沙尘暴应急监测方法研究

在沙尘暴应急监测方法研究中,通过对总悬浮颗粒物采样仪器及各种采样参数的研究确定和降尘采样器的研制,制定出沙尘暴应急监测方法。     

Periodicity and gradients in dispersal ofAlternaria linicola in linseed crops

Conidia ofAlternaria linicola produced on infected linseed crops were mainly dispersed by wind. The numbers of conidia in the air above linseed crops collected by a Burkard spore sampler were greatest between 1200 h and 1300 h, when the relative humidity was lowest. Although numbers of conidia collected decreased with increasing height within and above the crop canopy, air-borneA. linicola conidia were present up to 80 cm above the crop canopy. Conidia ofA. linicola were transported by wind up to at least 40 m downwind from an artificial line inoculum source, but their numbers decreased with increasing distance from the source. In 1991, 1992, and 1993, the dispersal ofA. linicola conidia above linseed crops followed a seasonal periodicity which was influenced by weather conditions and cultural practices. The greatest numbers of conidia were collected during July, August and early September and coincided with periods favourable for sporulation and with an increase in the incidence of the disease in the senescent crop. Air-borneA. linicola conidia produced on point or line inoculum sources (naturally infected linseed stem debris) were responsible for the spread of the disease in linseed crops. In 1992 and 1993, the disease was first detected downwind from the sources, but by the end of the growing seasons, it had spread in all directions and up to 20 m and 60 m from the sources, respectively. Disease gradients were initially steep near the inoculum sources but they became flatter with time due to the secondary spread of the disease.     

浑善达克沙地东部地区天然水体的水化学组成及其控制因素

浑善达克沙地东部地区位于内蒙古高原,其天然水体为淡水。利用原始型Durov三线图对其天然水体进行水化学分类,结果表明,地表水水化学类型属于碳酸氢盐组,而地下水属于碳酸氢盐组、混合组和硫酸盐组多种类型。天然水体样品在Gibbs图中的分布表明,岩性控制是形成该地区天然水体水化学组成的主要因素,这种情况不同于我国西部和中部沙漠由于蒸发强烈而受控于蒸发-结晶作用的天然水体。天然水体的离子比例关系表明,地下水中蒸发盐岩和硅酸盐岩的风化程度较高,而碳酸盐岩风化程度低,这可能是由于地下水的水-岩作用时间长、二氧化碳供给不充分引起的;相反,由于水-岩作用时间短、二氧化碳供给充分,地表水中蒸发盐岩和硅酸盐岩的风化程度较低,而碳酸盐岩风化程度高。     

茄子离体叶片光系统Ⅱ的冷激胁迫效应及热力学分析

 以耐冷性较强的短把黑圆茄和耐热性较强的黑帅圆茄为试材,经冷激胁迫后采用植物效率仪PEA,进行快速叶绿素荧光参数测定,并利用最大光化学效率Fv/F m和活性中心RC/CSo的标准状态变性自由能变△GD进行PSⅡ冷稳定性的热力学分析。随着冷激胁迫温度的降低和时间的延长,PSⅡ的Fv/Fm、实际光化学效率ΔF/Fm′、RC/CSo呈"S"型下降趋势;单位反应中心DIo/RC和非光化学猝灭qN呈"S"型上升趋势;综合分析反映出冷激胁迫下PSⅡ反应中心的可逆失活和依赖于叶黄素循环的热耗散的双重机制在保护PSⅡ防止光抑制中起到重要作用。另外,通过两品种间PSⅡ行为差异,引入了两组新的参数作为便于直观比较冷胁迫的评价指标。黑帅圆茄Fv/Fm、ΔF/Fm＇的半衰温度T1/2和t1/2值分别高于短把黑圆茄1.4 ℃和0.8 ℃。茄子叶片Fv/Fm和RC/CSo的△GD随着冷激胁迫温度的降低而减少呈瀑布型的下降趋势。黑帅圆茄的△GD值和变性中点温度Tm都低于短把黑圆茄。它们均反映出黑帅圆茄的耐冷性低于短把黑圆茄。     

