To compliment and extend these approaches, we present a study from an active landslide in a Lias Group clay slope, North Yorkshire, UK, examining combined P- and S-wave seismic refraction tomography (SRT) as a means of providing subsurface volumetric imaging of geotechnical proxies.
Neotectonic deformation in the western and central part of the Pannonian Basin was investigated by means of surface and subsurface structural analyses, and geomorphologic observations.
Methods and instruments are grouped into geophysical package, means of access to the subsurface, methods of chemical and structural characterization, and methods to assess physical conditions on the surface.
Simulated-annealing-based conditional simulations provide a flexible means of quantitatively integrating diverse types of subsurface data.
The development of remote sensing tools, such as side-looking airborne radar (SLAR), facilitated the observation of surface features as a means of acquiring information about the subsurface.
In the context of subsurface drainage, the mitigation of agricultural pollutants means intercepting water flows using green infrastructures such as constructed wetlands (CWs).
The main purpose of this research is to investigate Las Bombas volcano 3D subsurface architecture by means of geophysical methods.
Here, we investigate the utility of biofilms, which are microorganism assemblages firmly attached to a surface, as a means of reducing the permeability of deep subsurface porous geological matrices under high pressure and in the presence of SC-CO2, using a unique high pressure (8.9 MPa), moderate temperature (32 °C) flow reactor containing 40 millidarcy Berea sandstone cores.
Another important concept is that of subsurface diagnostic horizons.
A week later, scientists announced that they had detected strong signs of subsurface ice.
