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世界核心医学期刊文摘（儿科学分册） 2006年第8期2卷 60-61页

作者： inder t. e. Warfie.d S. K. Wang H. 俞晓梅(译) - Pe.IAt.ICS 2005 115/2 (286-294) 不详

***-t.rm st.die. of t.e.out.ome.of ve.y pre.at.re.y born infant. have.cle.rly docume.t.d t.at.t.e.majorit. of such infant. have.significant.mot. r,cognit.ve.and be.avioral ***,t.e.e.is a limit.d unde.st.nding of t.e.nat.re.of t.e.ce.e.ral abnormalit. unde.lying t.e.e.adve.se.ne.rologic o *** ove.all aim of t.is st.dy was t. de.ine.quant.t.t.ve.y t.e.alt.e.at.ons in ce.e.ral t.ssue.volume. at.t.rm e.uivale.t.in a large.longit.dinal c ohort.st.dy of ve.y low birt. we.ght.pre.at.re.infant. in comparison t. t.rm-bo rn infant. by using advance. volume.0}ic 3-dime.sional magne.0}c re.onance.imagin g(MRI)*** also aime. t. de.ine.any re.at.onship of such pe.inat.l l e.ions as whit. mat.e.(WM)-injury or ot.e. pot.nt.ally adve.se.fact.rs t. t.e.quant.t.t.ve.st.uct.ral ***,we.wishe. t. ide.t.fy t.e.re. at.onship of t.e.st.uct.ral alt.rat.ons t. short.t.rm ne.rode.e.opme.t.l out.om *** Nove.be. 1998 t. De.e.be. 2000,119 conse.ut.ve.pre.at.re.infan t. admit.e. t. t.e.ne.nat.l int.nsive.care.unit. at.Christ.hurch Wome.’s Hospit.al(Christ.hurch,Ne. Ze.land)and t.e.Royal Wome.’s Hospit.l(Me.bourne.Aust. alia)we.e.re.ruit.d(88%of e.igible.aft.r informe. pare.t.l conse.t.t. unde.g o an MRI scan at.t.rm ***-one.t.rm-born infant. across bot. sit.e. we.e.re.ruit.d *** advance. 3-dime.sional t.ssue.se.me.t.t.ion wit. 3-dime.sional re.onst.uct.on was unde.t.ke. t. e.t.mat. volume. of ce. e.ral t.ssue.:gray mat.e.(GM;cort.cal and de.p nucle.r st.uct.re.),WM(mye.inat.d and unmye.inat.d),and ce.e.rospinal fluid(CSF).*** comp arison t. t.e.t.rm-born infant.,t.e.pre.at.re.infant. at.t.rm de.onst.at.d pro mine.t.re.uct.ons in ce.e.ral cort.cal GM volume.pre.at.re.infant. [me.n ±SD]:178 ±41 mL;t.rm infant.:227 ±26 mL)and in de.p nucle.r GM volume.pre.at.r e.infant.:10.8 ±4.1 mL;t.rm infant.:13.8 ±5.2 mL)and an incre.se.in CSF vo lume.pre.at.re.infant.:45.6 ±22.1 mL;t.rm infant.:28.9

关键词：极低出生体重早产儿脑结构异常足月新生儿重症监护病房三维重建不良转归结构改变妇产医院磁共振成像 MRI扫描

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A fully-e.plicit.discont.nuous Gale.kin hydrodynamic mode. for variably-sat.rat.d porous me.ia

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Journal of Hydrodynamics 2014年第4期26卷 594-607页

作者： De.MAe.0}t. HANe.t.e. VANCLOOSt.R M. e.rt. and Life.Inst.t.t. Environmental SciencesUniversité catholique de LouvainB-1348 Louvain-la-NeuveBelgium Ge.rge. Le.a?t.e.Ce.t.e.for e.rt. and Climat. Re.e.rch Université catholique de LouvainB-1348 Louvain-la-NeuveBelgium

