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11.
根据干馏工艺流程配入适量氧气,可以降低载热气体需要预热的温度,以实现低能耗、易于工业生产的特点,设计了一套新型的有氧干馏工艺流程。有氧干馏工艺因其过程中存在可燃性混合物,有发生爆炸事故的可能性,通过实验对所收集的不同温度下的干馏气体的成分与含量进行了分析,结合爆炸极限理论,对该有氧干馏工艺流程的不同温度、不同惰性气体含量条件下可燃气体爆炸极限进行了分析计算。结果表明,可燃气体的浓度在整个反应升温过程中始终没有进入爆炸危险区域,说明该实验装置不具备爆炸危险性;对干馏工艺流程中氧气的输入量的控制,可以防止该工艺流程的火灾爆炸的发生。 相似文献
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Enrichment of potentially toxic elements in areas underlain by black shales and slates in Korea 总被引:6,自引:0,他引:6
Jin-Soo Lee Hyo-Taek Chon Jong-Shin Kim Kyoung-Woong Kim Hi-Soo Moon 《Environmental geochemistry and health》1998,20(3):135-147
The Okchon black shale in Korea provides an important example of natural geological materials containing toxic elements; the Chung-Joo, Duk-Pyung, Geum-Kwan, I-Won and Chu-Bu areas are underlain by these black shales and slates of the Guryongsan Formation. This formation is part of the Okchon Group which is found in the central part of Korea. Geochemical surveys were undertaken in these five study areas in the Okchon Zone in order to examine the level of enrichment and dispersion patterns of potentially toxic elements in rocks and soils. After appropriate preparation, samples were analysed by instrumental neutron activation analysis and inductively coupled plasma atomic emission spectrometry for a range of elements. Arsenic, Cu, Mo, V, U and Zn are highly enriched in the Okchon black shales and their mean concentrations are significantly higher than those in black slates. These elements are closely associated with one another from a geochemical viewpoint and may be enriched simultaneously. Mean concentrations of As, Mo and U in soils derived from black shales occurring in the Duk-Pyung and Chu-Bu areas are higher than the permissible level suggested by Kloke (1979), and the enrichment index decreases in the order of Duk- Pyung > Chu-Bu > Chung-Joo > Geum-Kwan = I-Won areas. Uranium-bearing minerals such as uraninite and brannerite have been identified in black shales from the Chung-Joo area by electron probe micro-analysis. Uraninite grains are closely associated with monazite and pyrite with a grain size ranging from 2m to 10m whereas brannerite grains occur as a euhedral form 50m in diameter. 相似文献
13.
As an insufficiently utilized energy resource,oil shale is conducive to the formation of characteristic microbial communities due to its special geological origins.However,little is known about fungal diversity in oil shale.Polymerase chain reaction cloning was used to construct the fungal ribosomal deoxyribonucleic acid internal transcribed spacer(r DNA ITS)clone libraries of Huadian Mine in Jilin Province,Maoming Mine in Guangdong Province,and Fushun Mine in Liaoning Province.Pure culture and molecular identification were applied for the isolation of cultivable fungi in fresh oil shale of each mine.Results of clone libraries indicated that each mine had over 50% Ascomycota(58.4%–98.9%)and 1.1%–13.5%unidentified fungi.Fushun Mine and Huadian Mine had 5.9% and 28.1% Basidiomycota,respectively.Huadian Mine showed the highest fungal diversity,followed by Fushun Mine and Maoming Mine.Jaccard indexes showed that the similarities between any two of three fungal communities at the genus level were very low,indicating that fungi in each mine developed independently during the long geological adaptation and formed a community composition fitting the environment.In the fresh oil-shale samples of the three mines,cultivable fungal phyla were consistent with the results of clone libraries.Fifteen genera and several unidentified fungi were identified as Ascomycota and Basidiomycota using pure culture.Penicillium was the only genus found in all three mines.These findings contributed to gaining a clear understanding of current fungal resources in major oil-shale mines in China and provided useful information for relevant studies on isolation of indigenous fungi carrying functional genes from oil shale. 相似文献
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以油页岩渣及其二氧化钛改性材料为吸附剂,探究它们去除水溶液中亚甲基蓝和六价铬的能力.通过实验,控制溶液的pH值、温度、初始浓度和接触时间,观察吸附效果变化特征,研究其动力学和热力学性能.实验表明,改性油页岩渣吸附亚甲基蓝和六价铬的吸附率是未改性的2—3倍,且改性油页岩渣对亚甲基蓝的吸附率可达97%,对六价铬的吸附率不到25%.吸附亚甲基蓝时,pH值越大,吸附效果越好;而吸附六价铬时,最适pH值为4.改性油页岩渣吸附亚甲基蓝实验符合准二阶动力学方程,计算得反应活化能为13.29 kJ.mol-1,表明此过程主要是物理吸附.在热力学方面,由范特霍夫方程计算得ΔG〈0、ΔH〉0,表明此过程自发吸热,可见此过程还伴有化学吸附.Langmuir和Freundlich等温模型拟合结果表明,Langmuir模型数据拟合甚佳,R2=0.9999,说明改性油页岩渣吸附亚甲基蓝是单分子层吸附.二氧化钛改性油页岩渣经7次回收利用后,对亚甲基蓝的吸附效果仅减少约1.5%. 相似文献
16.
