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地理学报  2015 

陆地表层人类活动强度:概念、方法及应用

DOI: 10.11821/dlxb201507004, PP. 1068-1079

Keywords: 人类活动强度,陆地表层,建设用地当量,土地利用/覆被类型,中国

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Abstract:

人类活动强度是表征人类对陆地表层影响和作用程度的综合指标。在定义陆地表层人类活动强度、建设用地当量等概念的基础上,建立了人类活动强度算法模型和土地利用/覆被类型的建设用地当量系数折算方法,并利用1984-2008年期间6个年份的土地利用数据,对中国进行了实证应用研究。结果表明中国的人类活动强度变化大致以2000年为界,前期增长相对缓慢,后期增长明显加快,1984年全国的人类活动强度为7.63%,到2008年上升为8.54%。2008年县级单元的人类活动强度按大于27%、16%~27%、10%~16%、6%~10%和小于6%划分为高、较高、中等、较低和低5个等级,其空间分布格局大致以贺兰山—龙门山—景洪线为界分为东、西两个部分。东部是高、较高和中等类型的集中分布区,低和较低类型呈条带状分布于山地、丘陵区;西部以低和较低类型为主体,在甘肃河西走廊、青海东部及新疆天山南北坡有零散的中等和较高类型分布。

References

[1]  YeDuzheng,FuCongbin,JiJinjun,etal.Orderlyhumanactivitiesandsubsistenceenvironment.AdvanceinEarthSciences,2001,16(4):453-460.[叶笃正,符淙斌,季劲钧,等.有序人类活动与生存环境.地球科学进展,2001,16(4):453-460.]
[2]  MilerRB.Interactionsandcollaborationinglobalchangeacrossthesocialandnaturalsciences.IMBIO,1994,23(1):19-24.
[3]  LiuYanhua,GeQuansheng,FangXiuqi,etal.GlobalenvironmentalchangeandthenationalsecurityofChina.AdvanceinEarthSciences,2006,21(4):346-351.[刘燕华,葛全胜,方修琦,等.全球环境变化与中国国家安全.地球科学进展,2006,21(4):346-351.]
[4]  ShiPeijun,LiNing,YeQian,etal.Researchonglobalenvironmentalchangeandintegrateddisasterriskgovernance.AdvanceinEarthSciences,2009,24(4):428-435.[史培军,李宁,叶谦,等.全球环境变化与综合灾害风险防范研究.地球科学进展,2009,24(4):428-435.]
[5]  IPCC.ClimateChange:SynthesisReport.WorkingGroupsI,IIandIIIContributiontothe5thAssessmentReport.2014.
[6]  RogerG.Barry.MountaincryosphericstudiesandtheWCRPclimateandcryosphere(CliC)project.JournalofHydrology,2003,282,Issues1-4:177-181.
[7]  WolframMauser,GernotKlepper,MartinRice,etal.Transdisciplinaryglobalchangeresearch:theco-creationofknowledgeforsustainability.CurrentOpinioninEnvironmentalSustainability,2013,5(3/4):420-431.
[8]  LeemansR,AsrarG,CanadellJG,etal.Developingacommonstrategyforintegratedglobalchangeresearchandoutreach:theEarthSystemSciencePartnership(ESSP).CurrOpinEnvironSustain,2009,1:4-13.
[9]  JillJ?ger.Theinternationalhumandimensionsprogrammeonglobalenvironmentalchange(IHDP).GlobalEnvironmentalChange,2003,13(1):69-73.
[10]  MichelLoreau,IsabelleOlivieri.Diversitas:aninternationalprogrammeofbiodiversityscience.TrendsinEcology&Evolution,1999,(14):2-3.
[11]  TurnerIBL,SkoleD,SandersonS,etal.Land-useandland-coverchangescience/researchplan,IGBPReportNo.35andHDPReportNo.7.Stochkholm:IGBP,1995.
[12]  LiXiubin.Areviewoftheinternationalresearchesonlanduse/coverchange.ActaGeographicaSinica,1996,51(6):553-557.[李秀彬.全球环境变化研究的核心领域:土地利用/土地覆被变化的国际研究动向.地理学报,1996,51(6):553-558.]
[13]  LOFresco,RLeemans,AEvanZeijl-Rozema.Landuseandcoverchange(LUCC)opensciencemeetingRoyalNetherlandsAcademyofArtsandSciences,Amsterdam,TheNetherlands,29-31January1996.LandUsePolicy,1996,13(4):332-334.
