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Two.special to.ics o. the avian influenza virus and o. epigenetics,have drawn much attentio.

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Science china(Life sciences) 2010年第12期53卷 1483-1484页

作者： HU Yo.gLin institute o. Bio.hysics,chinese academy o. sciences,beijing 100101,china institute o. Bio.hysics Chinese Academy of Sciences Beijing China

Several excellent well-o.ganized reviews and research papers o. two.special to.ics, "The challenges o. avian influenza virus: mechanism, epidemio.o.y, and co.tro." and "Mo.ecular

关键词： APo.EC gene Two.special to.ics o. the avian influenza virus and o. epigenetics,have drawn much attentio.

Geo.hemical characteristics o. rare earth elements in Wuhan sectio. o. the Yangtze River

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Jo.rnal o. Enviro.mental sciences 1995年第1期7卷 44-51页

作者： Wang Lijun Zhang Shen Zhang Chao.heng(institute o. Geo.raphy,chinese academy o. sciences,beijing 100101,china)Li Xiuxia(institute o. High Energy Physics,chinese academy o. sciences,beijing 100080,china) Inst o. Geo. Chinese Academy of Sciences Beijing China China

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关键词： geo.hemical characteristics rare earth elements Yangtze River

Reco.structio. o. temperature series in china fo. the last 5000 years

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Pro.ress in Natural Science:Materials Internatio.al 2006年第8期16卷 838-845页

作者： GE Quansheng, WANG Shunbing and ZHENG Jingyun (institute o. Geo.raphical sciences and Natural Reso.rces Research, chinese academy o. sciences, beijing 100101, china Graduate Scho.l o. the chinese academy o. sciences, beijing 100039, china) institute o. Geo.raphical sciences and Natural Reso.rces Research Chinese Academy of Sciences Beijing 100101 China Graduate Scho.l o. the chinese academy o. sciences Beijing 100039 China

A temperature series with a 100 year reso.utio. fo. the last 5000 years in china has been reco.structed by using 31 lo.gterm temperature pro.y series selected fro. recent publicatio.s in the last 20 years. The pro.y reco.ds include po.lens, stalagmites, lake-sediments, peat, ice co.es and histo.ical do.uments. The result reveals that in the millennial scale temperature variatio. it was warm in 3050-250 BC and it was co.d in 250 BC-1950 AD. In the abo.e two.perio.s there were many stages o. sub-scale temperature fluctuatio.s. The result also.sho.s an o.vio.s temperature discrepancy o. the century to.multi-century scale between the Eastern Mo.so.n Regio., the Qinghai-Tibet Regio. and the No.thwestern Regio. in 2850 BC, 2350 BC, 1350 BC, 950-350 BC, 50-250 AD, and 550 AD. A co.pariso. between the reco.structed series o. this paper and so.e No.th Hemisphere temperature series indicates that in the lo.gterm scale change, the temperature change in china is in phrase with that o. the No.thern Hemisphere during the last 5000 years, while o. the century to.multi-century scale there are differences at the beginning and end times, which may imply that temperature change do.s no. o.cur simultaneo.sly in different regio.s.

关键词： temperature series the last 5000 years china.

Mo.ELLING AND NUMERICAL So.UTIo.S o. A GAUGE PERIo.IC TIME DEPENDENT GINZBURG-LANDAU Mo.EL Fo. TYPE-Ⅱ SUPERCo.DUCTo.S

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Jo.rnal o. Co.putatio.al Mathematics 1997年第4期15卷 365-384页

作者： Zhi-ming Chen (institute o. Mathematics, chinese academy o. sciences, beijing, china) 中科院数学所北京

In this paper we seek the so.utio.s o. the time dependent Ginzburg-Landau mo.el fo. type-Ⅱ superco.ducto.s such that the asso.iated physical o.servables are spatially perio.ic with respect to.so.e lattice who.e basic lattice cell is no. necessarily rectangular. After appro.riately fo.ing the gange, the mo.el can be fo.mulated as a system o. no.linear parabo.ic partial differential equatio.s with quasi-perio.ic bo.ndary co.ditio.s. We first give so.e results co.cerning the existence, uniqueness and regularity o. so.utio.s and then we pro.o.e a semiimplicit finite element scheme so.ving the system o. no.linear partial dmerential equatio.s and sho. the o.timal erro. estimates bo.h in the L2 and energy *** also.repo.t o. so.e numerical results at the end o. the paper.

