使用地聚合物混合物减少泥灰岩破碎:来自摩洛哥非斯附近实验试验的经验教训

IF 0.5 Q3 GEOGRAPHY
M. Akdim, L. Mesrar, A. Alami, Selmaoui Sabah, R. Jabrane
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引用次数: 0

摘要

尽管地球上许多地区都有丰富的泥灰岩,但在实际问题中使用泥灰岩会产生许多问题,涉及其成分的质量、物理和化学特性及其增值成本。破碎是影响其工程行为、工艺和其他社会经济用途的主要关键因素之一。本文介绍了摩洛哥非斯地区中新世泥灰岩的物理化学性质。研究人员对它们进行了调查,以测量它们的变化,并观察它们如何影响泥灰岩的岩土特性。将泥灰岩样品与不同浓度的纤维素和火山灰混合,暴露在极端温度下,在实验室进行观察,并根据可靠的特性进行解释,以减少破碎风险,如凝聚力和材料的阻力。通过将纤维素和火山灰以不同的比例(1%,5%),(2%,10%),(3%,15%),(4%,20%),(5%,25%)添加到生泥泥中,我们使用各种技术和分析测试了其特性。我们主要使用x射线衍射,x射线荧光和扫描电镜技术,本研究了解了基于泥灰岩混合物的创新材料的可能生产。它强调对非斯(摩洛哥)地区中新世泥灰岩的估价,但它的目标更大,因为其结果可能适用于全世界的泥灰岩。主要目标是确定适合改善混合泥灰岩的物理化学性质的最佳阈值,从而降低泥灰岩破碎的风险。化学分析表明,样品中主要化学元素的含量略有变化,因此得出了结论。结果表明,灰泥中添加火山灰和纤维素后,Fe2O3和SiO2增加,有利于粘土的新生。出现新的伊利石和偏高岭石。当我们比较原始泥灰岩和混合泥灰岩的特征结果时,特别是在900°C和1000°C的温度下,这种差异很重要。矿物学分析表明,赤铁矿结晶良好。在混合泥灰岩中,这些结果通过电子显微镜分析得到了证实。这些结果集中证实了地聚合物混合物的积极影响,因为它们有助于减少泥灰岩破碎的风险,因为它的凝聚力和阻力变得强烈。这些新灰泥的特点具有创新性,呈现出材料转型的新程度。他们赞成在经济和工业活动中对海洋进行有利的开发。即使是局部实验,获得的结果的重要性可能是全世界的。石英、赤铁矿等矿物结晶完善,伊利石、高岭石向莫来石、偏高岭石转变。从这些曲线可以看出,随着火山灰和纤维素的加入,矿物的强度有所增加。石英(sio2)、莫来石(M)和偏高岭石(MK), CaO和al2o3有一个小峰。这些相通常主要发生在由焚烧废物和玻璃粉生产的水泥、陶瓷和玻璃陶瓷材料中(Asquini et al., 2008)。随着碎屑含量的增加,样品中CaO和al2o3的峰明显减少,而通过对泥灰泥原样品的分析可以观察到非晶相的存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Marl crumbling decrease using geopolymer mixtures: lessons from experimental tests in the vicinity of Fez, Morocco
: Despite its abundance in many regions of the planet, the marl’s use in practical issues engender many problems, in relation to its components’ quality, its physical and chemical characteristics and its valorization costs. The crumbling is among its major critical aspects that affect its engineering behavior, its handcraft and other socio-economic uses. This paper apprehends the physical and chemical properties of the Miocene marl in Fez vicinity (Morocco). They are investigated to measure their changes and see how they affect the marl’s geotechnical characteristics. Mixed with cellulose and pozzolan at different concentration degrees, the marl samples were exposed to extreme temperatures, observed in the laboratory and interpreted in terms of characteristics reliable to crumbling risk reducing as cohesion and materials’ resistance. By adding the cellulose and pozzolan to the raw marl at different percentages (1%, 5%), (2%, 10%), (3%, 15%), (4%, 20%), (5%,25%), we have tested its characteristics using various techniques and analyses. We mainly used X-ray diffraction, X-ray fluorescence and SEM techniques This study apprehends the possible production of innovative materials based on marl mixtures. It emphasizes the valorization of the Miocene marls in the region of Fez (Morocco) but its aims are larger as the results may be applied for marl worldwide. The main goal is to identify the best thresholds that are suited to improve the mixed marls’ physico -chemical properties and therefore reduce risks of crumbling in marl. The results are concluding as chemical analyses show a slight variation of major chemical elements in the samples’ contents. We note that after adding pozzolan and cellulose to marl, the Fe2O3 and SiO2 increase and favors neoformation of clays. New illite and metakaolinite appear. The difference is important when we compare results between characteristics of the raw marl and those of the mixed marls, in particular at temperatures of 900 °C and 1000 °C. The mineralogical analyzes have shown the appearance of well crystallized hematite. In mixed marl, these results were confirmed by the electron microscope analysis. The results converge to confirm the positive impact of geopolymer mixtures as they contribute to decrease the risks of marl crumbling as its cohesion and resistance become intense. These new marl’s characteristics are innovator and show a new degree of the material’ transformation. They favor the marl’s advantageous exploitation in economic and industrial activities. Even locally experimented, the importance of the obtained results may be worldwide. These results show a perfect crystallization of minerals such as quartz, hematite and the transformation of illite and kaolinite into mullite and metakaolinite. From these curves, it is observed that there is an increase in the intensities of the minerals with the addition of pozzolan and cellulose. Quartz (SiO 2 ), mullite (M) and metakaoilinte (MK) and a small peak for CaO and Al 2 O 3 are observed. These phases usually occur mainly in cement, ceramics and glass-ceramic materials produced from incinerated waste and glass powder (Asquini et al., 2008). The increments in the cullet content in the samples showed a marked reduction of peaks in CaO and Al 2 O 3 , while the presence of amorphous phases can be observed through the analysis of the raw marl sample.
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