[14]  RaffaelePelorosso,AntonioLeone,LorenzoBoccia.LandcoverandlandusechangeintheItaliancentralApennines:Acomparisonofassessmentmethods.AppliedGeography,2009,29(1):35-48.
[15]  LiuJiyuan,DengXiangzheng.DevelopmentofresearchmethodofLUCCspatio-temporalprocess.ChineseScienceBulletin,2009,54(21):3251-3258.[刘纪远,邓祥征.LUCC时空过程研究的方法进展.科学通报.2009,54(21):3251-3258.]
[16]  TangHuajun,WuWenbin,YangPeng,etal.Recentprogressesoflanduseandlandcoverchange(LUCC)models.ActaGeographicaSinica,2009,64(4):456-468.[唐华俊,吴文斌,杨鹏,等.土地利用/土地覆被变化(LUCC)模型研究进展.地理学报,2009,64(4):456-468.]
[17]  GeneralOfficeoftheStateCouncil([2010]No.46)].MajorfunctionalareaplanninginChina.2010.[中华人民共和国国务院.全国主体功能区规划.国务院文件46号,2010.]
[18]  FanJie,LiPingxing.ThescientificfoundationofmajorfunctionorientedzoninginChina.JournalofGeographicalSciences,2009,19(5):515-531.
[19]  ZhuangDafang,LiuJiyuan.StudyonthemodelofregionaldifferentiationoflandusedegreeinChina.JournalofNaturalResources,1997,12(2):105-111.[庄大方,刘纪远.中国土地利用程度的区域分异模型研究.自然资源学报,1997,12(2):105-111.]
[20]  XuZhigang,ZhuangDafang,YangLin.Constructionandapplicationofregionalquantitativemodelofhumanactivityintensity.JournalofGeo-informationScience,2009,11(4):452-460.[徐志刚,庄大方,杨琳.区域人类活动强度定量模型的建立与应用.地球信息科学学报,2009,11(4):452-460.]
[21]  ZhuHuiyi,LiXiubin.Discussionontheindexmethodofregionallandusechange.ActaGeographicaSinica,2003,58(5):643-650.[朱会义,李秀彬.关于区域土地利用变化指数模型方法的讨论.地理学报,2003,58(5):643-650.]
[22]  WenYing.Preliminarydiscussiononthemethodofquantitativeassessmentofhumanactivityintensity.ImpactofScienceonSociety,1998(4):55-60.[文英.人类活动强度定量评价方法的初步探讨.科学对社会的影响,1998(4):55-60.]
[23]  LiXiangyun,WangLixin,ZhangYushu,etal.AnalysisofrolesofhumanactivitiesinlanddesertificationinaridareaofNorthwestChina.ScientiaGeographicaSinica,2004,24(1):68-75.[李香云,王立新,章子舒,等.西北干旱区土地荒漠化中人类活动作用及其指标择.地理科学,2004,24(1):68-75.]
[24]  ZhangCuiyun,WangZhao.QuantitativeassessmentofhumanactivityintensityintheHeihecatchment.AdvanceinEarthSciences,2004,19(Suppl):386-390.[张翠云,王昭.黑河流域区域人类活动强度的定量评价.地球科学进展,2004,19(Suppl.):386-390.]
[25]  WangGuisheng,XieYaowen,WangXueqiang.EvaluationonhumanactivityinthemiddlereachesofHeiheRiverinhistoricalperiod:AcasestudyontheMingDynasty,QingDynastyandtheRepublicofChina.JournalofDesertResearch,2013,33(4):1225-1234.[汪桂生,颉耀文,王学强.黑河中游历史时期人类活动强度定量评价:以明、清及民国时期为例.中国沙漠,2013,33(4):1225-1234.]
[26]  HuZhibin,HeXingyuan,LiYuehui,etal.HumanactivityintensityanditsspatialdistributionpatterninupperreachofMinjiangriver.ChineseJournalofEcology,2007,26(4):539-543.[胡志斌,何兴元,李月辉,等.岷江上游地区人类活动强度及其特征.生态学杂志,2007,26(4):539-543.]
