去除煤矿生活污水二级生化处理出水中NH3-N的试验研究

采用间歇式静态杯罐试验方法,对残余NH3-N浓度5～15mg/L的某煤矿生活污水二级生化处理出水进行了次氯酸钠氧化法去除研究,考察了不同的次氯酸钠溶液投加量和不同反应时间等因素对NH3-N去除效果的影响,研究了反应期间pH的变化情况。试验结果表明,次氯酸钠氧化法可以有效地去除残余NH3-N,对于本试验中的某煤矿生活污水二级生化处理出水,在最佳次氯酸钠投药量为0.1%（Vcl/VH2O）,最佳反应时间在30～50min,其对NH3-N去除率为65.3%,经过氧化处理后,其水质可以达到工业循环冷却水处理设计规范（GB50050-2007）中对NH3-N≤5mg/L的要求。     

粉煤灰储能复合材料的实验研究

通过吸附、熔融浸滞将粉煤灰、月桂酸复合制备得到复合相变储能材料。通过DTA/TG、SEM测试分析,相变储能材料的相变峰值温度为46.01℃,且在44.0℃～55.0℃范围内有一个较大的吸热峰,可实现相变吸放热,且热稳定性好,粉煤灰基本不影响其热性能。微相结构显示粉煤灰能有效吸入大量的月桂酸,具有较好的吸附结合能力。     

煤炭企业节能减排问题与对策

通过对煤炭企业能耗状况和排污状况的分析,指出煤炭企业节能减排的紧迫性,并从人才紧缺、企业管理与节能减排工作脱节等方面分析了煤炭企业节能减排工作面临的问题,提出应发展循环经济,通过技术创新、管理创新、提高全员素质,促进煤炭企业节能减排。     

喷淋粘结剂在运煤列车中的应用探讨

煤炭在铁路运输过程中扬尘量大,喷淋粘结剂对控制煤炭扬尘具有积极作用,能有效减少煤炭在运输过程中的损失,减轻环境污染,消除对客货列车造成的安全隐患。本文较系统地论述了目前喷淋粘结剂在运煤列车中的研究开发现状,探讨了粘结剂开发与设计的技术思路和研究方向。     

浅议曲靖市煤矿资源开发中的生态环境建设

通过调查,分析了曲靖煤矿资源开发中存在的主要环境问题,对加强矿区生态环境建设提出了措施和建议。     

植被恢复对矸石山生态环境效应影响研究

以兴隆庄煤矿绿化矸石山和裸露矸石山为研究对象,研究了植被恢复对矸石山生态环境效应的影响.结果表明,植被的恢复重建了矸石山生态系统,改善了矸石山生态环境:气温平均降低3.7℃、空气相对湿度提高了7.1%,矸石山近地层SO2、NOx和TSP粉尘日均浓度分别降低了0.1471 mg/m3,0.0004 mg/m3 0.0389 Mg/m3矸石山植被的恢复增加了矸石山土壤比重,降低了土壤容重、提高了土壤有机质含量.     

煤与秸秆成型燃料的复合生命周期对比评价

利用复合生命周期对比评价方法,引入能量返还率、资源耗竭系数、环境影响负荷和生命周期成本4个参数,对煤和秸秆成型燃料在整个生命周期内的能源消耗、环境影响和经济性做了对比分析.同时,为了平衡能源、环境与经济三者之间的关系,建立EEE (Energy, Environment, Economic)综合指标进行整体评价.结果表明,在整个生命周期内,与煤相比,秸秆成型燃料的能量返还率低、资源耗竭系数小.秸秆成型燃料的全球变暖潜值、酸化潜值、富营养化潜值、工业烟尘、粉尘潜值及固体废弃物潜值均比煤小,因此,秸秆成型燃料的环境影响负荷比煤小.秸秆成型燃料的EEE指标值比煤小79.8%,所以,从平衡生命周期能源消耗、环境排放和经济性角度出发,秸秆成型燃料具有替代煤的潜力.但是,秸秆成型燃料的生命周期成本比煤高,其大力推广需要政府的财政补贴.     

