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弃渣场复杂工况下稳定性分析研究 被引量:2
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作者 闫宾 王昱 +1 位作者 方舒 李明阳 《水电与抽水蓄能》 2022年第5期23-29,共7页
针对目前弃渣场在水电站设计、建设、运营过程中得不到足够重视的情况,弃渣场失稳会对人民的生命财产安全带来很大威胁。拟选择具有代表性的典型弃渣场,以弃渣场基本稳定复核为基础,对可能存在的潜在风险进行分析,分别探讨了修坡和碾压... 针对目前弃渣场在水电站设计、建设、运营过程中得不到足够重视的情况,弃渣场失稳会对人民的生命财产安全带来很大威胁。拟选择具有代表性的典型弃渣场,以弃渣场基本稳定复核为基础,对可能存在的潜在风险进行分析,分别探讨了修坡和碾压、极端暴雨工况(排水失效)、渣体下垫面软化、边坡加固对渣体稳定性的影响,得出结论:当堆高不超30m时,堆高降低对渣体稳定性影响较小;应重视弃渣场渣底植被和表层软土的清理工作,地下水位监测及排水盲沟的布置;混凝土格构—插筋框格体系能有效提高弃渣边坡的抗滑稳定性。 展开更多
关键词 渣体稳定性 修坡 下垫层
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Effect of Different Aromatic Fractions on Colloidal Property of Tahe Atmospheric Residue 被引量:1
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作者 Yu Shuanglin Zhang Jiling +3 位作者 Cheng Tao Rong Lili Xue Peng Shan Honghong 《China Petroleum Processing & Petrochemical Technology》 SCIE CAS 2012年第3期17-23,共7页
Different amounts of FCC slurry oil and HVGO were added to Tahe atmospheric residue respectively. The colloi- dal stability and asphaltene agglomeration of atmospheric residue and mixed oils were characterized by mean... Different amounts of FCC slurry oil and HVGO were added to Tahe atmospheric residue respectively. The colloi- dal stability and asphaltene agglomeration of atmospheric residue and mixed oils were characterized by means of the mass fraction normalized conductivity and the small-angle X-ray scattering technology (SAXS). The results indicated that the sta- bility of Tahe atmospheric residue decreased with an increasing amount of these oil fractions. It was found that the decline of the colloidal stability was attributed to the component polarity difference between oil fractions and the atmospheric resi- due. Though the aromaticity of FCC slurry oil was higher than that of HVGO, the polarity of aromatics and resins of FCC slurry oil was lower than those of HVGO. So the degree of the colloidal stability was more seriously destroyed by FCC slurry oil. The dispersion of asphaltenes in Tahe atmospheric residue was changed by adding FCC slurry oil and HVGO. The particle size of as-ohaltenes increased alon~ with the decline of the colloidal stability 展开更多
关键词 RESIDUE colloidal stability polarity SAXS particle size
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