X-Ray Tomography of Soil Properties

Author(s):  
Jan W. Hopmans ◽  
Milena Cislerova ◽  
Tomas Vogel
Keyword(s):  
2017 ◽  
Author(s):  
William A Millington ◽  
Paula A Misiewicz ◽  
David R White ◽  
Edward T Dickin ◽  
Sacha J Mooney ◽  
...  

2017 ◽  
Vol 41 (6) ◽  
pp. 648-664 ◽  
Author(s):  
Sérgio Henrique Godinho Silva ◽  
Anita Fernanda dos Santos Teixeira ◽  
Michele Duarte de Menezes ◽  
Luiz Roberto Guimarães Guilherme ◽  
Fatima Maria de Souza Moreira ◽  
...  

ABSTRACT Determination of soil properties helps in the correct management of soil fertility. The portable X-ray fluorescence spectrometer (pXRF) has been recently adopted to determine total chemical element contents in soils, allowing soil property inferences. However, these studies are still scarce in Brazil and other countries. The objectives of this work were to predict soil properties using pXRF data, comparing stepwise multiple linear regression (SMLR) and random forest (RF) methods, as well as mapping and validating soil properties. 120 soil samples were collected at three depths and submitted to laboratory analyses. pXRF was used in the samples and total element contents were determined. From pXRF data, SMLR and RF were used to predict soil laboratory results, reflecting soil properties, and the models were validated. The best method was used to spatialize soil properties. Using SMLR, models had high values of R² (≥0.8), however the highest accuracy was obtained in RF modeling. Exchangeable Ca, Al, Mg, potential and effective cation exchange capacity, soil organic matter, pH, and base saturation had adequate adjustment and accurate predictions with RF. Eight out of the 10 soil properties predicted by RF using pXRF data had CaO as the most important variable helping predictions, followed by P2O5, Zn and Cr. Maps generated using RF from pXRF data had high accuracy for six soil properties, reaching R2 up to 0.83. pXRF in association with RF can be used to predict soil properties with high accuracy at low cost and time, besides providing variables aiding digital soil mapping.


Soil Research ◽  
1995 ◽  
Vol 33 (4) ◽  
pp. 621 ◽  
Author(s):  
LJ Janik ◽  
JO Skjemstad ◽  
MD Raven

Chemical analysis is an important but often expensive and time-consuming step in the characterization of soils. Methods used for soil analysis ideally need to be rapid, accurate and relatively simple and infrared partial least squares (PLS) analysis is potentially one such method. Mid-infrared diffuse reflectance Fourier transform (DRIFT) spectra of powdered soils present the major mineralogical and organic components within each soil, relative to their concentrations. The theory indicates that experimentally derived soil properties may be correlated with the infrared spectra of some of these components, and the covariance between soil properties and spectra can then be modelled by PLS loadings and scores. Factors and scores can be derived independently for each Soil property using PLS-1, an extension of the more general PLS-2 method. This study evaluates the use of PLS-1 for the qualitative and quantitative study of soils, and in particular to classify the soil spectra and their associated major element chemistry by their PLS loadings and Scores. A subset of 100 soils, selected from a complete set of 298 samples from throughout eastern and southern Australia, was analysed by X-ray fluorescence (XRF) for major oxides as a calibration or training set to model the PLS loadings, scores and linear regression coefficients. Linear regressions resulted with R(2) values of 0 . 973-0 . 917 for XRF versus PLS predicted values for SiO2, Al2O3 and Fe2O3. Regressions for the other oxides, e.g. TiO2, MgO and CaO, were generally curved with a linear calibration giving severe underestimations at high concentrations. The PLS loadings and regression coefficients were then used to model the complete soil set to produce scores and concentration predictions for all the samples. The samples were plotted in bivariate score maps to give a visual representation of the spectral variability within the entire soil set. Samples were selected from the boundaries of the groups of soils in these maps for mineralogical characterization using X-ray diffraction (XRD) analysis. The XRD results confirmed the mineralogy obtained from the infrared spectra and PLS weight loadings. For this study, the depiction of the samples in the score maps was found to be of particular importance for demonstrating similarities in composition of the samples.


Geoderma ◽  
2018 ◽  
Vol 329 ◽  
pp. 43-53 ◽  
Author(s):  
Benjamin M. Butler ◽  
Sharon M. O’Rourke ◽  
Stephen Hillier

2015 ◽  
Vol 79 (5) ◽  
pp. 1375-1385 ◽  
Author(s):  
Erick K. Towett ◽  
Keith D. Shepherd ◽  
Andrew Sila ◽  
Ermias Aynekulu ◽  
Georg Cadisch

Clay Minerals ◽  
1984 ◽  
Vol 19 (5) ◽  
pp. 737-744 ◽  
Author(s):  
B. F. L. Smith ◽  
B. D. Mitchell

AbstractMixed SiO2-Al2O3-Fe2O3 gel systems are a feature of many Scottish soils. They are usually associated with the surface of primary soil particles and consequently when present even in small amounts can have an effect on soil properties incommensurate with the proportion present. Currently, chemical dissolution methods provide the most satisfactory means of assessment. A range of chemical techniques, including dissolution by alkali, dithionite, acid oxalate and pyrophosphate, trimethylsilylation and fluoride exchange, have been used to examine the inorganic gel in a Scottish brown forest soil developed on glacial till derived from epidiorite. The reactivity of the gel, as determined by fluoride exchange, is similar to that reported for Japanese and New Zealand allophanic soils.


2020 ◽  
Vol 2020 ◽  
pp. 1-23 ◽  
Author(s):  
Fazal E. Jalal ◽  
Yongfu Xu ◽  
Babak Jamhiri ◽  
Shazim Ali Memon

Calcium-based stabilizer materials (CSMs) exhibit pozzolanic properties which improve the properties of clayey soils by hydration, cation exchange, flocculation, pozzolanic reaction, and carbonation. In this comprehensive review, comprising over past three decades from 1990 to 2019, a mechanistic literature of expansive soil stabilization by incorporating CSMs is presented by reviewing 183 published research articles. The advantages and disadvantages of CSMs as the ground stabilizing agent are succinctly presented, and the major outcomes of physicochemical effects on soil properties are discussed in detail. After blending with CSM, the main and interaction effects on soil properties with focus on chemical processes such as X-ray fluorescence, X-ray diffraction analyses, and microstructure interaction by using scanning electron microscopy and thermogravimetric analysis have been reviewed in light of findings of past researchers. This work will help geotechnical engineers to opt for suitable CSM in the field of geoenvironmental engineering in committing to sustainable construction of civil engineering structures over expansive soils.


2012 ◽  
Vol 185 (3) ◽  
pp. 2377-2394 ◽  
Author(s):  
Songul Akbulut ◽  
ReneVan Grieken ◽  
Mehmet A. Kılıc ◽  
Ugur Cevik ◽  
Giuliana G. Rotondo

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