石灰石中微量杂质对其脱硫活性的影响研究

石灰石的活性对湿法烟气脱硫工艺具有重要意义。采用间歇式硫酸消溶的方法，分别研究了石灰石中各微量杂质浓度对石灰石活性的影响，就其影响结果及其影响机理进行了理论分析，并用拟合曲线的方法预测各种杂质成分的影响程度。结果表明，二氧化硅和氧化铁的含量在一定范围内能提高石灰石的活性，超过此范围将使其活性降低，而氧化镁的存在能大幅提高石灰石的活性，氧化铝对石灰石活性影响不大。     

陶瓷烧成中气氛及温度对NOX生成的影响

通过对不同烧成气氛NOX的生成进行测试分析,得出还原气氛可抑制NOX的生成.但在没有催化剂存在的情况下,CO对NO的还原效果不显著;其次,在烧成温度较低(1 200 ℃以下)、高温阶段温度场均匀性较好且使用洁净燃料(即含氮量较小的燃料)的情况下,快速升温将导致NOX生成的增加,此时快速型NOX起主要作用;第三,烧嘴的合理布置、改善窑体结构和加强高温阶段窑内温度场的均匀性可以减少NOX的生成.     

Stimulation of reductive dechlorination of hexachlorobenzene in soil by inducing the native microbial activity

The reductive dechlorination and behaviour of ¹⁴C-hexachlorobenzene (HCB) was investigated in an arable soil. The activity of the native anaerobic microbial communities could be induced by saturating the soil with water. Under these conditions high rates of dechlorination were observed. After 20 weeks of incubation only 1% of the applied ¹⁴C-HCB could be detected in the fraction of extractable residues. Additional organic substances, like wheat straw and lucerne straw, however considerably delayed and reduced the dechlorination process in the soil. The decline of HCB was not only caused by dechlorination but also by the formation of non-extractable residues, whereby their amounts varied with time depending on the experimental conditions. Several dechlorination products were detected, indicating the following main HCB transformation pathway: HCB → PCB → 1,2,3,5-TeCB → 1,3,5-TCB → 1,3-DCB, with 1,3,5-TCB as main intermediate dechlorination product. The other TeCB-, TCB- and DCB-isomers were also detected in low amounts, showing the presence of more than one dechlorination pathway. Since the methane production rates were lowest when the dechlorination rates were highest, it can be assumed that methanogenic bacteria were not involved in the dechlorination process of HCB. The established ¹⁴C-mass balances show, that with increasing dechlorination and incubation times, the ¹⁴C-recoveries decreased.     

Effect of liming on sulfate transformation and sulfur gas emissions in degraded vegetable soil treated by reductive soil disinfestation

Reductive soil disinfestation (RSD), namely amending organic materials and mulching or flooding to create strong reductive status, has been widely applied to improve degraded soils. However, there is little information available about sulfate (SO₄^2 −) transformation and sulfur (S) gas emissions during RSD treatment to degraded vegetable soils, in which S is generally accumulated. To investigate the effects of liming on SO₄^2 − transformation and S gas emissions, two SO₄^2 −-accumulated vegetable soils (denoted as S1 and S2) were treated by RSD, and RSD plus lime, denoted as RSD₀ and RSD₁, respectively. The results showed that RSD₀ treatment reduced soil SO₄^2 − by 51% and 61% in S1 and S2, respectively. The disappeared SO₄^2 − was mainly transformed into the undissolved form. During RSD treatment, hydrogen sulfide (H₂S), carbonyl sulfide (COS), and dimethyl sulfide (DMS) were detected, but the total S gas emission accounted for < 0.006% of total S in both soils. Compared to RSD₀, lime addition stimulated the conversion of SO₄^2 − into undissolved form, reduced soil SO₄^2 − by 81% in S1 and 84% in S2 and reduced total S gas emissions by 32% in S1 and 57% in S2, respectively. In addition to H₂S, COS and DMS, the emissions of carbon disulfide, methyl mercaptan, and dimethyl disulfide were also detected in RSD₁ treatment. The results indicated that RSD was an effective method to remove SO₄^2 −, liming stimulates the conversion of dissolved SO₄^2 − into undissolved form, probably due to the precipitation with calcium.     

