验上,缺乏对长期氮沉降和降水变化背景下CH4通量的响应及其调控因素的认识.以青藏高原高寒草原为研究对象,在2013年搭建模拟氮沉降和降水格局改变实验平台.基于静态箱–气相色谱法测定2020年生长季(5-10月)土壤CH4通量.结果显示,高寒草原土壤呈CH4的汇.氮添加没有显著改变生长季和植物生长高峰CH4通量.然而,降水变化显著改变了生长季和植物生长高峰CH4通量,其中降水增加(+50%降水)降低了CH4的吸收(分别为–16%和–45%),降水减少(–50%降水)增强了CH4的吸收(分别为+73%和+33%).进一步研究发现,与植物属性和功能基因丰度相比,土壤环境因子主导了CH4通量变化(解释率>90%).其中CH4通量与土壤含水量和温度显著正相关,与土壤pH显著负相关.综上所述,在未来全球变化情景下,降水格局改变更能调节青藏高原高寒草原CH4通量的变化.(图6表1参37)     

Polycyclic aromatic hydrocarbons in the bulk precipitation and surface waters of Northern Greece

Bulk (wet and dry) precipitation and surface water sampling was undertaken in the main plain of central Macedonia in Northern Greece. Fourteen polycyclic aromatic hydrocarbons (PAHs) included in the US EPA's priority pollutant list were analysed. The concentrations determined in bulk precipitation were in general within the range of values worldwide reported. Concentrations were highest in the cold months. Deposition fluxes of PAHs were of the same order of magnitude as reported data. The greatest values were found when high concentrations of PAHs in precipitation coincided with large precipitation amounts. The concentrations of PAHs in surface waters (main rivers, tributaries, ditches, etc) were in general lower than those in bulk precipitation, and among the lowest reported for European rivers, excepting Np and Ph. Bulk deposition and domestic effluents are suggested as being the main PAH sources into surface waters.