4,695 research outputs found
Group portrait of Dr J. Leach, L. Chandler, C. McLennan, C. Barrett, A.J. Campbell, D. Le Souef, T. Tregallas, Z. Gray, Gregory Mathews at the R.A.O.U council meeting, March 10, 1914 [picture].
No full textInscription: "R A O U council meeting in Botanic Garden Melbourne Tuesday March 10 '14 to meet Gregory M Matthews [sic] esq. From Left to Right, Dr Leach, Mr Chandler, C. McLennan (Mallee Bird), C. Barrett, A.J. Campbell, D. Le Souef, T. Tregallas, Z. Gray, Gregory Mathews"--On reverse; Part of G.M. Mathews collection of portraits of ornithologists.; Title devised by cataloguer from inscription.; Also available in an electronic version via the Internet at: http://nla.gov.au/nla.pic-vn3799771; Papers of Gregory M. Mathews, 1900-1949; located at; National Library of Australia Manuscript collection MS 1465
Autobiography by Mrs. J. C. Jones
No full textTypescript of a biographical sketch of Johanna Christina (Larson) Jones, from an interview. Mrs. Jones was born in Sweden in 1854, and her family came to Utah in 1860, settling in Washington. She and her husband settled at Overton, Nevada. Typed by Louise R. Mathews for the WPA Historical Records Survey in 193
Mathews, Andrew J.
No full textImogene C. Mathews - wifehttps://stars.library.ucf.edu/cfm-ch-memoranda-1929/1118/thumbnail.jp
Howard Merry, D. M. Mathews, and V. C. Perini, Jr. at Matthews Ranch
No full textCopy negative of a picture of men thought to be Howard Merry, D. M. Mathews, V. C. Perini, Jr., and Judge J. R. Mathews standing outside at the Mathews Ranch. Howard Merry is holding a large piece of paper. In handwriting, above the man on the left's head is written "?Bud?" under the second man is written "Howard Merry," under the third man is written "Judge, J. R. Mathews," and at the bottom of the photograph is written, "Mathews Ranch, 729 Throckmorton Co Texas," with more that is cut off
C. H. A. Greene, Marietta, certificate to John Mathews
No full textCertificate granting J. Mathews permission to occupy and improve the land at Amberson's Bottom
Permeability evolution in sorbing media. Analogies between organic-rich shale and coal
No full textShale gas reservoirs like coalbed methane (CBM) reservoirs are promising targets for geological sequestration of carbon dioxide (CO2). However, the evolution of permeability in shale reservoirs on injection of CO2 is poorly understood unlike CBM reservoirs. In this study, we report measurements of permeability evolution in shales infiltrated separately by nonsorbing (He) and sorbing (CO2) gases under varying gas pressures and confining stresses. Experiments are completed on Pennsylvanian shales containing both natural and artificial fractures under nonpropped and propped conditions. We use the models for permeability evolution in coal (Journal of Petroleum Science and Engineering, Under Revision) to codify the permeability evolution observed in the shale samples. It is observed that for a naturally fractured shale, the He permeability increases by approximately 15% as effective stress is reduced by increasing the gas pressure from 1 MPa to 6 MPa at constant confining stress of 10 MPa. Conversely, the CO2 permeability reduces by a factor of two under similar conditions. A second core is split with a fine saw to create a smooth artificial fracture and the permeabilities are measured for both nonpropped and propped fractures. The He permeability of a propped artificial fracture is approximately 2- to 3fold that of the nonpropped fracture. The He permeability increases with gas pressure under constant confining stress for both nonpropped and propped cases. However, the CO2 permeability of the propped fracture decreases by between one-half to one-third as the gas pressure increases from 1 to 4 MPa at constant confining stress. Interestingly, the CO2 permeability of nonpropped fracture increases with gas pressure at constant confining stress. The permeability evolution of nonpropped and propped artificial fractures in shale is found to be similar to those observed in coals but the extent of permeability reduction by swelling is much lower in shale due to its lower organic content. Optical profilometry is used to quantify the surface roughness. The changes in surface roughness indicate significant influence of proppant indentation on fracture surface in the shale sample. The trends of permeability evolution on injection of CO2 in coals and shales are found analogous; therefore, the permeability evolution models previously developed for coals are adopted to explain the permeability evolution in shales
Charles Hyde, Washington City, letter to John Mathews, Springfield [Putnam].
No full textWants J. Mathews to pay the taxes on lands owned by C. Hyd
Child death reviews in the context of child abuse fatalities - learning from international practice
No full textMathews/Matthews, Julia, Death Certificate, 1916
No full textDeath certificate for Julia Mathews.
Age: 45 years
Death Date: May 18, 1916
Cause: Cirrhosis
Burial Date: May 21, 1916
Location: Zion Cemetery, Tampa, Hillsborough County, Florida
Father: J. Long of South Carolina
Mother: Penni Long
Undertaker: C. W. Patterson, G. G. Hall
Informant: Cara Hal
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