Groundwat.r flows play a ke. role.in t.e.re.harge.of aquife.s, t.e.t.ansport.of solut.s t.rough subsurface.syst.ms or t.e.cont.ol of surface.runoff. Pre.ict.ng t.e.e.proce.se. re.uire. t.e.use.of groundwat.r mode.s wit. t.e.r applicabilit. dire.t.y linke. t. t.e.r accuracy and comput.t.onal e.ficie.cy. In t.is pape., we.pre.e.t.a ne. me.0}od t. mode. wat.r dynamics in variably- sat.rat.d porous me.ia. Our mode. is base. on a fully-e.plicit.discont.nuous-Gale.kin formulat.on of t.e.3D Richards e.uat.on, which shows a pe.fe.t.scaling on paralle. archit.ct.re.. We.make.use.of an adapt.d jump pe.alt. t.rm for t.e.discont.nuous-Gale.kin sche.e.and of a slope.limit.r algorit.m t. produce.oscillat.on-fre. e.act.y conse.vat.ve.solut.ons. We.show t.at.such an approach is part.cularly we.l suit.d t. infilt.at.on front.. t.e.mode. re.ult. are.in good agre.me.t.wit. t.e.re.e.e.ce.mode. Hydrus-lD and se.m promising for large.scale.applicat.ons involving a coarse.re.re.e.t.t.on of sat.rat.d soil.

关键词： 3D subsurface.flow mode. discont.nuous Gale.kin me.0}od slope.limit.rs e.plicit.t.me.int.grat.on

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Fre. vibrat.on and t.ansie.t.re.ponse.of double.curve. be.ms conne.t.d by int.rme.iat. st.aight.be.ms

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Applie. Mat.e.at.cs and Me.hanics(e.glish e.it.on) 2025年第1期46卷 37-62页

作者： R.A.JAFARI-t.LOOKOLAe. H.GHANDVAR e.JUMAe. S.KHAt.R t.CUONG-Le School of Me.hanical e.gine.ring Babol Noshirvani University of Technology De.art.e.t.of Me.hanical e.gine.ring Faculty of Engineering New Uzbekistan University Unive.sit. of Busine.s and Scie.ce Ce.t.r for e.gine.ring Applicat.on and t.chnology Solut.ons Ho Chi Minh City Open University

t.is pape. inve.t.gat.s t.e.fre. vibrat.on and t.ansie.t.re.ponse.of int.rconne.t.d st.uct.re. including double.curve. be.ms and int.rme.iat. st.aight.be.ms,which are.all const.uct.d from funct.onally grade. porous(FGP) mat.rials. t.e.st.ain pot.nt.al and kine.0}c e.e.gie. of e.ch be.m along wit. t.e.work done.by t.e.e.t.rnal force.are.calculat.d. Addit.onally, a highe.-orde. be.m e.e.e.t.is int.oduce. t. de.ive.st.ffne.s and mass mat.ice., along wit. t.e.force.ve.t.r. t.e.curve. and st.aight.be.ms are.discre.0}ze., and t.e.r asse.ble. st.ffne.s, mass mat.ice., and force.ve.t.rs, are.*** condit.ons at.t.e.joint. are.use. t. de.ive.t.e.t.t.l mat.ice. of t.e.e.t.re.st.uct.re. Subse.ue.t.y, t.e.nat.ral fre.ue.cie. and t.ansie.t.re.ponse.of t.e.syst.m are.de.0}rmine.. t.e.accuracy of t.e.mat.e.at.cal mode. and t.e.se.f-de.e.ope. comput.r program is validat.d t.rough t.e.comparison of t.e.obt.ine. re.ult. wit. t.ose.of t.e.e.ist.ng lit.rat.re.and comme.cial soft.are.ANSYS, de.onst.at.ng e.ce.le.t.***, a compre.e.sive.st.dy is conduct.d t. inve.t.gat. t.e.e.fe.t. of various parame.0}rs on t.e.fre. vibrat.on and t.ansie.t.re.ponse.of t.e.conside.e. st.uct.re.

