积融雪控制下土壤大气间汞交换通量特征

位于松花江上游流域的夹皮沟金矿曾是我国采金量最大的矿区,广泛使用的混汞法提金工艺导致了严重的区域环境介质汞污染.为研究稳定性季节积雪及融雪控制过程土壤(雪)大气间汞交换通量特征,选择区域内典型"山-谷"地形结构单元,沿坡面等距进行布点,使用动态通量箱法测定了各采样点土壤(雪)大气间汞交换通量,使用塞曼效应汞分析仪(LUMEX Zeeman RA915+)测定了各采样点近地面(0～150 cm)垂直方向上大气汞浓度分布,分析了同步气象因子、积融雪控制下地表性质和近地面大气汞的垂直分布各因素对土壤(雪)大气间汞交换通量特征的影响.结果表明,冬季积雪和融雪期间,大气中汞均有沿山坡向谷底汇集的趋势,在积雪冷源性下垫面所致逆温层结控制下,汞交换通量表现为明显的由大气向土壤(雪)的沉降过程.融雪期间雪融后地表土壤大气间汞交换通量表现为释放与沉降过程交替,仍然积雪地表大气间汞交换通量沉降水平明显弱于积雪期.分析土壤(雪)大气间汞交换通量与其影响因素间关系发现,积雪期土壤(雪)大气间汞交换通量与大气汞浓度和大气温度间均具有显著的负线性相关关系;融雪期土壤(雪)大气间汞交换通量与大气汞浓度间具有明显的负线性相关关系,与大气温度间具有正线性相关关系;雪融后裸露土壤大气间汞交换通量与地温间呈现一定的正线性相关关系.     

Formation characteristics of polychlorinated dibenzo-p-dioxins, polychlorinated dibenzofurans, and coplanar PCBs in fly ash from a gasification–melting process of municipal solid waste

PCDDs/DF and Co-PCB (dioxin) formations were studied with ash from a newly developed gasification and melting process for municipal solid waste. Ash samples were heated in a laboratory-scale fixed-bed reactor. Emphasis was placed on the effects of the type and composition of ash, temperatures, gas residence time, and gaseous organic precursors. Investigations using macroscopic and homologue distribution analyses led to the following conclusion. The ash from the gasification–melting process had the ability to generate dioxins in flue gas. A possible carbon source is unburned carbon in the ash samples, although this was very low (less than 0.01%). An experimental result that the level of dioxins generated from preheated fly ash obtained from a conventional incinerator was much lower than that from nonheated fly ash supported this conclusion. Dioxin concentrations obviously showed temperature dependence and peaked at 350°C. Dioxins formed in a gasification–melting process ash were readily desorbed from the surface, probably because of the low carbon content of the ash. There was no experimental evidence that gaseous organic precursors fed to the reactor generated dioxins. Therefore, an organic precursor was not essential for the formation of dioxins. A good linear relationship obtained between PCDDs/DFs and gas residence time also supported the assumption. Received: February 14, 2000 / Accepted: June 30, 2000     

垃圾焚烧飞灰熔融渣特性分析

研究了熔融固化产物--熔融渣的特性.结果表明:熔融渣的主要成分为CaO,Al₂O₃和SiO₂,其含量占总质量的99%左右,而SO₃,K₂O,Na₂O和Cl在熔融渣中的含量明显降低,其质量分数分别从原始飞灰中的10.74%,8 58%,3.81%和20.59%降低到0.17%,0.04%,0.23%和0.11%;熔融渣中碱性氧化物和酸性氧化物的含量基本相同,碱度接近于1.0;重金属Cr和Zn的固定率较高,分别为94.2%和81 7%,而Cu,Pb和Cd的固定率较低,分别为31.4%,14.5%和24.6%;采用美国TCLP方法测试的熔融渣中重金属浸出量均低于国家危险废物浸出毒性鉴别标准限值.      