[27]  WangJinzhe,ZhangGuanghui,NieZhenlong,etal.QuantitativeassessmentofhumanactivityintensityinHutuohecatchment.JournalofAridLandResourcesandEnvironment,2009,23(10):41-44.[王金哲,张光辉,聂振龙,等.滹沱河流域平原区人类活动强度的定量评价.干旱区资源与环境,2009,23(10):41-44.]
[28]  ZhengWenwu,TianYaping,ZouJun,etal.SpatialsimulationofhumanactivityintensityinhillyredsoilregionofsouthernChina:AcasestudyinHengyangbasin,HunanProvince.JournalofGeo-informationScience,2010,12(5):628-633.[郑文武,田亚平,邹君,等.南方红壤丘陵区人类活动强度的空间模拟与特征分析:以衡阳盆地为例.地球信息科学学报,2010,12(5):628-633.]
[29]  WilliamE.Rees.Ecologicalfootprint,conceptof.EncyclopediaofBiodiversity,2001(2):229-244.
[30]  MathisWackernagel,WilliamE.Rees.Perceptualandstructuralbarrierstoinvestinginnaturalcapital:Economicsfromanecologicalfootprintperspective.EcologicalEconomics,1997,20(1):3-24.
[31]  AkiraSekiya,SayuriOkamoto.Evaluationofcarbondioxideequivalentvaluesforgreenhousegases:CEWNasanewindicatorreplacingGWP.JournalofFluorineChemistry,2010,131(3):364-368.
[32]  WuChuanjun,GuoHuancheng.ChineseLandUse.Beijing:SciencePress,1994.[吴传钧,郭焕成.中国土地利用.北京:科学出版社,1994.]
[33]  US-SGCR/CENR.Ourchangingplant,theFY1996U.S.globalchangeresearchprogram.Washington,D.C.:US-GCRIO,1996.
[34]  GraetzD.Landcover:Tryingtomakethetasktractable/ProceedingoftheWorkshoponGlobalLandUse/CoverModelling.NewYork,1993.
[35]  ZhuChunyang,LiFang,LiShuhua.Researchontheinfluenceofdifferentpavementstructuresinlandscapepathonrainfallinfiltrationprocess.ChineseLandscapeArchitecture,2009(3):91-97.[朱春阳,李芳,李树华.园林道路不同铺装结构对雨水入渗过程的影响.中国园林,2009(3):91-97.]
[36]  HouLizhu,FengShaoyuan,DingYueyuan,etal.Runoff-rainfallrelationshipformultilayerinfiltrationsystemsunderartificialrainfalls.TransactionsoftheCSAE,2006,22(9):100-105.[侯立柱,冯绍元,丁跃元,等.人工降雨条件下多层渗滤介质系统产流与入渗规律试验研究.农业工程学报,2006,22(9):100-105.]
[37]  LiuZhenhuan,LiYou,PengJian.Progressandperspectiveoftheresearchonhydrologicaleffectsofurbanimpervioussurfaceonwaterenvironment.ProgressinGeography,2011,30(3):275-281.[刘珍环,李猷,彭建.城市不透水表面的水环境效应研究进展.地理科学进展.2011,30(3):275-281.]
[38]  WangHongjie,LiXianwen,ShiXuezheng,etal.Distributionofsoilnutrientunderdifferentlanduseandrelationshipbetweensoilnutrientandsoilgranulecomposition.JournalofSoilandWaterConservation,2003,17(2):44-46,50.[王洪杰,李宪文,史学正,等.不同土地利用方式下土壤养分的分布及其与土壤颗粒组成关系.水土保持学报,2003,17(2):44-46,50.]
[39]  YuWeiqing,WangYujie,HuHaibo,etal.SoilwaterinfiltrationcharacteristicsanalysisunderdifferentvegetationonthehillygroundofYangtzeRiverDelta.ChineseJournalofSoilScience,2014,45(2):345-351.[余蔚青,王玉杰,胡海波,等.长三角丘陵地不同植被林下土壤入渗特征分析.土壤通报,2014,45(2):345-351.]
[40]  SheDongli,GaoXuemei,FangKai.Measurementofsoilsorptivityrateunderdifferentlandusesbydiscinfiltrometer.TransactionsoftheCSAE,2014,30(18):151-158.[佘冬立,高雪梅,房凯.利用圆盘入渗仪测定不同土地利用类型土壤吸渗率.农业工程学报,2014,30(18):151-158.]

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