高校环境专业实验教学存在的问题及对策

实验教学在高校环境专业教学工作中发挥着越来越重要的作用。通过对高校环境专业实验教学的现状和所存在的问题进行分析,提出了优化实验教学内容、改进实验教学方法和考核方式等改进措施,以提高高校环境专业实验教学水平。     

The effects of forest harvest intensity in combination with wind disturbance on carbon dynamics in Lake States Mesic Forests

Total forest carbon (C) storage is determined by succession, disturbances, climate, and the edaphic properties of a site or region. Forest harvesting substantially affects C dynamics; these effects may be amplified if forest harvesting is intensified to provide biofuel feedstock. We tested the effects of harvest intensity on landscape C using a simulation modeling approach that included C dynamics, multiple disturbances, and successional changes in composition. We developed a new extension for the LANDIS-II forest landscape disturbance and succession model that incorporates belowground soil C dynamics derived from the CENTURY soil model. The extension was parameterized and calibrated using data from an experimental forest in northeastern Wisconsin, USA. We simulated a 9800 ha forested landscape over 400 years with wind disturbance combined with no harvesting, harvesting with residual slash left on site (‘standard harvest’), and whole-tree harvesting. We also simulated landscapes without wind disturbance and without eastern hemlock (Tsuga canadensis) to examine the effects of detrital quantity and quality on C dynamics. We estimated changes in live C, detrital C, soil organic C, total C, and forest composition. Overall, the simulations without harvesting had substantially greater total C and continued to sequester C. Standard harvest simulations had more C than the whole tree harvest simulations. Under both harvest regimes, C accrual was not evident after 150 years. Without hemlock, SOC was reduced due to a decline in detritus and a shift in detrital chemistry. In conclusion, if the intensity of harvesting increases we can expect a corresponding reduction in potential C storage. Compositional changes due to historic circumstances (loss of hemlock) may also affect forest C although to a lesser degree than harvesting. The modeling approach presented enabled us to consider multiple, interacting drivers of landscape change and the subsequent changes in forest C.     

Quantitative standard of eco-compensation for the water source area in the middle route of the South-to-North Water Transfer Project in China

The Middle Route Project(MRP) of the South-to-North Water Transfer Scheme (SNWT) in China will require a very large financial expenditure to ensure the water supply and the associated water quality to northern China. An eco-compensation mechanism between the water service source areas and its beneficiaries is essential. This paper establishes an analytic framework of ecocompensation standard for the protection of the water source area, including both the calculation of ecocompensation based on opportunity cost method (OCM) and calculation of the burden sharing of eco-compensation between the water source area and the external water reception area based on the deviation square method (DSM). Taking Shiyan City, Hubei Province in China as a case study, our results show that the eco-compensation in the first-phase of MRP for the water source area in Shiyan, Hubei Province should be 1.63??10¹⁰ CNY, about four times of planned eco-construction investment budget (4.33??10⁹ CNY). In addition, the burden sharing of eco-compensation varied greatly in terms of different methods. It would be better to integrate the results of different single-factor burden sharing methods by determining the corresponding weighting coefficient with DSM and form one unanimous consent result by the interested parties.     

Sorption of DDTs on biofilms, suspended particles and river sediments: effects of heavy metals

The sorption by solid materials is one of the most important processes that affect the fate of hydrophobic organic pollutants in aquatic systems. Current studies focus on the sorption of hydrophobic pollutants by single natural solid material, whereas few studies compared the sorption behaviors of different solids. Furthermore, natural aquatic environment is a complex system where hydrophobic pollutants coexist with many other pollutants, but only limited studies reported the effects of coexisting components on the sorption. Here we studied the sorption of dichlorodiphenyltrichloroethanes (DDTs) by three common solids in natural water, i.e., biofilms, suspended particles and sediments. The effects of typical coexisting heavy metals on the sorption were also examined. The results show that the sorption is described by a dual-mode sorption model. Compared with sediments, more DDTs were sorbed by biofilms and suspended particles. Coexisting Pb, Cd and Cu increased the sorption of DDTs on sediments while decreasing the sorption on biofilms slightly, with little effect on the sorption on suspended particles. The different sorption behaviors of the solids were mainly determined by the composition of the solids: more organics were observed in biofilms and suspended particles.     