塔里木西南缘下地壳低速层的成因:斜长角闪岩的纵波速度和衰减的限制

在1 0GPa,室温～1200℃条件下,测量了新疆库地地区斜长角闪岩的纵波速度(Vp)和品质因子(Q值),得出在1 0GPa恒压下,Vp和Q值随温度和深度的变化关系。结果显示,Vp和Q值随温度的升高而下降,观察实验样品并结合Vp和Q值与熔体含量的关系,发现部分熔融是影响Vp和Q值变化的主要因素。依据实验结果,并结合区域上压力梯度和温度梯度资料计算了Vp和Q值随深度的变化。结果表明Vp和Q值先随深度的增加而缓慢增大,在32km左右开始突然减小,表明开始出现低速层。结合温度和熔体含量的关系得出,低速层的出现可能是部分熔融的结果。塔里木及周边地区的地震测深以及地震反演的结果也显示,在相同的温度和压力条件下,地壳内部32～44km的范围内存在低速层,同时高温高压的实验结果与阿拉木图地区的Vp值相当一致,可以推测塔里木西南缘下地壳的岩石成分中含有斜长角闪岩。     

蒙古栎林生态系统的辐射能量与水分关系的研究

本文把水分循环与辐射能量转换两个功能过程结合起来,研究蒙古栎林生态系统中的辐射能量与水分的关系。结果表明,森林作用层与林地作用层由于获得不同待征的辐射能量,导致水分交换的数量与方向不同。约74.5％的净辐射用于森林的水分蒸发散,而蒸发散又占降雨量77.45％。可见,辐射能量的大部分用于水分循环。本文还研究了辐射能量对融雪过程的影响,发现针阔混交林在冬季由于具有获得适度辐射能量的特点,使得它是一种较理想的融雪径流产流模式,为合理经营森林提供了依据。     

Research on low emission MSW gasification and melting system

In order to eliminate secondary pollution caused by municipal solid waste (MSW) incineration, a MSW gasification and melting process is proposed. The process is expected to reduce the emission of pollutants, especially heavy-metals and dioxins. In this paper, the combustible components of MSW and simulated MSW were gasified in a lab-scale fluidized bed at 400°C–700°C when the excess air ratio (ER) was between 0.2 and 0.8. The experimental results indicated that the MSW could be gasified effectively in a fluidized bed at approximately 600°C–700°C when excess air ratio was 0.2–0.4. The melting characteristics of two typical fly ash samples from MSW incinerators were investigated. The results indicated that fly ash of pure MSW incineration could be melted at approximately 1,300°C and that of MSW and coal co-combustion could be melted at approximately 1,400°C. When temperature was over 1,100°C, more than 99.9% of the dioxins could be decomposed and most of the heavy-metals could be solidified in the slag. Based on the above experiments, two feasible MSW gasification and melting processes were proposed for low calorific value MSW: (1) sieved MSW gasification and melting system, which was based on an idea of multi-recycle; (2) gasification and melting scheme of MSW adding coal as assistant fuel. __________ Translated from Environmental Science, 2006, 27(1): 69–73 [译自: 环境科学]     

某铅锌矿区农田重金属分布特征及其风险评价

为进一步探讨铅锌矿开采和冶炼地区农田重金属污染的分布特征和污染途径,以会泽县者海镇铅锌矿区周边农田土壤为研究对象,共布设496个采样点,测定表层土壤中重金属（Cd、Hg、Pb、Cu、Zn）的含量.利用自然邻点法对表层土壤中重金属含量进行插值拟合,以空间三维模型研究该地区农田土壤重金属污染特征,运用单因子指数、综合污染指数和潜在生态风险指数法对重金属污染程度进行评价,采用相关分析、主成分分析和聚类分析识别污染途径.结果表明：Cd、Hg、Pb、Cu和Zn的含量平均值（mg/kg）分别是云南省背景值的33.05、5.83、12.02、4.89和16.33倍;Cd、Hg、Pb、Zn含量空间分布表现为西北部浓度最高,且中部高于东西两侧,而Cu与此相反;单因子指数评价结果显示99.8%的土样达到Cd重度污染,其次是Cu（82.06%）、Zn（62.50%）;综合污染指数表明,研究区均处于重度污染程度,西北部尤为严重;综合生态风险评价表明,中部风险高两边低,Cd的贡献率最大占61%;相关分析结果显示,Zn、Cd、Pb、Hg之间呈显著正相关性（P < 0.01）,表明其污染途径相近;主成分分析和聚类分析表明,Cd、Hg、Pb、Zn污染途径主要与人类活动有关,Cu主要受自然因素影响,因此对该地区土壤重金属的修复和治理应综合考虑人为因素和自然因素的影响.     

