简介：国家林业和草原局，中国地质调查局，各司局，各单位：2018年8月18日，中共中央印发了新修订的《中国共产党纪律处分条例》（以下简称《条例》），这是党的十八大以来党中央对《条例》的第二次修订，进一步表明了用铁的纪律管全党治全党的坚定信心和决心，为推动全面从严治党向纵深发展提供了坚强纪律保证。

简介：牡丹江市国土资源局为深入学习贯彻习近平总书记在深入推进东北振兴座谈会上的重要讲话精神和考察黑龙江时的重要指示精神,近日,牡丹江市国土资源局开展了“学讲话、找短板、定任务、强保障”系列活动。9月28日,该局组织干部职工收看了习近平总书记到我省考察的新闻,随后,陆续开展了理论中心组学习、支部党员学习、报告会、讲党课、撰写学习心得等活动,把党员干部职工的思想统一到习总书记重要讲话精神上来,把行动统一到党中央关于东北振兴的决策部署上来。

简介：鹤岗市国土资源局为深入贯彻落实省厅解放思想推动高质量发展大讨论动员宣讲视频会议精神,近日,鹤岗市国土资源局党组召开动员会议,专题传达学习习近平总书记在深入推进东北振兴座谈会上的重要讲话和考察黑龙江的重要指示情神,对全系统开展解放思想推动高质量发展大讨论做出具体安排,动员系统上下统一思想、凝聚共识,高质量高标准抓好起步开局。

简介：民间信仰祠神是人们内心精神需求的外化，信众群体及相应的社会空间与地方祠神构成了相互依存、相互影响的辩证关系，是以祠神为标志和纽带的地方认同得以培育和维系的基础．本研究将宁波地区鄞县、慈溪、镇海、奉化、象山、定海6县方志中记载的与海洋相关的祠神进行统计，分析海神信仰作为宁波沿海地方标志及其与在区域历史时期社会经济活动和人群融合的关系．本研究认为，民间祠神的“功能”是推动民间祠神传播扩散的主要力量之一，并且是连结迁移人群和本土居民共同心理诉求和维系地方认同的重要纽带．

简介：［1］AnZS,WeiLY,LuYC,1985,ApreliminarystudyofsoilstratigraphyinLuochuanloessprofile.QuaternarySciences,6(1):166-173.(inChinese)［2］AnZS,KutzbacchJE,PrellWLetal.,2001.EvolutionofAsianmonsoonsandphasedupliftoftheHimalaya-TibetanplateausinceLateMiocenetimes.Nature,411:62-66.［3］BarbaraAM,1995.PalaeorainfallreconstructionsfrompedogenicmagneticsusceptibilityvariationintheChineseloessandpalaeosol.QuaternaryResearch,44(3):383-391.［4］DerbyshireE,MengXM,KempRA,1998.Provenance,transportandcharacteristicsofmodemaeoliandustinwesternGansuProvince,China,andinterpretationoftheQuaternaryloessrecord.JournalofAridEnvironments,39:497-516.［5］DingZL,LiuDS,LiuXMetal.,1989.37cyclessince2.5Ma.ChineseScienceBulletin,34(19):1494-1496.［6］DingZL,RutterNW,SunJMetal.,2000.Re-arrangementofatmosphericcirculationatabout2.6MaovernorthernChina:evidencefromgrainsizerecordsofloess-palaeosolandredclaysequences.QuaternaryScienceReviews,19:547-558.［7］DuJ,ZhaoJB,2004.SoilerosionregularitysinceHoloceneinShaolingtablelandofChang′an.JournalofDesertResearch,24(1):63-67.(inChinese)［8］FengZD,WangHB,OlsonCetal.,2004.Chronolgicaldiscordbetweenthelastinterglacialpaleosol(S1)anditsparentmaterialintheChineseLoessPlateau.QuaternaryInternational,117:17-26.［9］GuoZT,LiuDS,FedoroffNetal.,1998.ClimateextremesinloessofChinacoupledwiththestrengthofdeep-waterformationintheNorthAtlantic.GlobalandPlanetaryChange,18:113-128.［10］GuoZT,WillamFRuddiman,HaoQZetal.,2002.OnsetofAsiandesertificationby22MyragoinferredfromloessdepositsinChina.Nature,416:159-163.［11］HeinrichH,1988.OriginandconsequenceofcycliciceraftinginthenortheastAtlanticOceanduringpast130000years.QuaternaryResearch,29:142-152.［12］KempRA,DerbyshireE,

