陕北黄土高原正负地形研究(英文)

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    摘要 TheLoesspositiveandnegativeterrains(P-Nterrains),whicharewidelydistrib-utedontheLoessPlateau,arediscussedforthefirsttimebyintroducingitscharacteristic,demarcationaswellasextractionmethodfromhigh-resolutionDigitalElevationModels.Us-ing5m-resolutionDEMsasoriginaltestdata,P-Nterrainsof48geomorphologicalunitsindifferentpartsofShaanxiLoessPlateauareextractedaccurately.Thensixindicatorsforde-pictingthegeomorphologiclandscapeandspatialconfigurationcharacteristicofP-Nterrainsareproposed.ThespatialdistributionrulesoftheseindicatorsandtherelationshipbetweentheP-NterrainsandLoessreliefarediscussedforfurtherunderstandingofLoesslandforms.Finally,withtheintegrationofP-Nterrainsandtraditionalterrainindices,aseriesofun-supervisedclassificationmethodsareappliedtomakeaproperlandformclassificationinnorthernShaanxi.ResultsshowthatP-NterrainsareaneffectcluetorevealenergyandsubstancedistributionrulesontheLoessPlateau.AcontinuouschangeofP-NterrainsfromsouthtonorthinShaanxiLoessPlateaushowsanobviousspatialdifferenceofLoessland-formsandthepositiveterrainareaonlyaccountedfor60.5%inthisregion.TheP-Nterrainsparticipantlandformclassificationmethodincreasesvalidityoftheresult,especiallyintheLoesstableland,Loesstableland-ridgeandtheLoesslow-hillarea.ThisresearchissignificantonthestudyofLoesslandformswiththeDigitalTerrainsAnalysismethods.
    机构地区 不详
    出处 《地理学报:英文版》 2010年1期
    出版日期 2010年01月11日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)
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