利用某尾矿制备纳米SiO2

采用固相熔融法从尾矿中提取SiO2,利用超声辅助化学沉淀法制备纳米SiO2。分别研究了NaOH与尾矿质量比、反应温度、反应时间对SiO2提取率的影响,以及溶解水量、HCl浓度、终点pH、超声波功率和超声波频率对纳米SiO2性能的影响,研究表明,当NaOH与尾矿的质量比为1.4∶1,温度为325℃时灼烧25 min后用100 mL水溶解,滴加1.6 mol/LHCl酸化沉淀,终点pH调至8.5,在超声功率100 W,超声频率28 Hz的条件下,尾矿中SiO2提取率达到98.0%,产物中SiO2含量为98.40%,平均粒度为18 nm,得到的产品符合国家标准。     

融雪剂对大叶黄杨生长和生理特性的影响

为了研究融雪剂对道路绿化植物的影响,以大叶黄杨（Euonymus japonicus Thunb）为研究材料,研究了其在3种融雪剂（JLR-01、LBR-4、芦笛一号）不同施用量影响下的生长量和生理特性。结果表明：随着融雪剂LBR-4和芦笛一号的施用量的增大,大叶黄杨叶片的相对生长量和株高相对生长量、光合速率（Pn）、水分利用效率（WUE）、蒸腾速率（Tr）和气孔导度（Gs）随之减小,而低施用量的融雪剂JLR-01对大叶黄杨生长量、Pn、WUE和Tr有促进作用。随着融雪剂作用时间的延长,3种融雪剂的Pn和WUE也随之减小,Tr则是先减小后有所增大。当融雪剂施用量较小和胁迫时间较短时,Pn下降是因为气孔关闭;而当施用量较大和胁迫时间较长时,Pn下降是因为叶肉同化能力下降;3种融雪剂对大叶黄杨的胁迫程度由大到小的次序为：芦笛一号〉LBR-4〉JLR-01;大叶黄杨对3种融雪剂施用量的忍耐阈值在80 g.m-2左右,大叶黄杨对施用LBR-4和芦笛一号的耐受时间阈值大约为3周,对施用JLR-01的耐受时间阈值为3周以上。     

Numerical and experimental investigations on laser melting of stainless steel 316L metal powders

This paper presents numerical and experimental investigations on laser melting of SS grade 316L powder on top of AISI 316L substrate using a pulsed Nd:YAG laser. The objectives of the present study are to understand the effect of process parameters such as laser power, scanning speed and beam size on geometry characteristics of the melt zone and ball formation. We formulated a moving heat source problem and obtained transient temperature solutions using commercial finite element solver. The geometry characteristics of the melt zone are evaluated from the temperature solutions and compared with experimental results. The effect of laser parameters on the geometry, morphology and homogeneity of single track realization was methodically analyzed by utilizing characterization tools such as laser particle size analyzer, macro and microscopic inspection, Scanning Electron Microscope (SEM), X-Ray Diffraction (XRD) and Fourier Transform Infrared Spectroscopy (FTIR). The results presented in this paper are beneficial to realize homogenous layer formation in additive manufacturing processes involving powder melting by laser beam.