简介:Outerdensefibersarespecificsubcellularcomponentsofmammalspermflagella,apartfromtheaxonemeanditsassociatedproteins.Asoneoftheouterdensefiberscomponents,ODF3isessentialfortheformationofmammalspermflagella.Inthepresentstudy,weisolatedtheOdf3gene,1033bpinlength,fromZhikongscallopChlamysfarreri,whichwasnamedasCf-Odf3.ItwaspredictedthatCf-Odf3encodesaproteinof240aminoacidswhichcontains5discontinuousPro-Gly-Prorepeats.TheCf-Odf3transcriptsweredetectedinbothtestisandovaryofC.farreriatvariousstagesthroughqRT-PCR.TheCf-ODF3proteinsynthesizedbyprokaryoteswaspurifiedusingNi2+-NTAaffinitychromatographyandusedtoproduceitspolyclonalantibody.TheantibodyproductwaseffectiveandspecificaswasexaminedbyWesternblotting.TheCf-Odf3transcriptandCf-ODF3proteinwerelocatedinintragonadalsomaticcells(ISCs),spermatogoniaandspermatocytesofC.farreritestes,whilenotranscriptionofCf-Odf3andsynthesisofCf-ODF3weredetectedinspermatidsandspermatozoa.ThelocationofOdf3expressionisdifferentfromthatofvertebrateswhereODF3issynthesizedspecificallyinspermatidsandspermflagella.Moreover,theCf-Odf3expressionwasalsodetectedinISCs,oogoniaandoocytesofthescallopovaries.OurfindingrevealedadifferentcharacteristicofOdf3expressionbetweenscallopandvertebrates,whichimpliedthatCf-Odf3playedaroleinthegametogenesisofC.farreri.
简介:利用2013—2015年廊坊市环境监测数据及同期气象资料,采用相关分析等统计方法,分析廊坊市臭氧浓度的日变化特征、超标规律以及气象因素对其的影响。结果表明:臭氧浓度的日变化特征明显,为"1谷1峰"型,每日07:00—08:00左右达到谷值,15:00—16:00达到峰值;臭氧超标只集中出现在春季、夏季与秋季的部分月份,1—3月、11—12月不存在臭氧超标情况,超标现象日变化特征明显,主要出现在11:00—20:00。气象因素对臭氧浓度的影响很大,风向为西南风与东南风时臭氧超标率较高;臭氧超标时,地面天气类型主要为高压后部或高压底部,高空天气类型主要为脊前西北气流或平直西风环流;臭氧浓度与相对湿度呈显著负相关,与温度、日照呈显著正相关。
简介:TheJuly3,2015PishanM_S6.5earthquakeoccurredintheintersectionareaoftheTarimblockandWestKunlunblockwherethemoderate-strongearthquakeshavebecomeactiveinrecentyears.Thispaperhasstudiedtheseismicityparametersoftheearthquakesequencessuchastheb-valueinthePishanregionanditsvicinity.Inaddition,wealsorelocatedtheaftershocksofthePishanM_S6.5earthquakeusingtheseismicphasereportbythedouble-differencemethod.ThetemporalandspatialvariationcharacteristicsofthePishanearthquakesequenceintherupturezoneareanalyzed.Thestudyisofgreatsignificanceintheseismichazardassessmentinthisregion.
