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Drained basin

Drainage slopes within tank areas should ensure that any spills are drained away from tanks, manifolds or piping. Small fires that can occur in gutters or drains around tanks weaken connections to the storage tank and release the contents of the tank. Any gutter encircling the tank should be located at a safe distance from the tank and drain basins should not be located under tank mixers, major valves or manway entrances to the tank. The diked areas should be provided with an impervious surface that is will collect liquids towards a drainage collection point. [Pg.107]

The data described above can be used to predict the location of better source rocks in vertically drained basins, especially in deltaic-type environments with relatively young source rocks. With long-distance vertical migration, some of the biomarker parameters may become skewed. A number of factors must first be considered before applying this approach first, some of the parameters vary with maturity second, C30 steranes are not present in lacustrine samples and so the approach will not work in that situation and finally, it will not work where the oils were deposited prior to land plant evolution, since no vitrinite was present at that time. Oils from mixed source rocks also complicate the issue. The ability to predict source rock properties on the basis of biomarker distributions in cmde oils is a very interesting concept, since most exploration efforts try to discover oil and not source rocks. [Pg.3698]

Uocation and adequay of drains, spills, basins, dikes, and sewers... [Pg.90]

Flush inlet headers, laterals, and return lines Drain to prevent freezing Clean tower basin Adjust tower fans Service Air... [Pg.330]

Operator error probability under stressful conditions depends upon the time to complete a sequence of events. The total time available for limiting sequences was 7.9 hours which is the time to completely drain the cooling water basin. Sequence (6) required the most operator actions (11) was... [Pg.419]

During the distillation it is advisable to hold the Bunsen and to heat the rctoit with the bare flame. Under a pressure of 36 min. the acid distils at 245. The pale yellow oil which collects in the receiver is poured out into a basin whilst hot and allowed to cool. The cake of acid is spread on a poious ]jlate and left to drain, when it becomes nearly colourless, and, after one or two crystallisations from small quantities of spirit, is pure. [Pg.105]

Senkel, m. plummet (shoe) lace, senken, v.t. sink, submerge lower, depress. — V.T. sink, subside, settle sag, slope. Senk-grube,/. cesspool sump catch basin, -korper, m. sinker, bob. -klipe, /. (Textiles) dipping frame, -loch, n. sink hole catch basin drain, -lot, n. plumb bob, plummet, senkrecht, a. perpendicular, vertical, normal. Senkrechte,/. perpendicular, normal. Senkspindel, /. specific avity spindle, hydrometer. [Pg.408]

Screened Sump, Overflow. Float Valve Basin Drain, Wood Basin Only. [Pg.384]

Fig. 9-8 Histogram of dissolved solids of samples from the Orinoco and Amazon River basins and corresponding denudation rates for morpho-tectonic regions in the humid tropics of South America (Stal-lard, 1985). The approximate denudation scale is calculated as the product of dissolved solids concentrations, mean armual runoff (1 m/yr), and a correction factor to account for large ratios of suspended load in rivers that drain mountain belts and for the greater than average annual precipitation in the lowlands close to the equator. The correction factor was treated as a linear function of dissolved solids and ranged from 2 for the most dilute rivers (dissolved solids less than lOmg/L) to 4 for the most concentrated rivers (dissolved solids more than 1000 mg/L). Bedrock density is assumed to be 2.65 g/cm. (Reproduced with permission from R. F. Stallard (1988). Weathering and erosion in the humid tropics. In A. Lerman and M. Meybeck, Physical and Chemical Weathering in Geochemical Cycles," pp. 225-246, Kluwer Academic Publishers, Dordrecht, The Netherlands.)... Fig. 9-8 Histogram of dissolved solids of samples from the Orinoco and Amazon River basins and corresponding denudation rates for morpho-tectonic regions in the humid tropics of South America (Stal-lard, 1985). The approximate denudation scale is calculated as the product of dissolved solids concentrations, mean armual runoff (1 m/yr), and a correction factor to account for large ratios of suspended load in rivers that drain mountain belts and for the greater than average annual precipitation in the lowlands close to the equator. The correction factor was treated as a linear function of dissolved solids and ranged from 2 for the most dilute rivers (dissolved solids less than lOmg/L) to 4 for the most concentrated rivers (dissolved solids more than 1000 mg/L). Bedrock density is assumed to be 2.65 g/cm. (Reproduced with permission from R. F. Stallard (1988). Weathering and erosion in the humid tropics. In A. Lerman and M. Meybeck, Physical and Chemical Weathering in Geochemical Cycles," pp. 225-246, Kluwer Academic Publishers, Dordrecht, The Netherlands.)...
Two major rivers in California influenced by a Mediterranean climate are the Sacramento River and the San Joaquin River. The Sacramento River drains 72,132 km with a relief of 4,317 m. Mean discharge is 650 m /s with peak flows in the winter and early spring and with minimum flows in the late summer and early fall. The San Joaquin River drains 83,409 km with a relief of 4,418 m. Mean discharge is 130 m /s with peak flows in spring and low flows in late summer and fall. Population density is 24 people/km in the Sacramento River basin and 29 people/km in the San Joaquin basin. Agriculture in the Central Valley of California that encompasses parts of both basins is the primary user of water in both basins [1]. [Pg.57]

Finlayson BJ, Harrington JA, Fujimura R, et al. 1993. Identification of methyl parathion toxicity in Colusa basin drain water. Environ Toxicol Chem 12 291-303. [Pg.207]

The Ebro River basin is located in the NE of the Iberian Peninsula, occupying a total surface of 85,362 Km2. Most of the watershed surface area is in Spanish territory, but small parts drain in Andorra and in France (445 km2 and 502 km2, respectively). The Ebro River is the largest hydrographic basin in Spain, accounting for 17.3% of its total surface area. [Pg.2]


See other pages where Drained basin is mentioned: [Pg.468]    [Pg.597]    [Pg.4]    [Pg.71]    [Pg.93]    [Pg.3697]    [Pg.468]    [Pg.597]    [Pg.4]    [Pg.71]    [Pg.93]    [Pg.3697]    [Pg.22]    [Pg.123]    [Pg.259]    [Pg.299]    [Pg.446]    [Pg.449]    [Pg.449]    [Pg.128]    [Pg.238]    [Pg.1550]    [Pg.74]    [Pg.54]    [Pg.12]    [Pg.290]    [Pg.177]    [Pg.180]    [Pg.207]    [Pg.215]    [Pg.18]    [Pg.20]    [Pg.128]    [Pg.556]    [Pg.562]    [Pg.1309]    [Pg.397]    [Pg.291]    [Pg.61]    [Pg.23]    [Pg.31]    [Pg.32]    [Pg.37]   
See also in sourсe #XX -- [ Pg.346 , Pg.347 ]




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Draining

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