曝气复氧对底泥氮素生物地球化学循环影响的作用机制研究

通过分析底泥氮污染物释放规律和转化过程,以及底泥生境、氮形态变化和氮循环功能微生物群落结构变化的规律,探讨了不同曝气复氧条件影响底泥氮生物地球化学循环的生物代谢、物理化学联合作用的机制。结果表明：曝气复氧对底泥中氮的生物地球化学循环影响是一个包括微生物代谢作用和物理化学作用的复杂联合作用过程。水体好氧环境的改变主要引起参与底泥氮循环的硝化、亚硝化和反硝化功能菌群群落结构的演变,对异养菌和氨化菌的影响不大,证明环境好氧条件的改变对底泥有机质生物分解产生氨氮的微生物代谢过程影响不大,主要对底泥释放的氨氮硝化、反硝化等生物转化过程产生大的影响。不同溶解氧条件下,底泥释放的氮素在微生物作用下主要以NH4＋-N和NO3--N的形式进入试验体系,并在特定的氧化还原电位（临界值-200 mV）和pH（临界值6.70）条件下通过物理化学作用在底泥中以离子交换态氮（IEF-N）、碳酸盐结合态氮（CF-N）、铁锰氧化态氮（IMOF-N）及有机态和硫化物结合态氮（OSF-N）等不同形态氮相互转化,同时,在氮的转化和循环过程中部分输入上覆水体。在低溶解氧组实验条件下[ρ（DO）〈0.5 mg.L-1],底泥向水体输出氮总量为底泥可转化态氮的19.7%,主要为氨氮,最大释放速率达到289.13 mg.m-2.d-1,释放的质量浓度可达到18.8 mg.L-1;好氧条件下（DO饱和）,底泥向水体输出氮总量为底泥可转化态氮的1.8%;好氧-缺氧条件下为11.7%,主要以N2的形式释出系统。     

灵泉露天矿残煤回采边坡稳定性分析与评价

为了保证灵泉露天煤矿残煤回采时边坡安全,对其边坡稳定性进行了分析与评价.根据灵泉露天煤矿东帮边坡各剖面实际揭露分层物料各自物理力学性质,应用边坡数值计算软件计算模拟灵泉露天煤矿东帮边坡的稳定性.结果表明,东帮最终帮坡边坡角为32°～35°,能够保证残煤回采时边坡的安全性.同时,对影响灵泉露天煤矿东帮边坡稳定性的主要因素进行了分析评价.结果表明,粉砂岩容易吸水,但含水率的增加对C、φ值的影响幅度小于泥岩,泥岩不易吸水,亦不易排水,但含水率对泥岩的影响幅度大.因此,在采矿过程中应加强露天矿疏干排水工作,以使边坡岩体保持较高强度,从而保证边坡安全.     

不同农作物秸秆原料制备生物炭特性及重金属浸出行为

采用水稻秆、大豆秆、小麦秆和玉米秆为原料在550℃缺氧条件下制备生物炭,考察不同原料生物炭理化性质及热解后重金属(Cr﹑Ni、 Cu﹑As﹑Cd和Pb)迁移转化特征,及其在不同浸出液中的浸出行为.结果表明,4种原料制备的生物炭的理化特性和元素组成基本一致,其中玉米秆生物炭微孔体积(0.006 cm³·g^-1)和比表面积(110.120 m²·g^-1)低于其他原料生物炭.秸秆热解后重金属(除Cd外)含量增加了14.04%～410.81%,且大部分重金属(除Cd和Pb外)化学形态由不稳定态(弱酸提取态和可还原态)向稳定态(可氧化态和残渣态)转化.制备的生物炭中的重金属在超纯水和缓冲盐溶液中无浸出或浸出量较少,在乙酸溶液和腐殖酸溶液中浸出量较高.其中Cu在乙酸溶液中浸出量较高,为2.601～4.224 mg·kg^-1,As在腐殖酸溶液中浸出量较高,介于0.074～0.166 mg·kg^-1.热解后,各种重金属的环境质量指数(PI_i)和内梅罗...     