关键词： Math QT Mo.ELLING AND NUMERICAL So.UTIo.S o. A GAUGE PERIo.IC TIME DEPENDENT GINZBURG-LANDAU Mo.EL Fo. TYPE SUPERCo.DUCTo.S

High Thro.ghput SNP Geno.yping with Two.Mini-sequencing Assays

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Acta Bio.himica et Bio.hysica Sinica 2004年第6期36卷 379-384页

作者： Chunqing LUo.,2#, Libin DENG1#, and Changqing ZENG1,2* The institute o. Genetic and Develo.mental Bio.o.y, the chinese academy o. sciences, beijing 100101, china 2beijing Geno.ics institute, the chinese academy o. sciences, beijing 101300, china The institute o. Genetic and Develo.mental Bio.o.y the Chinese Academy of SciencesBeijing 100101 China beijing Geno.ics institute the Chinese Academy of SciencesBeijing 101300 China

Two.mini-sequencing metho.s, FP-TDI (template-directed dye-terminato. inco.po.atio. with fluo.escence-po.arizatio.) and MassArray (matrix assisted laser deso.ptio. io.izatio. time o. flight detectio. mass spectro.etry), were o.timized. A numeric standard was intro.uced to.evaluate the SNP sco.ing quality o. FP-TDI assay, thus made the o.timizatio. wo.k easier. At the same time, using multi-PCR techno.o.y, 8-plex geno.yping o. MassArray assay was successfully carried o.t, so.e so.twares were develo.ed and the data pro.ess o. MassArray was highly auto.ated. Then these two.metho.s were applied to. high thro.ghput SNP geno.yping, the accuracy, efficiency and ro.ustness were co.pared. The result sho.s FP-TDI is mo.e sensitive to.the co.centratio. o. SNPprimer and PCR pro.uct, as well as extensio. cycles, the SNPprimer length o. FP-TDI sho.ld be 24–30 bp lo.g, whereas MassArray assay prefers to.be as sho.t as o.ly 16 *** 6440 SNP sites o. human chro.o.o.e 3 were geno.yped in a sample o. 90 individuals, 4792 sites by FP-TDI assay and 1648 sites by MassArray assay, the success rates o. FP-TDI and MassArray were 67.7% and 93.6% respectively. The thro.ghput o. MassArray was higher than FP-TDI, and the co.t o. MassArray was lo.er, MassArray was mo.e suitable fo. high thro.ghput SNP geno.yping.

关键词： SNP geno.yping FP-TDI MassArray high thro.ghput

Trend o. urban system structure under the restrictio. o. water and land reso.rces in Xinjiang

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chinese Science Bulletin 2006年第A1期51卷 179-188页

作者： ZHANG Xiao.ei & LEIJun Xinjiang institute o. Eco.o.y and Geo.raphy, chinese academy o. sciences, Urumqi 830011, china institute o. Geo.raphical Science and Natural Reso.rces Research, chinese academy o. sciences, beijing 100101, china Graduate Scho.l, chinese academy o. sciences, beijing 100039, china Xinjiang institute o. Eco.o.y and Geo.raphy Chinese Academy of Sciences Urumqi China institute o. Geo.raphical Science and Natural Reso.rces Research Chinese Academy of Sciences Beijing China Graduate Scho.l Chinese Academy of Sciences Beijing China

根据在 Xinjiang 影响城市的开发和城市的系统结构的水和陆地资源上的研究，这篇论文分析利用地位和城市的水资源的缺乏。城市的水资源的消费和浪费在一个增加趋势，这被考虑。然而，在 Xinjiang 的大多数城市和镇在水资源的缺乏水资源... 详细信息

根据在 Xinjiang 影响城市的开发和城市的系统结构的水和陆地资源上的研究，这篇论文分析利用地位和城市的水资源的缺乏。城市的水资源的消费和浪费在一个增加趋势，这被考虑。然而，在 Xinjiang 的大多数城市和镇在水资源的缺乏水资源的废物是严肃的，特别在小镇上。megapo.is 和中等城市的发展被有限陆地资源显然限制。尽管有扩展小城市和镇的相对大的空格，水和陆地资源的输出好处是低的。为了完成城市的系统的顺序的扩大，在 Xinjiang 组织，在都市化的快速的发展拿一个圆和三条带和节俭资源的策略的城市的空间发展模式被建议。

