扎龙湿地龙湖重金属污染情况及其潜在生态风险评价

为了探讨龙湖中重金属污染情况,测定了龙湖中9个取样点的重金属元素含量,并从中选取Mn、Cu、Pb、As 4种重金属元素进行水质评价。通过灰色关联评价分析,所采集的9个样点中有8个样点都属于Ⅴ类水质、1个样点属于Ⅳ水质。采用Hakanson潜在生态风险指数法对龙湖沉积物进行重金属潜在生态风险评价分析,4种重金属的潜在风险顺序为Cu>As>Pb>Mn,其中每个样点的Cu元素都达到了极强的潜在生态危害,As元素的潜在生态危害程度都达到了强度生态危害。     

海河流域农村非点源污染现状及空间特征分析

采用污染排放系数法估算了2008年海河流域农村生活源、畜禽分散养殖、农田化肥流失3个主要农村非点源COD、TN、TP和NH3-N 4种污染物的排放量,并对其排放强度和空间分布特征进行了分析.结果表明,海河流域农村非点源污染源排放COD、TN、TP和NH3-N总量分别为2435826, 3042079, 540568, 1798760t/a,平均排放强度分别为11.10, 13.97, 2.98, 8.28t/(km2·a).海河流域内河北省的3个农村非点源的4种污染物排放量均居首位,农村居民生活源对海河流域非点源污染贡献最大,是流域非点源污染控制最主要的对象;子牙河水系农村非点源污染物排放总量最大,而徒骇马颊河水系排放强度最大,是海河流域内污染最严重的水系,其首要非点源污染源是山东省的农村生活源.流域内非点源污染排放量和排放强度均呈现区域性分布,山区和平原区分别呈现出低污染等级和高污染等级.     

我国电解锰行业氨氮污染分析与控制

我国"十二五"期间将氨氮纳入总量控制指标,电解锰行业氨氮污染控制变得非常紧迫。介绍了电解锰氨氮污染的现状,分析了电解锰氨氮污染的产生途径以及电解锰生产中的氨氮平衡,依据"源头消减、过程控制、末端循环"的清洁生产理念,提出了电解锰氨氮污染的控制措施。     

电力建设工程重大危险源动态风险界定及级别划分

针对电力建设工程中对危险源动态风险研究不足和混淆重大危险源概念导致的危险源难于分级管理与控制的问题,通过分析相关法律、规范等界定了电力建设工程施工作业场所重大危险源的概念,引入了危险源动态风险系数的概念,从系统安全的角度确定了动态风险系数的19个影响因素,基于此改进了LEC评价法,并划分了施工作业场所重大危险源级别。最后,结合工程实例说明了工程施工作业场所重大危险源定义和动态风险系数引入的必要性,测算了危险源实际风险度,并根据实际风险的划分结果建立了“3+2+1”危险源控制模式,实现了对作业场所重大危险源的有效控制。     

基于JACK的机务人员工作负荷评估

为了客观评估机务人员的工作负荷,选取作业能耗和姿态负荷作为评估机务人员工作负荷的指标。分解A320飞机主轮拆卸的维修任务,确定维修动作参数和姿态参数,使用JACK软件中的新陈代谢模块计算作业能耗,使用JACK软件中的RULA模块计算机务人员的姿态负荷,结果验证了该方法的可行性。相对于传统的评估工作负荷的方法,基于JACK仿真的方法具有省时高效的特点。     

Selenium and hazardous elements distribution in plant–soil–water system and human health risk assessment of Lower Cambrian,Southern Shaanxi,China

The natural selenium poisoning due to toxic Se levels in food chain had been observed in humans and animals in Lower Cambrian outcrop areas in Southern Shaanxi, China. To find out the distribution pattern of selenium and other hazardous elements in the plant, soil and water of Lower Cambrian in Southern Shaanxi, China, and their possible potential health risk, a total of 30 elements were analyzed and the health risk assessment of 18 elements was calculated. Results showed that the soil, plant and natural water of Lower Cambrian all had relatively high Se levels. In Lower Cambrian, the soil was enriched with Se, As, Ba, Cu, Mo, Ni, Zn, Ga, Cd and Cr (1.68 < I_geo < 4.48, I_geo; geo-accumulation index). In same plants, the contents of Se, Cd and Zn (except Cd in corn and rice, Zn in potato and corn) of Lower Cambrian were higher than that of the other strata. Ba and Ga in natural water were higher than that of the other strata, while K and Cs were opposite. The health risk assessment results showed that the people living in outcrop areas of Lower Cambrian had both high total non-carcinogenic risk of 18 elements (HI = 16.12, acceptable range: < 1) and carcinogenic risk of As (3.98E−04, acceptable range: 10⁻⁶–10⁻⁴). High contents of Se, As, Mo and Tl of Lower Cambrian may pose a health risk to local people, and food intake was the major pathway. For minimizing potential health risk, the local inhabitants should use the mix-imported food with local growing foods.

     

Stabilization of Cd-, Pb-, Cu- and Zn-contaminated calcareous agricultural soil using red mud: a field experiment

Red mud (RM) was used to remediate heavy metal-contaminated soils. Experiments with two different dosages of RM added to soils were carried out in this study. It was found that soil pH increased 0.3 and 0.5 unit with the dosage of 3 and 5% (wt%), respectively. At the dosage of 5%, the highest stabilization efficiencies for Cd, Pb, Cu and Zn reached 67.95, 64.21, 43.73 and 63.73%, respectively. The addition of RM obviously transferred Cd from the exchangeable fraction to the residual fraction. Meanwhile, in comparison with the control (no RM added), it reduced 24.38, 49.20, 19.42 and 8.89% of Cd, Pb, Cu and Zn in wheat grains at the RM addition dosage of 5%, respectively. At the same time, the yield of wheat grains increased 17.81 and 24.66% at the RM addition dosage of 3 and 5%, respectively. Finally, the addition of RM did not change the soil bacterial community. These results indicate that RM has a great potential in stabilizing heavy metals in calcareous agricultural soils.