简介:边界条件能显著地在强烈地震下面影响斜坡行为。为了为有限元素(FE)评估边界条件的重要性,一张饮料桌子的模拟在斜坡反应上试验,一验证三维(3D)非线性的FE模型被介绍,并且数字、试验性的结果被比较。为那个目的,基于公开源码的计算站台OpenSees,柔韧的图形的用户接口SlopeSAR被采用,它简化努力集中的预处理和processing以后阶段。网孔决定效果也被探讨。参量的研究被执行在在结束脸包含边界程度和边界条件的三种类型的FE模型上评估边界条件的影响。通常,在边界程度的变化生产不一致的斜坡变丑。为二张结束脸,修理y方向排水量不是适当的模仿饮料桌子实验,结束墙在僵硬、不平。另外,3D的长度的影响倾斜最高的脸和处于二之间的差别的一个重要角色在结束边界条件打的斜坡戏的宽度面对(修理y方向排水量并且修理(y,z)方向排水量)。总的来说,这研究加亮对在模拟和试验性的结果之间的比较的评价竟然与到期的考虑被执行到边界的效果,这调节。
简介:Inthispaper,wedeterminedanearthquakesequencelocationintheXingfengjiangareafromJune,2007toJuly,2014andthe3DP-wavevelocitystructurebyasimultaneousinversionmethod.Onthatbasis,westudiedtheoccurrencefeaturesofactivetectonicsandtheearthquakesourcemechanism.Theresultsshowthatthereservoirfracturesystemhasatendencytoincreasewithgradualdepthfromsoutheasttonorthwest,consistentwithgravitationalfieldresearchresults.Thereare4highvelocityzones(HVZ)underthedepthofthe7km-12kmcrustbetweentheXinfengjiangReservoirdamandXichangDistrict,Dongyuan.ThemaxvelocityofthebiggestHVZwhichisunderXichangis6.3km/s.Underthereservoirdamthereisastrongtectonicdeformationzone,asthecenterexitRenzishifault(F2),Nanshan-Aotoufaults(F4),Heyuanfault(F1)andShijiao-Xingang-Baitianfault(F5),7earthquakeswithML≥5.0(includingM6.1inMarch,1962)occurredatthehighgradientzoneoftheHVZⅢandHVZⅣedgewhichhasbeenunderthereservoirdamsince1960,withrelativityenergyreleasingmorethoroughly.ModerateseismicactivityoccurredattheHVZⅠedgewhichhasbeenunderXichangsince2012,andisadangerzoneforM5.0earthquakesinthefuture.
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简介:Consideringtheimportanceofblackcarbon(BC),thisstudybeganbycomparingthe20thcenturysimulationofSouthAsiansummerclimateinIPCCCMIP3,basedonthescenarioofmodelswithandwithoutBC.Generally,themulti-modelmeanofthemodelsthatincludeBCreproducedtheobservedclimaterelativelybetterthanthosethatdidnot.Then,the21stcenturySouthAsiansummerprecipitationwasprojectedbasedontheIPCCCMIP3projectionsimulations.Theprojectedprecipitationinthepresentapproachexhibitedaconsiderabledifferencefromthemultimodelensemblemean(MME)ofIPCCAR4projectionsimulations,andalsofromtheMMEofthemodelsthatignoretheeffectofBC.Inparticular,thepresentprojectionexhibitedadryanomalyoverthecentralIndianPeninsula,sandwichedbetweenwetconditionsonthesouthernandnorthernsidesofPakistanandIndia,ratherthanhomogeneouswetconditionsasseenintheMMEofIPCCAR4.Thus,thespatialpatternofSouthAsiansummerrainfallinthefuturemaybemorecomplicatedthanpreviouslythought.
简介:3D地震波走时计算是偏移、反偏移、层析等诸多地震勘探技术中的重要中间步骤。快速推进法计算3D地震波走时具有高效率、稳定性及适应能力强的特点,但快速推进法在震源附近区域的计算精度不高,降低了整个走时算法的计算精度。本文提出了一种联合3D走时计算方法来解决这一问题。该方法在震源附近小范围内使用计算精度较高的波前构建法计算走时,在剩余区域使用快速推进法计算走时,由于模型中绝大多数网格节点走时是通过快速推进法计算的,故新方法保留了快速推进法高效的特点,同时由于震源附近网格节点走时精度的提高,整个新算法的计算精度相对于快速推进法而言有了较大的改善。文中通过数值分析对上述结论进行了验证并使用三维岩丘模型验证了新方法的稳定性和适应能力。
简介:Thetyphoon,asamaturetropicalcyclonethatdevelopsinthewesternpartoftheNorthPacificOceanwithhighwindspeedandheavyrainfall,isoneofthemostlethalandcostlyofnaturaldisastersforthedenselypopulatedcountriesofEastAsia.Itcanbeeasilydetectedbyspace-bornesensorsoperatedatmicrowave,visibleorinfraredbands(Liuetal.,2014).SyntheticApertureRadar(SAR)is
