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The Erosion Effect of Kapton Film in a Ground-based Atomic Oxygen Irradiation Simulator 被引量:4
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作者 王海斗 MA Guozheng +3 位作者 XU Binshi XING Zhiguo LI Guolu ZHANG Sen 《Journal of Wuhan University of Technology(Materials Science)》 SCIE EI CAS 2014年第6期1277-1282,共6页
In order to investigate the effect of space environmental factors on spacecraft materials, a ground-based simulation facility for space atomic oxygen(AO) irradiation was developed in our laboratory. Some Kapton film... In order to investigate the effect of space environmental factors on spacecraft materials, a ground-based simulation facility for space atomic oxygen(AO) irradiation was developed in our laboratory. Some Kapton film samples were subjected to AO beam generated by this facility. The Kapton films before and after AO exposure were analyzed comparatively using optical microscopy, scanning electronic microscopy, atomic force microscopy, high-precision microbalance, and X-ray photoelectron spectroscopy. The experimental results indicate that the transmittance of Kapton film will be reduced by AO irradiation notably, and its color deepens from pale yellow to brown. Surface roughness of the AO-treated sample is already increased obviously after AO irradiation for 5 hours, and exhibits a flannel-like appearance after 15 hours’ exposure in AO beam. The imide rings and benzene rings in kapton molecule are partially decomposed, and some new bonds form during AO irradiation. The mass loss of kapton film increases linearly with the increase of AO fluence, which is resulted from the formation of volatile products, such as CO, CO2 and NOx. The breakage in structure and degradation in properties of AO-treated Kapton film can be attributed to the integrated effect ofimpaction and oxidization of AO beam. The test results agree well with the space flight experimental data. 展开更多
关键词 space environment simulation low earth orbit atomic oxygen Kapton film erosion mechanism
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不同形态河谷沉积物中稀土元素的粒径分布特征
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作者 尚月婷 张加琼 白茹茹 《土壤学报》 CAS CSCD 北大核心 2024年第3期746-756,共11页
稀土元素(REE)作为一种重要的土壤侵蚀示踪元素,明确其含量随土壤颗粒粒径的变化特征,对准确量化土壤侵蚀速率具有重要意义。本研究基于Samonova等采样测定的不同粒径范围(<1、1~10、10~50、50~250和250~1 000μm)土壤/沉积物颗粒中... 稀土元素(REE)作为一种重要的土壤侵蚀示踪元素,明确其含量随土壤颗粒粒径的变化特征,对准确量化土壤侵蚀速率具有重要意义。本研究基于Samonova等采样测定的不同粒径范围(<1、1~10、10~50、50~250和250~1 000μm)土壤/沉积物颗粒中的REE含量,分析了俄罗斯普罗特瓦河左岸河谷形态(“U”和“V”形谷)、地貌部位(坡面、沟坡/沟壁、沟道底部和洪积扇)、侵蚀(坡面、沟坡/沟壁)和沉积(沟道底部和洪积扇)环境对土壤/沉积物REE含量、富集系数等的影响。结果表明:(1)“U”和“V”形谷四类地貌下,轻稀土(LREE)、重稀土(HREE)和总稀土(ΣREE)含量均随颗粒粒径变粗呈降低趋势。在相同地貌部位,“U”形谷细颗粒(<50μm)中LREE、HREE和ΣREE含量较“V”形谷分别低14.6%~24.7%、10.0%~33.5%和14.2%~21.1%。(2)无论河谷形态和地貌部位,LREE和HREE均明显富集在细颗粒中,尤其是“V”形谷,LREE和HREE主要富集在<10μm的颗粒中。(3)对比侵蚀和沉积区,“U”和“V”形谷沉积区细颗粒中LREE和HREE的富集程度均显著(P<0.05)大于侵蚀区。可见,无论河谷形态、地貌部位和侵蚀沉积区,REE均主要富集在细颗粒中;但河谷形态和侵蚀、沉积对REE含量的粒径分布有重要影响。 展开更多
关键词 侵蚀区域 沉积区域 地貌部位 轻稀土元素 重稀土元素 富集
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