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多數(shù)據(jù)源土壤傳遞函數(shù)模型在水分模擬中的不確定性
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國家重點(diǎn)基礎(chǔ)研究發(fā)展計(jì)劃(973計(jì)劃)資助項(xiàng)目(2011CB100502)


Soil Pedotransfer Function of Multiple Data Source and Its Uncertainty in Water Simulation
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    摘要:

    基于前饋神經(jīng)網(wǎng)絡(luò)的傳遞函數(shù)模型,采用4種不同的數(shù)據(jù)源預(yù)測土壤水分特征曲線,并借助誤差統(tǒng)計(jì)指標(biāo)、Hydrus-1D水動(dòng)力學(xué)模型對傳遞函數(shù)模型的預(yù)測性能及其應(yīng)用不確定性進(jìn)行了分析,。結(jié)果表明,預(yù)測土壤水吸力1000,、10000,、15000cm對應(yīng)含水率θ1000,、θ10000,、θ15000時(shí),,相對于僅有顆粒組成變量的傳遞函數(shù)模型,增加容重和θ60(水吸力60cm對應(yīng)的含水率)傳遞函數(shù)模型的平均絕對誤差降低了42.86%、23.87%,、26.15%,;增加θ60和θ15000模型預(yù)測θ100、θ10000,、θ15000的平均絕對誤差比僅包含θ60模型降低了8.67%,、16.96%,、15.95%,。將模型預(yù)測的van Genuchten參數(shù)應(yīng)用于土壤水分模擬,增加θ60模型的平均絕對誤差比以顆粒組成為輸入變量模型的相應(yīng)值降低了11.11%,;相對于增加θ60的傳遞函數(shù),,額外再增加θ15000并未降低模型應(yīng)用過程中的不確定性。

    Abstract:

    Pedotransfer function was established to predict soil water retention curve by using the feed-forward neural networks methods. The prediction performance and application uncertainty of pedotransfer function were analyzed according to the error statistics index and Hydrus-1D water dynamics model. The results showed that mean absolute error value of θ1000, θ10000, θ15000(soil water retention θ1000, θ10000, θ15000 at soil water suction equal to 1000cm, 10000cm and 15000cm, respectively) using pedotransfer functions with particle size distribution, bulk density, θ60 as predictor was 42.86%,23.87% and 26.15% lower than the value of PTF1 using particle size distribution as predictor. Mean absolute error of θ100,θ10000,θ15000 using pedotransfer function which added θ15000 as predictor was 8.67%,16.96% and 15.95% lower than pedotransfer function using θ60(soil water θ60 at soil water suction equal to 60cm) as predictor. The parameters of van Genuchten equation were predicted using pedotransfer function were used to simulate soil water, the MAE value of PTF using θ60 as predictor was 11.11% lower than PTF using particle size distribution as predictor. Therefore, adding additional θ15000 cannot reduce the uncertainty of pedotransfer function application comparing with the pedotransfer function using particle size, bulk density θ60 as predictor.

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王改改,張玉龍,虞娜.多數(shù)據(jù)源土壤傳遞函數(shù)模型在水分模擬中的不確定性[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2012,43(11):45-50. Wang Gaigai, Zhang Yulong, Yu Na. Soil Pedotransfer Function of Multiple Data Source and Its Uncertainty in Water Simulation[J]. Transactions of the Chinese Society for Agricultural Machinery,2012,43(11):45-50.

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  • 在線發(fā)布日期: 2012-11-16
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