热带农业科学
熱帶農業科學
열대농업과학
CHINESE JOURNAL OF TROPICAL AGRICULTURE
2011年
6期
1-6
,共6页
香蕉%砖红壤%养分%空间变异
香蕉%磚紅壤%養分%空間變異
향초%전홍양%양분%공간변이
banana%latosol%nutrients%spatial variability
运用统计学和ArcGIS软件的地统计分析模块对海南砖红壤香蕉园59个土壤采样点两个取样土层(0~20 cm和20~40 cm)养分进行空间变异性研究。结果表明:香蕉园土壤各养分变异系数均为中等变异。0~20cm土层土壤各养分含量大于20~40 cm土层。0~20 cm和20~40 cm土层中的碱解氮、交换性钙和交换性镁及0~20 cm土层的有机质均符合高斯模型,0~20 cm土层速效磷与20~40 cm土层速效钾符合球状模型,而20~40 cm土层速效磷与0~20 cm土层速效钾符合圆形模型,20~40 cm土层有机质符合指数模型。各养分的变程范围为109.217~279.796 m,有机质具有强烈的空间相关性。0~20 cm土层速效钾的块金效应值小于20~40 cm土层,0~20 cm土层碱解氮、速效磷、交换性钙、交换性镁高于20~40 cm土层。有机质、20~40 cm土层速效磷、0~20 cm土层速效钾的块金效应小于25%,其它养分均在25%~75%,具有中等的空间相关性。确定了合理取样数,0~20 cm碱解氮、速效磷、速效钾、交换性钙、交换性镁、有机质合理取样数分别为:5、30、26、29、25、3;20~40 cm碱解氮、速效磷、速效钾、交换性钙、交换性镁、有机质合理取样数分别为:4、44、30、26、25、3,就可以满足变量施肥的要求。
運用統計學和ArcGIS軟件的地統計分析模塊對海南磚紅壤香蕉園59箇土壤採樣點兩箇取樣土層(0~20 cm和20~40 cm)養分進行空間變異性研究。結果錶明:香蕉園土壤各養分變異繫數均為中等變異。0~20cm土層土壤各養分含量大于20~40 cm土層。0~20 cm和20~40 cm土層中的堿解氮、交換性鈣和交換性鎂及0~20 cm土層的有機質均符閤高斯模型,0~20 cm土層速效燐與20~40 cm土層速效鉀符閤毬狀模型,而20~40 cm土層速效燐與0~20 cm土層速效鉀符閤圓形模型,20~40 cm土層有機質符閤指數模型。各養分的變程範圍為109.217~279.796 m,有機質具有彊烈的空間相關性。0~20 cm土層速效鉀的塊金效應值小于20~40 cm土層,0~20 cm土層堿解氮、速效燐、交換性鈣、交換性鎂高于20~40 cm土層。有機質、20~40 cm土層速效燐、0~20 cm土層速效鉀的塊金效應小于25%,其它養分均在25%~75%,具有中等的空間相關性。確定瞭閤理取樣數,0~20 cm堿解氮、速效燐、速效鉀、交換性鈣、交換性鎂、有機質閤理取樣數分彆為:5、30、26、29、25、3;20~40 cm堿解氮、速效燐、速效鉀、交換性鈣、交換性鎂、有機質閤理取樣數分彆為:4、44、30、26、25、3,就可以滿足變量施肥的要求。
운용통계학화ArcGIS연건적지통계분석모괴대해남전홍양향초완59개토양채양점량개취양토층(0~20 cm화20~40 cm)양분진행공간변이성연구。결과표명:향초완토양각양분변이계수균위중등변이。0~20cm토층토양각양분함량대우20~40 cm토층。0~20 cm화20~40 cm토층중적감해담、교환성개화교환성미급0~20 cm토층적유궤질균부합고사모형,0~20 cm토층속효린여20~40 cm토층속효갑부합구상모형,이20~40 cm토층속효린여0~20 cm토층속효갑부합원형모형,20~40 cm토층유궤질부합지수모형。각양분적변정범위위109.217~279.796 m,유궤질구유강렬적공간상관성。0~20 cm토층속효갑적괴금효응치소우20~40 cm토층,0~20 cm토층감해담、속효린、교환성개、교환성미고우20~40 cm토층。유궤질、20~40 cm토층속효린、0~20 cm토층속효갑적괴금효응소우25%,기타양분균재25%~75%,구유중등적공간상관성。학정료합리취양수,0~20 cm감해담、속효린、속효갑、교환성개、교환성미、유궤질합리취양수분별위:5、30、26、29、25、3;20~40 cm감해담、속효린、속효갑、교환성개、교환성미、유궤질합리취양수분별위:4、44、30、26、25、3,취가이만족변량시비적요구。
Use of traditional statistical and geostatistical analysis Arcgis software module 59 in Hainan banana two layers of soil samples(0~20cm and 20~40 cm) spatial variability of nutrients,the results show that the banana coefficient of variation of soil nutrients are moderate variation.The 0~20 cm nutrient content of soil layer is greater than 20~40 cm soil layer.0~20 cm and 20~40 cm soil layer in nitrogen,exchangeable calcium and exchangeable magnesium,and 0~20 cm layer of organic matter are in line with the Gaussian model,0~20cm soil available phosphorus and available 20~40 cm soil potassium by spherical model,while the 20~40cm soil available P and K 0~20 cm soil layer model consistent round,20~40 cm of soil organic matter in line with the exponential model.Variable range of the nutrients in the range of 109.217~279.796 m,organic matter has a strong spatial correlation.0 ~ 20cm of soil available K nugget effect is less than 20~40 cm soil layer,0~20 cm of soil nitrogen,available phosphorus,exchangeable calcium,exchangeable magnesium than 20~ 40 cm soil layer.Organic matter,20~40 cm soil available P,0~20 cm of soil available K nugget effect is less than 25%,other nutrients are in the 25% to 75%,and a moderate spatial correlation.To determine a reasonable number of samples,0~20 cm nitrogen,phosphorus,potassium,exchangeable calcium,exchangeable magnesium,a reasonable number of samples of organic matter were: 5,30,26,29,25,3;20~40 cm available N,available K,exchangeable Ca,exchangeable Mg,organic matter,a reasonable number of samples were 4,44,30,26,25,3 to meet the requirements of variable rate fertilization.