污染土壤中六六六和DDT在温室中的分布特征及动态变化研究

应用PUF材料空气被动采样技术,研究了密闭温室条件下污染土壤中有机氯农药[DDT和六六六(HCH)]含量的动态变化及其向空气中扩散的规律。结果表明:土壤中∑HCHs和∑DDTs总量随着培养时间的延长而降低;空气中HCH和DDT浓度在20d时达到峰值,20d以后浓度逐渐降低。培养60d后,土壤中∑HCHs的浓度随土层深度增加而增加,0~2cm土层中∑HCHs的浓度(9.4±0.69)mg·kg-1显著低于6~8cm土层中的浓度(12.11±0.83)mg·kg-1;∑DDTs在土壤中浓度随土壤层次呈现先升高后降低的变化趋势。在温室条件下有机氯农药的异构体和降解产物的组成也发生一定变化,土壤中HCHs和DDTs在一定程度上被激活,温室条件也可能促进HCHs和DDTs的土-气交换过程;温室环境促进了p,p′-DDT和o,p′-DDT向p,p′-DDD和p,p′-DDE转化,从而增大DDT和HCH的环境风险。     

Monitoring of subaqueous depots with active barrier systems for contaminated dredged material using dialysis samplers and DGT probes

Background, Aims and Scope  Disposal of dredged material in subaqueous depots is increasingly considered an economic and ecologically sound option in managing contaminated dredged material. The concept of subaqueous disposals capped with active barrier systems has been developed to minimize this risk of contaminant release. As such a depot represents a permanent installation within a sensitive ecosystem, it requires a thorough monitoring concept. It is the goal of this work to develop such a concept regarding general considerations and results of laboratory and field investigations. Methods  In addition to the state-of-the-art techniques developed for other under-water constructions, this monitoring concept is developed with particular respect to the chemical isolation of the dredged material from the overlying water body. It comprises the use of seepage meters, dialysis samplers, and DGT gel probes for determining the migration of selected target solutes. The capability of the dialysis samplers is demonstrated by comparing field results with model calculations. The appropriateness of DGT probes to assess the impact of humic substances on trace metal speciation and on copper toxicity is demonstrated with the aid of laboratory experiments. Results and Discussion  The experimental results show that, by using dialysis samplers, the temporal changes in concentration-depth-profiles of heavy metals in the pore solution can be monitored. Additionally, the application of DGT probes facilitates the in situ detection of labile species of a metal in the presence of dissolved humic substances, which serves to reflect its toxicity. Conclusions. Three subsequent monitoring phases are distinguished on the basis of both general considerations and the findings from field results: A hydraulic phase that is characterized by compaction and pore water expulsion, a geochemical phase in which the demobilization of pollutants can occur due to substantial changes in the physico-chemical conditions (pH, EH), and a steady-state-phase where pore water flow and geochemical conditions are approaching their minimum. Recommendations and Outlook  The monitoring concept suggested here provides a versatile tool to assess the chemical isolation of subaqueous sediment depots and other contaminated sediment sites. This is of great importance as subaqueous disposal is increasingly considered a future management strategy as space for upland disposal is limited and treatment, in general, proves to be too costly.     

Competition for electron donors among nitrate reducers,ferric iron reducers,sulfate reducers,and methanogens in anoxic paddy soil