简介：Glacierinventorycompilationduringthepast20yearsandmodificationsofthatfortheEasternPamirandBanggongLakeindicatethatthereare46,342modernglacierswithatotalareaandvolumeof59415km2and5601km3respectivelyinChina.Theseglacierscanbeclassifiedintomaritimeandcontinental(includingsub-continentalandextremelycontinental)types.ResearchesshowthatglaciersinChinahavebeenretreatingsincetheLittleIceAgeandthemasswastagewasacceleratedduringthepast30to40years.BeinganimportantpartofglaciologicalstudiesinChina,icecoreclimaticandenvironmentalstudiesonTibetanPlateauandintheAntarcticahaveprovidedabundant,highresolutioninformationaboutpastclimaticandenvironmentalevolutionovertheTibetanPlateauandAntarctica.ExceptfordifferentparametersrecordedinicecoresrelatingtoclimateandenvironmentchangesonTibetanPlateau,recordsfromicecoresextractedfromdifferentglaciersshowthatthediscrepanciesinclimaticandenvironmentalchangesonthenorthandsouthpartsoftheplateaumaybetheconsequenceofdifferentinfluencingeffectsfromterrestrialandsolarsources.GlaciologicalandmeteorologicalphenomenaimplythatLambertGlaciervalleyisanimportantboundaryofclimateintheeastAntarctica,whichisthoughttobeconnectedwithcyclonicactivitiesandCircum-polarWavesovertheAntarctica.

简介：PermafrostinChinaincludeshighlatitudepermafrostinnortheasternChina,alpinepermafrostinnorthwesternChinaandhighplateaupermafrostontheTibetanPlateau.Thehighaltitudepermafrostisabout92%ofthetotalpermafrostareainChina.Thesouthboundaryorlowerlimitoftheseasonallyfrozengroundisdefinedinaccordancewiththe0℃isothermallineofmeanairtemperatureinJanuary,whichisroughlycorrespondingtothelineextendingfromtheQinlingMountainstotheHuaiheRiverintheeastandtothesoutheastboundaryoftheTibetanPlateauinthewest.SeasonalfrozengroundoccursinlargepartsoftheterritoryinnorthernChina,includingNortheast,North,NorthwestChinaandtheTibetanPlateauexceptforpermafrostregions,andaccountingforabout55%ofthelandareaofChina.Thesouthernlimitofshort-termfrozengroundgenerallyswingssouthandnorthalongthe25°northernlatitudeline,occurringinthewetandwarmsubtropicmonsoonclimaticzone.Itsareaislessthan20%ofthelandareaofChina.

简介：为深入贯彻落实党的十九大和省委十二届二次全会精神,引导广大党员干部在建设现代化新龙江中发挥好先锋模范作用,10月11日,省国土资源厅开展了“新时代、新作为、新风采——做新时代不懈奋斗者”主题党日活动。

简介：本文阐述了中国亚热带的6个基本特点，亚热带北界和南界的划分问题，生态过渡带和亚热带划分的方法论，综合区划研究的必要性与重要性，以及尚需深入研究的若干重要自然地理界线问题．认为中国的亚热带从广义上说也是一个生态过渡带．深入研究中国亚热带形成的机制及其成因和演变趋势，将有利于整个亚热带的区域可持续发展．目前亚热带划分所用的指标比较初始、简略，亚热带的东部与西部所采用的指标也不完全一致，还需要经过艰苦的探索，提出一个既能反映客观实际，又能与国际研究接轨的较好方案．在亚热带的划分中需要加强新技术和新方法的应用．

简介：据首次全国湿地资源调查统计,我国湿地资源十分丰富,总面积为3848.55×104hm2,湿地陆生野生动物共25目、75科、724种,野生高等植物有225科815属2276种,划分为7个植被型组,16个植被型,180个群系.我国湿地正面临着来自人类的巨大威胁,如人类对湿地的盲目围垦和改造、湿地环境污染、生物资源的过度利用等,导致自然湿地数量持续减少、湿地生态功能退化乃至丧失,已难以保证所在地域生态平衡的需求.根据我国湿地面临的威胁和问题,近期应加强湿地保护立法和管理机构建设,并尽快实施.