简介:利用多种常规观测资料和NCEP/NCAR再分析资料,分析了2017年3月1日江苏北部出现的一次罕见冷空气雷雨大风天气过程的发生背景、地面要素和云团演变特征,同时从大气动力、热力和水汽条件出发分析了午后对流的成因。结果表明:此次过程发生前,江苏地区位于高空槽前,对流层中低层有冷式切变线伴随两股冷空气南下,受江苏省北部地面气旋阻挡,冷空气在上游堆积,当气旋东移入海冷空气爆发式南下时,造成严重的大风灾害。此次过程中,对流层中高层大气降温而低层回温使大气温度直减率增大,为对流发生提供不稳定条件,但水汽输送主要集中在低层,且高层大气无明显抽吸作用,导致此次过程未发生强对流性降水,主要以大风灾害性天气为主。
简介:Inthispaper,accordingtotheresultsofthesatelliteimageryinterpretationandfieldinvestigation,westudytheactivefeaturesandthelatestactivetimesoftheChuxiong-Nanhuafault,theQuaternarybasinsformationmechanism,andtherelationshipbetweenthefaultandthe1680ChuxiongMs6%earthquake.SeveralQuaternaryprofilesatLvhe,NanhuarevealthatthefaulthasoffsetthelatePleistocenedepositsoftheT2andT3terracesofLongchuanriver,indicatingthatthefaultwasobviouslyactiveinlateQuaternary,TheChuxiong-NanhuafaulthasbeendominatedbydextralstrikeslipmotioninthelateQuaternary,withanaveragerateof1.6-2.Omm/a.SeveralpullapartQuaternarybasinsofChuxiong,Nanhua,andZiwuetc.havedevelopedalongthefault.The1680ChuxiongMs6%earthquakeandseveralmoderateearthquakeshaveoccurrednearthefault.TheChuxiong-Nanhuafaultaretheseismogenicstructureofthoseearthquakes,thelatestfaultmovementwasinthelate-Pleistocene,andeventheHolocene.Inlargearea,theChuxiong-NanhuafaultandtheeasternQujiangfaultandtheShipingfaultcomposedasetofNW-trendingobliqueorientationactivefaults,andthemotioncharacteristicsareallmainlydextralstrikeslip.Themotioncharacteristics,liketheredriverfaultoftheSichuan-YunnanRhombicBlocksouthwesternboundary,areconcernedwiththeescapingmovementoftheSichuan-YunnanRhombicBlock.
简介:AssimilatingsatelliteradiancesintoNumericalWeatherPrediction(NWP)modelshasbecomeanimportantapproachtoincreasetheaccuracyofnumericalweatherforecasting.Inthisstudy,theassimilationtechniqueschemewasemployedinNOAA’sSTMAS(Space-TimeMultiscaleAnalysisSystem)toassimilateAMSU-Aradiancesdata.Channelselectionsensitivityexperimentswereconductedonassimilatedsatellitedatainthefirstplace.Then,realcaseanalysisofAMSU-Adataassimilationwasperformed.Theanalysisresultsshowedthat,followingassimilatingofAMSU-Achannels5-11inSTMAS,theobjectivefunctionquicklyconverged,andthechannelverticalresponsewasconsistentwiththeAMSU-Aweightingfunctiondistribution,whichsuggeststhatthechannelscanbeusedintheassimilationofsatellitedatainSTMAS.WiththecaseoftheTyphoonMorakotinTaiwanIslandinAugust2009asanexample,experimentsonassimilatedandunassimilatedAMSU-AradiancesdataweredesignedtoanalyzetheimpactoftheassimilationofsatellitedataonSTMAS.TheresultsdemonstratedthatassimilationofAMSU-Adataprovidedmoreaccuratepredictionoftheprecipitationregionandintensity,andespecially,itimprovedthe0-6hprecipitationforecastsignificantly.
简介:针对高分影像阴影检测精度易受水体、偏蓝色地物影响的问题,结合GF-1影像自身特点,提出一种集主成分变换、图像特征计算、逻辑非运算和形态学闭运算于一体的阴影检测方法。对GF-1影像多光谱数据、全色数据进行正射校正和信息融合,可实现光谱与分辨率信息的最大化利用,并最大程度地突出阴影信息,增大阴影与其他地物的差异。其次,建立基于主成分变换的阴影检测方法PC1/NIR和图像特征计算Rg_nir,得到初始阴影信息和水体信息;用初始阴影信息与水体信息作逻辑非运算,剔除水体,并利用形态学闭运算使得阴影区域更加连续、饱满。实验表明,该方法既能准确地检测出GF-1影像中的阴影信息,又能有效削弱水体、偏蓝色等地物的影响。
