Compaction and Permeability of Oil-Shale Aggregates at High Temperatures

1980 ◽  
Vol 20 (02) ◽  
pp. 95-104 ◽  
Author(s):  
D. Trimmer ◽  
H.C. Heard

Abstract We have measured the change in bulk volume and permeability of an oil-shale aggregate subjected to high temperatures and pressures in a one-dimensional strain loading configuration. At stresses of 0.69 to 6.2 MPa and temperatures as high as 700 deg. C, the 6-liter sample may compact by as much as one-third, and permeability may decrease by factors of 10 to 100. Then is no simple relationship between strain or porosity and permeability. Attempts to analyze the data in terms of a Kozeny-type equation were unsuccessful. Introduction Most proposed methods for extracting hydrocarbons from oil shale involve either injection of hot gases or in-situ combustion of air/oxygen in the shale to produce reaction temperatures in excess of 300 deg. C. Unfortunately, undisturbed oil shale is not permeable enough to permit the hot gases to circulate freely. Thus, before these processing methods can become technically and economically feasible, some satisfactory fracturing treatment must be developed.The advocates of modified in-situ processes for recovering oil from oil shale propose to solve the permeability problem by extracting about 20% of the shale and blasting in slots or raises to form a cylindrical or prismatic rubble column. In the Rubble In-Situ Extraction (RISE) process, a modified sublevel caving operation is used to form a rubble column 50 to 150 m wide and 100 to 300 m high. However, when such a rubble column is retorted by either in-situ combustion or heat transfer from hot, circulating gases, the mechanical properties of both the shale particles and the wall rock will deteriorate, and the initial permeability (and porosity) may decrease as a result of compaction in the aggregate. Compaction occurs because of body forces (product of density times acceleration) acting within the rubble column itself.Although it is not yet clear what permeability or porosity values are adequate for retort operation or even what the optimum rubble column sizes and aspect ratios are, it is clear that certain quantitative data will be needed to design a successful in-situ oilshale retort. For example, measurements of temperature- and time-dependent compaction and permeability in different grades of oil shale over the range of stresses and temperatures to be expected in a retort column must be made. Data also are needed on the effect of particle-size distribution on compaction and permeability for differing grades of shale. Finally, the temperature- and time-dependent strength and frictional behavior of the wall rock and the aggregate must be studied.In this paper, we present laboratory measurements of the permeability and compaction behavior of aggregates formed from 103-L/t oil shale during retorting to high temperatures under several constant stresses. Further work at other heating rates, particle-size distributions, and oil-shale grades remains to be done. Data on the mechanical behavior of solid samples and aggregates from a spectrum of oil-shale grades are reported elsewhere. Previous Work Data on the creep/permeability behavior of oil-shale aggregates of several grades and particle-size distributions have been reported by Tisot and Sohns, Burwell el al., and Needham. Those data relevant to this study are summarized in Table 1.Tisot and Sohns report creep/permeability data for four grades of oil-shale aggregate (113, 144, 190, and 265 L/t) tested at axial stresses of 155, 138, and 2.24 MPa. These tests were conducted on samples 5.08 cm long and 1.90 cm in diameter comprising oil-shale particles 0.48 to 0.95 cm in diameter. The samples were heated from ambient temperatures to 385 or 440 deg. C at 67 deg. C/hr and then maintained at that value for about 10 hours. SPEJ P. 95^

MRS Advances ◽  
2020 ◽  
Vol 5 (29-30) ◽  
pp. 1623-1623
Author(s):  
Adriana Valério ◽  
Sérgio L. Morelhão ◽  
Alex J. Freitas Cabral ◽  
Márcio M. Soares ◽  
Cláudio M. R. Remédios

2021 ◽  
Author(s):  
Liang Ran ◽  
Zhaoze Deng ◽  
Yunfei Wu ◽  
Jiwei Li ◽  
Zhixuan Bai ◽  
...  

Abstract. In-situ measurements of vertically resolved particle size distributions based on a tethered balloon system were carried out for the first time in the highland city of Lhasa over the Tibetan Plateau in summer 2020, using portable optical counters for the size range of 0.124~32 μm. The vertical structure of 112 aerosol profiles was found to be largely shaped by the evolution of the boundary layer (BL), with a nearly uniform distribution of aerosols within the daytime mixing layer and a sharp decline with the height in the shallow nocturnal boundary layer. During the campaign, the average mass concentration of particulate matters smaller than 2.5 μm in aerodynamic diameter (PM2.5) within the BL was around 3 μg m−3, almost four times of the amount in the free troposphere (FT), which was rarely affected by surface anthropogenic emissions. Though there was a lower level of particle mass in the residual layer (RL) than in the BL, a similarity in particle mass size distributions (PMSDs) suggested that particles in the RL might be of the same origin as particles in the BL. This was also in consistence with the source apportionment analysis based on the PMSDs. Three distinct modes were observed in the PMSDs for the BL and the RL. One mode was exclusively coarse particles up to roughly 15 μm and peaked around 5 μm. More than 50 % of total particle mass was often contributed by coarse mode particles in this area, which was thought to be associated with local dust resuspension. The mode peaking over 0.5~0.7 μm was representative of biomass burning on religious holidays and was found to be most pronounced on holiday mornings. The contribution from the religious burning factor rose from about 25 % on non-holidays to nearly 50 % on holiday mornings. The mode dominated by particles smaller than 0.3 μm was thought to be associated with combustion related emissions and/or secondary aerosol formation. In the FT coarse mode particles only accounted for less than 10 % of the total mass and particles larger than 5 μm were negligible. The predominant submicron particles in the FT might be related to secondary aerosol formation and the aging of existed particles. To give a full picture of aerosol physical and chemical properties and better understand the origin and impacts of aerosols in this area, intensive field campaigns involving measurements of vertically resolved aerosol chemical compositions in different seasons would be much encouraged in the future.


