单原子分散的Ir-N-C燃料电池阳极抗中毒催化剂

燃料电池的阳极抗中毒研究是重要课题,探索具有超高质量活性和抗CO毒化的阳极催化剂具有显著的科学意义和应用价值。本文成功制备了Ir原子级别分散在N掺杂碳的载体上的新催化剂,并且发现该Ir-N-C对甲酸具有良好的电催化氧化性能,其质量比活性为商业Pd/C的48倍。组装了燃料电池单电池进行测试,结果显示,Ir-N-C催化剂在单电池中的质量比功率密度高达281 mW/mg,较商业Pd/C催化剂提升了3倍。同时,Ir-N-C对CO毒化的耐受性大大增强,经过14000 s的长期测试后,其活性仅衰减68%,优于商业Pd/C催化剂（衰减85%）。并且,该催化剂能够简单有效的大批量制备,为单原子催化剂的大批量制备提供了新思路。     

汶川震区文家沟泥石流成灾机理与特征

文家沟位于绵竹市清平乡,属于 5 ·12 汶川Ms8.0级地震极重灾区。地震发生后的3个汛期内,文家沟曾先后发生5次典型泥石流灾害,其中以2010年8月13日泥石流灾害最为严重,规模与灾情巨大,社会影响深远。在对文家沟泥石流跟踪调查的基础上,探讨了泥石流的成灾机理和特征。研究表明:(1)文家沟泥石流是地震和强降雨共同作用的结果,其成因可归纳为震因与物源以及雨因与水源两个方面,在整个泥石流形成和发生的过程中,呈现出洪流-侵蚀下切-崩滑-席卷-进一步侵蚀下切-进一步崩滑-增大泥石流规模—……的"滚雪球式"循环过程; (2)泥石流发生所需的雨量、雨强条件和水动力条件都显著降低,泥石流规模和雨量之间呈现出明显幂函数关系; (3)发生过程呈现出持续时间长、运动距离远的特征; (4)成灾过程呈现出明显的链式效应,危害形式多样; (5)泥石流频率呈现出高发性,规模呈现出放大性。最后提出了文家沟泥石流研究与防治的建议。     

An efficient,scalable approach to hydrolyze flavonoid glucuronides via activation of glycoside bond

Hydrolyzing flavonoid glucuronides into corresponding aglycones posed some significant challenges. To improve acid-catalyzed hydrolysis process of flavonoid glucuronide, structures of glucuronide, hydrolysis parameters and post-processing were optimized. The optimized condition was performed by hydrolysis flavonoid glycoside methyl ester in a mixed solvent consisting of 2 mol/L H₂SO₄/EtOH/H₂O (1/8/1, v/v/v) at 95 °C for 7 h and resulted in up to 90% aglycone yields, minimal byproduct formations and milder hydrolysis conditions. Furthermore, the optimized method avoids tedious purification steps and is easily conducted on a relatively large-scale using economical and commercially available reagents.     

滑坡冲击铲刮变量的计算方法研究

高速远程滑坡运动过程中,冲击铲刮效应不仅增加滑坡的体积与规模,而且会增大滑坡成灾范围,风险预测与判断出现明显误差,导致灾难性事件的发生。目前对于高速滑坡的铲刮深度、铲刮范围和铲刮体积等变量计算往往是采用基于经验的铲刮率算法,其是通过体积增量来反算铲刮变量的数学方法,而实际情况中高速滑坡的冲击铲刮是滑体冲击力和地表可铲刮材料之间的力学屈服破坏作用的结果。本文基于接触力学、弹塑性力学和岩土力学,提出了地表可铲刮层在附加冲击荷载作用下铲刮变量的理论计算方法,认为竖向冲击和切向剪切是滑体冲击铲刮过程的两种主要作用方式。结合实际岩土体材料参数,发现不考虑切向荷载时,铲刮层塑性区主要以竖向破裂区为主,考虑切向荷载时,铲刮层塑性区沿切向迁移,直至塑性边界贯通至地表,符合实际情况,实现了对铲刮变量的定量化计算。     