取芯过程中煤芯温度分布特征模拟研究*

针对取芯过程瓦斯解吸受煤芯的温度影响不明,造成煤层瓦斯含量测不准的问题,开展对取芯过程煤芯温度分布特征研究。采用自主研制的取芯管自动测温装置在赵固二矿原生结构煤层（f=1.71）进行深度20 m的取芯试验,获得取芯管管壁温升变化规律,变化曲线分为4个阶段:缓慢上升、加速上升、减速上升、缓慢下降阶段;应用COMSOL建立含瓦斯煤传热模型,将管壁的温度变化设置为边界条件,模拟取芯过程煤芯与管壁之间的热交换。结果表明:在取芯时间30 min内,煤芯平均温度快速上升,之后上升速度趋于平稳;在煤芯内,相同时刻,等间距的轴向与径向距离,径向较轴向的温度梯度较大,径向传导快于轴向传导;取芯过程煤芯径向温度Ta与径向距离d、时间t满足指数函数关系。研究结果可为测定取芯过程煤芯的瓦斯损失量提供参考依据。     

Evaluation of ecological restoration success in mining‐degraded lands

This review article analyzes the importance of assessing the success of ecological restoration by using four indicators: assemblage of the plant and animal communities; enzyme activity; litter accumulation and decomposition; and the improvement of soil quality. These indicators can be used alone or in combinations. Even though the Society for Ecological Restoration International provided a primer containing nine attributes to use as standards for measuring ecological restoration, only three of these attributes could be easily applied due to their low costs and low time requirements. These three attributes include: diversity, vegetation structure, and ecological processes. This review article emphasizes that the criteria for the selection of the indicator species should be based upon: habitat types, abundance of species, ease of measuring, quantifying and interpreting the results, gradual enhancement with time and cost‐effectiveness, sensitivity, variability of response, size, residential status, and requirements of the area. Principal component analysis was applied to calculate the reclaimed mine soil quality index (RMSQI) and the forest soil quality index (FSQI) and the RMSQI value was compared with FSQI (optimum index value of reference ecosystem) to evaluate the restoration success. Available phosphorus, exchangeable magnesium, organic carbon, clay content, field moisture, available nitrogen, electrical conductivity, and pH are identified as the most influential parameters that regulate the health of reclaimed mine soil. Exchangeable calcium, magnesium, cation exchange capacity, sand, silt, clay content, field moisture, available phosphorus, and pH are the controlling properties for forest soil. The observed values of the above‐stated soil indicator properties were converted into a unitless score (0–1.00) and integrated into index calculations (RMSQI and FSQI). The contribution of each soil indicator properties on the calculated index was analyzed, which provides insight into the reason for the measured index. A higher RMSQI indicates better ecological restoration success. The calculated RMSQI was found to be 0.473 in the reclaimed dump, which is 6% lower than the reference ecosystem.     

Effects of tectonic stress environment on tectonophysical features of deformed coal

To study the effects of the tectonic stress environment on the tectonophysical features of deformed coal, No.8 Mine in the Pingdingshan mine area is used as a study area and the relationship between the development of deformed coal, distribution of fractures, formation of deformed coal and tectonic stress environment are analyzed. The results indicate that the thickness of the bedrock layer should be included in the analysis of the tectonic stress environment for a region of intense tectonic activity. Although the reverse faulting stress regime can control the development of deformed coal, the C seam is extremely sensitive to the stress regime. The most advantageous direction of the deformed coal fractures is consistent with the regional maximum principal stress, and the development of fractures is closely related to the evolution of the tectonic stress environment. The fracture density of the E seam presents a uniform distribution, yet that of the C seam is completely heterogeneous. Superposition and compounding of the tectonic communities evidently increase the fracture density of the deformed coal. There is a relatively apparent boundary between the different types of deformation, which gradually transform from brittle to ductile with a decreasing lateral pressure coefficient. A generalized deformation pattern of the deformed coal is proposed and can be divided into frictional sliding and solid flow.