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.     

A small difference in nuclear mass could make a big impact in the cosmos

In a recent paper [1] published in Physical Review Letters, scientists at the Institute of Modern Physics, Chinese Academy of Sciences, have reported their first results from the Cooler Storage Ring at the Heavy Ion Research Facility, a newly-constructed major scientific facility in Lanzhou, China. As a part of an international collaboration including colleagues from Europe, USA and Japan, they were able to identify in experiments the very     

Sufficient and necessary conditions of separability for bipartite pure states in infinite-dimensional systems

The PHC criterion and the realignment criterion for pure states in infinite-dimensional bipartite quantum systems are given. Furthermore, several equivalent conditions for pure states to be separable are generalized to infinite-dimensional systems.     

Reverberation nulling and echo enhancement at low frequency using waveguide invariance

Based on the fact that the transfer function vector between a source receiver array and the dominant scatterer of boundary reverberation at a range can be obtained from the corresponding reverberations scattered from this range cell, a reverberation nulling concept using time reversal processing has been proposed. However, current reverberation nulling methods have certain limitations when applied into practice, which would null boundary reverberation and target echo simultaneously. As a solution, a passive reverberation nulling and echo enhancement method at low frequency using waveguide invariance is proposed in this paper. In this method, the reverberation subspace for the target range cell is not obtained directly from the return signals scattered by the target range cell but from the return signals scattered by a range cell located before the target using waveguide invariance, so as to suppress the reverberation embodied in the target echo by passive reverberation nulling. Besides, a range-dependent optimal weighting vector rather than conventional projector matrix is deduced to null the reverberation component meanwhile maximizing the target echo, thereby enhancing the echo-to-reverberation ratio furthest. Numerical simulations in typical range-independent shallow water environment demonstrate the efficacy and the improved performance of the proposed method for echo-to-reverberation enhancement.     

分光光度法检测不同地区和类型稻种功能性成分的初步研究

 为研究不同地区和类型水稻品种糙米中γ-氨基丁酸和总黄酮等功能性成分,本实验采用分光光度法准确测定了中国、日本、韩国、国际稻作所和云南品种及云南野生稻γ-氨基丁酸和总黄酮的含量.结果表明:① 用分光光度法测定水稻籽粒中γ-氨基丁酸和总黄酮含量的方法是可靠的;② 不同地区和类型水稻品种功能成分含量存在差异;③ 相关分析表明,氨基丁酸与总黄酮的相关系数较高(r=0.575^**),在育种上可以实现多个相关性状间的遗传改良;④ 鉴定出墨江黄皮饵块谷、明恢86、墨江饵块谷、疣粒野生稻等18份高GABA和高总黄酮的水稻品种,可作为选育高黄酮和γ-氨基丁酸品种的亲本或直接作为功能稻开发利用.首次报道疣粒野生稻总黄酮质量分数达0.751%,在所有水稻品种中黄酮含量最高.     

锥度量空间中两对非相容映象的一个新的公共不动点定理

 自锥度量空间的概念被提出以来,已经有数位学者对其结构和性质进行了探讨.研究了锥度量空间中非相容映象对,并利用非相容映象对的性质和压缩条件得到一类映象的公共不动点定理,其结果推广了相关文献的结果.     

3GPP-LTE系统下行链路S-SCH检测算法的低复杂度实现

小区搜索是3GPP-LTE移动通信系统中的重要过程,研究了此过程中下行链路辅同步信道（S-SCH）的检测问题,指出了接收机在采用最大似然序列检测（MLSD）算法进行S-SCH检测时,具有较高的计算复杂度.给出了一种基于MLSD准则S-SCH检测算法的低复杂度实现方法,利用S-SCH序列的结构特点,缩小候选S-SCH序列...     

基于粒计算的商业数据流概念漂移特征选择

商业数据流具有动态性、漂移性等特性,概念漂移特征选择是数据流挖掘的重要工作之一.本文从数据流的特点和概念漂移特性出发,提出了数据流的概念形式化分析流程和基于粒计算构建数据流的概念形式化描述模型;商业数据流的概念漂移实际上取决于其概念外延的变化,文中使用包括外延偶合度和内涵偶合度在内的概念偶合度来描述概念间的相似性;经过粒化的数据流由概念格来表示,进而通过概念格对的松弛偶合度来分析数据流特征;结合概念偶合分析和数据流变化特征,阐述了一种基于数据流概念格对的松弛匹配偶合度算法,并据此分析概念格对来选择数据流的漂移特征.通过实例验证、评价了特征选择,证明其有效性.     

兰州地区晚新生代沉积的岩石磁学记录及其古环境意义

位于黄土高原和西北干旱区过渡带的兰州地区,在晚新生代发育了一套风成红黏土和冲积—河湖相沉积.这套地层详细的岩石磁学研究结果表明,磁化率等一些磁学参数在细节上可能反映成壤作用强弱,但在大的趋势上大致反映干旱化,在长尺度研究中可作为干旱化的指标.S-300mT等另一些磁学参数主要反映赤铁矿质量分数,与红度值明显相关,因此同红度一样可作为温度的指标.底部冲积一河湖相沉积中黏土的主要载磁矿物是磁铁矿和赤铁矿;中下部红黏土沉积的主要载磁矿物是磁赤铁矿和赤铁矿,可能含针铁矿;中上部红黏土主要的载磁矿物是磁赤铁矿、磁铁矿和赤铁矿,可能含针铁矿.利用岩石磁学恢复的古环境表明,兰州地区在8.35～7.2 Ma是一个较为温暖的以冲洪积和河湖相为主的沉积环境;7.2～3.5 Ma主要为干陆地环境,同主体黄土高原一样接受粉尘沉积;6.3 Ma风尘沉积在沉积物中开始占主导地位;5.2 Ma兰州及其周边地区发生了急剧干旱化,可能伴随着快速降温;3.5 Ma开始的青藏高原运动A幕使兰州盆地瓦解,并于1.4 Ma开始接受黄土沉积,成为了黄土高原的西缘部分.     

基于Markov逻辑网的句子压缩方法

提出了一种基于Markov逻辑网通过删除单词进行英文句子压缩的方法。通过一阶逻辑公式表示单词的局部特征以及单词之间的相互依赖关系,确定单词是否应该删除。与现有方法相比,该方法把判别式学习和整数规划的优点相结合,既融合了丰富的句子特征,又以逻辑公式方便地表示全局约束。在书面和口语两个新闻数据集上的实验结果表明:该方法与L3和SVTL系统相比具有明显优势,在压缩率接近时,以人工压缩结果为评测标准,压缩后句子的依存关系F-score有较大提高。