1,741,114 research outputs found
Report of the SB 839 Governance Task Force
No full textThis archived document is maintained by the Oregon State Library as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Title from PDF cover (viewed on April 3, 2015)."The legislation required the establishment of a task force . . . to look at the structure for water development project loans and grants under SB 839 and develop any proposals for changing the structure that the Governance Task Force determines warranted"--Page 4.Includes bibliographical references.Mode of access: Internet from the Oregon Government Publications Collection.Text in English
Athabasca School District 839
Get PDFDocuments - Letters from Athabasca District #839 School Boards listing expenses and/or requesting funding from the Town of Athabasca for the 1926, 1927 and 1944 school years. Expenditures, including teacher/secretary/caretaker salaries, utilities, insurance, and repairs, are listed. Some teachers, personnel are mentioned by name (8 pages
Senate Bill 839 Science Subgroup report
Get PDFThis archived document is maintained by the Oregon State Library as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Title from PDF cover (viewed on July 3, 2014)Includes bibliographical references (pages 41-43)Mode of access: Internet from the Oregon Government Publications Collection.Text in Englis
Storage management of Umatilla russet potatoes
No full textBulletin no. 839 Moscow, Idaho :University of Idaho, College of Agriculture, Cooperative Extension System, 2003-01-01. Author(s): Brandt, Tina L.; Kleinkopf, Gale; Olsen, Nora; Love, Stephe
Senate Bill 839 Economic Subgroup report
Get PDFThis archived document is maintained by the Oregon State Library as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Title from PDF cover (viewed on July 3, 2014)Includes bibliographical references (pages 37-38)Mode of access: Internet from the Oregon Government Publications Collection.Text in Englis
(Table 1) Summary of basalt unit thickness, vesicularity, number of flow units, and average porosity at ODP Site 135-839
No full textAn inflatable drill-string packer was used at Site 839 to measure the bulk in-situ permeability within basalts cored in Hole 839B. The packer was inflated at two depths, 398.2 and 326.9 mbsf; all on-board information indicated that the packer mechanically closed off the borehole, although apparently the packer hydraulically sealed the borehole only at 398.2 mbsf. Two pulse tests were run at each depth, two constant-rate injection tests were run at the first set, and four were run at the second. Of these, only the constant-rate injection tests at the first set yielded a permeability, calculated as ranging from 1 to 5 * 10**-12 m**2. Pulse tests and constant-rate injection tests for the second set did not yield valid data. The measured permeability is an upper limit; if the packer leaked during the experiments, the basalt would be less permeable. In comparison, permeabilities measured at other Deep Sea Drilling Project and Ocean Drilling Program sites in pillow basalts and flows similar to those measured in Hole 839B are mainly about 10**-13 to 10**-14 m**2. Thus, if our results are valid, the basalts at Site 839 are more permeable than ocean-floor basalts investigated elsewhere.
Based on other supporting evidence, we consider these results to be a valid measure of the permeability of the basalts. Temperature data and the geochemical and geotechnical properties of the drilled sediments all indicate that the site is strongly affected by fluid flow. The heat flow is very much less than expected in young oceanic basalts, probably a result of rapid fluid circulation through the crust. The geochemistry of pore fluids is similar to that of seawater, indicating seawater flow through the sediments, and sediments are uniformly underconsolidated for their burial depth, again indicating probable fluid flow. The basalts are highly vesicular. However, the vesicularity can only account for part of the average porosity measured on the neutron porosity well log; the remainder of the measured porosity is likely present as voids and fractures within and between thin-bedded basalts. Core samples, together with porosity, density, and resistivity well-log data show locations where the basalt section is thin bedded and probably has from 15% to 35% void and fracture porosity. Thus, the measured permeability seems reasonable with respect to the high measured porosity. Much of the fluid flow at Site 839 could be directed through highly porous and permeable zones within and between the basalt flows and in the sediment layer just above the basalt. Thus, the permeability measurements give an indication of where and how fluid flow may occur within the oceanic crust of the Lau Basin
[Missouri Pacific, Locomotive 839]
No full textVerso: [handwritten] Bridge 15 Dec. 1908. This eng. Was MP 839
Atroposelective total synthesis of strecintide 839
No full textThe first total synthesis of the recently isolated strecintide 839 is reported. Strecintide 839 is one of the RiPP natural products that have been vigorously isolated in recent years and is known to possess the extremely rare and highly strained atrop-Trp-Trp linkage. This study details the comprehensive investigation into the construction of the highly strained atrop-Trp-Trp linkage and its application in the total synthesis of strecintide 839
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