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Books on the topic 'Deep water flow'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

O'Reilly, Andrew M. A method for simulating transient ground-water recharge in deep water-table settings in central Florida by using a simple water-balance/transfer-function model. U.S. Geological Survey, 2004.

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2

O'Reilly, Andrew M. A method for simulating transient ground-water recharge in deep water-table settings in central Florida by using a simple water-balance/transfer-function model. U.S. Geological Survey, 2004.

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3

Barker, René A. Regional hydrology and simulation of deep ground-water flow in the southeastern coastal plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina. U.S. G.P.O., 1992.

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4

Wirojanagud, Prakob. Numerical modeling of regional ground-water flow in the Deep-Basin Brine aquifer of the Palo Duro Basin, Texas Panhandle. Bureau of the Economic Geology, University of Texas at Austin, 1986.

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5

Division, Alberta Fisheries Management. Report on Red Deer River instream flow needs study. Golder Associates, 1999.

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6

D, Crevello Paul, and Harris Paul M. 1931-, eds. Deep-water carbonates: Buildups, turbidites, debris flows and chalks : a core workshop. SEPM, 1985.

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7

Goater, Lori. Aquatic environment impact ratings a method for evaluating SSRB flow scenarios: Red Deer River case study. 4th ed. Alberta Environment, 2008.

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8

Wolfe, William J. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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9

J, Wolfe William. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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10

Wolfe, William J. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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11

Wolfe, William J. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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12

D, Crevello Paul, Harris Paul M, and Society of Economic Paleontologists and Mineralogists., eds. Deep-water carbonates: Buildups, turbidites, debris flows and chalks : a core workshop : SEPM Core Workshop no. 6, New Orleans, March 23-24, 1985. Society of Economic Paleontologists and Mineralogists, 1985.

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13

P, Dunning C., Milwaukee (Wis ), Geological Survey (U.S.), and United States. Environmental Protection Agency. Region V., eds. Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin. U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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14

P, Dunning C., Milwaukee (Wis ), Geological Survey (U.S.), and United States. Environmental Protection Agency. Region V., eds. Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin. U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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15

Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin. U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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16

Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin. U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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17

D, Crevello Paul, Harris Paul M. 1949-, and Society of Economic Paleontologists and Mineralogists., eds. Deep-water carbonates: Buildups, turbidites, debris flows and chalks : a core workshop. Society of Economic Paleontologists and Mineralogists, 1985.

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18

D, Crevello Paul, ed. Deep-water carbonates, buildups, turbidites, debris flows and chalks: A Core Workshop, New Orleans, March 23-24, 1985. Society of Economic Paleontologists and Mineralogists, 1985.

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19

1951-, Crevello Paul D., ed. Deep-water carbonates, buildups, turbidites, debris flows and chalks: A Core Workshop, New Orleans, March 23-24, 1985. Society of Economic Paleontologists and Mineralogists, 1985.

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20

D, Crevillo Paul, Harris Paul M, and Society of Economic Paleontologists and Mineralogists., eds. Deep-water carbonates: Buildups, turbidites, debris flows and chalks : a core workshop, New Orleans, March 23-24, 1985. Society of Economic Paleontologists and Mineralogists, 1985.

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21

1951-, Crevello Paul D., ed. Deep-water carbonates, buildups, turbidites, debris flows and chalks: A Core Workshop, New Orleans, March 23-24, 1985. Society of Economic Paleontologists and Mineralogists, 1985.

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22

Froese, Marc D. Formal International Institutions and the Regulation of Flows of Goods and Services. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190846626.013.399.

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Trade governance rests upon certain economic assumptions and the ensuing political compromises made possible by the growth of an incremental legal consensus. The main economic assumptions are that trade will deliver upon the objectives of socio-economic development, stable, long-term employment opportunities and poverty reduction. These assumptions are theoretically sound, but are increasingly challenged by the complex political realities of global trade. The study of trade in the field of international political economy (IPE) has deep roots in the postwar disciplines of economics and politica

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23

Clarke, Andrew. Temperature, growth and size. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0013.

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Growth involves two flows of energy. The first is chemical potential energy in the monomers used to construct the proteins, lipids, polysaccharides and nucleic acids forming the new tissue. The second is the metabolic energy (ATP or GTP) used to construct the new tissue; this is the metabolic cost of growth and can be expressed as a dimensionless fraction of the energy retained in the new tissue. Its value is ~0.33. Typical temperature sensitivities for growth in the wild lie in the range Q10 1.5 – 3. Within species there may be evolutionary adjustments to growth rate to offset the effects of

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24

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes

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