江苏省含低放射性废渣清洁解控技术规范探讨

以江苏省稀土行业废渣实际情况为背景,基于国内外对天然放射性物质(NORM)的管理限值水平,通过理论研究和模型构建,建立了废渣中放射性核素质量活度与现场γ剂量率之间的关系。通过现场实验和样品γ谱核素分析结果进行模型修正,在留有足够安全冗余的情况下确定现场γ剂量率筛选水平,并提出了一套操作性较强的NORM废物γ剂量率筛选现场检验程序。     

两性修饰红薯渣对紫色土吸附Cu2+的影响

采用十二烷基二甲基甜菜碱对红薯渣（R）做两性修饰,修饰比例分别为0、100%和200%,将得到的3种两性修饰红薯渣（R、100BS-R和200BS-R）以1%质量分数加入紫色土（PS）中,制成PS（对照）、PSR、PS100BS-R和PS200BS-R 4种混合土样。用批量处理法探究各供试土样对Cu2+的吸附等温特征,并考察温度、pH值和离子浓度对Cu2+吸附的影响。结果表明：各混合土样对Cu2+的吸附等温线均符合Langmuir模型,最大吸附量为99.46 mmol/kg~136.53 mmol/kg,Cu2+吸附量呈现PS200BS-R>PS100BS-R>PSR>PS的趋势。温度和pH值升高均有利于Cu2+被吸附,当离子浓度为01 mol/L时吸附效果最佳。     

锰磁活性炭的制备及其性能表征

以酶解提制烟碱后的烟渣和电解锰渣回收锰为原料,制备具备磁性和发达孔隙的活性炭。利用氮气吸附技术、红外光谱（FTIR）表征与分析了活性炭表面的孔隙结构和物化性质,考察了活性炭对亚甲基蓝的吸附性能和磁学性能。结果表明：以Mn／C基质废弃物为原料制得活性炭具有磁学性能;适量锰的添加有利于活性炭微孔的形成和发育;采用一步焙烧法有助于磁化物和活性炭基体相互作用形成化学键合,提高饱和磁化强度,实现废弃资源的充分利用。     

进口含锌物料的表征和鉴别

采用X射线荧光光谱(XRF)、X射线衍射光谱(XRD)等分析手段,对4种进口疑似固体废物的含锌物料进行了表征。通过分析含锌物料的主要元素组成、物相组成和常规理化特征,结合外观特征,与含锌矿物、含锌产品及相关文献资料等进行比对,推导出含锌物料的产生来源。然后,参照我国《进口废物管理目录》得出鉴别结论。结果表明:4种含锌物料分别为锌矿、湿法冶炼锌浸出渣、热镀锌灰和固定CO2产物;后3种属于我国目前禁止进口的固体废物。     

染料溶液的臭氧脱色效率和残留物的分析研究

选用偶氮、蒽醌和菁型三类染料中的11种作为研究对象,考察不同反应时间下臭氧对染料色度脱除和溶液pH值变化的影响,并对降解后溶液中的残留物进行定量分析.结果表明,除分散染料外,所有可溶性染料在20min内的脱色率均达到79%以上;不同应用类型染料的脱色速率顺序为:活性＞酸性＞直接＞阳离子＞分散,在可溶性染料中,同类型的分子质量小的染料脱色速率较快.酸性物质的生成使得溶液的pH值随反应时间的推移而下降,最终pH值都低于4.5,pH值与脱色率在总体上的变化趋势一致.臭氧氧化脱色表现为复杂的染料分子被降解成为简单的有机化合物,染料分子中的-SO3H和-Cl基团大部分生成了SO2-4和Cl-,而PO3-4仍以游离的H2PO4-存在于溶液中,氮则是根据其基团的不同而部分被降解生成NO-3,降解溶液中不存在NO-2.     

