高温时H13钢中初生碳氮化物的分解研究

利用光学显微镜、扫描电镜和电子探针研究了H13钢中初生碳氮化物高温分解时的形貌、尺寸、成分变化规律.原始初生碳氮化物主要为10~30μm的长条状(Vx,Mo1-x)(Cy,N1-y)及少量方形的(Tix,V1-x)(Cy,N1-y).在1200℃保温2.5 h后碳氮化物边缘变为凹凸不平的锯齿状,然后形成细小的分解颗粒,10 h后碳氮化物平均长度减小为12.9μm,主要为(Tix,V1-x)(Cy,N1-y).当经过1250℃ ×5 h保温后87%的碳氮化物发生分解,(Vx,Mo1-x)(Cy,N1-y)溶解消失,碳氮化物长度在20μm以下,当保温时间延长到10 h后碳氮化物长度均在10μm以下,70%为方形并且93%分解形成细小颗粒,未分解的碳氮化物为(Tix,V1-x)(Cy,N1-y).电子探针分析(Tix,V1-x)(Cy,N1-y)的分解与Fe元素扩散有关,高温时Fe在(Tix,V1-x)(Cy,N1-y)中含量逐渐增加而Ti、V减少,优先在边部曲率半径较小部位或缺陷处分解,形成0.1~1μm的细小分解颗粒,并由外向内以区域溶解方式使原始碳氮化物逐渐消失.双亚点阵模型分析两种碳氮化物的平衡溶解温度和组成有关,试样中大部分(Tix,V1-x)(Cy,N1-y)平衡溶解温度在1200~1246℃之间,与实验吻合较好.     

Mechanical behavior of a near α titanium alloy under dynamic compression: Characterization and modeling

Dynamic compression tests under strain rates from 870 s^?1 to 2100 s^?1 were conducted for a near α Ti–8Al–1Mo–1V titanium alloy with equiaxed microstructure. Compression behavior, adiabatic shearing and band microstructure were investigated via characterization and calculation. The results demonstrate that all dynamic constitutive curves exhibited obvious stress fluctuation phenomenon with double increase-decrease changing stages at the primary stage of compression. The dislocation multiplication theory can be used to explain this phenomenon. After the stress fluctuation period, work hardening coexisted with the thermal softening, resulting in the slow hardening tendency in constitutive curves. J-C model was utilized to quantify the dynamic constitutive curves. The deviations between the predicted and experimental curves under high strain rates may be attributed to the over-consideration of thermal softening effect in J-C model. Adiabatic shearing band (ASB) began to form under the strain rate of 2100 s^?1. A total shearing strain of 8.1 within ASB achieved in 8.9 μs, corresponding to a local strain rate of about 9.1 × 10⁵ s^?1 and is over 430 times of the macro strain rate. Post annealing was conducted on ASB before EBSD characterization. Due to the static recrystallization during annealing, the α phase within ASB generally presented as ultra-fine grains less than 1 μm in diameter.     

烃族组成对柴油储存安定性影响研究

针对柴油储存过程中质量衰变问题，利用典型柴油样品，开展烃化合物对中国成品柴油储存安定性影响规律研究。烃组成分析测定结果表明，柴油中总芳烃和链烷烃之间存在很强的相关性（相关系数为0.90）。综合采用相关分析、逐步线性回归等方法，建立了安定性指标与烃组成的关联模型，拟合验证表明模型可靠，可以直接用于柴油储存安定性预测；研究确定了柴油储存安定性的主要影响物质，按照对储存安定性指标影响的严重程度将烃类物质分为三个等级，其中苊烯和三环芳烃对柴油质量衰变影响最大，链烷烃对十六烷值和热值影响最大。     

邛崃山脉不同地质背景茶叶的生化成份研究

以邛崃山脉4个茶叶产区3个品种为材料,取春稍1芽2叶制成蒸青样和炒青样进行生化成份分析.结果表明邛崃山脉茶叶受地质大环境控制的生化成份变化幅度小,由西北至东南是呈线性关系.水浸出物、茶多酚、儿茶素总量、酯型儿茶素和非酯型儿茶素由西北至东南是呈线性递增关系;而氨基酸和CAF由西北自东南是呈线性递减关系.线性方程的常数作为茶叶生化成份的标准值具有科学性,既可作为制定茶叶标准的依据,也可作为邛崃山脉茶叶地理标志保护产品的生化指标.地质背景、生态环境、品种和制作工艺都会影响茶叶的生化成份,从而影响茶叶的品质.     

QK空间上紧的复合算子的性质

本文研究了QK空间上紧的复合算子Qφ的两个性质.论文给出了如果在D上的符号函数φ的上确界小于1,则Cφ在QK空间上是紧的.还限定了在φ为某些条件下,Cφ在QK空间与Bloch空间上的紧性是等价的.     

体质量对中华鳖(Pelodiscus sinensis)生化组成和质量能的影响

分别测定了在实验室条件下养殖的23只稚鳖(终末体质量为15.7～46.4 g)和38只幼鳖(终末体质量为57.5～283.7 g)鳖体的生化组成和质量能.结果表明:随着稚鳖、幼鳖体质量的增加,稚鳖和幼鳖鳖体的蛋白质、脂肪的质量分数和质量能均升高,而水分则随之降低(P＜0.01).稚鳖鳖体的灰分质量分数与体质量相关关系不明显(P＞0.05),而幼鳖的灰分质量分数随体质量增加而降低(P＜0.05).实验证实,以体质量为自变量来预测中华鳖稚鳖和幼鳖的蛋白质、脂肪的质量分数和质量能的方法是简单、可行的.     

栾树不同单株种子品质差异性分析

对采自江西农业大学校园内10株栾树种子的播种品质和营养成分含量进行分析,结果表明：不同单株栾树种子发芽品质和营养物质的积累存在差异,在采种母树选择上,除种源外还要考虑单株的筛选;10个单株中,5号千粒重最重,达9.04 g,种子发芽性状及营养物质积累均处于较高水平,为10个单株中的优良单株;种子千粒重、含水量达到极显著...     

惠民南部地区油水物化性质与油气运移方向和模式

油水物化性质变化可以从古水文演化角度反应油气运移方向.本文以惠民凹陷南部地区沙河街组三段为例,利用原油密度、黏度、地层水矿化度、水型及离子组合参数变化特征,研究油气运移规律.平面上,研究区原油密度、黏度整体具有西北高、东南低的分布规律,局部具有一低四高的分布特征,反映出原油密度、黏度随运移距离的增加而增大;地层水矿化度具有以夏口断裂为中心,向南北两侧逐渐变小的分布特征,矿化度高值区的分布与夏口断层油气运移聚集有关;地层水水型和离子组合参数变化特征表明沿夏口断裂带具有两个油气聚集区,分别为双丰、江家店-瓦屋鼻状构造.通过对油气运聚关系的分析,以油气源、输导因素为基础,沿油气主要运移方向,建立了研究区近源侧向砂体输导、近源混向反Z型输导、远源混向阶梯状输导、远源混向多级反Z型输导4种油气运移模式.     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.     

Changes in physical features of Glacier No. 1 of the Tianshan Mountains in response to climate change

This study analyzes the changes in glacier zones and snow composition of Glacier No.1 in the Tianshan Mountains of China since 1961,and their possible relations with climate.It is found that precipitation dominated the snow composition and that air temperature and precipitation controlled the distribution of glacier zones,but interannual change in precipitation had a relatively large effect on glacier zones and snow composition during 1963–1981 (P10) and 1963–1989 (P11).However,during 1982–2007 (P20) and 19...