scholarly journals Gas diffusivity‐based characterization of aggregated soils linking to methane migration in shallow subsurface

2021 ◽  
Author(s):  
M. Shanujah ◽  
Chamindu Deepagoda ◽  
Kathleen M. Smits ◽  
V. Shreedharan ◽  
T. G. Paramrswaran ◽  
...  
2003 ◽  
Vol 75 (2) ◽  
pp. 235-248 ◽  
Author(s):  
Dilce F. Rossetti

The geological characterization of shallow subsurface Neogene deposits in northeastern Pará State using Ground Penetrating Radar (GPR) revealed normal and reverse faults, as well as folds, not yet well documented by field studies. The faults are identified mostly by steeply-dipping reflections that sharply cut the nearby reflections causing bed offsets, drags and rollovers. The folds are recognized by reflections that are highly undulating, configuring broad concave and convex-up features that are up to 50 m wide and 80 to 90 ns deep. These deformation structures are mostly developed within deposits of Miocene age, though some of the faults might continue into younger deposits as well. Although the studied GPR sections show several diffractions caused by trees, differential degrees of moisture, and underground artifacts, the structures recorded here can not be explained by any of these ''noises''. The detailed analysis of the GPR sections reveals that they are attributed to bed distortion caused by brittle deformation and folding. The record of faults and folds are not widespread in the Neogene deposits of the Bragantina area. These GPR data are in agreement with structural models, which have proposed a complex evolution including strike-slip motion for this area from the Miocene to present.


2013 ◽  
Vol 12 (3) ◽  
pp. vzj2013.03.0061 ◽  
Author(s):  
T.K.K. Chamindu Deepagoda ◽  
Per Moldrup ◽  
Markus Tuller ◽  
Mette Pedersen ◽  
Jose Choc Chen Lopez ◽  
...  

Author(s):  
D. Martí Linares ◽  
I. Marzán ◽  
J. Sachsenhausen ◽  
J. Álvarez-Marrón ◽  
I. Cienfuegos ◽  
...  

2021 ◽  
Author(s):  
Guillaume Blanchy ◽  
Paul McLachlan ◽  
Matteo Censini ◽  
Jacopo Boaga ◽  
Andrew Binley ◽  
...  

<p>Advanced modeling of hydrological processes in mountain catchments requires accurate characterization of the shallow subsurface, and in particular the depth to the soil/bedrock interface. Frequency domain electromagnetic induction (EMI) methods are well suited to this challenge as they have short acquisition times and do not require direct coupling with the ground; consequently they can be highly productive. Moreover, although traditionally used for revealing lateral electrical conductivity changes, EMI inversion is increasingly used to quantitatively resolve both lateral and vertical changes. These quantitative models can then be used to inform several properties relevant for hydrological modelling (e.g. water content, permeability).</p><p>In this work the open-source software EMagPy is used to compare between EMI data collected with a multi-coil device (i.e. a single frequency device with multiple receiver coils) and a multi-frequency device (i.e. a single inter-coil distance and multiple frequencies). The latter instrument is easier to handle because of its shorter length and lower weight, and thus it is potentially more suitable for the rugged topography of mountain slopes. However it is important to compare the value of information (e.g. sensitivity patterns and data quality) obtained from both instruments.</p><p>To begin with, the performance of both devices is assessed using synthetic modeling. Following from this the analysis is focused on two mountainous catchments: one located in the Alpine region above 2000 m a.s.l., the other in a Mediterranean catchment in Southern Italy. Both sites have differing geological and hydrological conditions and provide a useful comparison to determine the suitability of multi-frequency and multi-coil devices, and highlight necessary considerations of EMI acquisition.</p>


2018 ◽  
Vol 17 (1) ◽  
pp. 180026 ◽  
Author(s):  
T.K.K. Chamindu Deepagoda ◽  
Kathleen Smits ◽  
J.R.R.N. Jayarathne ◽  
Benjamin M. Wallen ◽  
Timothy J. Clough

2020 ◽  
Vol 84 (2) ◽  
pp. 387-398 ◽  
Author(s):  
J. R. R. N. Jayarathne ◽  
T. K. K. Chamindu Deepagoda ◽  
Timothy J. Clough ◽  
M.C.M. Nasvi ◽  
Steve Thomas ◽  
...  

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