超音速火焰喷涂金属陶瓷复合涂层的耐磨性能研究   总被引：1，自引：1，他引：0       下载免费PDF全文

周永宽  康嘉杰  岳文  付志强  梁健  朱丽娜  王成彪 《探矿工程》2020,47(4):72-79

为改善深部钻具关键易损构件的耐磨性能,采用超音速火焰喷涂(HVOF)技术在35CrMo钢基体上制备了WC-10Co4Cr涂层,利用扫描电子显微镜(SEM)、X射线能谱仪(EDS)、X射线衍射仪(XRD)、显微硬度仪、维氏硬度计和摩擦磨损试验机测试分析了涂层的微观结构、力学性能和摩擦磨损行为。结果表明：利用HVOF技术制备的WC-10Co4Cr涂层具有致密的微观结构和优异的力学性能,其孔隙率为1.3±0.1%,显微硬度为1392±45 HV0.3,断裂韧性为7.11±0.10 MPa·m1/2;与35CrMo钢基体相比,涂层具有更加优异的耐磨损性能,并且随着滑动速度的增加,WC-10Co4Cr涂层的摩擦系数下降、磨损率增大;WC-10Co4Cr涂层的磨损失效机制主要包括磨粒磨损、粘着磨损和疲劳磨损。  相似文献   

Paleohydrological Changes in the Western Tibetan Plateau over the Past 16,000 years Based on Sedimentary Records of n‐Alkanes and Grain Size     

WANG Mingd  YANG Yaping  ZHANG Jiawu  HOU Juzhi 《《地质学报》英文版》2020,94(3):707-716

Both monsoons and westerlies have exerted influence on climate dynamics over the Tibetan Plateau (TP) since the last deglaciation, producing complex patterns of paleohydroclimatic conditions. Diverse proxy records are essential to forge a robust understanding of the climate system on the TP. Currently, there is a general lack of understanding of the response of inland lakes over the TP to climate change, especially glacier‐fed lakes. Paleohydrological reconstructions of such lakes could deepen our understanding of the history of lake systems and their relationship to regional climate variability. Here we use records of n‐alkanes and grain size from the sediments of Bangong Co in the western TP to reconstruct paleohydrological changes over the past 16,000 years. The Paq record (the ratio of non‐emergent aquatic macrophytes versus emergent aquatic macrophytes and terrestrial plants) is generally consistent with the variations in summer temperature and precipitation isotopes. The changes in grain‐size distributions show a similar trend to Paq but with less pronounced fluctuations in the early‐middle Holocene. The new data combined with previous results from the site demonstrate that: 1) Bangong Co experienced relatively large water‐level fluctuations during the last deglaciation, with a steadily high lake‐level during the early‐middle Holocene and a decreasing lake‐level in the late Holocene; 2) The lake level fluctuations were driven by both high summer temperatures via the melting water and monsoon precipitation. However, the dominant factor controlling lake level changed over time. The lake‐level history at Bangong Co deduced from the n‐alkanes and grain‐size records reveals the past hydrological changes in the catchment area, and stimulates more discussion about the future of glacier‐fed lakes under the conditions of unprecedented warming in the region.  相似文献