关键词：城镇体系结构水资源土地资源供水能力新疆

Co.PLICATED FILL-SCo.RBEHAVIo.S o. THE YELLo. RIVER ANDTHE CHANNEL-Fo.MING PRo.ESSES

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Internatio.al Jo.rnal o. Sediment Research 1999年第2期14卷 259-266页

作者： XU Jio.gXin (1 institute o. Geo.raphy, chinese academy o. sciences, beijing 100101, china)

Based o. the data fro. 159 events at the To.gguan statio. o. the Yello. River, we have fo.nd the rule to.describe the co.plicated relatio.ship between the fill-sco.r features and the event-maximum suspended co.centratio. (C_max). The depth o. sco.r is large if the C_max is lo.. and is small if C_max is high. Ho.ever, if C_max increases to.the ranges o. hyperco.centrated flo.s, sco.r o.curs again. Co.tro.led by the fo.ego.ng co.plicated fill-sco.r behavio.s, the channel adjustment o. the Yello. River is also.co.plicated. When the suspended co.centratio. is lo., channel sco.r o.curs, and thereby the channel shape tends to.be narro.er and deeper, and the thalweg mo.e sinuo.s. When the suspended co.centratio. increases, channel fill o.curs, leading to.an increase in the channel width-depth ratio.and a decrease in the channel sinuo.ity. Ho.ever, when the suspended co.centratio. further increases and exceeds a certain thresho.d, channel sco.r o.curs again, and the adjustment o. channel mo.pho.o.y turns to.the o.po.ite directio.. The rules o.tlined in the paper fo. the channel adjustment o. the lo.er Yello. River may pro.ide a new thinking fo. the regulatio. o. the channel mo.pho.o.y o. the lo.er Yello. River after the clo.ure o. the Xiao.angdi Dam, thro.gh the regulatio. o. the lo.er Yello. River’s water and sediment by cho.sing so.e specific o.eratio. mo.es o. the reservo.r Either by releasing clear water o. by releasing man-made hyperco.centrated flo.s, the do.nstream channel may tend to.be narro.ed, deeper and mo.e sinuo.s.

关键词： Channel adjustment Fill-sco.r behavio. Hyperco.centrated flo.s Lo.er Yello. River

VARIATIo. o. SEDIMENT YIELD AS RIVER BASIN AREAIN THE MIDDLE YELLo. RIVER BASIN

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Internatio.al Jo.rnal o. Sediment Research 1999年第2期14卷 333-337页

作者： LU Jinfa (institute o. Geo.raphy, chinese academy o. sciences, beijing, 100101,china)

Bo.h decrease and increase o. sediment yield were o.served in main tributaries basins o. the Middle Yello. River as basin area increases. Bio.climatic and mo.pho.o.ic features exert mo.t impo.tant co.tro. o. the relatio.ship between specific sediment yield and drainage basin area. Sediment yield data fro. vario.s enviro.ments sho. different trends o. variatio. in sediment yield fo. lo.ss. ro.k and ro.k/lo.ss mixed regio.s.

关键词： Sediment yield Basin area Yello. River

Co.pariso. o. flo. shear stress and energy expenditure between sand-and gravel-bed rivers and so.e geo.o.pho.o.ical implicatio.s

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chinese Science Bulletin 1999年第13期44卷 1224-1228页

作者： XU Jio.gxininstitute o. Geo.raphy, chinese academy o. sciences , beijing 100101, china institute o. Geo.raphy Chinese Academy of Sciences Beijing China

Based o. data fro. mo.e than 100 alluvial rivers, a systematic co.pariso. o. flo. shear stress and energy expenditure has been made between sand- and gravel-bed rivers, by plo.ting the relatio.ships between channel shape (i.e. channel width-depth ratio. and hydraulic indices in a two.dimensio.al plane. These relatio.ships sho. clearly that the fo.r channel patterns, i.e. sand-bed meandering, sand-bed braided, gravel-bed meandering and gravel-bed braided, are lo.ated in 4 different areas that can be divided by 2 straight lines.

关键词： sand-bed river gravel-bed river channel pattern channel pattern discriminatio..