Exploring Nonlinear Mechanical Behaviour of Rocks at LANCE
SMARTS - Spectrometer for Materials Research at Temperature and Stress
Atomic-scale stress-strain information obtained from the neutron Rietveld data indicate that the strain experienced by the crystalline quartz is ~1/5 of the macroscopic strain (the rest taken up by the grain contacts and bonds in the rock). No hints of nonlinearity whatsoever are evident in the neutron data.
Conclusion? The grain bond system (a small fraction of the total rock) is responsible for all the peculiar quasi-static nonlinearity we see.
Beamlines at the LANSCE (Los Alamos Neutron Science Center)/Lujan Center - LANSCE produces intense sources of pulsed protons and spallation neutrons from a tungsten target. Proton beam currents during all the experiments varied from 100 to 110 µA.
The Neutron Powder Diffractometer has the unique capability of simultaneous high-Q Rietveld and pair-density function analyses, enabling determination of the average and local structures of complex materials with high accuracy. The questions these experiments are designed to answer are (1) can neutrons "see" the grain bond system and if so, (2) can neutrons help to ascertain the role(s) of intergranular bonds vs. the bulk crystalline volume in the nonlinear behaviour of rocks? Results below show evidence of non-crystalline silica in a pure quartz sandstone.
Above - Rietveld analysis shows an excellent match with crystalline quartz; there are no other crystal phases in Fontainebleau sandstone.
Above - A revised model adding ~7% amorphous silica to the crystal model makes a greatly improved fit.
Above - When the PDF data (red crosses) is compared to a perfect quartz model, there is a large discrepancy in the nearest neighbor peaks.
Above - PDF data (red) of amorphous silica shows that only the nearest neighbor peaks are sharp and correspond with those of the crystal (blue).
HIPPO's proximity to the neutron spallation source and its numerous detectors mean it can watch atomic plane structures change in real time. Counting for 1 minute or less is sufficient for a Rietveld analysis of the scattering data. Scattering experiments were performed to observe the crystalline structure of sandstone samples undergoing periodic temperature changes. Modulus (resonance frequency) and temperature was tracked as a function of time. Neutron results -unit cell volume- show none of the peculiar macroscopic nonlinear behavior.
History - Modulus drop observed after a temperature change IN either direction for a sample of Berea sandstone
Sandstone sample in holder, thermocouples, and a piezoelectric source and receiver all mounted in an isothermal temperature chamber and mylar thermal radiation shielding.
Corresponding shift of frequency as temperature changed.
Plot of temperature and unit cell volume during the experiment.
Work supported by Office of Basic Energy Sciences, DOE, with Los Alamos National Laboratory Institutional Support.
HTML conversion by Jeff Simpson.