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A field-portable acoustic sensing device to measure soil moisture

机译:一种用于测量土壤水分的现场便携式声学传感装置

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For the last couple of decades, the idea of soil water measurement has gained widespread importance due to the spiraling crisis of global water resources. While several methods are being commonly used for soil water measurement, most of them do not satisfy all the essential requirements for water monitoring under field conditions including rapid on-site measurement and cost-effectiveness. This study was conducted to evaluate the efficacy of a novel field-portable acoustic sensing device on soil moisture measurements. The conventional Brutsaert's model was followed involving the continuous wave zero-crossing method to measure the acoustic velocity and considering the phase shift due to the amplifier and ambient temperature. The gravimetric moisture content (GMC) was calibrated using the acoustic velocity for 70 samples representing seven textural classes and variable soil organic carbon (OC). Results indicated the monotonous reduction of the acoustic velocities of p-wave with increasing GMC. In general, soils with higher clay content reflected higher acoustic velocities. However, sandy soils with high OC content were less prone to compaction and produced comparatively higher acoustic velocities than soils with higher clay content. A linear mixed effect (LME) model indicated that one unit increase in the acoustic velocity resulted in a 0.086% decrease in GMC. Moreover, LME parameters-based K-means clustering further highlighted the influence of soil texture for controlling the acoustic velocity. The use of LME justified the use of GMC as the target instead of the degree of saturation. Linear and quadratic models fitted for individual LME-based clusters produced R-2 values ranging from 0.80 to 0.88 and 0.82-0.88, respectively. Moreover, combined linear (R-2 = 0.61; RMSE = 52.12 m/s) and quadratic (R-2 = 0.64; RMSE = 50.48 m/s) models incorporating all 70 samples via bootstrapping produced comparable accuracies for GMC prediction, but yielded inferior results than the individual cluster-based models. In conclusion, the acoustic sensing device showed its potential for soil water content monitoring, leading to efficient irrigation planning. More research is warranted for texture-wise calibration development incorporating a wide assortment of soil types and on-site evaluation.
机译:在过去几年的几十年中,由于全球水资源的螺旋危机,土壤水量测量的思想受到了广泛的重要性。虽然几种方法通常用于土壤水量测量,但大多数都不满足现场条件下水监测的所有必要要求,包括快速现场测量和成本效益。进行该研究以评估新型现场便携式声学传感装置对土壤湿度测量的功效。遵循传统的Brutsaert的模型,涉及连续波零交叉方法测量声速度,并考虑由于放大器和环境温度引起的相移。使用代表七种纹理类别和可变土壤有机碳(OC)的70个样本的声速校准重力含水量(GMC)。结果表明,随着GMC的增加,P波声速度的单调降低。通常,具有较高粘土含量的土壤反映了更高的声速。然而,具有高OC含量的沙质土壤易于压实并产生比具有更高粘土含量的土壤的声速相对较高。线性混合效果(LME)模型表明声速度的一个单位增加导致GMC降低0.086%。此外,基于LME参数的K-Means聚类进一步强调了土壤纹理对控制声速度的影响。使用LME证明了GMC作为目标而不是饱和度。适用于基于单独的LME的簇的线性和二次模型产生的R-2值分别为0.80至0.88和0.82-0.88。此外,组合线性(R-2 = 0.61; RMSE = 52.12 m / s)和二次(R-2 = 0.64; RMSE = 50.48米米/秒)模型通过自举制备了GMC预测的可比精度,但产生了比基于群集的模型更低的结果。总之,声学传感装置展示了土壤含水量监测的潜力,导致有效的灌溉计划。有关纹理明智的校准开发,有必要进行更多的研究,其中包含各种各样的土壤类型和现场评估。

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