Prediction of Soil Organic Carbon for Ethiopian Highlands Using Soil Spectroscopy
Author(s) -
Tadele Amare,
Christian Hergarten,
Hans Hurni,
Bettina Wolfgramm,
Birru Yitaferu,
Yihenew G. Selassie
Publication year - 2013
Publication title -
isrn soil science
Language(s) - English
Resource type - Journals
ISSN - 2090-875X
DOI - 10.1155/2013/720589
Subject(s) - coefficient of determination , mean squared error , soil test , correlation coefficient , partial least squares regression , soil carbon , mathematics , analytical chemistry (journal) , mineralogy , algorithm , geology , soil water , chemistry , soil science , statistics , environmental chemistry
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.
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