简介：［1］BrownL,1995.WhoWillFeedChina:Wake-upCallforaSmallPlanet.TheWorldWatchEnvironmentalAlertSeries.NortonandCo.,NewYork,USA.［2］CaiYunlong,1990.Land.In:ZuoDakang(eds.),ADictionaryofModernGeography.Beijing:TheCommercialPress,ppl11.(inChinese)［3］CaoM,MaS,HanC,1995.Potentialproductivityandhumancarryingcapacityofanagro-ecosystem:ananalysisoffoodproductionpotentialofChina.AgriculturalSystems,47:387-414.［4］ChenLiding,WangJun,FuBojieetal.,2001.Land-usechangeinasmallcatchmentofnorthernLoessPlateau,China.Agriculture,Ecosystems&Environment,86(2):163-172.［5］DaiFC,LeeCF,ZhangXH,2003.GIS-basedgeo-environmentalevaluationforurbanland-useplanning:acasestudy.EngineeringGeology,61(4):257-271.［6］DingChengri,2003.LandpolicyreforminChina:assessmentandprospects.LandUsePolicy,20:109-120.［7］FuBojie,WangJun,ChenLidingetal.,2003a.TheeffectsoflanduseonsoilmoisturevariationintheDanangoucatchmentoftheLoessPlateau,China.Catena,54:197-213.［8］FuCongbin,2003b.Potentialimpactsofhuman-inducedlandcoverchangeonEastAsiamonsoon.GlobalandPlanetaryChange,37(3-4):219-229.［9］FischerG,SunLaixiang,2001.Modelbasedanalysisoffutureland-usedevelopmentinChina.Agriculture,Ecosystems&Environment,85(1-3):163-176.［10］GuoXiaomin,NiuDekuietal.,2000.TheexplorationofdevelopingfruitindustrymodewithsoilandwaterconservationinsouthJiangxiarea.ResearchofSoilandWaterConservation,7(3):187-218.(inChinese)［11］HeXiubin,LiZhanbin,HaoMingdeetal.,2003.Down-scaleanalysisforwaterscarcityinresponsetosoil-waterconservationonLoessPlateauofChina.Agriculture,EcosystemsandEnvironment,94:355-361.［12］HeiligGK,1999.CanChinafeeditself?Asystemforevaluationofpolicyoptions.ScienceforGlobalInsight,IIASA,Laxenburg(CD-ROMVers.1.1).［13］HuWei,1997.HouseholdlandtenurereforminChina:itsim

简介：城市湿地公园是生态型城市建设中城市绿地系统和城市水系统的重要组成部分,已引起全社会的普遍重视,并获得广泛发展,尤其在华东地区发展势头较快,但是,指导中国城市湿地公园建设与保护的基础理论研究还比较缺乏。因此,通过统计分析中国城市湿地公园的地理布局特征、发展现状,综合分析了近年来对城市湿地公园的研究视角与最新进展。针对城市湿地公园发展中存在的问题,指出城市湿地公园未来主要的研究方向和内容。

简介：Sandydesertificationislanddegradationcharacterizedbywinderosionmainlyresultedfromtheexcessivehumanactivitiesinarid,semiaridandpartofsub-humidregionsinnorthernChina.Theresearchonsandydesertificationhasexperiencedmorethan5decadesofarduouscourseofthestrugglealongwiththeestablishmentanddevelopmentofChina′sdesertscience.Researchesinthisfieldhavemadeagreatcontributiontothenationaleconomicconstruction,andenvironmentalprotection.Thispaperfocusesonpresentingthemajorprogressandachievementsinthesandydesertificationresearchduringthelast50years,includingthestagesofstudyonsandydesertification,backgroundenvironmentofsandydesertificationanditschanges,theconception,causes,process,monitoringandassessmentofsandydesertification,thevegetationsuccession,landscapeecology,plantphysiology,impactsonecosystem,high-effectiveuseofwaterandlandresourcesandsustainabledevelopmentinsandydesertifiedregions,sandydesertificationcontrolmodelsandtechniquesetc.