伊洛河流域河水来源及水化学组成控制因素

伊洛河是黄河中游南岸重要支流,由伊河和洛河在洛阳偃师汇合而成.流域上游矿产资源开采活动较多,下游城镇密集,工农业活动分布广泛.为探究不同类型人为活动对伊洛河流域河水水化学组成的影响,分别在丰水期(8月)和平水期(12月)采集伊洛河流域干流和支流河水样品,借助水体氢氧同位素组成和阴阳离子组成的时空分布特征,阐明水体来源以及水化学组成控制因素,说明人为活动的影响途径和方式.结果表明:①洛河干流河水丰水期和平水期δD和δ~(18)O均值分别为-56‰和-7.9‰以及-55‰和-8.1‰,伊河干流河水丰水期和平水期δD和δ~(18)O均值分别为-49‰和-6.9‰以及-53‰和-7.8‰,丰水期和平水期河水主要接受当地大气降水补给;②洛河及伊河干流河水水化学类型均为HCO_3-SO_4-Ca-Mg型,丰水期干流河水Ca~(2+)和HCO~-_3当量浓度占比低于平水期,而丰水期SO_4~(2-)当量浓度占比则高于平水期,显示丰水期较多硫酸盐输入;③碳酸和硫酸参与流域内碳酸盐岩和硅酸盐岩风化过程,洛河流域碳酸盐岩风化较明显,伊河流域硅酸盐岩风化较明显;④伊洛河流域人为输入影响表现在上游河水水化学组成受到金属矿产采选活动影响,下游河水水化学组成受工业废水和城镇生活污水的影响;⑤伊洛河流域上游和下游两种不同类型人为活动是河水硫酸盐硫同位素组成空间上变化的重要原因,上游河水硫酸盐硫同位素组成偏负,证实来自硫化物矿物氧化过程产生的硫酸盐贡献较大,进而间接证实硫酸参与岩石化学风化过程.下游河水硫酸盐硫同位素值偏正,与工业废水和城镇生活污水有关.     

中国分省道路交通二氧化碳排放因子

基于本地化的综合移动源排放模型（Motor Vehicle Emission Simulator,MOVES）模型模拟典型机动车的CO₂排放因子,并建立排放因子与速度变化关系的评估方程,结合各省路网平均速度与区域电网排放因子核算中国31个省份分车型的CO₂排放因子.同时,综合考虑载客汽车的载客量和客座率,载货汽车的载重量和载货率,建立各省单位客运,货运周转量的机动车CO₂排放因子库.结果表明,各类机动车的平均CO₂排放因子分别为：柴油公交车0.880kgCO₂/km,重型货车0.877kgCO₂/km,电动公交车0.676kgCO₂/km,中型货车0.508kgCO₂/km,轻型货车0.374kgCO₂/km,柴油小客车0.227kgCO₂/km,微型货车0.216kgCO₂/km,汽油小客车0.203kgCO₂/km,电动小客车0.108kgCO₂/km,摩托车0.062kgCO₂/km.车辆满载时,柴油公交车和电动公交车的人均CO₂排放量比汽油小客车分别降低了63%和73%,电动小客车的人均CO₂排放量较汽油和柴油小客车分别下降了46%和51%.较高的机动车保有量,频繁的道路拥堵导致上海,北京和重庆等市的机动车CO₂排放因子相对较高.倡导公共交通,提高客座率,降低私家车使用频率,推广纯电动汽车并通过减少道路拥堵以提高车速是降低道路交通CO₂排放量的有效途径.     

长期饥饿后SPNA微颗粒污泥系统性能恢复

为了确定长期饥饿后连续流一段式部分亚硝化-厌氧氨氧化（SPNA）工艺的性能恢复情况,采用连续流反应器,考察了在室温下（11~23℃）经历161d饥饿期的SPNA系统性能恢复策略的可行性及脱氮性能和菌群结构变化.通过控制DO浓度及进水氨氮负荷,逐渐实现亚硝酸盐氧化菌（NOB）的抑制和淘汰、氨氧化菌（AOB）和厌氧氨氧化菌（AnAOB）的活性恢复和富集.在68d内系统总氮去除率恢复至72.13%,氨氮去除率恢复至94.75%.微颗粒污泥（³200μm）的占比从42.04%升至60.98%.微生物群落结构分析发现,停止运行161d后系统Candidatus Kuenenia的相对丰度升至25.53%,表现出较强的抵抗饥饿条件的能力,系统恢复后其相对丰度逐渐降低,接近反应器饥饿前水平.AOB的高底物利用能力是系统恢复的前提,AnAOB活性的提高是系统恢复的关键.系统性能的成功恢复表明室温下161d饥饿期对系统造成的影响是可逆的,长期室温下储存SPNA污泥是可行的.