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ID:28756213
大小:7.74 MB
页数:39页
时间:2018-12-13
《垄作方式下土壤风蚀过程研究——以草原风沙土为例》由会员上传分享,免费在线阅读,更多相关内容在学术论文-天天文库。
1、风速为0.42rn/s.0.68m/s的风沙流结构,结果表明:随着摩阻风速与土垄间距的增大,集沙仪中风蚀物的跃移高度均有所增加,五种土垄间距且摩阻风速为0.51m/s时,沙粒的跃移高度基本均达到了50.60cm:随着摩阻风速的增大,各高度输沙量都有所增加,但不同土垄间距的输沙量增加的幅度不同,不同土垄间距的实验样品0.10cm高度输沙量占总输沙量的百分比变化也不同:实验样品在O.42~0.68m/s的摩阻风速下,随着高度的增加,集沙量基本都呈对数函数规律减小。(5)由于集沙量大部分集中在O-30cm高度内,所以只研究了
2、30cm高度内风蚀物平均粒径与风速的关系,结果表明:在同一土垄间距下,随着风速的增加,同一高度处的沙粒平均粒径逐渐增大,但规律不是很好;同一风速下,随着土垄问距的增大,各高度层沙粒平均粒径基本呈增大的趋势;在垄距与风速相同的条件下,风蚀物的平均粒径随垂直高度的分布总体上呈现出减小的趋势;平均粒径在距离地表30cm以上时,大部分实验样品出现了先增大,后减小的情况。这说明,平均粒径随着高度的增加并不是严格按照递减的规律,这与前人关于平均粒径随着高度的增加呈指数函数递减的结论有一定的差异,说明土垄对风蚀物平均粒径垂直变化有一
3、定的影响。关键词:土壤风蚀土垄间距风沙流结构输沙量粒度特征IV万方数据AbstractSoilwinderosionistheprocessofwinderosion,transportationandaccumulationofsurfacesoil,anditisaprocessofinteractionbetweenwindandsurfaceparticles.Winderosiondestroysthesurface,whichresultsinthelossofsoilfineparticulateands
4、oilnutrients,resultingindesertification.Winderosionisparticularlyseriousinarid,semi-aridandsemihumidregions,andithasbeenoneofthemostimportantresearchareasbothathomeandabroad.Butatpresent,mostoftheresearchfocusesonthebaresoil,andsoilwinderosionundervegetationcove
5、r,soilwinderosionunderridgetillageisstillrare.Therefore,thearticleselectedtheZhenglanBannerAreaofInnerMongoSaAutonomousRegionasthetypicalarea,collectedthegrasslandyaeoliansandysoilastheresearchobject,anddesignedfivedifferentspacingofsoilridge.Thispaperbasedonthe
6、windtunnelsimulationtestoffivefrictionvelocity,studiedtherelationshipbetweentotaltransportsedimentandsoilridgespacing,windspeed,andanalyzedsandfloWcharacteristicofveaicalstructure,theruleofwinderosionsedimentgrainsizevarimion.Mainresultsarethefollowing:(1)Ridget
7、illageCanchangethesurfacemicrotopographyandincreasesurfaceroughness,effectivelyinhibitsoilerosion.Theweakeningeffectofdifferentheightandspacingridgeisdifferent.(2)Winderosionwasmainlyconcentratedin0—30cmofthesandcollectinginstrument,whichshowedthatthesanddriftmo
8、vementwasakindofthematerialhandingprocessofclosingtothesurface.(3)Analysisoftherelationshipbetweentotalsedimentloadandimpactfactorshowedthatthewindspeedandsoilridgesp
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