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Prediction of Soil Organic Carbon for Ethiopian Highlands Using Soil Spectroscopy

机译:利用土壤光谱法预测埃塞俄比亚高地的土壤有机碳

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Soil spectroscopy was applied for predicting soil organic carbon (SOC) in the highlands of Ethiopia. Soil samples were acquired from Ethiopia’s National Soil Testing Centre and direct field sampling. The reflectance of samples was measured using a FieldSpec 3 diffuse reflectance spectrometer. Outliers and sample relation were evaluated using principal component analysis (PCA) and models were developed through partial least square regression (PLSR). For nine watersheds sampled, 20% of the samples were set aside to test prediction and 80% were used to develop calibration models. Depending on the number of samples per watershed, cross validation or independent validation were used. The stability of models was evaluated using coefficient of determination (), root mean square error (RMSE), and the ratio performance deviation (RPD). The (%), RMSE (%), and RPD, respectively, for validation were Anjeni (88, 0.44, 3.05), Bale (86, 0.52, 2.7), Basketo (89, 0.57, 3.0), Benishangul (91, 0.30, 3.4), Kersa (82, 0.44, 2.4), Kola tembien (75, 0.44, 1.9), Maybar (84. 0.57, 2.5), Megech (85, 0.15, 2.6), and Wondo Genet (86, 0.52, 2.7) indicating that the models were stable. Models performed better for areas with high SOC values than areas with lower SOC values. Overall, soil spectroscopy performance ranged from very good to good.
机译:土壤光谱学被用于预测埃塞俄比亚高地的土壤有机碳(SOC)。从埃塞俄比亚国家土壤测试中心获取土壤样品,并进行直接田间采样。使用FieldSpec 3漫反射光谱仪测量样品的反射率。使用主成分分析(PCA)评估异常值和样本关系,并通过偏最小二乘回归(PLSR)建立模型。对于九个流域采样,将20%的样本留作测试预测,并将80%的样本用于建立校准模型。根据每个流域的样本数量,使用交叉验证或独立验证。使用确定系数(),均方根误差(RMSE)和比率性能偏差(RPD)评估模型的稳定性。用于验证的(%),RMSE(%)和RPD分别为Anjeni(88,0.44,3.05),Bale(86,0.52,2.7),Basketo(89、0.57、3.0),Benishangul(91,0.30) ,3.4),Kersa(82、0.44、2.4),Kola tembien(75、0.44、1.9),Maybar(84. 0.57、2.5),Megech(85、0.15、2.6)和Wondo Genet(86、0.52、2.7) ),表明模型是稳定的。与具有较低SOC值的区域相比,具有较高SOC值的区域模型的性能更好。总体而言,土壤光谱学的性能范围从非常好。

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