2003 ◽  
Vol 3 (3) ◽  
pp. 881-891 ◽  
Author(s):  
M. Fiebig ◽  
A. Stohl ◽  
M. Wendisch ◽  
S. Eckhardt ◽  
A. Petzold

Abstract. During airborne in situ measurements of particle size distributions in a forest fire plume originating in Northern Canada, an accumulation mode number mean diameter of 0.34 mm was observed over Lindenberg, Germany on 9 August 1998. Realizing that this is possibly the largest value observed for this property in a forest fire plume, scenarios of plume ageing by coagulation are considered to explain the observed size distribution, concluding that the plume dilution was inhibited in parts of the plume. The uncertainties in coagulation rate and transition from external to internal mixture of absorbing forest fire and non-absorbing background particles cause uncertainties in the plume's solar instantaneous radiative forcing of 20-40% and of a factor of 5-6, respectively. Including information compiled from other studies on this plume, it is concluded that the plume's characteristics are qualitatively consistent with a radiative-convective mixed layer.


Author(s):  
Justyna Edgar ◽  
Richard C. Ghail ◽  
James Lawrence ◽  
Jacqueline Skipper ◽  
Philippa J. Mason

The Eocene Harwich Formation, underlying the Greater London (UK) area, presents many construction problems for design and location of tunnels, pipelines, and other engineering infrastructure projects. Variable deposits make up the sequence of the Harwich Formation. These include cemented fault zones, hard grounds, loose gravel and sand that, when unexpectedly encountered, can cause construction delays and increase costs. Here, we interpret borehole cores and logs, in-situ observations coupled with borehole derived samples, and calculate particle-size distributions to develop a general facies model that accounts for the lithological distribution within the Harwich Formation. This provides an improved geological framework for proposed subsurface construction that can reduce inherent engineering uncertainties, not only in the London region, but potentially in other similar geological environments.


2021 ◽  
Vol 21 (19) ◽  
pp. 15259-15282
Author(s):  
Christoph Mahnke ◽  
Ralf Weigel ◽  
Francesco Cairo ◽  
Jean-Paul Vernier ◽  
Armin Afchine ◽  
...  

Abstract. The Asian summer monsoon is an effective pathway for aerosol particles and precursors from the planetary boundary layer over Central, South, and East Asia into the upper troposphere and lower stratosphere. An enhancement of aerosol particles within the Asian monsoon anticyclone (AMA), called the Asian tropopause aerosol layer (ATAL), has been observed by satellites. We discuss airborne in situ and remote sensing observations of aerosol microphysical properties conducted during the 2017 StratoClim field campaign within the AMA region. The aerosol particle measurements aboard the high-altitude research aircraft M55 Geophysica (maximum altitude reached of ∼20.5 km) were conducted with a modified ultra-high-sensitivity aerosol spectrometer – airborne (UHSAS-A; particle diameter detection range of 65 nm to 1 µm), the COndensation PArticle counting System (COPAS, detecting total concentrations of submicrometer-sized particles), and the New Ice eXpEriment – Cloud and Aerosol Spectrometer with Detection of POLarization (NIXE-CAS-DPOL). In the COPAS and UHSAS-A vertical particle mixing ratio (PMR) profiles and the size distribution profiles (for number, surface area, and volume concentration), the ATAL is evident as a distinct layer between ∼370 and 420 K potential temperature (Θ). Within the ATAL, the maximum detected PMRs (from the median profiles) were ∼700 mg−1 for particle diameters between 65 nm and 1 µm (UHSAS-A) and higher than 2500 mg−1 for diameters larger than 10 nm (COPAS). These values are up to 2 times higher than those previously found at similar altitudes in other tropical locations. The difference between the PMR profiles measured by the UHSAS-A and the COPAS indicate that the region below the ATAL at Θ levels from 350 to 370 K is influenced by the nucleation of aerosol particles (diameter <65 nm). We provide detailed analyses of the vertical distribution of the aerosol particle size distributions and the PMR and compare these with previous tropical and extratropical measurements. The backscatter ratio (BR) was calculated based on the aerosol particle size distributions measured in situ. The resulting data set was compared with the vertical profiles of the BR detected by the multiwavelength aerosol scatterometer (MAS) and an airborne miniature aerosol lidar (MAL) aboard the M55 Geophysica and by the satellite-borne Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP). The data of all four methods largely agree with one another, showing enhanced BR values in the altitude range of the ATAL (between ∼15 and 18.5 km) with a maximum at 17.5 km altitude. By means of the AMA-centered equivalent latitude calculated from meteorological reanalysis data, it is shown that such enhanced values of the BR larger than 1.1 could only be observed within the confinement of the AMA.


Sign in / Sign up

Export Citation Format

Share Document