湖北省湖泊水环境化学特征及其与人类活动的关系

通过对湖北省近３０个湖泊水环境化学的分析，探讨了湖北省湖泊水质状况和湖水的化学稳定性，指出远离工业区和居民生活区的湖泊水质一般较好，城区或城效型湖泊在不同程度上受到了工业废水和生活污水的影响。控制，消除湖泊污染是今后经济、社会和环境建设不可忽视的重要工作。     

Soil surface Hg emission flux in coalfield in Wuda,Inner Mongolia,China

Hg emission flux from various land covers, such as forests, wetlands, and urban areas, have been investigated. China has the largest area of coalfield in the world, but data of Hg flux of coalfields, especially, those with coal fires, are seriously limited. In this study, Hg fluxes of a coalfield were measured using the dynamic flux chamber (DFC) method, coupled with a Lumex multifunctional Hg analyzer RA-915+ (Lumex Ltd., Russia). The results show that the Hg flux in Wuda coalfield ranged from 4 to 318 ng m^?2 h^?1, and the average value for different areas varied, e.g., coal-fire area 99 and 177 ng m^?2 h^?1; no coal-fire area 19 and 32 ng m^?2 h^?1; and backfilling area 53 ng m^?2 h^?1. Hg continued to be emitted from an underground coal seam, even if there were no phenomena, such as vents, cracks, and smog, of coal fire on the soil surface. This phenomenon occurred in all area types, i.e., coal-fire area, no coal-fire area, and backfilling area, which is universal in Wuda coalfield. Considering that many coalfields in northern China are similar to Wuda coalfield, they may be large sources of atmospheric Hg. The correlations of Hg emission flux with influence factors, such as sunlight intensity, soil surface temperature, and atmospheric Hg content, were also investigated for Wuda coalfield.

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Evaluation of acidity in late Permian outcrop coals and its association with endemic fluorosis in the border area of Yunnan,Guizhou, and Sichuan in China

The junction area of Yunnan, Guizhou, and Sichuan provinces is the heaviest coal-burning endemic fluorosis zones in China. To better understand the pathogenicity of endemic fluorosis in this area, 87 coal samples from the late Permian outcrop or semi-outcrop coal seams were collected in eight counties of the junction area of Yunnan, Guizhou, and Sichuan provinces. The total fluorine and sulfate content, etc. in the coal was determined using combustion-hydrolysis/fluoride-ion-selective electrode method and ion chromatography, respectively. The results show that the total fluorine concentrations in the samples ranged from 44 to 382 µg g^?1, with an average of 127 µg g^?1. The average pH of the coals is 5.03 (1.86–8.62), and the sulfate content varied from 249 to 64,706 µg g^?1 (average 7127 µg g^?1). In addition, the coals were medium- and high-sulfur coals, with sulfur mass fraction ranging from 0.08 to 13.41%. By heating the outcrop coals, HF release from the coal was verified quantitatively without exception, while simulated combustion directly confirmed the release of sulfuric acid (H₂SO₄). The acid in coal may be in the form of acidic sulfate (\({\text{HSO}}_{4}^{ - }\)/H₂SO₄) because of a positive relationship between pH and \(p\left( {{\text{SO}}_{4}^{2 - } } \right)\) in the acidic coal. The possible reaction mechanism would be that a chemical reaction between the acid (H₂SO₄ or \({\text{HSO}}_{4}^{ - }\)) and fluorine in the coal occurred, thereby producing hydrogen fluoride (HF), which would be the chemical form of fluorine released from coal under relatively mild conditions. The unique chemical and physical property of HF may bring new insight into the pathogenic mechanism of coal-burning endemic fluorosis. The phenomenon of coal-burning fluorosis is not limited to the study area, but is common in southwest China and elsewhere. Further investigation is needed to determine whether other endemic fluorosis areas are affected by this phenomenon.     

