Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current

Sea surface temperature (SST) records in the South Yellow Sea during the last 6200 years are reconstructed by the unsaturation index of long-chain alkenones (K 37 U ’) in sediment core ZY2 from the central mud area.The SST records varied between 14.1 and 16.5°C (15.6°C on average),with 3 phases:(1) A high SST phase at 6.2-5.9 cal ka BP;(2) A low and intensely fluctuating SST phase at 5.9-2.3 cal ka BP;and (3) A high and stable SST phase since 2.3 cal ka BP.Variation of the SST records is similar to intensity of the Kuroshio Current (KC),and corresponds well in time to global cold climate events.However,the amplitude of the SST response to cooling events was significantly different in different phases.The SST response to global cooling event was weak while the KC was strong;and the SST response was strong while the KC was weak.The difference in amplitude of the SST response is possibly caused by the modulation effect of the Yellow Sea Warm Current which acts as a shelf branch of the KC and a compensating current induced by the East Asia winter monsoon.The warm waters brought by the Yellow Sea Warm Current cushion the SST decrease induced by climate cooling,and both the Kuroshio and East Asian winter monsoon play important roles in the modulation mechanism.The SST records display a periodicity of 1482 years.The same period was found in the KC records,indicating that variation of the SST records in the central South Yellow Sea is strongly affected by KC intensity.The same period was also found in Greenland ice cores and North Atlantic and Arabian Sea sediment cores,showing a regional response of marine environmental variability in the East China Seas to that in the global oceans.     

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.     

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.     

2010年7月8日英山特大暴雨过程的成因分析

利用GFS(0.5°×0.5°)6 h再分析资料、LAPS资料以及FY-2c卫星云图资料、武汉区域雷达拼图产品和自动站实时资料,对2010年7月8日发生在英山的特大暴雨过程进行了分析.结果表明:控制湖北地区的副高南退时,副高外围东移的短波槽引导北方冷空气下滑是此次过程的触发机制;低层切变、低空急流、露点锋和地面辐合线引起了低层辐合、中层辐散、低层θse锋生及中上层θse锋区下移,提供了有利的动力条件;750～1 000 hPa的高湿区是水汽条件;温度槽温度脊的配合、对流有效位能的持续增加和湿位涡上正下负的配置为此次过程提供了不稳定能量.     

应用Hermit插值方法修正Dome-A自动气象站记录的雪层温度

随着冰盖表面雪的积累或消融,自动气象站(AWS)上所携带的传感器相对于地表的高度/深度不断变化,给观测数据带来误差.本文利用分段三次Hermit插值的方法对Dome A地区的AWS历史雪层温度数据进行修正.结果表明,雪层的修正量随着雪的积累率的增加而增大,在夏半年为正,在冬半年为负.该方法对于浅层雪温的修正有较好的效果.     

基于ESP压力调节器制动能量回馈系统

为了实现液压制动系统制动能量回收功能和提高制动能量回收效率,提出了基于ESP压力调节器制动能量回馈方法,阐述了该方法的工作原理,设计了制动能量回馈系统硬件在环仿真实验台,研究了制动能量回馈系统的可行性。采用硬件在环仿真实验方法研究了基于ESP压力调节器制动能量回馈系统可行性,验证了制动过程平稳性和制动效能。实验结果表明:基于ESP压力调节器制动能量回馈系统可以最大效率回收制动能量,保证制动过程平稳,满足制动效能要求。     

溅射金膜对氧化铝陶瓷纳秒脉冲真空沿面闪络的影响

研究了溅射金膜对氧化铝陶瓷在真空环境中、纳秒脉冲高电压作用下沿面闪络特性的影响规律.通过对氧化铝陶瓷表面粗糙度、电极接触形式的研究,并结合表面态陷阱、界面能带结构、电荷注入过程的分析,探究了影响氧化铝陶瓷溅射金膜后沿面闪络电压的主要原因.在50 ns/1.2μs脉冲下、电极间距10 mm时,测量各试样的闪络电压60次,取后30次平均值作为稳定的闪络电压.研究结果发现,氧化铝陶瓷在溅射金膜电极试样的闪络电压比直接压接电极试样的闪络电压低,这是因为在不同电极接触方式下,氧化铝陶瓷材料的表面态对真空中的电子发射和材料表层的电荷注入的影响不同所致.     

管道机器人弯管运动转体原因分析

为避免管道机器人弯管内运行时发生转体现象而影响管内任务的执行,对机器人转体的原因进行了深入研究.以建立的管道机器人弯管运行的位姿模型为基础,对机器人的受力状况进行了分析,建立了机器人过弯时的转体力矩模型.通过对转体力矩的分析,揭示了管道机器人弯管运行时发生转体的根本原因,并指出了管道机器人弯管运行的最佳姿态角.理论计算表明:当机器人以最佳姿态角运行时,机器人转体力矩几乎为0,不发生转体;当机器人以其他姿态角运行时,将出现一个不为0的转体力矩,该力矩使机器人向平衡姿态角方向转体,直至机器人姿态稳定为止.在实际应用时,使机器人在平衡姿态角运行为最佳.仿真结果与理论计算基本一致,该研究为人弯管内的姿态稳定运行提供了一定的理论依据.     

高压高浓度CO2烟气辐射换热特性分析与计算

针对高压O2/CO2燃烧方式下高浓度CO2和水蒸气混合气体烟气的辐射换热问题,建立了一种新的宽带关联k分布模型.为了验证模型的有效性,以O2/CO2燃烧方式下炉内CO2和水蒸气生成状况为例,采用该模型与离散坐标法相结合的方法计算了不同温度(1 000~2 500 K)和压力(0.1~1.5 MPa)下一维无限大平行平板间混合气体的辐射强度和CO24.3μm谱带累积分布函数,并与逐线计算、全光谱关联k分布模型和基于指数的宽带关联k模型的计算结果进行了比较.结果表明:随着压力的增加,所提出的宽带关联k分布模型与逐线计算的结果吻合较好,与文献报导的两个模型相比,不仅计算精度有所提高,而且对混合气体的处理更加简便灵活,因此更适于高压下烟气辐射特性的计算.     

基于聚类分析的申贷信用等级评价方法

 为了解决申贷信用等级评价问题,介绍了解决银行申请贷款信用等级评价中聚类分析采用的基本概念及术语,提出了2种聚类算法包括基于信贷数据的聚类算法δ-kmeans;基于高维信贷数据的聚类算法ASC,并通过实验对其性能进行比较分析,实验表明:①δ-kmeans算法在信贷风险的控制上取得较好效果;②相比传统k-means和Coweb算法,ASC算法在聚类高维信贷数据上更加有效.利用k-means算法对银行信贷数据的聚类动力学关系进行分析.最后,给出了聚类分析算法在银行信贷领域应用的的难点.