Size distributions of manure particles released under simulated rainfall

Manure and animal waste deposited on cropland and grazing lands serve as a source of microorganisms, some of which may be pathogenic. These microorganisms are released along with particles of dissolved manure during rainfall events. Relatively little if anything is known about the amounts and sizes of manure particles released during rainfall, that subsequently may serve as carriers, abode, and nutritional source for microorganisms. The objective of this work was to obtain and present the first experimental data on sizes of bovine manure particles released to runoff during simulated rainfall and leached through soil during subsequent infiltration. Experiments were conducted using 200 cm long boxes containing turfgrass soil sod; the boxes were designed so that rates of manure dissolution and subsequent infiltration and runoff could be monitored independently. Dairy manure was applied on the upper portion of boxes. Simulated rainfall (ca. 32.4 mm h(-1)) was applied for 90 min on boxes with stands of either live or dead grass. Electrical conductivity, turbidity, and particle size distributions obtained from laser diffractometry were determined in manure runoff and soil leachate samples. Turbidity of leachates and manure runoff samples decreased exponentially. Turbidity of manure runoff samples was on average 20% less than turbidity of soil leachate samples. Turbidity of leachate samples from boxes with dead grass was on average 30% less than from boxes with live grass. Particle size distributions in manure runoff and leachate suspensions remained remarkably stable after 15 min of runoff initiation, although the turbidity continued to decrease. Particles had the median diameter of 3.8 microm, and 90% of particles were between 0.6 and 17.8 microm. The particle size distributions were not affected by the grass status. Because manure particles are known to affect transport and retention of microbial pathogens in soil, more information needs to be collected about the concurrent release of pathogens and manure particles during rainfall events.     

太湖湖泊缓冲带不同类型草林复合系统中氮、磷的溶出与沉降特征

以太湖竺山湾缓冲带中湿地岸带、支浜岸带、人工防护林3种主要类型的草林复合系统为研究对象,分别对其自身氮、磷溶出及沉降特征进行了研究,从而揭示缓冲带本身对地表径流和地下渗流的影响。结果表明,3种样地中总氮的溶出率在0.3%~2.5%,平均溶出率表现为人工防护林支浜岸带湿地岸带;总磷的溶出率在0.8%~4.0%,平均溶出率表现为支浜岸带湿地岸带人工防护林。氮、磷在向下沉降的过程中表现出不同的规律。各样地不同深度土壤渗透液中总氮浓度的变化趋势不一,基本表现为随深度增加而增加,总氮浓度为湿地岸带人工防护林支浜岸带;总磷浓度的变化趋势也不尽相同,与总氮相比,总磷的沉降效果不显著。综合来看,3种草林复合系统对污染物的沉降效果为湿地岸带人工防护林支浜岸带。     

污水污泥中重金属污染物的溶出过程研究

污水污泥中污染物尤其是重金属的水体浸出作为重要的二次污染途径备受关注。为了探讨污水污泥中重金属的溶出规律,对上海7个污水处理厂的污水污泥进行了重金属总量分析,并采用水平振荡法对上述污水污泥中重金属进行了溶出动力学研究。结果表明,污水污泥中Cu、Cr和Zn的含量均较高,之后依次是Pb、As、Cd和Hg;污水污泥中重金属溶出动力学过程分为快速反应和慢速反应两个过程,可以用Elovich方程进行模拟;污水污泥中各重金属的溶出负荷差异较大,Cu、Cr和Zn的溶出负荷较大,其他较小,但各重金属相对于污水污泥中重金属总量的溶出百分比差异不大,基本处于10%以下。     

滇池流域不同土壤类型和土地利用方式的土壤中溶解性有机碳的流失特性研究

采集滇池流域不同土壤类型、不同土地利用方式下的土壤样品,进行土壤中溶解性有机碳(DOC)的静态解吸实验,通过测定不同时间下溶入水相的COD量,探究不同土壤类型及土地利用方式下DOC的流失特性,从而揭示不同土地利用方式对滇池流域面源污染的影响.结果表明,同一土地利用方式的不同类型土壤中DOC的溶出平衡时间为壤土＞粘土＞粘壤土,其中退耕区(粘壤土＞粘土＞壤土)、大棚(粘土＞粘壤土=壤土)土壤不符合该规律,溶出平衡时间基本为1.5～2.5h;不同的土壤类型和土地利用方式下,DOC的溶出率为1.00％～2.75％,同一土地利用方式的不同类型土壤中DOC的溶出率存在一定差别,这是由于不同类型的土壤中砂粒、粉粒、粘粒的含量有所差异.     

湿法脱硫中石灰石溶解特性的模型及实验研究

在石灰石-石膏湿法烟气脱硫中,石灰石的溶解影响到浆液吸收SO2的能力及吸收塔持浆池的大小.根据传质及化学离子平衡理论,建立了石灰石的溶解模型,并通过实验对模型进行了验证,结果表明,模拟结果与实验值基本一致,模型较好地反映出石灰石的溶解过程;在浆液pH较低的情况下,通过增强搅拌强度,可以明显提高石灰石的溶解速率,而在浆液...