JGN型耐高温建筑结构胶抗震加固性能研究

为有效增强建筑结构的抗震性能、提高建筑抗震水平,对JGN型耐高温建筑结构胶抗震加固性能展开研究。将高活性酚醛胺(T－31)作为主固化剂、聚酰胺树脂(PA)为辅助固化剂,结合气相白炭黑、超细石英砂、石棉纤维、纳米材料、环氧树脂等材料,制备JGN型耐高温建筑结构胶。在高温环境下,使用万能试验机分析不同配比条件对结构胶抗震加固性能的影响。测试主要以拉伸强度、压缩强度以及压缩弹性模量为指标。测试结果表明：当固化剂质量比为45∶15、气相白炭黑掺量为4.5%、超细石英砂掺量为10%、石棉纤维掺量为10.5%、纳米SiO₂掺量为3.5%、纳米CaCO₃掺量为2.5%时,JGN型耐高温建筑结构胶的拉伸强度和压缩强度更大,压缩弹性模量得到优化,结构胶的抗震加固性能达到最佳状态。     

3D reconstruction of porous media using a batch normalized variational auto-encoder

Computational Geosciences - The 3D reconstruction of porous media plays a key role in many engineering applications. There are two main methods for the reconstruction of porous media: physical...     

The initial impoundment of the Baihetan reservoir region (China) exacerbated the deformation of the Wangjiashan landslide: characteristics and mechanism

Landslides - Reservoir landslides greatly threaten reservoir safety. Understanding the deformation characteristics and mechanism of reservoir landslides can help evaluate their stability and...     

兰州第四纪黄土/古土壤序列物源演变: 来自于碳酸盐矿物的证据*

黄土/古土壤的物源研究对于揭示第四纪气候变化和青藏高原隆升历史具有重要意义。本研究以位于黄土高原西部1.4 Ma以来的兰州黄土/古土壤沉积序列为研究对象,基于X射线衍射技术分析了黄土/古土壤中的主要矿物组成,侧重于碳酸盐矿物含量,追溯了兰州黄土/古土壤的直接物源。结果显示: (1)1.4 Ma以来兰州地区黄土/古土壤沉积物的主要直接源区为柴达木盆地沙漠区和阿拉善干旱区。(2)基于二元混合模型计算的潜在原始源区对兰州黄土白云石和总碳酸盐矿物的相对贡献率以及长石与石英比值结果一致支持1.4 Ma以来兰州黄土原始物源发生了多次变化。1.4~1.1 Ma和0.9~0.3 Ma青藏高原东北缘造山带(昆仑山、祁连山)和中亚造山带对兰州黄土的贡献相当,而1.1~0.9 Ma和0.3 Ma以来,中亚造山带对兰州黄土的物源贡献增加,这可能分别是对中更新世气候转型和0.3 Ma以来青藏高原及邻近地区干冷气候增强的响应。1.15 Ma和0.8 Ma兰州黄土/古土壤中高的白云石含量、碳酸盐矿物总含量以及0.8 Ma长石与石英比值的快速升高可能是对“昆黄运动”的响应,进而造成了昆仑山、祁连山对黄土高原物源贡献的增加。     

塔里木盆地西南缘叶城地区新元古代冰期事件

新元古代冰期事件记录了“雪球地球”事件重要的地质信息。塔里木盆地周缘新元古代冰碛岩地层露头发育,是研究新元古代冰期事件的理想基地。由于发育多套新元古代火山岩,盆地东北缘库鲁克塔格地区新元古代冰碛岩地层时代已获得较多年代学数据约束;但盆地周缘其他地区新元古代冰碛岩地层公开报道年代学数据较少,不能准确限定其沉积时代,导致冰期事件对比存在争论。为此,本文选择塔里木盆地研究程度较低的西南缘叶城地区新元古代冰碛岩地层,开展岩石学、同位素年代学、岩石地球化学等研究,明确其冰期沉积特征,约束其沉积时代,开展冰期事件对比,讨论古气候风化条件等。南华系波龙组和雨塘组冰碛岩地层具有较低的化学蚀变指数(CIA),分别代表新元古代2次寒冷的冰川气候记录。冰川沉积及其相邻层位的碎屑锆石U-Pb年代学数据显示,波龙冰期的起始年龄晚于(710±13) Ma,与全球Sturtian冰期对应;雨塘冰期的起始年龄不会早于(656±18) Ma,其结束年龄可被南华系顶界年龄635 Ma或上覆震旦系库尔卡克组碎屑锆石年龄(634±9) Ma限定,与全球Marinoan冰期对应。     