Comparison of quartz sand, anthracite, shale and biological ceramsite for adsorptive removal of phosphorus from aqueous solution 总被引:1,自引:0,他引:1
The choice of substrates with high phosphorus adsorption capacity is vital for sustainable phosphorus removal from waste water in constructed wetlands. In this study, four substrates were used: quartz sand, anthracite, shale and biological ceramsite. These substrate samples were characterized by X- ray diffractometry and scanning electron microscopy studies for their mineral components (chemical components) and surface characteristics. The dynamic experimental results revealed the following ranking order for total phosphorus (TP) removal efficiency: anthracite 〉 biological ceramsite 〉 shale 〉 quartz sand. The adsorptive removal capacities for TP using anthracite, biological ceramsite, shale and quartz sand were 85.87, 81.44, 59.65, and 55.98 mg/kg, respectively. Phosphorus desorption was also studied to analyze the substrates' adsorption efficiency in wastewater treatment as well as the substrates' ability to be reused for treatment. It was noted that the removal performance for the different forms of phosphorus was dependent on the nature of the substrate and the adsorption mechanism. A comparative analysis showed that the removal of particulate phosphorus was much easier using shale. Whereas anthracite had the highest soluble reactive phosphorus (SRP) adsorptive capacity, biological ceramsite had the highest dissolved organic phosphorus (DOP) removal capacity. Phosphorus removal by shale and biological ceramsite was mainly through chemical adsorption, precipitation or biological adsorption. On the other hand, phosphorus removal through physical adsorption (electrostatic attraction or ion exchange) was dominant in anthracite and quartz sand. 相似文献
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18.
中国页岩气开发过程环境管理现状与对策分析研究 总被引:1,自引:0,他引:1
中国页岩气资源储量丰富,随着页岩气商业勘探开发的不断推进,引发的生态环境问题日益突出.从页岩气开采工艺来看,开发对水、大气、土壤及生态地质环境等都有一定的影响.此外,中国页岩气开发过程中还存在法规标准体系不健全、监管机制缺乏、环境准入机制不明等问题.因此,针对页岩气开发所带来的环境风险,亟需完善法律法规与标准体系、严格监督管理、制定开发环境规划.同时,建设环保示范工程,加大环保科研投入,降低页岩气开发的环境影响,实现页岩气开发的绿色可持续发展. 相似文献
19.
针对页岩气特殊的开发方式及环评难度比常规气大的特点,运用"压力-状态-响应"框架模型,建立了页岩气开发对生态环境影响的评价指标体系。引入曲线投影的方式,并将投影寻踪方法和动态聚类方法相结合,提出了曲线投影寻踪动态聚类的定量评价方法;基于样本各指标的曲线投影和动态聚类方法寻找最佳投影方向,并建立相应的生态环境影响评价优化模型。结合全局最优经验指导和信息素交流,采用改进的蚁群算法对优化模型进行求解。该算法维持蚁群的多样性,且收敛性较好,同时也避免出现局部最优。对四川省威远页岩气区块进行了实例分析,结果表明:2010年、2011年和2014年的环评属于差类(4级),2012年和2013年的环评属于中类(3级),其中植被覆盖率、空气质量优良率、地表水质达标率、废水排放量、公众对环境的满意度、二氧化硫排放量和废水排放量达标率等指标对生态环境评价的影响较大。在页岩气开发初期,由于开发技术落后,再加上环保投资不高,环保意识不强,造成生态环境问题较为严重。随着学习借鉴美国的经验,及页岩气的开发技术进一步提高,加上国家对生态环境保护的重视,威远页岩气区块生态环境恶化得到有效的遏制。但开发时间越长,开采难度越大,将会产生更多更大的生态环境问题。分析结果与威远页岩气开发区域的实际情况相符,为页岩气气田生态环境影响评价奠定了科学基础。投影寻踪动态聚类方法具有无需设定参数、操作简单、客观等优点,是页岩气开发对生态环境影响评价的一种新方法。 相似文献
20.
下志留统龙马溪组发育黑色泥岩,分布在贵州北部。为阐明其沉积环境和页岩气成藏条件,研究分析了沉积特征和地球化学特征。泥岩具粉砂泥质结构或泥质结构,岩层多为薄层,普遍具水平层理,含浸染状黄铁矿颗粒,表明沉积水动力弱、沉积速率较低。泥岩的Mo、V、U的富集系数都大于1,Ce异常的平均值为-0.033,特定元素比值(V/Cr、Ni/Co、V/(V+Ni)和Ce/La)都显示泥岩形成于缺氧环境。总体上,龙马溪组黑色泥岩的沉积环境为水体较深、沉积速率较低、呈缺氧还原状态。龙马溪组黑色泥岩的TOC含量在2.78%~4.36%之间,平均值为3.79%;镜质体反射率(Ro)在1.88%~2.16%之间,平均值为1.99%,反映有机质已达成熟-过成熟的干气阶段;有效厚度在10~100 m之间,脆性矿物含量一般在20%~30%之间,埋深大概在0~3 500 m。地层厚度从南至北逐渐增大,其余参数各剖面相似。因此,具有页岩气资源潜力的区域大致在桐梓-绥阳以北地区。这些特征综合表明龙马溪组黑色泥岩具备形成页岩气藏的良好条件,存在较高的页岩气资源潜力。 相似文献