电石渣在煤泥水混凝中的作用机理研究

电石渣在煤泥水混凝中的作用机理 :电石渣对煤泥水混凝作用不是补给了 OH- ,而是提供了大量的 Ca2 + 。Ca2 +通过压缩双电层 ,破坏了煤泥颗粒的稳定性 ,从而使煤泥颗粒发生凝聚。OH-和 Ca( OH) 2 对煤泥水的混凝不直接起作用。     

简述日本降低燃煤锅炉NOX产生的实用技术

简要介绍了日本降低燃煤锅炉ＮＯＸ产生的实用技术，从ＮＯＸ的产生机制入手，以抑制ＮＯＸ的产生为目的，叙述了改善燃烧方法及改善燃烧器的原理，模式图及实用现状。     

西部生态脆弱区矿山不同开采强度下生态系统服务时空变化——以神府矿区为例

以神府矿区为例,选取土地利用、植被覆盖、土壤、气象等生态环境与统计数据指标,利用RS和GIS技术构建生态系统服务遥感测量评估指标体系,评估研究区2005-2015年生态系统服务变化及时空分布特征,进一步探究神府矿区不同开采强度对生态系统服务的影响并进行驱动力分析。研究结果表明：（1）2005年、2010年、2015年研究区的总生态系统服务分别为1.598×10¹⁰元、1.905×10¹⁰元、2.134×10¹⁰元,呈现逐年递增的趋势;（2）生态系统服务功能中水土保持价值比例最大,草地的单位面积生态系统服务价值最高,耕地、草地生态系统为该地区贡献了最多的生态系统服务价值;（3）研究区生态系统服务分布表现为由东北向西南逐渐降低的趋势,不同开采强度下的生态系统服务增长变化较为相似,煤炭开采区域生态系统服务未显著下降,整体较为平稳。对生态系统服务变化的驱动分析表明在近年来相对改善的气候环境与人工修复共同作用下,神府矿区生态系统服务未发生明显的缩减。此类半干旱生态脆弱矿区国土空间生态修复适宜通过主动的“保护性开发”以及“人工诱导+自然修复”为主的方式,避免大范围与高强度的水土扰动型治理,通过适度的人为干预保证与维持区域内生态系统服务的功能。研究成果不但揭示高强度煤矿开采下的生态环境变化,也对西部生态脆弱区环境做了定量评估;同时,为将来的矿区重建提供了重要的依据。     

煤飞灰中铬铁元素的形态分析研究

用连续提取法将煤飞灰中的铬、铁元素依结合态区分为水溶态,交换态,表面氧化物和碳酸结合态,铁锰氧化物结合态,金属有机物和硫化物结合态,磁性四氧化三铁结合态和硅铝酸盐矿物态,用原子吸收法及X-衍射分析进行测定。并对煤飞灰化学形态分布进行了讨论。     

岩溶山区煤炭开采的环境影响与对策浅析

岩溶山区的煤炭开采必将时生态环境造成影响和破环．为确保煤炭生产与生态环境的协调发展，根据岩溶山区资源环境与生态特点。采取积极有效的综合防治措施，以及收取环境恢复治理保证金的建议，可望通过实践取得成效．     

二苯噻吩的微生物脱硫及其在脱煤中有机硫的应用

评述了煤中有机硫的模型化合物二苯噻吩的微生物脱硫最新进展，对二苯噻吩的特异性脱硫的微生物和机理作了较新的介绍并提出了独到的看法，指出了当今存在的问题和今后的研究方向及其在脱煤中有机硫的应用前景。     

石灰凝胶阻化剂防灭火技术在高硫矿的应用研究

在分析现有凝胶阻化剂防灭火机理的基础上 ,笔者针对我国高硫煤矿采空区发火特点 ,研制出石灰凝胶阻化剂的配方 ,并对其防灭火机理进行了详细探讨 ,确定了喷洒该种阻化剂的工艺过程及其应注意的问题。根据现场试验的测定数据表明 ,石灰凝胶阻化剂对高硫煤矿的防灭火效果好     

Risk attitudes and mitigation among gold miners and others in the Suriname rainforest

This article analyses the question: do attitudes towards risk influence participation in small‐scale gold mining, a hazardous activity that generates uncertain income? This question is examined by measuring and comparing the risk attitudes of gold miners and non‐mining community members in the rainforest of Suriname, South America. The author presents a multivariate model to predict the duration of work in mining areas as a function of risk tolerance, age, education, and household demographics. The results suggest that a greater tolerance to risk increases the duration of a person's mining career. However, attitudes explain only a fraction of the variation in occupational choices. Qualitative data suggest that these choices are primarily shaped by local barriers to human capital development and by national economic volatility. Given their marginal position in society and the multitude of mining risk mitigation strategies, it is questionable whether gold mining exposes Suriname forest peoples to greater risks than other subsistence alternatives. The author argues that sensitivity to local historical and cultural conditions would improve the efficiency of policies aimed at developing a more sustainable mining industry. By zooming in on the daily lives of miners, anthropology can complement macro‐scale analyses and contribute to policy interventions in the small‐scale mining sector.     

Strategies for sustainable development of the small-scale gold and diamond mining industry of Ghana

The small-scale gold and diamonds mining industry is of great importance to Ghana. Since its regularization in 1989 the sector has produced and sold over 1.5 million troy ounces of gold and 8.0 million carats of diamonds. During the same period the sector also provided direct employment to over 100,000 people and improved the socioeconomic life of many individuals and communities. However, these were largely achieved at a cost to the environment in areas where mining is carried out and there is the need to develop the industry in a sustainable manner. This paper looks at the developments in the small-scale gold and diamonds mining industry in Ghana and proposes some strategies on how the concepts of sustainable development could be applied to the industry.     

Microbial cycling of iron and sulfur in acidic coal mining lake sediments

Lakes caused by coal mining processes are characterized by low pH, low nutrient status, and high concentrations of Fe(II) and sulfate due to the oxidation of pyrite in the surrounding mine tailings. Fe(III) produced during Fe(II) oxidation precipitates to the anoxic acidic sediment, where the microbial reduction of Fe(III) is the dominant electron-accepting process for the oxidation of organic matter, apparently mediated by acidophilic Acidiphilium species. Those bacteria can reduce a great variety of Fe(III)-(hydr)oxides and reduce Fe(III) and oxygen simultaneously which might be due to the small differences in the redox potentials under low pH conditions. Due to the absence of sulfide, Fe(II) formed in the upper 6 cm of the sediment diffuses to oxic zones in the water layer where itcan be reoxidized by Acidithiobacillus species. Thus, acidic conditions are stabilized by the cycling of iron which inhibits fermentative and sulfate-reducing activities. With increasing sediment depth, the amount of reactive iron decrease, the pH increases above 5, and fermentative and as yet unknown Fe(III)-reducing bacteria are also involved in the reduction of Fe(III). Sulfate is reduced apparently by the activity of spore-forming sulfate reducers including new species of Desulfosporosinus that have their pH optimum similar to in situconditions and are not capable of growth at pH 7. However, generation of alkalinity via sulfate reduction is reduced by the anaerobic reoxidation of sulfide back to sulfate. Thus, the microbial cycling of iron at the oxic-anoxic interface and the anaerobic cycling of sulfur maintains environmental conditions appropriate for acidophilic Fe(III)-reducing and acid-tolerant sulfate-reducing microbial communities.