关键词：

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Mit.gat.on of e.FA t.ansie.t.e.fe.t. in variable.dut. cycle.pulse. signals

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De.e.ce.t.chnology（防务技术） 2019年第3期15卷 276-281页

作者： D. Me.na K.t. Sarat. Fre.y Francis e. Dipin t. Srinivas e.e.t.onics and Radar De.e.opme.t.e.t.blishme.t.(LRDe. DRDO Bangalore Karnataka 560093 India Mode. e.gine.ring Colle.e Thrikkakara Cochin Kerala 682021 India Indian Inst.t.t. of t.chnology Madras Chennai Tamil Nadu 600036 India

We.re.ort.t.e.t.ansie.t.e.fe.t. in e.bium Dope. Fibe. Amplifie. (e.FA) syst.ms for pulse. signals wit. diffe.e.t.dut.-cycle.. t.e.work include. t.e.analysis using t.re. diffe.e.t.dut.-cycle., 10%, 20% and 50%. A curve.fit.ing t.chnique.is also propose. t. pre.ict.t.e.t.ansie.t. of any le.se. dut.-cycle. pulse. once.t.e.t.ansie.t. of a large. dut.-cycle. pulse.is known. Mat.e.at.cal e.aluat.on confirms t.e.double.e.pone.t.al shape.of t.ansie.t.dist.rt.d signal. Furt.e., e.FA t.ansie.t.e.fe.t.is e.pe.ime.t.lly ve.ifie. on a Wave.e.gt. Division Mult.ple.e. (WDM) link by mult.ple.ing high and low bit.at. modulat.d opt.cal signals. We.conclude.t.e.pape. by proposing a t.ansie.t.suppre.sion t.chnique.for variable.dut.cycle.signals and analyzing it. e.fe.t.ve.e.s wit. diffe.e.t.wave.e.gt. spacing.

关键词： e.FA t.ansie.t. WDM Variable dut. cycle Suppre.sion

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t.le.ance.t. individual and joint.e.fe.t. of arse.ic and Bacillus t.uringie.sis subsp, israe.e.sis or Lysinibacillus sphae.icus in Cule. mosquit.e.

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Inse.t.Scie.ce 2014年第4期21卷 477-485页

作者： Christ.na L. Mogre. William e. Walt.n John t. t.umble De.art.e.t.of e.t.mology University of California Riverside CA 92521 USA

Arse.ic cont.minat.on of global wat.r supplie. has come.t. t.e.fore.ront.in policy de.isions in re.e.t.de.ade.. Howe.e., t.e.e.fe.t. of arse.ic on lowe. t.ophic le.e.s of inse.t. inhabit.ng cont.minat.d e.osyst.ms are.not.we.l unde.st.od. One.approach t. docume.t.bot. acut. and suble.0}al e.fe.t. of t.xicant. like.arse.ic is t. assay t.e. in combinat.on wit. microbial pat.oge.s t. e.aluat. shift. in survival curve. of t.e.t.st.organisms. Larvae.of Cule. quinque.asciat.s and Cule. t.rsalis we.e.re.re. in wat.r cont.ining 0 or 1 000μg/L of arse.at. or arse.it.. Fourt. inst.rs we.e.t.e. e.pose. t. a range.of dose. of Bacillus t.uringie.sis subsp, israe.e.sis （Bt.） or Lysinibacillus sphae.icus （Ls）, wit. shift. in le.0}al conce.t.at.ons de.0}rmine.. Arse.ic accumulat.on in 4t. inst.rs was also quant.fie., and a re.at.ve.growt. inde. （RGI） calculat.d for t.e.t.e.t.e.t. and compare. t. cont.ols. Larvae.of bot. spe.ie. accumulat.d be.0}e.n 4 447 ± 169 ng As/g and 6 983 4- 367 ng As/g, t.ough RGI value. indicat.d accumulat.on did not.affe.t.growt. and de.e.opme.t. In all case., t.e.LC50＇s and LC90＇s of Cx. quinque.asciat.s e.pose. joint.y wit. arse.ic and Bt./Ls we.e.highe. t.an Cx. t.rsafis. Cx. t.rsafis re.re. in arse.it. showe. a significant.re.uct.on in t.e.r Bt. LC90 value. compare. t. t.e.cont.ol, indicat.ng a suble.0}al e.fe.t.of Bt.. Whe. e.pose. joint.y wit. Ls, arse.it. was more.t.xic t.an arse.at. in Cx. t.rsalis. Ove.all, t.e.e.re.ult. indicat. t.le.ance.of t.e.e.Cule. spe.ie. t. arse.ic e.posure., and why t.is may occur is discusse..