文家沟巨型岩质滑坡高速远程运移特征分析

文家沟滑坡是汶川地震诱发的巨型高速远程岩质滑坡,其运移特征尚不明确。在现场调查的基础上,结合遥感解译,进一步深入研究其运移特征。分析得出,滑体自滑源区差异性启动,途经斜坡区铲刮坡表岩土体,随后以滑行、飞行等方式进入沟谷区,沿沟铲刮两岸坡体继续下行,与岸坡发生了5次明显的冲撞,逐步解体碎屑化,于第3次冲撞后开始大规模减速堆积,最终于沟口区停积。结果表明,地形是滑体运移堆积的主控因素,滑体的解体碎屑化和冲撞山体时的爬高、抛摔、越顶现象以及冲击气浪的形成等是高速行程的具体表现,碰撞是导致全程解体碎屑化的主要途径。     

Non-linear couplings,from the early to the late time universe

Deciphering the mechanisms at play in the formation and evolution of the large-scale structure of the universe is part of the scientific goals of many projects of observational cosmology. In particular, large-scale structure observations can be used to infer mode-coupling effects, whether they come from the physics of the early universe or from its late time evolution. Specificities of such couplings are presented, noting that in principle they can be directly detected through bispectra of the cosmic microwave background temperature anisotropies or density in the local universe. The existence of such couplings have however more far-reaching consequences for the growth of the structure. Those are sketched as well as their possible observational impacts.     

A note on “A LP-based heuristic for a time-constrained routing problem”

In their paper, Avella et al. (2006) investigate a time-constrained routing problem. The core of the proposed solution approach is a large-scale linear program that grows both row- and column-wise when new variables are introduced. Thus, a column-and-row generation algorithm is proposed to solve this linear program optimally, and an optimality condition is presented to terminate the column-and-row generation algorithm. We demonstrate by using Lagrangian duality that this optimality condition is incorrect and may lead to a suboptimal solution at termination.     

永泰县城峰镇旗山小区后山滑坡现场应急调查及处置分析

2010年5月20日,受连续降雨影响,福建省永泰县城峰镇旗山小区后山发现有滑坡地质灾害隐患,后山中下部产生多条35~80m长拉裂缝,坡脚崩塌不断,潜在滑坡规模约8×10⁴m³,存在继续下滑的危险,情况十分危急,威胁坡脚居民2565人的生命和约5.38亿元财产。本文在对灾害现场进行详细地质调查的基础上,结合现场测绘、监测等手段,对该滑坡体的基本特征进行了较深入的调查研究,对滑坡发生及成灾原因进行了初步分析。结果表明,滑坡区地形条件及岩土体特征是滑坡发生的基本条件,连续降雨的饱水加载作用以及雨水沿节理裂隙结构面的下渗软化作用是诱发滑坡发生的直接原因。同时,根据滑坡险情特征,提出了应处置建议及应急卸载措施。最后,根据监测结果信息化指导应急卸载工作,确保了施工安全及受灾群众的生命财产安全。本次成功排险,对指导福建海沿地区地质灾害应急处置工作提供了科学依据。     

Large-scale forcing with less communication in finite-difference simulations of stationary isotropic turbulence

This study proposes a new forcing scheme suitable for massively-parallel finite-difference simulations of stationary isotropic turbulence. The proposed forcing scheme, named reduced-communication forcing (RCF), is based on the same idea as the conventional large-scale forcing scheme, but requires much less data communication, leading to a high parallel efficiency. It has been confirmed that the RCF scheme works intrinsically in the same manner as the conventional large-scale forcing scheme. Comparisons have revealed that a fourth-order finite-difference model run in combination with the RCF scheme (FDM-RCF) is as good as a spectral model, while requiring less computational costs. For the range 80 < Re_λ < 540, where Re_λ is the Taylor microscale-based Reynolds number, large computations using the FDM-RCF scheme show that the Reynolds dependences of skewness and flatness factors have similar power-laws as found in previous studies.     

青海玉树Ms7.1级地震地质灾害主要特征

2010年4月14日7时49分,青海省玉树县发生Ms7.1级地震。玉树地震产生较连续的地表破裂和大量房屋破坏,并诱发了滑坡、崩塌和震裂山体。此外,地震诱发的砂土液化、水渠溃决等加剧了局部山体地质灾害。通过现场调查和地震前后玉树县地质灾害发育状况,简要阐述了地震地质灾害的主要发育特征,包括震后地质灾害数量明显增加、地震地质灾害分布受活动断裂控制、低位滑坡为主、地质灾害链生效应显著等,并对灾后重建过程中的地质灾害防治提出了建议。