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Bogging

After yon choose the com pn tat ion method and options, you can use Start bog on the file menu to record results, such as total energies, orbital en ergies, dipole m om en Ls, atom ic charges, en Lhalpics of formalion (foritieCNDO, IN DO, MIXDO/3, MNDO, AMI, PM3, ZINDO/1, and ZINDO/S mclh ods), etc. [Pg.120]

Virtually anywhere water contacts organic matter in the absence of air is a suitable place for methanoarchaea to thrive—at the bottom of ponds bogs and rice fields for example Marsh gas (swamp gas) IS mostly methane Methanoarchaea live inside termites and grass eating animals One source quotes 20 L/day as the methane output of a large cow... [Pg.66]

Materials that have been buried underwater cause a special problem. Waterlogged woods and leathers (139), although quite stable under such burial conditions, are ia danger of irreversible damage through drying out upon recovery. Indeed, after excavations from bogs or upon recovery from underwater sites, these items need to be stored underwater until laboratory treatment. [Pg.426]

Sur cia.1 Deposits. Uraniferous surficial deposits maybe broadly defined as uraniferous sediments, usually of Tertiary to recent age which have not been subjected to deep burial and may or may not have been calcified to some degree. The uranium deposits associated with calcrete, which occur in Australia, Namibia, and Somaha in semiarid areas where water movement is chiefly subterranean, are included in this type. Additional environments for uranium deposition include peat and bog, karst caverns, as well as pedogenic and stmctural fills (15). [Pg.185]

According to the autochthonous, in situ theory of coal formation, peat beds and subsequently coal were formed from the accumulation of plants and plant debris in place. According to the allochthonous theory, the coal-producing peat bogs or swamps were formed from plant debris that had been transported, usually by streams or coastal currents, to the observed burial sites. [Pg.212]

The principal marine deposits were formed during the Tertiary period and more particularly the upper Miocene epoch. Deposits of freshwater origin date from the PHocene to Miocene epochs to more recent times, dating to as late as 100,000 years ago. U.S. commercial deposits are at or comparatively near the surface. Bog deposits are exploited and lake beds are dredged for use in other parts of the world. [Pg.56]

The fibrous strands that composed the mounds adhering to the tube wall were examined and identified as seed hairs from grass. Subsequently, fibrous material was collected from the cooling tower basin and seed pods from grass growing in a bog located adjacent to and upwind of the cooling towers. This material was also examined and found to be identical to the seed hairs that composed the mounds adhering to the tube wall. [Pg.257]

Fluid coking is very insensitive to poor gas-solids contacting, but has one problem not faced by cat cracking or hydroforming. If the heavy residual oil is fed too fast to the reactor, the coke particles will become wetted and stick together in large unfluidizable lumps. Correct control of feed rate is necessary to prevent this bogging. [Pg.27]

The final area of concern is to develop a practical design philosophy for composite structures. Is there a philosophy that will enable us to account for and accommodate all the essential behavioral characteristics of composite materials Can we do it without getting bogged down in overly complicated issues ... [Pg.371]

Remember that the point of this exercise is to identify broad characteristics of representative systems. Avoid getting bogged down in detailed discussions or analyses of specific management systems, since the relevant systems identified will be considered in detail as part of evaluating your company s current PSM status. [Pg.67]

The leaves oI the so-called Bog Myrtle,. Vyrica ijtiU, which (as s the case with ilyrUti caiiferj] must not be ccinfused with tbe true Myrtle also yield an easeniial oil in small quantity. According... [Pg.119]

Braunstsin, m. pyrolusite, manganese dioxide (roter) rhodochrosite (schwarzer) hausman-nite, -blende, /. alabandite. -kies, m. ala-bandite. -kiesela m. rhodonite, -rahm, -schsum, m, bog manganese, wad. braunstichig, a. brownish. [Pg.80]

Eisen-graupen, /.pi. granular bog iron ore. gnind, m, iron liquor, iron mordant, -guss, m. iron casting cast iron. [Pg.124]

