Inorganic Plume Delineation Using Surface High-Resolution Electrical Resistivity at the BC Cribs and Trenches Site, Hanford

2007 ◽  
Vol 6 (4) ◽  
pp. 946-958 ◽  
Author(s):  
Dale F. Rucker ◽  
James B. Fink
Energies ◽  
2019 ◽  
Vol 12 (22) ◽  
pp. 4302 ◽  
Author(s):  
Abdulrauf R. Adebayo ◽  
Lamidi Babalola ◽  
Syed R. Hussaini ◽  
Abdullah Alqubalee ◽  
Rahul S. Babu

The petrophysical characterization of tight gas sands can be affected by clay minerals, gas adsorption, microfractures, and the presence of high-density minerals. In this study, we conducted various petrophysical, petrographic, and high-resolution image analyses on Saudi Arabian tight sand in order to understand how a complex pore system responds to measurement tools. About 140 plug samples extracted from six wells were subjected to routine core analyses including cleaning, drying, and porosity–permeability measurements. The porosity–permeability data was used to identify hydraulic flow units (HFU). In order to probe the factors contributing to the heterogeneity of this tight sand, 12 subsamples representing the different HFUs were selected for petrographic study and high-resolution image analysis using SEM, quantitative evaluation of minerals by scanning electron microscope (QEMSCAN), and micro-computed tomography (µCT). Nuclear magnetic resonance (NMR) and electrical resistivity measurements were also conducted on 56 subsamples representing various lithofacies. NMR porosity showed good agreement with other porosity measurements. The agreement was remarkable in specific lithofacies with porosity ranging from 0.1% to 7%. Above this range, significant scatters were seen between the porosity methods. QEMSCAN results revealed that samples with <7% porosity contain a higher proportion of clay than those with porosity >7%, which are either microfractured or contain partially dissolved labile minerals. The NMR T2 profiles also showed that samples with porosity <7% are dominated by micropores while samples with porosity >7% are dominated by macropores. Analysis of the µCT images revealed that pore throat sizes may be responsible for the poor correlation between NMR porosity and other porosity methods. NMR permeability values estimated using the Shlumberger Doll Research (SDR) method are fairly correlated with helium permeability (with an R2 of 0.6). Electrical resistivity measurements showed that the different rock types fall on the same slope of the formation factors versus porosity, with a cementation factor of 1.5.


2021 ◽  
Vol 58 (3) ◽  
pp. 109-117
Author(s):  
Ching-Ying TSOU ◽  
Kousei YAMABE ◽  
Daisuke HIGAKI ◽  
Takayoshi SASAGAWA ◽  
Tomo KIRIU ◽  
...  

1998 ◽  
Vol 12 (22) ◽  
pp. 2263-2278 ◽  
Author(s):  
S. Chakraborty ◽  
B. Schnell ◽  
G. Thummes ◽  
A. K. Majumdar

High-resolution transverse magnetoresistance (TMR) data in γ- Cu 100-x Mn x alloys (x = 36, 60, 73, 76 and 83) are presented till 7.5 T at 4.2, 20.5 and 63 K and longitudinal (LMR) magnetoresistance at 4.2 K. They show positive magnetoresistance till 7.5 T in the Mn-rich (x≥60) alloys while an overall negative one in the alloy with x = 36 at all temperatures. However, the data at 4.2 K in x=36 clearly demonstrate a positive magnetoresistance till 3 T which becomes negative at higher fields. The data for the Mn-rich alloys (x ≥ 60) at 4.2 and 20.5 K are well described by the electron–electron interaction effects (EEI) along with localisation and normal magnetoresistance. In the two regions of high (4 to 7.5 T) and low (0 to 1 T) fields, distinctly dominant contribution of EEI effects compared to that of localisation has been observed. For x = 36, an additional term due to the cluster-glass (CG) phase (=-β CG H2) has to be considered in explaining its overall negative magnetoresistance. However, the EEI/localisation effects have hardly any significant contribution at 63 K. The contribution of the combined EEI and localisation effects has been separated convincingly from the normal magnetoresistance (C N ) and the cluster-glass (β CG ) terms. The temperature dependence of the normal magnetoresistance follows the Kohler's rule while the cluster-glass term shows a behavior similar to those of the dilute spin glasses. Moreover, the present interpretation of magnetoresistance is found to be very much consistent with that of the electrical resistivity (ρ(T)).


2018 ◽  
Vol 25 (3) ◽  
pp. 209-218 ◽  
Author(s):  
Osamah Saad Al-Saadi ◽  
Volkmar Schmidt ◽  
Michael Becken ◽  
Thomas Fritsch

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