Acta Agriculturae Zhejiangensis ›› 2022, Vol. 34 ›› Issue (6): 1297-1305.DOI: 10.3969/j.issn.1004-1524.2022.06.20
• Biosystms Engineening • Previous Articles Next Articles
WANG Jun1,2(), LU Zhou2, LUO Ming2, XU Feifei2, ZHANG Xu1,*(
)
Received:
2021-07-15
Online:
2022-06-25
Published:
2022-06-30
Contact:
ZHANG Xu
CLC Number:
WANG Jun, LU Zhou, LUO Ming, XU Feifei, ZHANG Xu. Inversion of soil moisture content of winter wheat at turning green period based on multispectral remote sensing by unmanned aerial vehicle[J]. Acta Agriculturae Zhejiangensis, 2022, 34(6): 1297-1305.
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URL: http://www.zjnyxb.cn/EN/10.3969/j.issn.1004-1524.2022.06.20
深度 Depth/cm | 样本集 Dataset | 样本数量 Sample size | 最小值 Minimum | 最大值 Maximum | 平均值 Mean | 标准差 Standard deviation | 变异系数 Coefficient of variation |
---|---|---|---|---|---|---|---|
10 | 总集Whole set | 39 | 0.347 | 0.456 | 0.393 | 0.024 | 0.060 |
建模集Modeling set | 30 | 0.347 | 0.456 | 0.394 | 0.026 | 0.065 | |
检验集Verification set | 9 | 0.363 | 0.412 | 0.392 | 0.016 | 0.041 | |
20 | 总集Whole set | 39 | 0.368 | 0.507 | 0.476 | 0.048 | 0.101 |
建模集Modeling set | 30 | 0.403 | 0.507 | 0.489 | 0.044 | 0.091 | |
检验集Verification set | 9 | 0.368 | 0.504 | 0.440 | 0.038 | 0.087 |
Table 1 Statistics of soil moisture characteristics of sampling points in study area
深度 Depth/cm | 样本集 Dataset | 样本数量 Sample size | 最小值 Minimum | 最大值 Maximum | 平均值 Mean | 标准差 Standard deviation | 变异系数 Coefficient of variation |
---|---|---|---|---|---|---|---|
10 | 总集Whole set | 39 | 0.347 | 0.456 | 0.393 | 0.024 | 0.060 |
建模集Modeling set | 30 | 0.347 | 0.456 | 0.394 | 0.026 | 0.065 | |
检验集Verification set | 9 | 0.363 | 0.412 | 0.392 | 0.016 | 0.041 | |
20 | 总集Whole set | 39 | 0.368 | 0.507 | 0.476 | 0.048 | 0.101 |
建模集Modeling set | 30 | 0.403 | 0.507 | 0.489 | 0.044 | 0.091 | |
检验集Verification set | 9 | 0.368 | 0.504 | 0.440 | 0.038 | 0.087 |
Fig. 2 Method of soil moisture monitoring by multi spectral remote sensing with unmanned aerial vehicle UAV, Unmanned aerial vehicle; PLSR, Partial least squares regression. The same as below.
指标Index | VIF | 指标Index | VIF |
---|---|---|---|
蓝Blue | 35.935 | 近红外Near-infrared | 46.548 |
绿Green | 27.135 | NDVI | 101.345 |
红Red | 24.573 | EVI | 99.657 |
红边Red edge | 48.147 | PDI | 34.640 |
Table 2 Statistical analysis of variance inflation factor (VIF)
指标Index | VIF | 指标Index | VIF |
---|---|---|---|
蓝Blue | 35.935 | 近红外Near-infrared | 46.548 |
绿Green | 27.135 | NDVI | 101.345 |
红Red | 24.573 | EVI | 99.657 |
红边Red edge | 48.147 | PDI | 34.640 |
建模方法 Modeling method | 深度 Depth/cm | 建模结果 Modeling result | R2 | RMSE |
---|---|---|---|---|
逐步回归法 Stepwise regression | 10 | Y=-0.396B1-0.232B2-0.068N+0.508 | 0.885 | 0.009 |
20 | Y=-2.695B2+0.960B5+1.019E-1.072P+1.298 | 0.782 | 0.016 | |
岭回归法 Ridge regression | 10 | Y=0.021B1-0.084B2-0.301B3-0.252B4-0.086B5-0.063N+0.064E-0.255P+0.428 | 0.762 | 0.013 |
20 | Y=-0.125B1-0.244B2+0.068B3-0.330B4-0.009B5+0.075N-0.101E-0.304P +0.871 | 0.668 | 0.023 | |
偏最小二乘法 Partial least squares regression | 10 | Y=0.076B1-0.293B2-0.255B3-0.179B4+0.204B5-0.755N+0.983E-0.151P +0.643 | 0.838 | 0.009 |
20 | Y=-1.085B1-0.101B2-0.400B3-0.514B4+0.803B5-0.557N-0.034E-0.339P +0.938 | 0.737 | 0.020 |
Table 3 Multiple regression models of soil moisture based on reflectance of different bands
建模方法 Modeling method | 深度 Depth/cm | 建模结果 Modeling result | R2 | RMSE |
---|---|---|---|---|
逐步回归法 Stepwise regression | 10 | Y=-0.396B1-0.232B2-0.068N+0.508 | 0.885 | 0.009 |
20 | Y=-2.695B2+0.960B5+1.019E-1.072P+1.298 | 0.782 | 0.016 | |
岭回归法 Ridge regression | 10 | Y=0.021B1-0.084B2-0.301B3-0.252B4-0.086B5-0.063N+0.064E-0.255P+0.428 | 0.762 | 0.013 |
20 | Y=-0.125B1-0.244B2+0.068B3-0.330B4-0.009B5+0.075N-0.101E-0.304P +0.871 | 0.668 | 0.023 | |
偏最小二乘法 Partial least squares regression | 10 | Y=0.076B1-0.293B2-0.255B3-0.179B4+0.204B5-0.755N+0.983E-0.151P +0.643 | 0.838 | 0.009 |
20 | Y=-1.085B1-0.101B2-0.400B3-0.514B4+0.803B5-0.557N-0.034E-0.339P +0.938 | 0.737 | 0.020 |
建模方法 Modeling method | 深度 Depth/cm | R2 | RMSE | RPD |
---|---|---|---|---|
逐步回归法 Stepwise regression | 10 | 0.899 | 0.005 | 3.091 |
20 | 0.865 | 0.016 | 2.220 | |
岭回归法 Ridge regression | 10 | 0.843 | 0.008 | 2.020 |
20 | 0.814 | 0.020 | 1.095 | |
偏最小二乘法 Partial least squares regression | 10 | 0.856 | 0.008 | 2.142 |
20 | 0.831 | 0.017 | 2.136 |
Table 4 Accuracy of soil moisture content inversion
建模方法 Modeling method | 深度 Depth/cm | R2 | RMSE | RPD |
---|---|---|---|---|
逐步回归法 Stepwise regression | 10 | 0.899 | 0.005 | 3.091 |
20 | 0.865 | 0.016 | 2.220 | |
岭回归法 Ridge regression | 10 | 0.843 | 0.008 | 2.020 |
20 | 0.814 | 0.020 | 1.095 | |
偏最小二乘法 Partial least squares regression | 10 | 0.856 | 0.008 | 2.142 |
20 | 0.831 | 0.017 | 2.136 |
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