Moor-boden, m. marshy soil, -erde, /, bog earth, peaty soil, muck soil, moorig, a. boggy, peaty. [Pg.304]

Moor-kohle,/. moor coal (black subbituminous coal), -lauge, /. extract from bog earth or peat, -mergel, m. bog marl, -salz, n, salt from peaty soil, -wasser, n. peat water. Moos, n. moss, -achat, m. moss agate, moosartig, a. moss-like, mossy. [Pg.304]

Morknenschutt, m. (fleol.) moraino deposit. Morast, m, bog, marsh, swamp, morass. Morasterz, n. bog ore. [Pg.304]

Ohr, n. (Tech.) ear, lug, handle, eye. loop, catch bog iron ore. dhrchen, n. auricle little ear eyelet. Ohren>schmalz, n. ear wax, cerumen, -stein, m., -steinchen, n. otolith. [Pg.326]

Orts-funktion, /. position ftmction. -isomerie, /. place isomerism, position isomerism, Ortsteln, m, Min.) bog iron ore hardpan, ortsverinderlich, a. movable, portable, Orts-verinderung,/. change of position, -wech-sel, m. change of position or location, -zahl, /. position number, index number. [Pg.329]

Rasen, m. turf, sod, lawn furry coatiug, fur. -asche,/. turf ashes, -bleiche,/. grass bleaching, sun bleaching, -eisenerz, n., -eisenstein, m., -erz, n. bog iron ore. rasieren, v.t. shave raze. [Pg.356]

Sumpf, m. Swamp, marsh, bog (Tech.) pit, sump basin pool (of mercury) wave absorbent, -boden, m. marshy or swampy ground or soil, -eisenstein, m. bog iron ore. [Pg.437]

Sumpf-erz, n. bog ore. -gas, n. marsh gas. sumpfig, a. Swampy, marshy, boggy. Sumpf-kalk, m. slaked lime, -luft, /. marsh gas. -moos, n. swamp moss, sphagnum (moss), -nelke, /. piirple avens (Geum rivale). -ol, n. sump oil. -pfianze, /. marsh plant, -porsch, -porst, m. marsh tea (Ledum pa-lusirei. -silge,/. marsh parsley (Peucedanum palustre). [Pg.437]

Torf-asche, /. peat ashes, -boden, m. peat soil, -eisenerz, n. bog iron ore. -erde, /. peaty soil, peat mold, -faser,/. peat fiber, -gas, n, peat gas. -geruch, m. peaty odor, -ge-schmack, m. peaty taste, fiavor of peat, torfhaltig, a. containing peat, peaty, torfig, a. peaty. [Pg.448]

Wiesen-erz, n. meadow ore, bog iron ore. -flachs, m. purging flax, -heu, n. meadow hay. -kalk, m. hmestone from springs, freshwater hmestone. -klee, m. red clover. [Pg.514]

N = number of tubes in bundle Bog = baffle cut area, expressed as fraction, representing opening as percent of shell cross-section area. [Pg.217]


See other pages where Bogging is mentioned: [Pg.212]    [Pg.502]    [Pg.502]    [Pg.502]    [Pg.239]    [Pg.20]    [Pg.154]    [Pg.444]    [Pg.418]    [Pg.188]    [Pg.232]    [Pg.2358]    [Pg.82]    [Pg.83]    [Pg.62]    [Pg.78]    [Pg.125]    [Pg.126]    [Pg.276]    [Pg.288]    [Pg.505]    [Pg.1]    [Pg.21]    [Pg.382]   
See also in sourсe #XX -- [ Pg.89 ]




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Acidity peat bogs

Bog Mosses

Bog bodies

Bog iron ore

Bog manganese

Bog myrtle

Bog oak

Bog plants

Bog soils

Bog whortleberries

Bog-Hansen

Bog-bean

Bogs, lead

Ombrotrophic bog

Peat bogs

Peat bogs, lead

Soils from bogs

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