土壤质地对比率法测量饱和土壤水通量方向精度的影响
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国家自然科学基金项目(41571257)


Impact of Soil Texture on Accuracy of Saturated Soil Water Flux Direction Measurement Through Ratio Method
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    摘要:

    土壤水通量方向是饱和土壤流场的关键参数。受质地影响,土壤孔隙连通性和与之相关的土壤水流方向具有随机性,应在一定的空间尺寸下测量水通量方向。基于矢量合成原理,结合比率法可测量饱和土壤水通量方向。因此设计了一种五针热脉冲探头,测量平面内任意2个相互垂直的水通量,并通过矢量合成确定水通量方向。在饱和砂土、砂壤土和粉壤土中进行试验,每种土壤重复填装3次。试验结果表明,该方法测量土壤水通量方向的精度受土壤质地影响显著。当试验水通量大于4cm/h时,饱和砂土、砂壤土和粉壤土中角度测量值平均绝对值百分比误差(MAPE)分别为4.96%、6.18%和15.06%,表明水通量角度测量精度随着土壤质地变细逐渐下降。与水通量小于4cm/h相比,水通量大于4cm/h时砂土、砂壤土和粉壤土角度测量值标准差分别减小10.40°、6.65°和6.71°,表明水通量角度测量精度随着水通量增加而提高。在试验水通量大于6cm/h的砂土和大于3cm/h的砂壤土中得到了较稳定的水通量角度测量值(绝对误差小于7.5°),粉壤土中未得到稳定的角度测量值。说明在不同水通量和水力梯度下不同质地填装土壤孔隙连通性存在差异,进而影响了水通量角度测量精度。另外,土壤颗粒与探头间距的几何尺寸关系也会影响比率法测量精度。研究结果对热脉冲技术发展及其实际应用具有推动作用。

    Abstract:

    The direction of soil water flux is a key parameter in saturated soil flow fields. Soil texture significantly affects pore connectivity, which introduces randomness into the direction of water flow. Therefore, measuring water flux direction requires consideration of an appropriate spatial scale. The direction of saturated soil water flux can be determined by combining the ratio method with the principle of vector composition. Based on the above requirements, a penta–needle heat pulse probe (PHPP) was designed to measure water flux magnitude in any two mutually perpendicular directions within a plane and to determine flux direction through vector composition. Experiments were conducted in saturated sand, sandy loam, and silt loam, with each soil type repacked three times. The experimental results showed that the accuracy of this method in measuring soil water flux direction was significantly influenced by soil texture. For fluxes greater than 4 cm/h, the mean absolute percentage errors (MAPE) of angle measurements in sand, sandy loam, and silt loam were 4.96%, 6.18%, and 15.06%, respectively. This indicated that the accuracy of water flux direction measurements was decreased with finer soil texture. Compared with fluxes below 4 cm/h, the standard deviations of angle measurements in sand, sandy loam, and silt loam were decreased by 10.40°, 6.65° and 6.71°, respectively, for fluxes above 4 cm/h. This indicated that the accuracy of water flux direction measurements was improved with the increase of flux. Stable water flux angle measurements, with absolute errors below 7.5°, were achieved in sand at fluxes above 6 cm/h and in sandy loam above 3 cm/h, but not in silt loam. These findings suggested that pore connectivity in packed soils varied with texture under different fluxes and hydraulic gradients, thereby affecting measurement precision. Additionally, the geometric relationship between soil particle size and probe spacing affected the measurement accuracy of the ratio method. Optimizing the probe spacing of the PHPP based on soil particle size distribution may improve the reliability of water flux angle measurements by using the vector composition method. These findings can contribute to the development and practical application of heat pulse technology.

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卢富运,武阳,杨锡坚,王伟.土壤质地对比率法测量饱和土壤水通量方向精度的影响[J].农业机械学报,2026,57(4):399-406. LU Fuyun, WU Yang, YANG Xijian, WANG Wei. Impact of Soil Texture on Accuracy of Saturated Soil Water Flux Direction Measurement Through Ratio Method[J]. Transactions of the Chinese Society for Agricultural Machinery,2026,57(4):399-406.

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  • 收稿日期:2025-05-21
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  • 在线发布日期: 2026-02-15
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