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Thunbergii trees were established, and the sun survivorship curves were drawn with field data. The results showed that in the three plots, the height and basal diameter growth of regenerated young P. thunbergii trees had exponential, linear, and quadratic functional relations with age and the age structure was of spindle, discrete, and pyramid types, respectively. Most of the regenerated young trees were distrbuted at 0.3-1.2 m from their nearest standing trees, and the individuals of the young trees decreased near to or far from the nearest standing trees. Inplots Ⅰ and Ⅲ, the expected average life of regenerated young P. thunbergii trees had a decreasing trend with their increasing age, and the survival number of the population also decreased with increasing population age. The survivorship craves of regenerated young P. thunbergii trees in the two plots approximated to the type of Deevey Ⅱ, indicating that the young P. thunbergii populations in the plots were at stable development stage. The population structure of regenerated young P. thunbergii trees in plot Ⅱ was lesser integral, suggesting that the population was of declining types being related to human disturbance, slope and other environmental factors.

结果表明:(1) 3个样地中幼龄植株高生长、基径生长与年龄均分别呈指数函数、直线和二次函数关系;(2) 3个样地黑松幼龄植株年龄结构存在着明显差异,分别表现为纺锤形、残缺型和金字塔型;(3)幼龄植株主要集中分布在距最近立木0.3~1.2m,离立木越近或越远幼龄植株均逐渐减少;(4)对样地Ⅰ和样地Ⅲ黑松幼龄植株生命表和存活曲线的分析表明,随年龄的增加,黑松幼龄植株生命期望值基本上呈递减趋势,黑松幼龄植株种群存活数也随着年龄的增加而降低;样地Ⅰ和样地Ⅲ黑松幼龄植株种群存活曲线近似于Deevey Ⅱ型,表明2个样地黑松幼龄植株种群处于稳定发展阶段;(5)样地Ⅱ幼龄植株种群结构很不完整,表明该种群属于衰退型,与人为干扰及坡度等有关。

We choose 20 cases of fungal rhinosinusitis who were treated in our department between the year 2007.4 and 2008.4 as our study group and 5 cases of purely nasal septum deviation as control group. The 20 cases contain 19 cases of fungus ball and 1 case of chronic invasive fungal rhinosinusitis. Their age fluctuate from 19 to 80, and the average age is 51 . All of the 25 cases blood samples were taken to detect the 1-3-β-D glucosan with the kit produced by Beijing jinshanchuan technology company and under the MB—80 quickly microorganismal detection system.

采用北京金山川科技公司生产的试剂盒及MB—80微生物快速检测系统分别检测中国医科大学附属盛京医院耳鼻喉科于2007年4月至2008年2月经鼻窦内窥镜手术治疗,并经术后病理证实为真菌性鼻窦炎患者(19例为真菌球型,1例为慢性侵袭性真菌性鼻窦炎)的血液样品20例,患者年龄19岁—80岁,平均年龄51岁,采取中国医科大学附属盛京医院耳鼻喉科于2008年1月住院单纯鼻中隔偏曲患者的血液样品5例作为对照组,患者年龄16—56岁,平均年龄32岁(以上血样标本的采集患者均已签署知情同意书)。

The original Seluohe Group contains at least four parts: Late Archean metamorphic rocks (zircon SHRIMP protolith ages 2517~2534 Ma), Late Paleozoic metamorphosed volcanic-sedimentary strata (zircon SHRIMP 252 Ma), Permian gneissic granitic complex (zircon SHRIMP 260 Ma), and Jurassic mylonitized granites (zircon SHRIMP 168 Ma).

原划分的色洛河群至少由4部分组成:新太古代变质火山-沉积地层(锆石SHRIMP年龄为2517~2534 Ma)、晚古生代变质火山-沉积地层(英安岩锆石SHRIMP年龄为252 Ma)、二叠纪片麻状杂岩体(锆石SHRIMP年龄为260 Ma)和侏罗纪糜棱岩化花岗岩(锆石SHRIMP年龄为168 Ma)。

On the basis of whole grain evaporation age on single zircons using a double filament for different genetic zircons in metalassenite and metarhyolite of Luoyu formation,Yunkai group,the formation age of volcanic rock is 922 Ma;later geologic events is 643 Ma ̄716 Ma or 427 Ma ̄473 Ma...

本文采用颗粒锆石分层蒸发法分别对云开群罗罅组变英安岩及变流纹岩中不同成因锆石进行年龄测定,获得该火山岩之形成年龄为922Ma,940Ma;后期地质事件年龄为643Ma~716Ma,427Ma~473Ma及物源区的年龄为1616Ma,2084Ma。

Variance in chemical components of the former is similarto the latter;the content of α-cellulose,lignin increase with the growth of age,the content of extract,hemicellucose,polysaccharose and mineral elementsdecrease with the grow of age;pH value is acid and increase with growth.

