scholarly journals Estimating the soil clay content and organic matter by means of different calibration methods of vis-NIR diffuse reflectance spectroscopy

2016 ◽  
Vol 155 ◽  
pp. 510-522 ◽  
Author(s):  
Said Nawar ◽  
Henning Buddenbaum ◽  
Joachim Hill ◽  
Jacek Kozak ◽  
Abdul M. Mouazen
2001 ◽  
Vol 1 ◽  
pp. 122-129 ◽  
Author(s):  
Alan Olness ◽  
Dian Lopez ◽  
David Archer ◽  
Jason Cordes ◽  
Colin Sweeney ◽  
...  

Mineralization of soil organic matter is governed by predictable factors with nitrate-N as the end product. Crop production interrupts the natural balance, accelerates mineralization of N, and elevates levels of nitrate-N in soil. Six factors determine nitrate-N levels in soils: soil clay content, bulk density, organic matter content, pH, temperature, and rainfall. Maximal rates of N mineralization require an optimal level of air-filled pore space. Optimal air-filled pore space depends on soil clay content, soil organic matter content, soil bulk density, and rainfall. Pore space is partitioned into water- and air-filled space. A maximal rate of nitrate formation occurs at a pH of 6.7 and rather modest mineralization rates occur at pH 5.0 and 8.0. Predictions of the soil nitrate-N concentrations with a relative precision of 1 to 4 μg N g–1of soil were obtained with a computerized N fertilizer decision aid. Grain yields obtained using the N fertilizer decision aid were not measurably different from those using adjacent farmer practices, but N fertilizer use was reduced by >10%. Predicting mineralization in this manner allows optimal N applications to be determined for site-specific soil and weather conditions.


2021 ◽  
Author(s):  
Gabriela Naibo ◽  
Rafael Ramon ◽  
Gustavo Pesini ◽  
Jean Michel Moura-Bueno ◽  
Claudia Alessandra Peixoto Barros ◽  
...  

<p>The intense soil use with inadequate management can result in the constant transport of sediments with chemical elements absorbed to aquatic systems. The diffuse reflectance spectroscopy in the near infrared (NIR) and medium (MIR) spectral bands associated with chemometry and machine learning, is an analytical technique that has the potential to quantify the concentration of chemical elements in the environment. However, there is no consensus on the best combination of calibration methods, spectral pre-processing and spectral ranges. Thus, the objective of this study was to evaluate the use of this technique, with the combination of different spectral bands, pre-processing techniques and machine learning to estimate the concentration of chemical elements on soil and sediment samples. In this study we used a soil and sediment database from samples collected in the Guaporé River catchment, in southern Brazil. A total of 316 soil samples and 196 sediment samples were dried, disaggregated and sieved at 63 μm. Organic carbon (CO) was quantified by wet oxidation and the total concentration of 21 elements (Al, Ba, Be, Ca, Co, Cr, Cu, Fe, K, La, Li, Mg, Mn, Na, Ni, P, Pb, Sr, Ti V and Zn) were quantified by ICP-OES after microwave assisted digestion for 9,5 min at 182ºC with HCl and HNO<sub>3 </sub>concentrated in the proportion of 3:1. The NIR (1000-2500 nm) and MIR (2500-25000 nm) spectra were obtained in all soil and sediment samples. Two machine-learning methods were tested: Partial Least Squares Regression (PLSR) and Support Vector Machine (SVM), associated with three different spectrum pre-processing methods: Detrend (DET), Savitzky-Golay Derivative (SGD) and Standard Normal Variate (SNV), compared to raw data (RAW). Performance was assessed by the coefficient of determination (R²) and the relationship between performance and interquartile distance (RPIQ). The SVM model resulted in better predictions compared to the PLSR in all evaluated cases, as indicated by the average adjustment values of the model (R²=0.87 for SVM and 0.62 for PLSR), and by the RPIQ values (7.14 for SVM and 2.22 for PLSR). The pre-processing method increased the accuracy of the estimates in the following order: RAW<SNV< DET<SGD. The best performance in relation to the spectral range was observed for the MIR region, being significantly superior to the NIR and NIR+MIR combination. The adjustment of the models calibrated with soil (R²=0.91) and sediment (R²=0.90) data was higher compared to the calibrated with the combination soil + sediment (R²=0.78). For RPIQ, the calibration model with soil data showed the highest RPIQ value (9.29), being higher and differing significantly from the others. In general, the results show that the combination of different calibration methods, spectral pre-processing and spectral ranges has an effect on the accuracy of the estimates. The studied elements can be estimated by means of diffuse reflectance spectroscopy, however it should be noted that this technique has an associated error in the estimates due to the heterogeneity of the chemical structure of the elements in the soil and sediment matrix and the reference samples obtained by chemical methods.</p>


1990 ◽  
Vol 41 (6) ◽  
pp. 761 ◽  
Author(s):  
PN Nelson ◽  
E Cotsaris ◽  
JM Oades ◽  
DB Bursill

Dissolved organic carbon (DOC) is of major importance for freshwater ecology and water treatment, particularly in Australia. Work comparing two small catchments, one yielding water with high DOC concentrations (Lawless) and the other yielding water with low DOC concentrations (Retreat Valley), is described. Differences between stream DOC concentrations in the two catchments were related to differences between the properties of the catchment soils. The Retreat Valley soils had higher C contents than the Lawless soils, but the C was less soluble, resulting in lower DOC concentrations in soil core leachates. The lower solubility of C in the Retreat Valley soils was the result of a higher clay content and hence a higher surface area for adsorption reactions. The Retreat Valley soils had a higher adsorption capacity for organic matter than did the Lawless soils. The clay contents of soils was found to be an important factor influencing stream DOC concentrations throughout the Mt Lofty Ranges, and the prediction of DOC concentrations in streams on a broad scale is discussed.


1997 ◽  
Vol 5 (2) ◽  
pp. 67-75 ◽  
Author(s):  
M. Blanco ◽  
J. Coello ◽  
H. Iturriaga ◽  
S. Maspoch ◽  
C. de la Pezuela

The results obtained by implementing Principal Component Regression (PCR) according to three different criteria for choosing principal components (PCs), and those provided by Partial Least-Squares Regression (PSLR), in the determination of the active compound in a pharmaceutical preparation by near infrared diffuse reflectance spectroscopy are compared. The PCR-top down criterion used is commonly implemented in commercially available software: it selects consecutive PCs beginning with that possessing the largest eigenvalue. The other two criteria used do not assume the PCs with the largest eigenvalues to be the best predictors for the response variable; rather, the PCR-correlation criterion chooses only those PCs exhibiting the highest correlation with the response variable, and the PCR-best subset criterion selects those that provide the lowest predicted residual sum of squares ( PRESS) for an external prediction set. All the calibration methods tested exhibited a similar predictive ability (prediction errors ranged from 1.34% to 1.49%); however, the number of PCs used in the regression varied among them. The PLSR technique did not excel the methods based on selecting the best PCs for regression. Also, the PCR-correlation and PCR-best subset methods provided the same results and used fewer PCs than the PCR-top down method.


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