     

The origin of high hydrocarbon groundwater in shallow Triassic aquifer in Northwest Guizhou,China

Original high hydrocarbon groundwater represents a kind of groundwater in which hydrocarbon concentration exceeds 0.05 mg/L. The original high hydrocarbon will significantly reduce the environment capacity of hydrocarbon and lead environmental problems. For the past 5 years, we have carried out for a long-term monitoring of groundwater in shallow Triassic aquifer in Northwest Guizhou, China. We found the concentration of petroleum hydrocarbon was always above 0.05 mg/L. The low-level anthropogenic contamination cannot produce high hydrocarbon groundwater in the area. By using hydrocarbon potential, geochemistry and biomarker characteristic in rocks and shallow groundwater, we carried out a comprehensive study in Dalongjing (DLJ) groundwater system to determine the hydrocarbon source. We found a simplex hydrogeology setting, high-level water–rock–hydrocarbon interaction and obviously original hydrocarbon groundwater in DLJ system. The concentration of petroleum hydrocarbon in shallow aquifer was found to increase with the strong water–rock interaction. Higher hydrocarbon potential was found in the upper of Guanling formation (T₂g³) and upper of Yongningzhen formation (T₁yn⁴). Heavily saturated carbon was observed from shallow groundwater, which presented similar distribution to those from rocks, especially from the deeper groundwater. These results indicated that the high concentrations of original hydrocarbon in groundwater could be due to the hydrocarbon release from corrosion and extraction out of strata over time.

     

中国道路交通部门减排技术及成本研究

道路交通作为交通部门碳排放的重要来源,将在实现"碳达峰、碳中和"目标的过程中承担重任。碳减排技术成本的研究有利于平衡道路交通机动化发展和"碳达峰、碳中和"目标的实现,是实现道路交通可持续发展的重要措施。为此,基于乘用车、商用客车、轻型商用货车和重型商用货车等车型,结合发动机技术、变速器技术、辅助系统技术和整车技术和新能源车应用等16种关键节能减排技术的减排潜力和成本,建立了2020-2035年我国道路交通碳排放的边际减排成本（MAC）曲线,评估了通过推广车辆节能技术和新能源车等措施来实现减排目标的累积成本。主要得到以下结论:1）相同的车辆节能减排技术,应用在重型商用货车的单位减排成本远小于其他车型,新能源车在乘用车的应用具有很大的减排潜力,但是与其他车型相比并不具有成本优势。2）燃料电池新能源车的单位减排成本远高于纯电动和插电混合动力新能源车,未来需降低燃料电池的生产成本以及氢气的制备、储存和运输成本。3）2020-2035年的减排总成本曲线显示总减排成本先增加后下降的趋势,这表明随着节能减排技术的合理推广,该部门减排阻力在不断下降。     

Changes in CO2 flux for different recovery processes of desertification in the alpine meadows of Northwest Sichuan北大核心CSCD

Desertification has emerged as a serious threat to the alpine meadows of Northwest Sichuan in recent decades. Artificial vegetation had certain effects on desertification recovery, while how the CO2 flux changed and its reasons are still unclear. During the growing season in 2016 (i.e., from July to September), we selected the desertified alpine meadows with different recovery degrees, including the early stage of restoration, the middle stage of restoration, the late stage of restoration, and control (the unrecovered desertification meadow) as four transects. CO2 flux was measured by the instrument LI-8100, and the microenvironment factors that affected CO2 flux changes were analyzed. The results showed that the carbon sequestration function of desertified alpine meadows gradually increased with the degree of recovery. Net ecosystem exchange (NEE) were -1.61, -3.55, and -4.38 μmol m-2 s-1 in the early, mid-term, and late transects, respectively, and the most dramatic changes occurred from the early stage to mid-term stage, increasing by 120.50%. Both ecosystem respiration (ER) and soil respiration (SR) were enhanced significantly with restoration (P < 0.05). In mid or late July, NEE, ER, and SR reached their maximum values, and thereafter, the indicators varied to near zero (P < 0.05). During the whole growing season, the daily dynamic in CO2 flux for the control alpine meadow was mild and retained the trend of continuous release all day, but that in the desertified alpine meadow was a single peak pattern. Moreover, with restoration process, the peak of CO2 flux increased and reached a peak in the late stage of the recovery process. The regression analysis showed that there was a significant positive correlation between CO2 flux and vegetation coverage, aboveground biomass, and soil moisture (0-5 cm) (P < 0.01), and a weak correlation with 0-5-cm soil temperature (P < 0.01). This indicates that topsoil moisture (5 cm) is a more significant factor for CO2 flux than topsoil temperature during the growing season in the restoration of desertified alpine meadows in Northwest Sichuan. In general, the vegetation recovery significantly improved the carbon-sequestration ability of the desertified alpine meadows during the growing season in Northwest Sichuan, and at the middle stage of restoration, the carbon-sequestration ability improved significantly due to vegetation restoration and increase in topsoil (0-5 cm) moisture. © 2018 Science Press. All rights reserved.