基于真实三维结构的玉米冠层生化参数垂直分布的定量化分析

为了定量研究作物生化参数在冠层中的垂直分布情况,本文以2000年栾城实验测量的玉米冠层自上而下不同叶位叶片的光谱数据为基础,利用PROSPECT模型进行反演,获得每层叶片的叶绿素(a b)含量、等效水厚度、干物质含量等叶片的生化参数.通过比较发现:玉米冠层叶绿素等含量生化参数具有明显的随高度垂直分层现象,最明显的就是叶片的叶绿素含量,最大和最小叶绿素含量的相对差值甚至可以达到最大值的79.1%.在此基础上,根据实测玉米冠层结构,利用扩展L系统生成玉米真实三维结构冠层场景.通过统计计算每层叶片的生化参数,进而得到冠层生化参数的垂直分布.这为进一步基于冠层光谱的参数反演和定量分析以及农业应用等研究奠定了理论基础.     

《瘗鹤铭》雷门鼓事试析

《瘗鹤铭》引用的雷门鼓事传说,在《金山本》中表述为“山阴降迹”,而在其他文本中则为“雷门去鼓”。前者表示鼓震洛阳、仙鹤神异的事迹;后者体现的是鼓破不鸣鹤飞的内容。对照铭文,用典是为了突出仙家身世,故当以《金山本》的表述最具原真,并从中折射出东晋侨民怀念故都洛阳的情感。     

二维可控细胞自动机伪随机序列发生方法研究

提出了一种新的细胞自动机———二维可控细胞自动机。根据二维可控细胞自动机的性质,提出了一 种具有梯型结构的二维可控细胞自动机的伪随机序列发生方法。计算机模拟表明,具有梯型结构的二维可控细 胞自动机伪随机序列发生器实现简单,产生的序列具有速度高、统计特性好等优点。新的细胞自动机在对称密 码学中有广泛地应用。     

先进变凸度工作辊辊形及其控制特性

跟踪某2250 mm热轧生产线CVC辊形实际窜辊数据发现,连续变凸度(CVC)辊形常窜到两端极限位置.分析表明,CVC辊形的二次凸度调控能力随带钢宽度减小而呈二次方下降趋势,表现出对较窄带钢凸度控制能力的明显不足.Smart-Crown辊形也存在同样问题.提出一种新的先进变凸度(AVC)工作辊辊形曲线,其二次和四次凸度与窜辊量呈线性关系,且随着四次凸度控制能力的增大,二次凸度控制能力随带钢宽度的变化明显放缓,有助于提高宽带钢或超宽带钢轧机对不同宽度带钢的板形控制能力.     

凯氏原圆线虫Protostrongylus(Pulmostrongylus)kamenskyi Schulz,1930在我国的首次发现(圆线目:原圆科)

采自雪兔Lepus timidus Linnaeus肺内寄生的一种线虫,经鉴定为凯氏原圆线虫Protostrongylus(Pulmostrongylus)kamenskyi Schulz,1930,隶属于圆线目Strongylata原圆科Protostrongylidae.此种线虫为我国新纪录种,对该种线虫进行了光镜和扫描电镜观察.     

Rapid growth and sterility of growth hormone gene transgenic triploid carp

Triploid carp (100%) with 150 (3n=150) chromosomes were obtained by crossing the females of improved tetraploid hybrids (♀, 4n=200) of red crucian carp (♀)×common carp (♂) with the males of diploid yellow river carp (♂, 2n=100). The crosses yielded transgenic triploid carp (positive triploid fish, 44.2% of the progeny) and non-transgenic triploid carp (negative triploid fish). Histological examination of the gonads of 24-month-old positive triploid fish suggested they were sterile and the fish were not able to produce mature gametes during the breeding season. Morphologically, both the positive and negative triploid fish were similar. They had a spindle-shaped, laterally compressed, steel grey body with two pairs of barbells. Most of the quantifiable traits of the triploid carp were intermediate between those of the two parents. The positive and negative triploid fish were raised in the same pond for 2 years. The mean body weight of the positive triploid fish was 2.3 times higher than the negative triploid fish. The weight of the largest positive triploid fish was 2.91 times higher than that of the largest negative triploid fish. Thus, we produced fast-growing transgenic triploid carp that have a reduced ecological risk because of their inability to mate and produce progeny.     

Premixed jet flame characteristics of syngas using OH planar laser induced fluorescence

Lean premixed flame characteristics of several typical low calorific value (LCV) syngases (basis CO/H2/CH4/CO2/N2),including bituminous coal,wood residue,corn core,and wheat straw gasification syngas,were investigated using OH planar laser induced fluorescence (PLIF) technology.OH radical distributions within the turbulent flame were measured for different turbulence intensities.Flame structures of syngases were analyzed and characterized with respect to burnt and unburnt regions,flame curvature (sharp cusp),local extinction (holes and penetration),OH reaction layer thickness,wrinkling,and other features,with OH-PLIF instantaneous images and statistical analysis.Results show that H2 content,LCV,and turbulence intensity are the most effective factors influencing the OH radical intensity and thickness of OH radical layers.The bituminous coal gasification syngas with relatively higher LCV and H2 content tends to burn out easily.Through changes in thickness of the OH radical layers and signal intensities,the reaction layer can be compressed by intensifying turbulence and thereby the combustion processes of syngas.     

Characteristics of strontium isotopes and their implications in the Qixing Cave of Guizhou,China

The strontium isotopic compositions (87Sr/86Sr) of samples including soils, bedrock, soil waters, drip waters and their corresponding speleothems in the Qixing Cave (QXC), Guizhou Province, China, were systemically measured and analyzed. The results indicate that there are significant Sr isotopic differences among samples. The mean 87Sr/86Sr ratios in drip water for the samples 1#, 4# and 9# were 0.709568, 0.709139 and 0.708761, respectively, which possibly result from different flow paths, residence times, and other hydrogeological processes in the unsaturated zone overlying QXC. Meanwhile, levels of 40.8%, 57.6% and 72.4% of Sr in drip waters for 1#, 4# and 9#, respectively, were derived from bedrock dissolution, which was calculated by the mixture model of the two end-members (soil and bedrock). There is, however, no positive correlation between the relative proportion from bedrock dissolution (δ13C value is 1.8‰) and drip water δ13CDIC values. The mean drip water δ13CDIC value in 1# is the heaviest (–4.5‰) with the lowest contribution rate of bedrock dissolution, whereas the value in 9# is the lightest (–9.3‰) with the highest contribution rate of bedrock dissolution. The proportion from host rock dissolution in 4# is higher than that in 1# and lower than that in 9#, while its mean drip water δ13CDIC value (–8.6‰) is higher than that of 9# and lower than that for 1#. This suggests that the prior calcite precipitation (PCP) processes in the unsaturated zone overlying the cave are responsible for the δ13CDIC value differences between different drip waters, and not bedrock dissolution. Furthermore, this study also demonstrates that the 87Sr/86Sr ratios of speleothems in the 1# and 4# mainly reflect the variation in the relative proportions from the soil system (soil water) and bedrock dissolution overlying the cave. It is, therefore, feasible to use the strontium isotopic signals of speleothems as an indicator for soil chemical weathering intensity, and consequently as a monsoon proxy in the study area.     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.     

非双倍测度下多线性Calderón-Zygmund算子及其交换子在Herz型空间上的有界性

本文引入非齐型空间上的Herz空间,并证明了多线性Calderon-Zygmund算子及其交换子在这些空间上的有界性.