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土壤有機碳空間變異性對采樣密度的響應研究
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國家自然科學基金資助項目(41071152)和公益性行業(yè)(農(nóng)業(yè))科研專項資助項目(201103005—01—01)


Spatial Variability Response of Soil Organic Carbon to Sampling Density Change
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    摘要:

    以北京地區(qū)土壤有機碳(SOC)為目標變量,,對比4種不同采樣密度下SOC質(zhì)量比空間變異的結構變化以及在不同采樣密度下不同空間預測方法對SOC質(zhì)量比空間預測不確定性方面的表現(xiàn),。結果表明,SOC質(zhì)量比關于地形因子的趨勢屬于宏觀趨勢,以低采樣密度的趨勢擬合效果最優(yōu);隨著采樣密度的增加,SOC質(zhì)量比及其去趨勢后殘差的系統(tǒng)內(nèi)部隨機變異逐漸增強,結構變異逐漸減弱,變異函數(shù)的分布也越平穩(wěn),,空間預測的不確定性也逐漸減小。另外,,變異函數(shù)的變程可能也影響空間預測的不確定性,;增加采樣密度和引入地形因子輔助的回歸克里格法均可以提高北京地區(qū)SOC質(zhì)量比的預測精度;在預測精度不降低的情況下,,引入地形因子輔助可以在一定程度上減少采樣的數(shù)量,。

    Abstract:

    Soil organic carbon (SOC) in Beijing was taken as target variable and four different sampling densities were designed to investigate the structural changes of the variogram and uncertainty of spatial prediction with the study scale changes. The results showed that the mass ratio of SOC was macroscopically related to terrain factor and low sampling density data were the most optimal for use in fitting the trend values. As sampling density increasing, the variogram distribution of SOC mass ratio and its residuals flattened out gradually. The random variation was growing strongly, and the structural variation and uncertainty of spatial prediction decreased gradually. In addition, the range of variogram might also affect the uncertainty of spatial prediction. Increasing sampling density and regression Kriging method aided by terrain factors can improve the prediction accuracy of mass ratio of SOC. Therefore, soil monitoring and management introducing auxiliary variable can cut the number of sampling points to some extent without reducing prediction accuracy.

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葉回春,黃珊瑜,張世文,張立平,黃元仿,黃亞捷.土壤有機碳空間變異性對采樣密度的響應研究[J].農(nóng)業(yè)機械學報,2014,45(12):215-223. Ye Huichun, Huang Shanyu, Zhang Shiwen, Zhang Liping, Huang Yuanfang, Huang Yajie. Spatial Variability Response of Soil Organic Carbon to Sampling Density Change[J]. Transactions of the Chinese Society for Agricultural Machinery,2014,45(12):215-223.

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  • 收稿日期:2014-04-27
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  • 在線發(fā)布日期: 2014-12-10
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