1,742,821 research outputs found
Trykk 833
No full text833 med tittel: Bestemmelser om hullkortbehandling av billettregnskaper : innenlandsk trafik
Sul Pittore di Monaco 833
No full textThe Painter of Munich 833, studied by J.Gy. Szilágyi, who attributed to him 5 vases, has always been closely related
to the Ivy leaf Group. In this article it’s proposed to distinguish two different painters, the first, with the old name of
Painter of Munich 833 more tied to the Attic tradition, for iconography and stylistic models, author of two amphorae
(Munich 833 and tomb 170 Osteria necropolis of Vulci), the second, with the new name of the Symplegma Painter,
nearer to Greek East ceramography for his stylistic models, author of three amphorae (Louvre E723, Metropolitan
Museum 22.139.83 and fragments in Budapest). The Painter of Munich 833 could be an Attic Painter, near to Amasis
and related , moved to Etruria during the second half of the sixth century, around 540-520 B.C
C17-833 camelina
Get PDFCamelina (Camelina sativa) elite germplasm C17-833 was developed at the Agriculture and Agri-Food Canada Saskatoon Research and Development Centre. It was developed through hybridization of camelina cultivar AAC 10CS0048 and F4 line 11CS0231-24-10 and subsequent pedigree selection. C17-833 yields significantly higher (114%) than the check cultivar AAC 10CS0048. It also has significantly higher seed oil content (42.6 vs. 41.9%) and significantly larger seeds (126%). C17-833 has very good resistance to downy mildew disease caused by Hyalonospora camelinae and is adapted to all soil zones of the Canadian Prairies.The presentation of the authors' names and (or) special characters in the title of the pdf file of the accepted manuscript may differ slightly from what is displayed on the item page. The information in the pdf file of the accepted manuscript reflects the original submission by the author
Geochemistry of volcanivlastic sediments of ODP Sites 134-832 and 134-833
No full textVolcaniclastic sediments of North Aoba Basin (Vanuatu) recovered during Ocean Drilling Program (ODP) Leg 134 show a mineralogical and chemical overprint of low grade hydrothermal alteration superimposed on the primary magmatic source compositions. The purpose of this study was to identify authigenic mineral phases incorporated in the volcaniclastic sediments, to distinguish authigenic chemical and mineralogical signals from the original volcaniclastic mineralogical and chemical compositions, and to determine the mechanism of authigenic minerals formation.
Mineralogical, micro-chemical and bulk chemical analyses were utilized to identify and characterize authigenic phases and determine the original unaltered ash compositions. 117 volcaniclastic sediment samples from North Aoba Basin Sites 832 and 833 were analyzed. Primary volcaniclastic materials accumulated in North Aoba Basin can be divided into three types. The older basin-filling sequences show three different magmatic trends: high K, calc-alkaline, and low K series. The most recent accumulations are rhyodacitic composition and can be attributed to Santa Maria or Aoba volcanic emissions.
Original depositional porosity of volcaniclastic sediments is an important factor in influencing distribution of authigenic phases. Finer-grained units are less altered and retain a bulk mineralogical and chemical composition close to the original pyroclastic rock composition. Coarser grained units (microbreccia and sandstones) are the major hosts of authigenic minerals. At both sites, authigenic minerals (including zeolites, clay minerals, Mg-carbonates, and quartz) exhibit complex zonation with depth that crosses original ash depositional boundaries and stratigraphic limits. The zeolite minerals phillipsite and analcime are ubiquitous throughout the altered intervals. At Site 832, the first zeolite minerals (phillipsite) occur in Pleistocene deposits as shallow as 146 meters below seafloor (mbsf). At Site 833 the first zeolite minerals (analcime) occur in Pleistocene deposits as shallow as 224 mbsf. The assemblage phillipsite + analcime + chabazite appears at 635 mbsf (Site 832) and at 376 mbsf (Site 833). Phillipsite + analcime + chabazite + thomsonite + heulandite are observed between 443 and 732 mbsf at Site 833. Thomsonite is no longer observed below 732 mbsf at Site 833. Heulandite is present to the base of the sections cored. The zeolite assemblages are associated with authigenic clay minerals (nontronite and saponite), calcite, and quartz. Chlorite is noticeable at Site 832 as deep as 851 mbsf. Zeolite zones are present but are less well defined at Site 832. Dolomite and rare magnesite are present below 940 m at Site 832.
The coarse-grained authigenic mineral host intervals exhibit geochemical signatures that can be attributed to low grade hydrothermal alteration. The altered intervals show evidence of K2O, CaO, and rare earth elements mobilization. When compared to fine-grained, unaltered units, and to Santa Maria Island volcanics rocks, the altered zones are relatively depleted in rare earth elements, with light rare earth elements-heavy rare earth elements fractionation.
Drilling at Site 833 penetrated a sill complex below 840 m. No sill was encountered at Site 832. Complex zonation of zeolite facies, authigenic smectites, carbonates and quartz, and associated geochemical signatures are present at both sites. The mineralogical and chemical alteration overprint is most pronounced in the deeper sections at Site 832. Based on mineralogical and chemical evidence at two locations less than 50 km apart, there is vertical and lateral variation in alteration of the volcaniclastic sediments of North Aoba Basin. The alteration observed may be activated by sill intrusion and associated expulsion of heated fluids into intervals of greater porosity. Such spatial variation in alteration could be attributed to the evolution of the basin axis associated with subduction processes along the New Hebrides Trench
ALVIN 833 Dive 833
No full textALVIN 833 Dive 833The runtime for this video is 12m 14s.Alvin dive 833 took place on September 17, 1978 during voyage LU-100. The Chief Scientist was F. Grassle in the operating area of Dos#2. The purposewas described as 'BIOLOGY' and the sponsor as 'J.A.', or Joint Agreement of National Science Foundation, Office of Naval Research, and National Oceanic and Atmospheric Administration.The items in this collection are embargoed in the system in keeping with copyright requirements. However, they are available to users upon request. Please contact the MBLWHOI Library to access the items at [email protected] of this material was supported by a Recordings at Risk grant from the Council on Library and Information Resources (CLIR). The grant program is made possible by funding from The Andrew W. Mellon Foundation. CLIR is an independent, nonprofit organization that forges strategies to enhance research, teaching, and learning environments in collaboration with libraries, cultural institutions, and communities of higher learning. To learn more, visit www.clir.org and follow CLIR on Facebook and Twitter.2200-01-0
Estimating water requirements for hard red spring wheat for final irrigations
No full textBulletin no. 833 Moscow, Idaho :University of Idaho, College of Agriculture, Cooperative Extension System, 2001-05-01. Author(s): Ashley, Roger O.; Robertson, Larry D.; Seyedbagheri, Mir M.; Hopkins, Ivan C
Union Pacific (UP) 833
No full textA photograph print showing Union Pacific (UP) 833, 4-8-4, at Cheyenne, WV
Santa Fe (ATSF) 833
No full textA photograph print showing Santa Fe (ATSF) 833, 0-8-0, Kansas City, KS
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