Historical trends of organochlorine pesticides (OCPs) recorded in sediments across the Tibetan Plateau

Sediment cores from four lakes across the Tibetan Plateau were used as natural archives to study the time trends of organochlorine pesticides (OCPs). The total concentrations of dichlorodiphenyltrichloroethane (ΣDDT) and hexachlorocyclohexane isomers (ΣHCH) were in the range of 0.04–1.61 and 0.08–1.88 ng/g based on dry weight (dw), while the input fluxes were in the range of 0.3–236 and 0.7–295 pg/cm²/y in the core sediments, respectively. The input fluxes of ΣDDT and ΣHCH generally peaked in sediment layers corresponding to the 1970s–1990s and peaked in top sediment layers. The ratio of α/γ-HCH decreased in the top layer sediments, implying that the contribution of lindane (pure γ-HCH) has been increasing in recent years. In addition, the ratio of o,p′-DDT/p,p′-DDT increased significantly over the last 15–20 years, suggesting that dicofol (characterized by high ratio of o,p′-DDT/p,p′-DDT about 7.0) has recently become a relatively more important source of DDT compared to technical DDT itself. The time trends of OCPs recorded in lake sediments examined the impact on such remote alpine regions by human activities.     

医疗废物高温蒸汽集中处置工艺设计

以某市医疗废物集中处置中心为例,介绍8 t/d规模的高温蒸汽系统工艺设计,包括工艺流程以及产生的有害物质的处理,并对医疗废物高温蒸汽处理系统的设计技术进行探讨。     

高效复合微生物菌群在垃圾堆肥中的应用

利用高效复合微生物菌群对生活垃圾和污泥混合堆肥,通过测定堆肥过程中总菌数、温度、有机物、C/N比等,较系统地研究了高效复合微生物菌群在生活垃圾、污泥混合堆肥系统中的作用.试验证明:在生活垃圾和污泥共堆肥系统中,调节堆料比为厨房垃圾:污泥:粉煤灰土:成熟堆肥污泥:干草=41.6:27.8:13.8:11.1:5.5,有机物约为60%,总氮14%,全磷0.69%,全钾1.25%;初始含水率为58.5%,初始C/N比=30i供气量控制在0.8L/min·kg挥发性有机物,处理1、处理2、处理3堆料中分别接种2%、3%、5%(质量分数)的高效复合微生物菌群,与加入3%灭活菌的对照组进行对比实验.对照组、处理1、处理2和处理3堆肥系统垃圾腐熟时间分别为30d、24d、18d和12d;说明高效复合微生物菌群可以加速生活垃圾和污泥的降解,保证堆肥过程的顺利进行.处理3与对照组相比,堆腐时间缩短了18d,同时成品堆肥中含有大量具有生物活性的微生物,是一种良好的生物活性有机肥料.     

粉煤灰的粉体特性及其对减水效应的影响

通过对粉煤灰颗粒形貌、平均粒径、粒度分布等粉体特性参量的测定和计算分析 ,发现粉煤灰的减水效应主要来自圆球形玻璃微珠的滚珠轴承润滑作用或对水泥絮凝结构的分散作用。过细的粉煤灰大掺量取代水泥后有可能会降低其减水效应     

优势工程菌在H/O工艺中处理制药废水的研究

采用水解 (H)—好氧 (O)生化工艺研究了优势复合工程菌对抗生素工业废水有机质的降解能力并进行了处理条件试验研究。探讨了预处理、生化温度、pH值、水力停留时间、进水有机物浓度等因素对生化处理工艺的影响。试验结果表明 ,在选定的条件下 ,水解单元COD的降解率达 71 9%。好氧单元COD的降解率达 62 9% ,总去除率达 98 5%。达到国家规定的制药行业排放标准 ,出水的COD平均浓度低于 30 0mg/L。     

抚顺市二氧化硫2010年预测和综合防治规划及对策

以抚顺市国民经济、社会发展、城市总体规划为依据，根据二氧化硫排放量，采用修正后的箱体模型预测2010规划年的二氧化硫环境质量；再按照达标性原则，确定削减量。在此基础上，提出了综合防治规划及对策。     

Historical mercury contamination in sediments and catchment soils of Diss Mere, UK

A 5.3 m sediment core and soil samples were taken from Diss Mere and its catchment. The sediment core was dated and Hg analysed on the sediment and soil samples. The Hg record of the sediment core shows that Diss Mere has been contaminated for the past thousand years and the historical trends in sediment contamination are in good agreement with the development of the weaving industry in Diss and hemp cultivation in the region. Mercury contamination in Diss Mere has been significant and reached a peak in the mid-19th century with sediment Hg concentrations over 50 μg g⁻¹. Elevated Hg concentrations were also found in contemporary soils in residential areas with former industrial land use. Although local hemp cultivation and the traditional weaving industry were abandoned a hundred years ago, Hg contamination caused by these activities still exists in the catchment, and affects the lake.