莼菜( Brasenia schreberi )冬芽对 Cr6+污染的抗性反应

研究了Cr6 +污染对莼菜冬芽外部形态及过氧化物酶、硝酸还原酶活性、叶绿素、O-·2 、MDA的含量等生理指标的影响 .结果显示 :Cr6 +对莼菜毒害机制在于抑制酶活性和损害细胞膜系统 .在培养第三天时叶绿素的含量随着Cr6 +浓度的增加而降低 ;过氧化物酶的活性在 10mg/L中最高 ;硝酸还原酶活性除在 5mg/L中的略微升高外 ,在 10 - 4 0mg/L之间随着Cr6 +培养浓度的升高而降低 ;O-·2 的含量在 5mg/L中的最高 ,在 10mg/L中略高于对照 ,在随后培养中随浓度的升高而降低 ,MDA的含量变化趋势和O-·2 相似     

金龟子绿僵菌甘露糖6-磷酸异构酶基因cDNA序列的克隆及分析

通过绿僵菌属甘露糖6-磷酸异构酶基因保守核苷酸区域设计简并性引物,采用RT-PCR及RACE-PCR技术成功克隆了金龟子绿僵菌mpi基因cDNA序列。该基因cDNA序列全长为1 513 bp,开放阅读框长度为1 328 bp,共编码441氨基酸。BLAST分析发现该基因演绎的氨基酸序列与其它真菌同源性较高,蛋白结构分析表明MPI蛋白是较保守的蛋白磷酸酶结构特征,主要由α螺旋和不规则卷曲构成。     

Origin of glacial–fluvial landforms in the Azas Plateau volcanic field, the Tuva Republic, Russia: Role of ice–magma interaction

The basaltic Azas Plateau volcanic field is located in the Tuva Republic of the Russian Federation. The area was glaciated multiple times, and the field is characterized by the formation of subglacial volcanoes called tuyas, but subaerial volcanoes and lava fields also exist. A combined study of remote sensing and field observations in the vicinity of the tuyas in the southeastern Azas Plateau volcanic field identified landforms that are best explained by the j6;kulhlaup hypothesis. The landforms include elongated hills, paleochannels, and butte and basin topography. These landforms are hypothesized to have formed by both erosion and deposition caused by high-energy water streams. The triggering for the hypothesized j6;kulhlaups was either melting of ice by subglacial volcanism and/or destabilization of ice-dammed/subglacial reservoirs. The age estimation of the flood events is difficult, but they probably occurred during the ice ages of the Quaternary, as late as in the Middle-Late Pleistocene.     

基于源路由的IPv6网络瓶颈带宽定位和估计

网络瓶颈带宽是网络性能的重要指标,现有的瓶颈测量工具只能定位和估计端到端路径的瓶颈带宽,无法定位和估计网络各处的瓶颈带宽,不能满足各种网络设计、管理及应用的需求。文中基于IPv6网络的源路由机制,设计能够定位和估计整个IPv6网络瓶颈带宽的算法和测量包序列,提出基于现代最优化原理的动态规划和分支定界算法,实现了测量工具Netneck。部署在1台探测主机的Netneck就可以定位和估计整个IPv6网络的瓶颈,能够满足全网瓶颈测量的需求。通过部署在CNGI-6PlanetLab平台的大量CERNET2 IPv6网络实验,验证了该算法和工具的有效性。     

利用Access97和VB6的ADO开发工程勘察数据库

根据开发工程勘察数据库的经历,介绍了利用YB6的ADO和Access97开发工程勘察数据库的步骤、方法和技巧,以及开发过程中可能遇到的问题和解决办法。     

鄂尔多斯盆地史家湾地区长6油层组层序-岩相古地理

通过岩心描述、岩石薄片鏊定和古生物、物源区和测井曲线等资料的综合分析,对鄂尔多斯盆地史家湾地区上三叠统长6油层组沉积相和层序地层学特征进行了详细研究,确定长6油层组属于河控型三角洲沉积体系.可划分为1个长期、3个中期和10个短期旋回层序.以古盐度的定量计算和盐度分区为依据,进一步确定了史家湾地区长6油层组沉积期的古湖岸线位置.在此基础上,以物源区和沉积相、层序分析成果为基础,选取中期旋回层序的上升和下降相域为等时地层单元编制史家湾地区长6油层组各时期层序-岩相古地理图,结果表明各时期古地理面貌和砂体展布格局主要受湖平面升、降和物源区方向控制.最有利储层发育的水上一水下分流河道主要出现在各中期旋回的湖侵相域,砂体的延伸方向与东北部的主物源方向相平行,此研究成果对史家湾地区长6油藏的后续勘探有重要的指导意义.     

How Well Do CMIP6 and CMIP5 Models Simulate the Climatological Seasonal Variations in Ocean Salinity?

This paper includes a comprehensive assessment of 40 models from the Coupled Model Intercomparison Project phase 5 (CMIP5) and 33 models from the CMIP phase 6 (CMIP6) to determine the climatological and seasonal variation of ocean salinity from the surface to 2000 m. The general pattern of the ocean salinity climatology can be simulated by both the CMIP5 and CMIP6 models from the surface to 2000-m depth. However, this study shows an increased fresh bias in the surface and subsurface salinity in the CMIP6 multimodel mean, with a global average of ?0.44 g kg^?1 for the sea surface salinity (SSS) and ?0.26 g kg^?1 for the 0–1000-m averaged salinity (S1000) compared with the CMIP5 multimodel mean (?0.25 g kg^?1 for the SSS and ?0.07 g kg^?1 for the S1000). In terms of the seasonal variation, both CMIP6 and CMIP5 models show positive (negative) anomalies in the first (second) half of the year in the global average SSS and S1000. The model-simulated variation in SSS is consistent with the observations, but not for S1000, suggesting a substantial uncertainty in simulating and understanding the seasonal variation in subsurface salinity. The CMIP5 and CMIP6 models overestimate the magnitude of the seasonal variation of the SSS in the tropics in the region 20°S–20°N but underestimate the magnitude of the seasonal change in S1000 in the Atlantic and Indian oceans. These assessments show new features of the model errors in simulating ocean salinity and support further studies of the global hydrological cycle.     

CMIP6二氧化碳移除模式比较计划（CDRMIP）概况与评述

地球工程是指通过人工方法在大规模尺度上干预气候系统,使地球气候降温的一种手段。CO₂移除是地球工程的主要途径之一。文中概述了CO₂移除地球工程的科学背景、各种CO₂移除方法的利弊、大尺度应用CO₂移除方法可能产生的气候效应和风险,以及CO₂移除方案在未来气候情景研究中的现状。在第六次国际耦合模式比较计划（CMIP6）框架下开展的CO₂移除模式比较计划（CDRMIP),为深入研究CO₂移除地球工程减缓气候变化的效能和气候系统对其的响应提供了统一试验方案和平台。CDRMIP的开展,对地球工程和气候变化研究具有重要的促进作用。