末次间冰期赵店动物群的地层时代探讨

报道了在山西襄汾赵店采砂场,黄土下部砂层中发现了哺乳动物群化石,并对化石出土层位的时代和古环境进行了分析.在赵店的动物群化石中除最后鬣狗和虎外,基本上与丁村动物群相同,出土层位也与丁村组相似.从化石出土层位上覆黄土古土壤序列分析,化石层与S1古土壤发育时代相当,其时代上限为距今7.5万年,当属末次间冰期,气候相对温暖湿润.     

产学合作——台湾技职教育界“最后一哩”计划及其启示

随着社会转型、技术升级以及产业结构调整,台湾的技职教育越来越难以适应社会的发展,供需产生结构性失调,许多年轻人毕业即面临失业。为此,台湾教育主管部门提出从校园到企业的“最后一哩”技职教育改造工程。该文介绍了“最后一哩”就业学程的做法及其启示。     

Diatoms from the southwestern continental slope, South China Sea, and their paleoenvironmental significance since the last glacial times

A quantitative study was undertaken on diatoms from cores (SA08-34) obtained from the southwestern continental slope of the South China Sea (SCS). A total of 165 diatom species belonging to 45 genera were identified. We constructed a stratigraphic subdivision and correlation according to the characteristics of diatom assemblages together with ¹⁴C dating and carbonate analysis. We also discuss the sedimentary environment in the sea area since the last glacial times. The research shows that the diatom assemblages coincide with interglacial and glacial times, and changes in diatom abundance reflect the instability of the climate in the southern part of the SCS, such that short-term, temperature descending events correlate with the interglacial interval. The abundance of diatoms is relevant to interglacial and glacial times, since high abundance values were associated with an interglacial interval, and low abundance values with the last glacial maximum. We assume that strong upwelling developed in the interglacial interval, the development of which was influenced by variations of monsoons in the East Asian region.     

鞋楦底部棱边提取与底面展平

鞋楦是制鞋的基准,楦底部棱边在制鞋工艺中具有重要作用。从鞋楦三维面形光电自动测量系统获取的鞋楦三维数据点模型出发,提出了一种基于二阶差分的尖点识别方法,进而获得了鞋楦底部棱边的信息,并在此基础上给出了展平鞋楦底面的方法,得到了鞋楦底面的展平图.手工复楦方法和面积计算方法均表明楦底棱边提取具有较高精度.     

丢番图方程（1＋ck）~r＝（1＋cn）~r

本文证明了当ｎ，ｒ为正整数，ｓ为非负整数，ｃ＝８０ｓ＋９，丢番图方程（１＋ｃｋ）ｒ＝（１＋ｃｎ）ｒ，无整数解     

关于Diophantine方程x~(φ(n))+y~(φ(n))＝z~n

利用初等数论方法,讨论了一类不定方程正整数解的存在性,给出了Diophantine方程x~(φ(n))+y~(φ(n))=z~n是否有正整数解的一个判定准则.     

A high-resolution clay mineralogical record in the northern South China Sea since the Last Glacial Maximum,and its time series provenance analysis

High-resolution clay mineralogical analysis of Core MD05-2904 in the northern South China Sea (SCS) covering the period since the Last Glacial Maximum shows that illite (29%–48%), smectite (14%–45%), chlorite (17%–28%), and minor kaolinite (6%–14%) comprise the clay mineral assemblage, and that time series variation does not present glacial-interglacial cyclicity. Provenance analysis indicates three end-member sources: almost all smectite derives from Luzon, all kaolinite is sourced from the Pearl River, and illite and chlorite originate from both the Pearl River and Taiwan. By comparing clay mineral compositions in surface sediments from the three major source areas and of the SCS, we reconstructed a time series of clay mineral contribution from the major provenances to the northern slope of the SCS using the linear separation method for illite crystallinity. There were three stages of provenance change. (1) During 24.1–17.5 ka BP, contributions from Taiwan and Luzon were similar (30%–40%), while that from the Pearl River was only 25%. (2) During 17.5–14.0 ka BP, the contribution from Luzon decreased rapidly to 20%–25%, while that from Taiwan increased to 35% from an average of 25% at 18 ka BP, and that from the Pearl River increased largely to 40%. (3) During the Holocene, differences in contributions from the three major provenances increased: the contribution from Luzon increased slightly and then remained at 27%–35%, that from Taiwan increased rapidly and then remained at 55%–60%, and that from the Pearl River decreased to 15%. The change in clay mineral contributions from different provenances is influenced mainly by clay mineral production, monsoon rainfall denudation, oceanic current transport, and sea-level change.     

柴油机喷油嘴针阀动态特性的初步研究

柴油机油嘴油槽中的压力变化率可达20～40MPa/ms,因此针阀的启闭过程是一个动态过程。本文建立了针阀上升和下降过程的动态运动方程,并与静力平衡方程作了比较。理论与试验研究证明,针阀动态开启压力明显高于静态,而动态关闭压力又明显低于静态,且与发动机工况有关。针阀的动态落座特性使喷射后期油粒直径变大,喷雾质量变差,并可能危及排放指标及油嘴寿命。     

Vegetation evolution and millennial-scale climatic fluctuations since Last Glacial Maximum in pollen record from northern South China Sea

A large number of paleoclimate records reveal subMilankovitch climatic fluctuations on the millennial-scalesuperimposing on the Earth orbital cycles[1], such as theHeinrich ice draft events in the Atlantic (each intervalabout 7000–10000 a)[2,3], the Dansgaard/Oeschger (D-O)events (millennial-scale) in Greenland Ice Cores and theBond cycle composed of a Heinrcih event after severalD-O events[4]. At present, most recent work on millennial-scale climatic fluctuations focuses on the high lat…     

A continuous 3000—year precipitation record of ENSO variability during LGM from a stalagmite in Nanjing

A glacial stalagmite chronology from Nanjing has been established by the TIMS-U series dating and annual band counting methods. The annually layering sequence spanning the 3000-year period from 18179 to 14900 calendar years before the present (aBP) was analyzed for evidence of East Asian summer monsoon precipitation variability during the Last Glacial Maximum (LGM). Power spectral analysis of the sequence shows a distinct interannual (2—7 years) band of enhanced variability suggestive of El Ni駉-Southern Oscillation (ENSO) teleconnections into East China during the LGM when climatic boundary conditions were different from those of today. The lower frequency bands (4—7 years) variability becomes weaker from 18179 to 14900 aBP, sup-porting the precession forcing model. The reappearance of the ENSO band in the coldest climatic boundary conditions during the Heinrich Event 1, however, suggests the stimula-tion of the enhanced East Asia winter monsoon to the El Ni駉 events.