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" ... velocity. The discharge curve under normal conditions is concave toward the horizontal axis and is generally parabolic in form. In the preparation of the rating table the discharge for each tenth or half tenth on the gage is taken from the curve.... "
Congressional Serial Set - Seite 15
1905
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Bulletin, Ausgaben 8-18;Ausgabe 20

North Carolina. Division of Mineral Resources - 1899 - 812 Seiten
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to...that they shall either be constant or increasing. The determination of daily discharge of streams with changeable beds is a difficult problem. In case...
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Report of the Director of Forestry ...

Canada. Forestry Branch - 1909 - 452 Seiten
...half-tenth on the gauge is taken from the curve. The differences between successive discharges are •th?u taken and adjusted according to the law that they shall either be constant or increasing. The deter.i;ination of daily discharge of streams with changeable beds is a difficult problem. In cass...
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Geological Series, Bulletin

Virginia. Division of Mineral Resources - 1905 - 682 Seiten
...the discharge for each tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to...that they shall either be constant or increasing. Prior to the fall of 1903 wire gages were used at many of the stations for observing the stage of the...
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Water-supply and Irrigation Papers of the United States ..., Ausgaben 129-133

Geological Survey (U.S.) - 1905 - 1144 Seiten
...tenth or half tenth on the gage is found from the curve. The first and second differences of these discharges are then taken and adjusted according to the law that they shall either he constant or increasing, never decreasing. The discharges in the table are then changed in accordance...
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Congressional Serial Set

1906 - 1176 Seiten
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to the law that they shall be either constant or increasing. The determination of daily discharge of streams with changeable beds...
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Water-supply and Irrigation Papers of the United States Geological Survey

1896
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to the law that they shall be either constant or increasing. The determination of daily discharge of streams with changeable beds...
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Geological Survey Water-supply Paper, Bände 214-219

Geological Survey (U.S.) - 1907 - 880 Seiten
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to the law that they shall be either constant or increasing. The determination of daily discharge of streams with changeable beds...
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Bulletin, Ausgaben 19-20

1904 - 470 Seiten
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to...that they shall either be constant or increasing. The determination of daily discharge of streams with changeable beds is a difficult problem. In case...
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Bulletin - [North Carolina, Geological Survey Section], Ausgabe 20

North Carolina. Geological Survey Section - 1911 - 396 Seiten
...for each tenth or half tenth on the gage is taken from the curve. The differences between successive discharges are then taken and adjusted according to...that they shall either be constant or increasing. The determination of daily discharge of streams with changeable beds is a difficult problem. In case...
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Water-supply and Irrigation Papers of the United States Geological Survey

Geological Survey (U.S.) - 1906 - 1066 Seiten
...the discharge for each tenth on the gage is taken from the curve. The differences between- successive discharges are then taken and adjusted according to...that they shall either be constant or increasing. DEFINITIONS. The volume of water flowing in a stream, the "run-off," is expressed in various terms,...
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