Abstract :
55 surface and sub-surface samples of expansive soils were collected. Clay mineral composition and smectite contents were measured using XRD and dye absorption methods. The effective smectite contents were calculated. Meanwhile, the visible-short wave infrared spectra of the swelling soils was collected, the spectral absorption indices, such as wavelength position, depth, width, asymmetry, area, were calculated automatically. Then, the correlation relationships between the spectral indices and the smectite contents and the colloid contents and clay contents of the swelling soils were statistically analyzed. The results show that the very high, high, medium, weak potential soils can be identified according to the relative strengths of the 2200 nm, 1900 nm, 1400 nm absorptions in the spectral features of the swelling soils. The laboratory spectral measurement and analysis techniques to the dried and homogenous swelling soils can be productively used for quickly, economically, and conveniently identifying swelling soils, estimating the contents of smectite, colloid, and clay in fields
Keywords :
X-ray diffraction; clay; minerals; soil; spectral analysis; statistical analysis; terrain mapping; 1400 nm; 1900 nm; 2200 nm; XRD; clay mineral composition; colloid content; correlation relationship; dye absorption method; laboratory spectral measurement; relative strength; smectite content index; spectral absorption index; spectral feature; statistical analysis; swelling soil; visible-short wave infrared spectra; wavelength area; wavelength asymmetry; wavelength depth; wavelength position; wavelength width; Area measurement; Electromagnetic wave absorption; Geologic measurements; Laboratories; Lakes; Minerals; Remote sensing; Soil measurements; Wavelength measurement; X-ray scattering;