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ID:34368679
大小:650.19 KB
页数:11页
时间:2019-03-05
《干旱荒漠区土壤有机质空间变异特征》由会员上传分享,免费在线阅读,更多相关内容在教育资源-天天文库。
1、万方数据第24卷第12期生态学报V01.24,No.122004年12月ACTAECOLOGICASINICADec.,2004干旱荒漠区土壤有机质空间变异特征(1黄元仿1,周志宇孙,苑小勇1,张红艳1中国农业大学,北京100094;2.兰州大学草地农业科技学院,甘肃730020)摘要:以内蒙古阿拉善左旗为例,研究了干旱荒漠区土壤有机质的空间变异特征。传统统计分析结果表明,研究区内土壤有机质含量总体水平较低,平均为6.659/kg;变异系数为1.42,属强变异。在半方差结构分析和球状模型套合的基础上,结合普通
2、K“ging插值方法,分析了土壤有机质的地统计特征。比较不同趋势效应和异向性的普通Kriging插值的误差结果表明,宜考虑各向异性和二阶趋势效应。获得了研究区土壤有机质含量的等值线图,并分析了其空间分布规律。关键词:干旱荒漠区;土壤有机质;空间变异;趋势效应SpatialVariabilityOfsoilorganicmattercontentinanariddesertareaHUANGYuan—Fan91,ZHOUZhi—Yu2,YUANXiao—Yon91,ZHANGHong—Yanl(1.∞imAg—
3、f“zf“mzUni口Prs妇,BP衲glo0094,C^inn;2:厶以z^。“【,ni材椰幼,G彻s“730020,c^in口).Acf口&DfDgf伽Sf—f∞,2004,24(12):2776~2781.Abstract:AlxaLeftBannerinthewestoftheInnerMongoliaAutonomousRegion,China,isatypicalariddesertareainthemiddletemperatezonebetweenthenorthernborderofChin
4、aandtheeasternAlxaPlateau.Duetoovergrazingandhumanactivities,soildegradation(ordesertification)intheareaisbecomingincreasin91yseVereduetolossofsoilorganicmatter(SOM).LowSOMcontentimpactssoilqualitydirectlyinthisariddesertarea.Understandingthespatialvariatio
5、nanddistributionpatternofSOMcontentisneededforsustainabledeveIopmentintheregion.Inthisstudy,thespatialVariationofSOMcontentinA1xaLeftBannerwasdeterminedusingbothtraditionalstatisticsandgeostatisticstoproVideinformationforunderstandingdesertificationmechanis
6、msandpreventingso订degradation.Basedonlocallandforms,103soilsamples(O~20cm)werecollectedfromtheareawithintheHelanMountainwatershed,onthewesternborderoftheWulanbuheDesert,thenorthernborderoftheTenggeliDesertandthesouthernborderoftheGobiregion.TheSOMcontentwas
7、analyzedusingtheWalkley—Blackwetcombustionmethod.Thegeostatisticalcharacteristics,spatialtrendandazimuthofanisotropicaxleofSOMcontentwereanalyzedusingtheGeostatisticalAnalyst,ArcGIS8.1.WecreatedacontourmapofSOMcontentforthestudyareausingKriginginterp01ation
8、.Traditionalstatisticalanalysis(descriptivestatistics)showeddifferencesinSoMcontentamongdifferentsoiltypes.Thecoefficientofvariation(CV)ofSOMcontentwasgreatestinAeoliansandysoil(CV1.10)andsmallestinSub
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