Slurries of anoxic paddy soil were either freshly prepared or were partially depleted in endogenous electron donors by prolonged incubation under anaerobic conditions. Endogenous NO ₃ ^– was reduced within 4 h, followed by reduction of Fe³⁺ and SO ₄ ^2– , and later by production of CH₄. Addition of NO ₃ ^– slightly inhibited the production of Fe²⁺ in the depleted but not in the fresh paddy soil. Inhibition was overcome by the addition of H₂, acetate, or a mixture of fatty acids (and other compounds), indicating that these compounds served as electron donors for the bacteria reducing NO ₃ ^– and/or ferric iron. Addition on NO ₃ ^– also inhibited the reduction of SO ₄ ^2– in the depleted paddy soil. This inhibition was only overcome by H₂, but not by acetate or a mixture of compounds, indicating that H₂ was the predominant electron donor for the bacteria involved in NO ₃ ^– and/or SO ₄ ^2– reduction. SO ₄ ^2– reduction was also inhibited by exogenous Fe³⁺, but only in the depleted paddy soil. This inhibition was overcome by either H₂, acetate, or a mixture of compounds, suggesting that they served as electron donors for reduction of Fe³⁺ and/or SO ₄ ²⁺ . CH₄ production was inhibited by NO ₃ ^– both in depleted and in fresh paddy soil. Fe³⁺ and SO ₄ ^2– also inhibited methanogenesis, but the inhibition was stronger in the depleted than in the fresh paddy soil. Inhibition of CH₄ production was paralleled by a decrease in the steady state concentration of H₂ to a level which provided a free enthalpy of less than G=–17 kJ mol^-1 CH₄ compared to more than G=–32 kJ mol^-1 CH₄ in the control. The results indicate that in the presence of exogenous fe³⁺ or SO ₄ ²⁺ , methanogenic bacteria were outcompeted for H₂ by bacteria reducing Fe³⁺ or SO ₄ ²⁺ .Deceased on 27 December 1992     

基于GPRS的土壤风蚀实时监测系统研制与测试

为克服野外观测和风洞测试的缺点与不足,提高观测数据的连续性、科学性与可靠性。该文综合无线传感网络技术、传感器技术、电子技术和网络通信技术,研制了热敏式风速传感器、分流对冲式风沙分离器和具有无线组网与自动数据采集处理功能的近地表风速廓线仪和多通道集沙仪,建立了基于GPRS网络的土壤风蚀监测系统,实现了被测区域环境温度、相对湿度、大气压力、近地表风速廓线和风沙流结构等参数的同步采集、实时处理和远程监测等功能。试验结果表明:风速传感器输出电压在0.3～4.3 V之间,响应时间小于3 s,有效测量范围在0～17 m/s,测量精度随风速增大而降低,在6和17 m/s风速下的测量精度分别为0.1和0.3 m/s;风沙分离器的降速效率和风沙分离效率分别在96%和99.8%以上,平均等动力性≥92%;称量系统有效测量范围在0～170 g,精度达0.01 g,短期静态误差和长期累积误差分别不超过±0.02 g和±0.04 g;9、12、15和18 m/s风速下的平均集沙效率达91.98%;无线通信建立时间≤5 s,中心汇聚节点可在3 s内实现一次节点遍历和数据汇聚,有效传输距离达140 m以上;风速廓线节点和集沙仪节点单次最大工作时长不低于6和22 h。在野外试验条件下,系统软硬件部分均运行稳定可靠,自组网数据传输的丢包率和错误次数为0,环境温度、相对湿度和大气压力的偏差分别小于2℃、4%和10 hPa;测得的近地表风速廓线与风沙流结构均符合指数分布规律,满足大尺度、跨区域野外土壤风蚀同步研究的需求。     

药雾浓度沉降曲线拟合方法的试验)(简报)

为了解温室大棚等密闭空间喷雾后的药雾浓度衰减规律,该文以常温烟雾机在棚室中喷雾后的药雾浓度为研究对象,针对D.K.Giles的药雾浓度沉降曲线拟合方法进行了改进,相对于老方法将采样时间段内获得的药雾浓度值置于中间时刻点进行拟合,新方法将该值分别对应于该时间段内3个不同时刻点进行拟合分析。新方法同时还建立了比较曲线拟合优劣的一种工程判据,据此判据得出在5 min的采样时间段条件下,将采样数据作为该采样时间段内第2 min时刻点的药雾浓度值,然后进行拟合,所得药物总质量和实际施用药物总质量相对误差最小,仅为1.6%。研究还表明,在浓度沉降过程中,某一采样周期内的浓度值主要由这一时间段的前段采样所贡献。