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不同土層土壤水分特征曲線的空間變異及其影響因素
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劉繼龍,博士生,,主要從事農(nóng)業(yè)水土工程研究,,Email: dra [email protected]

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國(guó)家自然科學(xué)基金資助項(xiàng)目(50879072,、50609022),、“十一五”國(guó)家科技支撐 計(jì)劃資助項(xiàng)目(2006BAD11B04)和國(guó)家“863”高技術(shù)研究發(fā)展計(jì)劃資助項(xiàng)目(2006AA10020 9)


Spatial Variability of Soil Water Retention Curve in  Different Soil Layers and Its Affecting Factors
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    摘要:

    利用多重分形和聯(lián)合多重分形方法,,對(duì)陜西楊凌地區(qū)0~20cm和20~40cm土層van Genuchten模型參數(shù) 的空間變異性及其影響因素進(jìn)行了研究,。結(jié)果表明:0~20cm和20~40cm土層參數(shù)α 都具有明顯的多重分形特征,,空間變異性較強(qiáng),,且分別是由低值和高值分布引起的,;參數(shù) n和θs的多重分形特征不明顯,空間變異性較弱,。0~20cm和20~40cm土層v an Genuchten模型參數(shù)與土壤物理特性的相關(guān)特征并不完全相同,,在觀測(cè)尺度上,0~20c m土層參數(shù)α與Sand,、Silt顯著相關(guān),,參數(shù)n與Sand、SOM顯著相關(guān),,θs與Sa nd顯著相關(guān),;20~40cm土層參數(shù)α與SOM顯著相關(guān),參數(shù)n和θs都與Sand ,、Silt,、SOM顯著相關(guān);在多尺度上,,0~20cm土層參數(shù)α與Sand,、Silt的相關(guān)程度最 高,20~40cm土層參數(shù)α與BD,、SOM的相關(guān)程度最高,。

    Abstract:

    Spatial variability of van Genuchten model parameters and its affecting factors in 0~20cm and 20~40cm soil layers were studied with multifractal and joint multifractal methods. The results showed that in 0~20cm and 20~40cm soil layers parameter had obvious multifractal characteristics, and its spatial varia b ility was strong caused by the distribution of lower and higher values respectiv ely. The multifractal characteristics of parameter n and θs were not obvious, and the spatial variability was weak. Correlation characteristics betwe en van Genuchten model parameters α and soil physical properties in 0~20 cm and 20~40cm soil layers were analyzed. At the observation scale, the corre lations between parameter n and sand and silt content were significant, the parameter n and sand and organic matter content had remarkable relationship, and θs was significantly related to sand content in 0~20cm soil layer. The relationship between parameters α and organic matter content was remarkabl e, and the parameter n and θs were significantly related to sand, sil t and organic matter content in 20~40cm soil layer. At the multiple scales, c orrelations between parameters α and sand and silt content were most obviou s in 0~20cm soil layer, and parameters α were remarkably related to bulk density and organic matter content in 20~40cm soil layer. 

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劉繼龍,馬孝義,張振華.不同土層土壤水分特征曲線的空間變異及其影響因素[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2010,41(1). Liu Jilong, Ma Xiaoyi, Zhang Zhenhua. Spatial Variability of Soil Water Retention Curve in  Different Soil Layers and Its Affecting Factors[J]. Transactions of the Chinese Society for Agricultural Machinery,2010,41(1).

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