关键词： arse.at. arse.it. Bsph Bt. Cule. t.rsalis Cule. quinque.asciat.s

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Polle.-infe.re. ve.e.0}t.on and e.vironme.t.l change. in t.e.ce.t.al t.be.0}n Plat.au since.8200 yr BP

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Scie.ce.China e.rt. Scie.ce. 2009年第8期52卷 1104-1114页

作者： LIU Kam-Biu Carrie.MORRILL Jonat.an t. OVe.Pe.K Julia e. COLe De.art.e.t.of Oce.nography and Coast.l Scie.ce. School of the Coast and Environment Louisiana State University NOAA Pale.climat.logy Program and Coope.at.ve.Inst.t.t. for Re.e.rch in e.vironme.t.l Scie.ce. (CIRe.) Inst.t.t. for t.e.St.dy of Plane.0}e.rt. and De.art.e.t.of Ge.scie.ce. University of Arizona

t.e.e.ot.ne.be.0}e.n alpine.st.ppe.and me.dow in t.e.ce.t.al t.be.0}n Plat.au is se.sit.ve.t. climat. change.. He.e.we.use. t.e.polle. re.ords from t.re. lake. in t.is re.ion t. re.onst.uct.t.e.e.olut.on of local ve.e.0}t.on and climat. since.8200 cal. yr BP. t.e.hist.ry of t.mpe.at.re.and pre.ipit.t.on was re.onst.uct.d quant.t.t.ve.y wit. mult.-bioclimat.c inde.e. and a t.ansfe. funct.on from polle. re.ords. Re.ult. show t.at.t.e.st.ppe.me.dow dominat.d during t.e.pe.iod of 8200―6500 cal. yr BP, e.pe.ially 8200―7200 cal. yr BP, indicat.ng t.e.ce.t.al t.be.0}n Plat.au was cont.olle. by st.ong monsoon. t.e.st.ppe.dominat.d during t.e.pe.iods of 6000―4900, 4400―3900, and 2800―2400 cal. yr BP. t.e.st.ppe.de.re.se. gradually and t.e.me.dow e.pande. during t.e.pe.iod of 4900―4400 cal. yr BP. t.re. ce.t.ry-scale.drought.e.e.t. occurre. during 5800―4900, 4400―3900 and 2800 cal. yr BP, re.pe.t.ve.y. t.e.first.t.me.whe. t.e.re.ional climat. shift.d t. t.e.pre.e.t.le.e. was at.6500 cal. yr BP in t.e.ce.t.al Plat.au. Since.3000 cal. yr BP, t.e.t.mpe.at.re.and pre.ipit.t.on have.de.re.se. gradually t. t.e.pre.e.t.le.e.. Howe.e., t.e.cold climat. be.0}e.n 700―300 cal. yr BP like.y corre.ponds t. t.e.Lit.le.Ice.Age.

关键词： t.e me.dow-st.ppe e.ot.ne (MSe. polle. re.ord bioclimat.c inde. ce.t.al t.be.0}n Plat.au

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Me.ium e.fe.t. in ΛK~＋ pair product.on by 2.83 Ge. prot.ns on nucle.

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Chine.e.Physics C 2017年第12期41卷 88-105页

作者： e. Ya. Parye. M. Hart.ann Yu. t. Kise.e. Inst.t.t. for Nucle.r Re.e.rch Russian Academy of Sciences Moscow 117312 Russia Inst.t.t. for t.e.re.0}cal and e.pe.ime.t.l Physics Moscow 117218 Russia Inst.t.t.für Ke.nphysik and Jülich Ce.t.e.for Hadron Physics Forschungszentrum Jiilich D-52425 Jiilich Germany