简介：人类对自然界的认识过程总是由浅入深循序渐进的。回顾过去，中国黄土成因经历了从“水成”到“风成”这样一个曲折的认识过程。通过分析黄土成因争论的历程，得到如下启示：1）过去的黄土成因争论源于人们不认识黄土层中的古土壤，因此识别地层中古土壤对重建古地理环境具有重大意义。2）水平层状地层并非都是水平沉积层理，也有可能是古土壤发生层次，具有水平层理的沉积地层则可能意味着在水中沉积形成，而古土壤层则是在地表环境形成。3）古土壤层的特点是古土壤层具有土壤发生层次，因此各层次之间一般呈现为渐变特征。而沉积地层通常具有明显的顶部和底部，显示着截然变化。4）在总结新生代古土壤特点的基础上，重新认识更老地层的古地理环境，发挥古土壤在研究地层成因、重建古气候等方面的作用。

简介：AstochasticmodelfordailyprecipitationsimulationinChinawasdevelopedbasedontheframeworkofa′Richardson-type′weathergeneratorthatisanimportanttoolinstudyingimpactsofweather/climateonavarietyofsystemsincludingecosystemandriskassessment.ThepurposeofthisworkistodevelopaweathergeneratorforapplicationsinChina.Thefocusisonprecipitationsimulationsincedeterminationofotherweathervariablessuchastemperatureisdependentonprecipitationsimulation.AframeworkoffirstorderMarkovChainwithGammaDistributionfordailyprecipitationisadoptedinthiswork.Basedonthisframework,fourparametersofprecipitationsimulationforeachmonthat672stationsalloverChinaweredeterminedusingdailyprecipitationdatafrom1961to2000.Comparedwithpreviousworks,ourestimationfortheparameterswasmadeformorestationsandlongerobservations,whichmakestheweathergeneratormoreapplicableandreliable.Spatialdistributionsofthefourparametersareanalyzedinaregionalclimatecontext.Theseasonalvariationsoftheseparametersatfivestationsrepresentingregionaldifferencesarediscussed.Basedontheestimatedmonthlyparametersat672stations,dailyprecipitationsforanyperiodcanbesimulated.A30-yearsimulationwasmadeandcomparedwithobservationsduring1971-2000intermsofannualandmonthlystatistics.Theresultsaresatisfactory,whichdemonstratestheusefulnessoftheweathergenerator.

简介：9月26日，中国第9次北极科学考察队圆满完成历时69天的考察，乘坐“雪龙”号科考船顺利返回上海。这是自然资源部成立后组织实施的首次极地考察，也是完善北极观测网、开展北极业务化观测与监测的重要航次。

简介：本研究通过收集国内已发表的文献中具有凋落物分解常数的数据，采用SPSS13．0软件综合分析中国森林凋落物分解速率的影响因素．结果发现：凋落物类型对凋落物分解速率有显著影响（P〈0．05），凋落叶氮含量与分解速率呈极显著正相关（P〈0．01）．在同一样地的研究中，混合分解的凋落叶分解常数极显著高于单独分解的（P〈0．01）．叶习性对凋落叶分解速率没有显著影响（P〉0．05），但在中国的温带地区则有显著影响（P〈0．05）．在全国尺度上树种组成对凋落物分解速率没有显著影响（P〉0．05）．凋落叶分解速率与经度、年均温和降水量成极显著正相关（P〈0．01），与纬度和海拔成极显著负相关（P〈0．01）．凋落叶分解速率的Q10值为1．768．网袋孔径与土壤类型对凋落叶分解速率亦均有极显著影响（P〈0．01）．

简介：湿地退化、恢复和重建是当前湿地科学领域的研究热点，也是中国湿地研究中的核心问题。作为一种典型的海岸湿地，河口湿地在围垦、水利工程建设和环境污染等多重因素的干扰下，面临着自然来水减少、水盐失衡、植被退化、生境质量下降等多种威胁。介绍了当前中国河口湿地的分布情况以及四大主要河口湿地的退化现状，针对已经开展的河口退化湿地恢复的现状，总结了目前中国河口退化湿地恢复所面临的问题，并展望了今后河口退化湿地恢复研究的趋势：开展河口湿地生态系统演替与退化机制研究；发展河口湿地生态恢复技术；加强河口湿地生态恢复示范研究以及建立动态监测和管理系统。

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简介：中国地理学的发展经历了漫长而辉煌的古代、短暂而平淡的近代和复兴昌盛的现代3个阶段。为了迎接中国地理学进入21世纪发展的新阶段，作者认为必须强调做好以下几个方面的工作：(1)改革地理教育；(2)提高资源与环境的研究水平；(3)认真为农业服务；(4)重视区域研究；(5)加强理论研究。