简介:Modelinggeomechanicalpropertiesofshalestomakesenseoftheircomplexpropertiesisattheforefrontofpetroleumexplorationandexploitationapplicationandhasreceivedmuchresearchattentioninrecentyears.Ashale'skeygeomechanicalpropertieshelptoidentifyits'fracibility'itsfluidflowpatternsandrates,anditsin-placepetroleumresourcesandpotentialcommercialreserves.Themodelsandtheinformationtheyprovide,inturn,enableengineerstodesigndrillingpatterns,fracture-stimulationprogramsandmaterialsselectionthatwillavoidformationdamageandoptimizerecoveryofpetroleum.Awide-rangeoftools,technologies,experimentsandmathematicaltechniquesaredeployedtoachievethis.Characterizingtheinterconnectedfracture,permeabilityandporositynetworkisanessentialstepinunderstandingashaleshighly-anisotropicfeaturesonmultiplescales(nanotomacro).Well-logdata,anditspetrophysicalinterpretationtocalibratemanygeomechanicalmetricstothosemeasuredinrocksamplesbylaboratorytechniquesplaysakeyroleinprovidingaffordabletoolsthatcanbedeployedcost-effectivelyinmultiplewellbores.Likewise,microseismicdatahelpstomatchfracturedensityandpropagationobservedonareservoirscalewithpredictionsfromsimulationsandlaboratorytestsconductedonidealised/simplifieddiscretefracturenetworkmodels.Shalescomplexwettability,adsorptionandwaterimbibitioncharacteristicshaveasignificantinfluenceonpotentialformationdamageduringstimulationandtheshort-termandlongtermflowofpetroleumachievable.Manygasflowmechanismsandmodelsareproposedtakingintoaccountthemultipleflowmechanismsinvolved(e.g.,desorption,diffusion,slippageandviscousflowoperatingatmultipleporositylevelsfromnano-tomacro-scales).Fittinghistoricalproductiondataandwelldeclinecurvestomodelpredictionshelpstoverifywhethermodel'sgeomechanicalassumptionsarerealisticornot.Thisreviewdiscussesthetechniques
简介:柱体的垂直摆动与不同直径比率Dd/Dc和厚度比率td/Dc被3D学习(三维)在这份报纸开发的数字模型,并且通过2D与结果相比获得了(二维)数字模型。高顺序的迎风的计划被使用稳定计算,并且集中被多格子方法加速。2D和3D模拟结果之间的差别的质、量的分析与一个依附底部的磁盘在流动地特征和垂直地震荡的柱体的水动力学系数上揭示3D效果。液体领域上的3D效果主要在三个流旋涡的模式的意义被反映:x相对在2D模拟产生的旋涡在锋利的边附近在流动地上有更大的效果。在沿着轴的取向的片,沿着光线的轴的y比沿着环绕的方向的x,更在速度上显示光线的效果在磁盘的锋利的边附近比环绕的效果读了。旋转相互作用在水平飞机的液体的z在举运动期间是不足道的。基于2D和3D模拟结果,分开增加的集体系数和抑制比率的增加的政体的转弯的点被识别。直径比率Dd/Dc和厚度比率td/Dc详细被讨论。
简介:利用2012年夏季山西省太原、大同、临汾3个温室气体观测站的近地面O_3及相关前体物NOx、NO2、NO、CO观测数据及同期气象观测资料,分析山西省夏季O_3体积分数与污染状况、O_3的时间变化特征及O_3与其前体物体积分数的相关性,同时分析气温、相对湿度、风速、降水和日照时数等气象因素对O_3体积分数的影响。结果表明:山西太原、大同、临汾3个城市的O_3小时体积分数与日最大8h平均体积分数都有超标情况发生,夏季O_3污染以临汾最严重、大同相对最轻;一日内O_3小时体积分数最大值出现在15:00左右,最小值出现在06:00左右,日变化呈单峰型分布,其中临汾O_3小时体积分数的昼夜变化振幅最大、大同最小;各城市NOx、NO2、NO、CO等前体物体积分数均呈现白天低、夜间高的日变化过程,与O_3日变化呈负相关;气温是影响夏季O_3体积分数的最重要因素,其次为相对湿度,风速贡献最小,夏季O_3体积分数高值多在高温低湿的午后,且太原、临汾O_3体积分数受局地气象因素影响比大同显著。
简介:目前,为了贯彻落实绿色发展理念,浅层地温能已经得到了越来越广泛的关注。从国家到地方出台了很多政策、法规支持着这种新型可再生能源的开发利用,其发展前景十分广阔。但各地因地理环境、浅层地温能资源禀赋条件和开发利用方式不同,而呈现较大的差异发展。如何能更好地利用浅层地温能,最大限度地做到资源的高效、节约利用,是我们当前需要解决的重点问题。为此,本文在多年浅层地温能研究与实践工作的基础上,总结经验,创新思路,开创可持续发展道路,提出因地制宜、多能并举的发展模式,以浅层地温能为主,充分结合其他可再生能源的开发利用方式,归纳为“四个结合”,并给出浅层地温能未来发展的几点建议,以供参考和借鉴。