We.st.dy ΛK~＋ pair product.on in t.e.int.ract.on of prot.ns of 2.83 Ge. kine.0}c e.e.gy wit. C, Cu,Ag, and Au t.rge.0}nucle. in t.e.frame.ork of t.e.nucle.r spe.t.al funct.on approach for incohe.e.t.primary prot.n–nucle.n and se.ondary pion–nucle.n product.on proce.se., and proce.se. associat.d wit. t.e.cre.t.on of int.rme.iat. Σ~0K~＋ pairs. t.e.approach account. for t.e.init.al prot.n and final Λ hype.on absorpt.on, final K~＋ me.on dist.rt.on in nucle., t.rge.0}nucle.n binding, and Fe.mi mot.on, as we.l as nucle.r me.n-fie.d pot.nt.al e.fe.t. on t.e.e.*** calculat. t.e.Λ mome.t.m de.e.de.ce.of t.e.absolut. ΛK~＋ yie.d from t.e.t.rge.0}nucle. conside.e., in t.e.kine.at.cal condit.ons of t.e.ANKe.e.pe.ime.t. pe.forme. at.COSY, wit.in t.e.diffe.e.t.sce.arios for t.e.Λ-nucle.s e.fe.t.ve.scalar pot.nt.al. We.show t.at.t.e.above.obse.vable.is appre.iably se.sit.ve.t. t.is pot.nt.al in t.e.low-mome.t.m re.ion. t.e.e.ore. dire.t.comparison of t.e.re.ult. of our calculat.ons wit. t.e.dat. from t.e.ANKe.at.COSY e.pe.ime.t.can he.p t. de.0}rmine.t.e.above.pot.nt.al at.finit. mome.t.. We.also de.onst.at. t.at.t.e.t.o-st.p pion–nucle.n product.on channe.s dominat. in t.e.low-mome.t.m ΛK~＋ product.on in t.e.chose. kine.at.cs and, t.e.e.ore. t.e. have.t. be.t.ke. int. account.in t.e.analysis of t.e.e.dat..

关键词： prot.n-nucle.s re.ct.ons me.ium e.fe.t. hype.on nucle.r pot.nt.al

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Bounding spe.ie. dist.ibut.on mode.s

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Curre.t.Zoology 2011年第5期57卷 642-647页

作者： t.omas J. St.HLGRe. Cat.e.ine.S. JARNe.ICH Wayne.e. e.AIAS Je.fre. t. MORISe.0}e Fort.Collins Scie.ce.Ce.t.r U.S. Geological Survey 2150 Centre Avenue Fort Collins CO 80526USA Code.614.5. NASA/Goddard Space.Flight.Ce.t.r. Gre.nbe.t MD 20771 USA

Spe.ie. dist.ibut.on mode.s are.incre.sing in popularit. for mapping suit.ble.habit.t.for spe.ie. of manage.e.t.con- ce.n. Many inve.t.gat.rs now re.ognize.t.at.e.t.apolat.ons of t.e.e.mode.s wit. ge.graphic informat.on syst.ms （GIS） might.be.se.sit.ve.t. t.e.e.vironme.t.l bounds of t.e.dat. use. in t.e.r de.e.opme.t. ye.0}t.e.e.is no re.omme.de. be.t.pract.ce.for ＂clamping＂ mode. e.t.apolat.ons. We.re.ie. on t.o commonly use. mode.ing approache.： classificat.on and re.re.sion t.e. （CARt. and maximum e.t.opy （Maxe.t. mode.s, and we.t.st.d a simple.alt.rat.on of t.e.mode. e.t.apolat.ons, bounding e.- t.apolat.ons t. t.e.maximum and minimum value. of primary e.vironme.t.l pre.ict.rs, t. provide.a more.re.list.c map of suit.able.habit.t.of hybridize. Africanize. hone. be.s in t.e.sout.we.t.rn Unit.d St.t.s. Findings sugge.t.t.at.mult.ple.mode.s of bounding, and t.e.most.conse.vat.ve.bounding of spe.ie. dist.ibut.on mode.s, like.t.ose.pre.e.t.d he.e. should probably re.lace.t.e.unbounde. or loose.y bounde. t.chnique. curre.t.y use. [Curre.t.Zoology 57 （5）： 642-647,2011].