早园竹的化学成分含量随年龄的变异规律基本类似于毛竹,α-纤维素含量、木质素含量随着年龄增大而增大;抽提物、半纤维素、聚戊糖、灰分含量随着年龄增大而降低;pH值呈酸性,酸性随着年龄增大而减弱。

From the point of microstruction,bamboo volume fraction of bundlesheath,single bundle sheath area,fiber width,cell wall thickness increase withthe growth of age,fraction of cell wall changes like density,increases with thegrowth of age,the 2 age-degree bamboo is the biggest.The reason why 2 age-degree fraction of cell wall more than 3 age-degree bamboo is the former has thegreater fraction of parenchyma;1 age-degree bamboo has the greatest fiberlength,fiber length and width ratio and vessel length.The difference in bamboofiber length,vessel length and width among other age-degrees is not distinct.

从构造角度来说,竹材的纤维束比量、单个维管束纤维束面积、纤维宽度、胞壁厚度随着年龄的增大而增大,胞壁率随年龄变化规律与密度相似,随年龄增大而增大,以2度竹最大,2度竹胞壁率比3度竹大主要由于薄壁组织比量较大所致;纤维长度、纤维长宽比、导管长度以1度竹最大,其它年龄纤维长度、导管形态变化不明显。

I wonder if I could, Go back to old Hollywood When presidents dropped blonde bombshells Instead of creating their lives to hell The way we're living makes no sense Take me back, take me back To the age of innocence I wanna go back then Take me back, take me back To the age of innocence Back to the age of innocence I wanna get older, don't fight my age Take me back to those simpler days I wonder how it all happened I wanna get older, don't fight my age Don't wanna be the page on the scalpel's blade So please tell me, please tell me What ever happened?

我想如果我能,回到旧好莱坞当总统下降金发弹壳而不是创建自己的生命地狱我们的方式生活是没有意义的带我回家,带我回家无罪的年龄我想回去,然后带我回家,带我回家无罪的年龄回到纯真时代我要变老,不要打我的年龄带我回到那些简单的日子我不知道这一切是如何发生的我要变老,不要打我的年龄不想放在手术刀刀片页所以,请告诉我,请告诉我没有发生什么?

The isotopic abundances of rare gases and cosmic-ray exposure ages of asteroid meteorites, planetary meteorites and the Apollo lunar samples applied to clue up and understanding cosmic-ray exposure history of parent bodies of different meteorite types, collision events, the relationship between cosmic-ray exposure ages and heliocentric distance of the parent bodies, irradiation history of precompaction exposure of chondrules, pairing meteorites for the Antarctic meteorites and desert meteorites, the ejection history of planetary meteorites, and relative ages of lunar craters and so on.

小行星陨石、行星陨石及阿波罗月球样品的稀有气体同位素丰度和宇宙射线暴露年龄,已广泛应用于探索和了解不同类型陨石母体的宇宙射线暴露历史、冲击碰撞事件、暴露年龄与日心距离的关系、吸积形成母体前硅酸盐球粒的辐照历史、南极和沙漠陨石中成对陨石的判别、行星陨石的溅射历史及月坑的相对年龄等关键词:宇宙射线暴露年龄;陨石;球粒陨石;无球粒陨石;火星陨石;中铁陨石

Zircons were picked out from diabases in The Luobusa ophiolite, whose ~(206)Pb/~(238)U apparent ages SHRIMP U-Pb dating show very complex , but a majority of which distribute between the 148.3Ma and 174.2Ma.

罗布莎蛇绿岩辉绿岩中的锆石SHRIMP U-Pb ~(206)pb/~(238)U表观年龄呈现复杂的分布格局,主体年龄在148.3~174.2Ma范围之内,获得高精度的锆石谐和年龄为162.9±2.8Ma,即罗布莎蛇绿岩的形成年龄

Refer to the research findings of CHengDu Research Institute of Geosciences and Minerals(1990) and Nanjing Research Institute of Geography and Lake of Chinese Academy of Sciences(1989), according to the Guidebook of China Stratum(2000), the chronostratigraphy of Kunming Basin is divided into 4 age: the bottom of the Quaternary corresponding to M/G Boundary, age is 2.6Ma;the Bottom of the Mid-Pleistocene corresponding to B/M Boundary, age is 0.78Ma;the Bottom of the Upper-Pleistocene corresponding to the Blake event, age is 0.128Ma;the Bottom of the Holocene corresponding to the Gothenburg event,age is 0.012Ma.

本次研究获得了大量的测年数据,参考成都地质矿产研究所(1990)及中科院南京地理与湖泊研究所(1989)等的研究成果,按照中国地层指南(2000)的方案,厘定了昆明盆地第四纪年代地层划分:第四系底界对应古地磁松山反向期与高斯正向期界线处,年龄为2.6Ma;更新统中部底界对应古地磁布容正向期与松山反向期界线,年龄为0.78Ma;更新统上部底界对应古地磁布莱克事件附近,年龄约0.128Ma:全新统底界对应古地磁哥德堡事件附近,年龄约0.012ma。

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