Dynamics of novel insecticide HNPC-A9908 residue in vegetable-field ecosystem

HNPC-A9908 （o-（3-phenoxybenzyl）-2-methylthio-1-（4-chlorophenyl） propyl ketone oxime）, a novel oxime insecticide, is a highly effective and broad-spectrum insecticide which can be widely used to control many species of foliar insects on various crops. A study was conducted to evaluate the fate of HNPC-A9908 and study the degradation dynamics of HNPC-A9908 residue in vegetable field ecosystem. The results showed that degradation of HNPC-A9908 was much faster in vegetable pakchoi than in soil, and its half-life in pakchoi and soil was 1.32 and 3.75 d, respectively. The final residue of HNPC-A9908 in pakchoi was at the undetectable level to 0.122 mg/kg. As a conclusion, a dosage of 90 g/hm^2 was suggested and considered to be safe to human beings and animals.     

HPLC法检测灭蝇胺在黄瓜和土壤中的残留

建立了高效液相色谱测定灭蝇胺在黄瓜和土壤中残留的方法,灭蝇胺的最小检出量为4×10-10g.对黄瓜样品,在005—50mg·kg-1时,平均回收率为762—862%;变异系数为04—20%,最低检出浓度为002mg·kg-1.对土壤样品,在02—50mg·kg-1时,平均回收率为854—881%;变异系数为06—14%,最低检出浓度为002mg·kg-1.     

铬渣水泥固化体稳定性研究

采用水泥固化的方法对铬渣进行处理。在水泥与铬渣、砂、水、硅酸钠的质量比为1：0．6：0．45：0．15：0．1时固化效果较好。固化体经28d的养护后,表面Cr^6 的浸出率为10^-5数量级,即使破碎至5mm以下的粒度,其Cr^6 的浸出质量浓度仍在国家标准以下。模拟酸溶试验和固化体抗压强度测试结果表明,固化体用于填埋是长期安全的。     

Dynamics of Organic Carbon and Microbial Biomass in Alluvial Soil With Tillage and Amendments in Rice-wheat Systems

Rice-wheat cropping systems of the Indo-Gangetic plains (IGP) occupying 12 million ha of productive land are important for the food security of South Asia. There are, however, concerns that yield and factor productivity trends in these systems are declining/stagnating in recent years. Decrease in soil organic carbon is often suggested as a reason for such trends. A field experiment was conducted to study the soil organic carbon (SOC) and soil microbial biomass carbon (MBC) dynamics in the rice-wheat systems. Use of organic amendments and puddling of soil before rice transplanting increased SOC and MBC contents. Microbial biomass carbon showed a seasonal pattern. It was low initially, reached its peak during the flowering stages in both rice and wheat and declined thereafter. Microbial biomass carbon was linearly related to SOC in both rice and wheat indicating that SOC could be used as a proxy for MBC.     

Identification of the bound residue composition derived from 14C-labeled chlorsulfuron in soil by using LC-MS and isotope tracing method

A new method for extracting the bound residue(BR) derived from ^14C-iabeled chlorsulfuron in soils was developed, and the technique of combining LC-MS with isotope tracing method was subsequently applied to identify the composition of the ^14C-BR in a loamy Fluvent derived from manne deposit. The results showed that the ^14C- [ 2- amino-4- methoxyl-6- methyl- 1,3,5 ]-triazine, ^14C- [ 2-amino-4-hydroxyl-6-methyl-1,3,5]-tdazine and ^14C-chlorsulfuron parent compound constituted the main composition of the ^14C-BR denved from ^14C-labeled chlorsulfuron in the soil. The radioactive ratio of three compounds accounted for 39.8 %, 35.4 % and 17.9 % of total recovered radioactivity, respectively. However, a small amount(3.6 % of total recovered radioactivity) of the complex of ^14C- [ 2-amino-4-hydroxyl-6-methyl-1,3,5]-tdazine might have existed in the ^14C-BR in association with an unknown soil substrate. 2-chlorobenzenesulfonamide was also detected to be one of the components of the BR. The results could well explain the mechanism of phytotoxicity caused by the BR derived from chlorsulfuron in soil. In addition, the mechanism of BR formation in soil was also discussed in details.