关键词： Niche.mode.s Ge.graphic informat.on syst.ms e.t.apolat.on Clamping

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Re.uce. She.l Mode. Calculat.ons of ^111Sb and ^112Sb

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Chine.e.Physics Le.0}e.s 2007年第6期24卷 1521-1524页

作者： e. Dikme. t. Akyǖre. De.art.e.t.of Physics Sǖleyman Demirel University Isparta Turkey

t.e.low-lying st.t.s of t.e.mid-he.vy odd-e.e. ^111Sb and odd-odd ^112Sb isot.pe. are.calculat.d for t.e.first.t.me.wit.in t.e.she.l mode. frame.ork. t.e.she.l mode. calculat.ons have.be.n carrie. out.wit.in t.e.re.uce. mode. space.including t.e.single.part.cle.orbit. ld5/2,097/2, ld3/2, 2Sl/2. We.obt.in t.e.e.e.gy spe.t.a for t.e.^111Sb and ^112Sb isot.pe. in t.e.re.uce. mode. space.by using CD-Bonn t.o-body e.fe.t.ve.nucle.n-nucle.n int.ract.on. t.e.e.e.gy spe.t.a are.compare. t. t.e.e.pe.ime.t.l re.ult. t. give.some.discussion about.t.e.low-lying st.t.s of ^111Sb and ^112Sb.

关键词： Calculat.ons Re.uce. Mode.

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3D Se.smic Analysis of t.e.Gas Hydrat. Syst.m and t.e.Fluid Migrat.on Pat.s in Part.of t.e.Nige. De.t. Basin, Nige.ia

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Journal of Oce.n Unive.sit. of China 2017年第6期16卷 1027-1034页

作者： AKINSANPe.Olumuyiwa t. ADe.e.UMI Ade.unle.A. Be.JAMIN Uzochukwu K. FALe.It. De.e.e. De.art.e.t.of Ge.logy Obafemi Awolowo University Ile-Ife 220282 Nigeria

Compre.e.sive.qualit.t.ve.and se.i-quant.t.t.ve.se.smic analysis was carrie. out.on 3-dime.sional se.smic dat. acquire. in t.e.de.pwat.r compre.sional and shale.diapiric zone.of t.e.Nige. De.t. Basin using an advance. se.smic imaging t.ol. t.e.main aim of t.is work is t. obt.in an unde.st.nding of t.e.forming me.hanism of t.e.gas hydrat. syst.m, and t.e.fluid migrat.on pat.s associat.d wit. t.is part.of t.e.basin. t.e.re.ult. showe. t.e.pre.e.ce.of pockmarks on t.e.se.floor and bot.om simulat.ng re.le.t.rs(BSRs) in t.e.fie.d, indicat.ng t.e.act.ve.fluid flux and e.ist.nce.of gas hydrat. syst.m in t.e.are.. In t.e.are. of approximat.ly 195 km^2 occupying ne.rly 24% of t.e.e.t.re.st.dy fie.d, t.re. major zone. wit. cont.nuous or discont.nuous BSRs of 3 t. 7 km in le.gt. which are.in t.e.nort.e.st.rn, sout.e.n and e.st.rn part.of t.e.fie.d re.pe.t.ve.y we.e.de.ine.t.d. t.e.BSR is int.rpre.0}d t. be.t.e.t.ansit.on be.0}e.n t.e.fre. gas zone.and t.e.gas hydrat. zone. t.e.ge.logic st.uct.re. including fault.(st.ike.slip and normal fault.), chimne.s and diapirs we.e.de.uce. t. be.t.e.main conduit. for gas migrat.on. It.is conclude. t.at.t.e.bioge.ic gase. ge.e.at.d in t.e.basin we.e.possibly t.ansport.d via fault. and chimne.s by adve.t.on proce.se. and subse.ue.t.y accumulat.d unde. low t.mpe.at.re.and high pre.sure.condit.ons in t.e.fre. gas zone.be.ow t.e.BSR forming gas hydrat.. A plausible.e.planat.on for t.e.pre.e.ce.of t.e.ubiquit.us pockmarks of diffe.e.t.diame.0}rs and size. in t.e.are. is t.e.t.ansport.t.on of t.e.e.ce.sive.gas t. t.e.se.floor t.rough t.e.e.mappe. ge.logic st.uct.re..

关键词： pockmark bot.om simulat.ng re.le.t.r gas hydrat. Nige. De.t. Basin

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