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基于HWSD的GSAC模型網(wǎng)格化產(chǎn)流參數(shù)估計(jì)與校正
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國家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2016YFC0400101),、國家自然科學(xué)基金項(xiàng)目(51009026、41271046),、中國電力建設(shè)股份有限公司科技課題項(xiàng)目(DJ-ZDZX-2016-02)和農(nóng)業(yè)部農(nóng)業(yè)水資源高效利用重點(diǎn)實(shí)驗(yàn)室開放課題項(xiàng)目(2015002)


Grid Runoff Parameters Estimation and Adjustment of GSAC Model Based on HWSD
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    摘要:

    針對基于網(wǎng)格的薩克拉門托模型(GSAC)產(chǎn)流參數(shù)難以估計(jì)的問題,,提出利用世界和諧土壤數(shù)據(jù)庫(HWSD)土壤屬性數(shù)據(jù)估計(jì)和校正該模型產(chǎn)流參數(shù)的方法。首先,,采用HWSD土粒百分含量和土壤質(zhì)地分類數(shù)據(jù)估算流域各網(wǎng)格頂層(T層)與底層(S層)土壤的凋萎系數(shù),、田間持水量、飽和含水量等土壤水分常數(shù),;再采用一個氣候指數(shù)和HWSD的T層張力水容量,、田間持水量及凋萎系數(shù)推求GSAC模型上層厚度,繼而利用上層厚度將流域各網(wǎng)格的HWSD土壤水分常數(shù)轉(zhuǎn)換為GSAC 模型上,、下層土壤水分常數(shù),;最后利用GSAC 模型上層厚度與轉(zhuǎn)換了的土壤水分常數(shù)估計(jì)流域各網(wǎng)格的產(chǎn)流參數(shù),;在估計(jì)產(chǎn)流參數(shù)的同時(shí),采用12個系數(shù)對這些產(chǎn)流參數(shù)進(jìn)行校正,,所有的校正系數(shù)通過自由搜索(FS)算法率定GSAC模型確定,。呼蘭河流域的應(yīng)用結(jié)果表明:基于HWSD土壤屬性數(shù)據(jù)估計(jì)GSAC 模型網(wǎng)格化產(chǎn)流參數(shù)的方法簡便易行,利用校正產(chǎn)流參數(shù)驅(qū)動的GSAC模型在率定期與驗(yàn)證期的納什效率系數(shù)(NSEC)分別為0.81和0.83,,與不校正產(chǎn)流參數(shù)情況相比,,校正產(chǎn)流參數(shù)的GSAC模型能夠取得更高的模擬精度。

    Abstract:

    The grid-based Sacramento (GSAC) model divides a basin into discrete areas using grids. Conventionally, it is difficult to achieve the grid parameter for runoff module of GSAC model. With an aim to solve this problem, a method for estimating the runoff parameters of GSAC model using the soil property data of harmonized world soil database (HWSD) was proposed, in which the physical and chemical characteristics of each soil layer were given on the basis of the division of topsoil (0~30cm) and subsoil (30~100cm). Firstly, the percentages of sand and clay content and texture classification in topsoil (T-layer) and subsoil (S-layer) of HWSD were extracted. And the data was used to estimate the soil water constants such as wilting point, field capacity and saturated water content in each grid. Secondly, the upper layer thickness of GSAC model was adjusted using wilting point, field capacity and tension water capacity of T-layer, and a climatic index defined as ratio of mean annual precipitation to potential evapotranspiration. In each grid, the soil water constants of T-layer and S-layer were converted into those in the upper layer and lower layer of GSAC model by upper layer thickness. Finally, runoff parameters in each grid were estimated using the upper layer thickness and the converted soil water constants of GSAC model. Meanwhile, totally 12 adjustment coefficients were used to adjust the runoff parameters, and all the adjustment coefficients were determined by the GSAC model via the free search (FS) algorithm. The results of model application in the Hulan River Basin indicated that it was feasible to estimate runoff parameters of GSAC model using HWSD soil property data;the better runoff simulation results were obtained by GSAC model using the adjusted runoff parameters;and Nash efficiency coefficients (NSEC) were 0.81 and 0.83 of the calibration phase and verification phase, respectively.

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王斌,丁星臣,黃金柏,宮興龍,朱士江,王貴作.基于HWSD的GSAC模型網(wǎng)格化產(chǎn)流參數(shù)估計(jì)與校正[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2017,48(9):250-256,,249. WANG Bin, DING Xingchen, HUANG Jinbai, GONG Xinglong, ZHU Shijiang, WANG Guizuo. Grid Runoff Parameters Estimation and Adjustment of GSAC Model Based on HWSD[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(9):250-256,,249.

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  • 收稿日期:2017-01-17
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  • 在線發(fā)布日期: 2017-09-10
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