Consistent long-term Holocene warming trend at different elevations in the Altai Mountains in arid central Asia

Recent results indicate contrasting Holocene moisture histories at different elevations in arid central Asia (ACA). However, relatively little is known about Holocene temperature changes at different elevations. Here we report an independently dated peat brGDGTs-based MBT'_5ME record from the Narenxia peatland (NRX) in the southern Altai Mountains. The record suggests a long-term warming trend since ~7.7 cal. kyr bp , with a warmer stage during ~7–5.5 cal. kyr bp , a cold stage during ~5.5–4 cal. kyr bp , and a warming trend over the last ~4 kyr. The long-term warming trend indicated by the NRX MBT'_5ME record is largely consistent with Holocene temperature records from nearby sites covering an altitudinal range of ~1700–4100 m above sea level. This consistent long-term warming trend at different elevations differs from the long-term Holocene drying/wetting trends at high/low elevations of the Altai Mountains. We propose that the warming trend and consequent permafrost thawing at high elevations could have resulted in increased meltwater runoff, which would have contributed to the long-term wetting trend at low elevations. Our findings potentially provide an improved understanding of regional climate change and associated water resource availability, with implications for their possible future status.     

安徽安庆M_S4.8级地震现场调查启示与震害特征分析

本文通过安庆MS4.8级地震现场调查和震害特征分析,探讨了5.0级左右中强地震现场调查的自身安全保障、灾民恐惧心理安抚,以及震害分布、震害损失、人员伤亡等,旨在为将来5.0级左右中强破坏性地震开展现场调查和研究震害特征等提供参考。     

Jianshangou Bed of the Yixian Formation in West Liaoning,China

The Jianshangou fossil locality was first found byChang Zhenglu and his colleagures in 1962, now thearea of Jianshangou, Sihetun and Huangbanjigou be-comes famous all over the world for its yielding feath-ered dinosaurs, Confuciusornis and Archaefructus. Thename of Jianshangou Bed was proposed by the firstauthor of present paper as an informal suggesting unitduring the research on Jehol fossils of western Liaon-ing in 1963 and 1964. The unit was named then asJianshan Bed[1], indicating th…     

LiMn_2O_4的溶液─凝胶─酯化法合成反应机制

本文以溶胶─凝胶─酯化法合成LiMn2O4尖晶石粉体材料，用FT—IR、TG—DTA以及XRD研究了LiMn2O4的形成机制。整个反应过程可分为凝胶的形成和干凝胶的分解两阶段，前体物在液相中经络合、酯化、聚合而形成凝胶，不同的投料Li／Mn（摩尔比）值使凝胶分解形成LiMn2O4经历不同的反应历程，也使产物具有不同的物相组成。     

Li_2S─B_2O_3体系玻璃基团结构表征

本文利用高温路融反应及液氮淬冷技术制Li2S─B2O_3体系玻璃采用。IR、Raman振动光谱方法对玻璃的基团结构进行了表征并讨论了基团结构随组成的变化对玻璃稳定性能的影响。实验发现．随Li2S含量增加．玻璃结构经历了由平面网络转变为三维网络．最终离解为孤立的小基团的变化过程。     

量热法研究Li2S—B2O3玻璃晶化动力学

采用惰性气体保护下的高温熔融反应及氮淬冷技术,制备了xLI2S·（1—X）B2O23玻璃。利用DSC量热法研究了玻璃的非等温晶化动力学,计算得到晶化活化能E,Avrami指数n及晶化热—△H等动力学参数。实验发现,xLi2S·（1—X）B2O3硫氧化物能在X≤0．45的区域形成玻璃,x=0．25玻璃组份具有最强的抗晶化能力,而x=0．45玻璃组份最易晶化。玻璃的晶化为一热激活过程,且主要由表面成核机理控制。玻璃晶化活化能在180—100μm颗粒范围有最大值,晶化热—△H与峰值温度Tp满足线性关系。     

Hymenoptera (wasps,bees and ants) in mid-Cretaceous Burmese amber: A review of the fauna

The Burmese amber assemblage of Hymenoptera with its 47 constituent families is now the richest in Cretaceous. A collection of Burmite (Burmese amber) from the Hukawng Valley, Myanmar at the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences was examined, revealing that Burmite inclusions contain a very highly diverse hymenopteran fauna with as many as ten families found new for the Burmese fossil assemblage. The mid-Cretaceous hymenopteran fauna of Burmese amber is revised at the family level. A high level of the first family occurrences and endemism is demonstrated suggestive of an insular syndrome affected the mid-Cretaceous Burmese biome, as well as somewhat contradictory features in composition of the hymenopteran families there.     

LiMn2O4的溶胶-凝胶-酯化法合成及性能Ⅲ电学及电化学性能

以库仑滴定法测定了实验电池Ｌｉ／ＤＭＥ＋ＥＣ－ＬｉＰＦ６／ＬｉＭｎ２Ｏ４的ＥＭＦ曲线,有三个放电平台分别位于４．０８Ｖ,３．９７Ｖ及２．９８Ｖ,４Ｖ区平台较宽。８００℃烧结的样品初台放电容量为１２６ｍＡｈ／ｇ,低温样品的容量衰减较小。     

基于Django框架的可视化地震目录服务系统1

为提高测震台网地震目录数据的服务水平,构建了基于Django框架的可视化地震目录服务系统。该系统以Django框架为基础,在前端工具包Bootstrap的管理下,通过Highcharts图形库和高德地图实现了地震目录的可视化服务,为地震目录的对外服务提供了一种较为高效便捷的途径。