Effects of reinforcement ratio on seismic performance of hypothetical stations determined by full-scale central column tests

Bulletin of Earthquake Engineering - The reinforcement ratio of central column member has remarkable effect on the seismic behaviour of double-box stations. To investigate the effects of...     

Excessive greenhouse gas emissions from wastewater treatment plants by using the chemical oxygen demand standard

Chemical oxygen demand(COD)is widely used as an organic pollution indicator in wastewater treatment plants.Large amounts of organic matter are removed during treatment processes to meet environmental standards,and consequently,substantial greenhouse gases(GHGs)such as methane(CH₄)are released.However,the COD indicator covers a great amount of refractory organic matter that is not a pollutant and could be a potential carbon sink.Here,we collected and analysed COD data from 86 worldwide municipal wastewater treatment plants(WWTPs)and applied a model published by the Intergovernmental Panel on Climate Change to estimate the emission of CH₄ due to recalcitrant organic compound processing in China’s municipal wastewater treatment systems.Our results showed that the average contribution of refractory COD to total COD removal was55%in 86 WWTPs.The amount of CH₄ released from the treatment of recalcitrant organic matter in 2018 could have been as high as 38.22 million tons of carbon dioxide equivalent,which amounts to the annual carbon sequestered by China’s wetlands.This suggests that the use of COD as an indicator for organic pollution is undue and needs to be revised to reduce the emission of GHG.In fact,leaving nontoxic recalcitrant organic matter in the wastewater may create a significant carbon sink and will save energy during the treatment process,aiming at carbon neutrality in the wastewater treatment industry.     

广西五圩矿田箭猪坡锑多金属矿综合信息找矿模型

【研究目的】通过箭猪坡锑多金属矿综合信息找矿模型的研究,对于进一步开展深部矿体定位预测具有重要意义。【研究方法】本文基于箭猪坡矿床锑多金属矿找矿工作,研究了深部成矿模式,分析了可控源音频大地电磁测深（CSAMT）、瞬变电磁测量（TEM）、地电化学测量等方法在深部找矿中的作用和效果。【研究结果】可控源测量能反映深部断裂带的延深情况,瞬变电磁测量低电阻率能有效识别矿化带或控矿断裂带,地电化学测量Pb、Zn、Sb元素变化曲线峰值能指示矿化体的存在。【结论】箭猪坡锑多金属矿地质-物探-化探测量综合信息找矿模型的建立为五圩地区深部找矿提供了可以识别的探测目标,CSAMT、TEM及地电化学测量综合方法能探测控矿断裂的深部特征,综合信息特征的找矿方法是构造控矿的有效技术手段。创新点：采用地质-物探-化探综合找矿方法构建多源信息找矿模型,预测深部矿体的位置、规模。     

海底硬岩钻探的现状与前景分析

海底硬岩是世界大洋钻探实现“莫霍钻”目标必然钻遇的地层。世界大洋钻探实施的航次中已多次钻遇海底硬岩,不仅采获了岩心样品,也在钻进施工中发现了诸多问题。本文搜集了近年来世界大洋钻探实施的309、312、335、360和384等有关海底硬岩钻探航次的资料,在对航次情况简要介绍的基础上,重点阐述了目前海底硬岩钻探在钻头、井壁稳定以及取心工具等方面遇到的挑战以及采取的应对措施,并对今后海底硬岩钻探的发展进行了展望。