2 edition of Computation of fluvial-sediment discharge / by George Porterfield. found in the catalog.
Computation of fluvial-sediment discharge / by George Porterfield.
George Porterfield
Published
1972
by U.S. Govt. Print. Off., For sale by the Superintendent Documents in Washington, D.C
.
Written in English
Edition Notes
Other titles | Applications of hydraulics. |
Series | Techniques of water-resources investigations of the United States Geological Survey -- bk. 3, ch. C3. |
Contributions | Geological Survey (U.S.) |
The Physical Object | |
---|---|
Pagination | vi, 66 p. : |
Number of Pages | 66 |
ID Numbers | |
Open Library | OL18158298M |
difference bedload sampler: U.S. Geological Survey open-file report, 18 p. Porterfield, George, , Computation of fluvial-sediment discharge: U.S. Geological Survey Techniques of Water-Resources Investigations, Book 3, Chapter C3, 66 p. U.S. Geological Survey, , National handbook of recommended methods for water-. DISCHARGE, CUBIC FEET PER SECOND WATER YEAR OCTOBER TO SEPTEMBER DAILY MEAN VALUES [e, estimated] Day Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep 1 20 e 58 52 21 41 69 2 16 e 48 37 16 30 33 3 e 28 28 14 23 19
Documentation of a computer program to simulate aquifer-system compaction using the modular finite-difference ground- water flow model, by S.A. Lealce and D.E. Prudic. pages. Book 3Applications of Hydraulics. U.S. Government Printing Office, Washington, DC, p. George Porterfield; measurement, laboratory procedures, and computation of fluvial-sediment discharge.
A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the full-text. Porterfield, George, , Computation of Fluvial-Sediment Discharge, Techniques of Water- Resources Investigations of the United States Geological Survey, Chapter C3, Book 3, 66 p. U.S. Geological Survey, a, Water Resources Data for USA, accessed Septem , at.
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COMPUTATION OF FLUVIAL-SEDIMENT DISCHARGE. George Porterfield Abstract. This report is one of a series concerning the con- cepts, measurement, laboratory procedures, and computation of fluvial-sediment discharge.
Material in this report includes procedures and forms used to. Computation of fluvial-sediment discharge (Techniques of water-resources investigations of the United States Geological Survey) [Porterfield, George] on *FREE* shipping on qualifying offers. Computation of fluvial-sediment discharge (Techniques of water-resources investigations of the United States Geological Survey)Author: George Porterfield.
COMPUTATION OF FLUVIAL-SEDIMENT DJSCHARGE George Porterfield Abstract This report is one of a series concerning the con- cepts, measurement, laboratory procedures, and computation of fluvial-sediment discharge. Material in this report includes procedures and forms used to compile and evaluate particle-size and concentration data, to compute.
Additional Physical Format: Online version: Porterfield, G. (George). Computation of fluvial-sediment discharge. Washington, D.C.: U.S.G.P.O.: For sale by the. qw PUBLICATION -- TWRI Book 3, Chapter C3, Computations of fluvial-sediment discharge, by George Porterfield qw PROGRAMS AND PLANS--Instructions for use of sediment samplers for the collection of samples to be analyzed for organic substances.
This report is one of a series concerning the concepts, measurement, laboratory procedures, and computation of fluvial-sediment discharge. Material in this report includes procedures and forms used to compile and evaluate particle-size and concentration data, to compute fluvial-sediment discharge, and to prepare sediment records for publication.
Trove: Find and get Australian resources. Books, images, historic newspapers, maps, archives and more. English, Book edition: Computation of fluvial-sediment discharge / by George Porterfield.
Porterfield, George. Get this edition; User activity. Tags (0) Lists (0) Comments (0 Computation of fluvial-sediment discharge / by George. Porterfield, George,Computation of fluvial-sediment discharge: Techniques of Water-Resources Investigations of the U.S.
Geological Survey, Book 3, Chapter C3. Stevens, Herbert H., Jr.,Computer program for the computation of total sediment discharge: Techniques of Water-Resources Investigations of the U.S. Geological Survey, COMPUTATION OF FLUVIAL-SEDIMENT DISCHARGE U.S. Geological Survey, Techniques of Water-Resources Investigations, Book 3, Chapter C3.
By George Porterfield. Copy of daily water discharge and water level. An efficient way to evaluate the adequacy of sampling is to plot the concentrations values on the gauge-heightrecord as soon as possible after the data are available. In the following paragraphs we draw heavily on George Poterfield's "Computation of Fluvial Sediment Discharge" - Techniques of water.
Computation of fluvial-sediment discharge, by George Porterfield: USGS—TWRI Book 3, Chapter C3. Field methods for measurement of fluvial sediment, by T.K.
Edwards and G.D. Glysson: USGS—TWRI Book 3, Chapter C2. TECHNIQUES OF WATER-RESOURCES INVESTIGATIONS OF THE Computation of continuous records of streamflow, by Edward J.
Kennedy. 53 pages. Computation of fluvial-sediment discharge, by George Porterfield. 66 pages. TWI 4-A1. Some statistical tools in hydrology by H.C. Riggs. 39 pages. TWI 4-A2. Frequency curves, by H.C. Fluvial sediment concepts, by H.
Guy: USGS— TWRI Book 3, Chapter C1. 55 pages. 3-C2. Field methods for measurement of fluvial sediment, by Thomas K. Edwards and G. Douglas Glysson: USGS— TWRI Book 3, Chapter C2. 80 pages. 3-C3. Computation of fluvial-sediment discharge, by George Porterfield: USGS— TWRI Book 3, Chapter C3 File Size: KB.
ýr-Resources Investigati ates Geological Survey A A MODULAR FINITE-ELEMENT MODEL (MODFE) FOR AREAL COMPARISONS WITH ANALYTICAL SOLUTIONS A A BOOK 6 CHAPTER A4 STE PDR I.
Techniques of Water-Resources Investigations of the United States Geological Survey Computation of fluvial-sediment discharge, by George Porterfield. Field methods for measurement of fluvial sediment, by H.P.
Guy and V.W. Norman: USGS--TWRI Book 3, Chapter C2. 59 pages. 3-C3. Computation of fluvial sediment discharge, by George Porterfield: USGS--TWRI Book 3, Chapter C3. 66 pages.
Porterfield’s () computational method (for which there is no quantitative method for (). D, in terminology for fluvial sediment, annual book of standards, water and environmental technology, West Conshohocken, Pennsylvania, ASTM Porterfield, George. Computation of fluvial-sediment discharge, U.S.
Geological Survey. Fluvial sediment transportation is segregated into two distinct modes (Figure 2): (1) suspended load and (2) bedload. Suspended load refers to particles that are continuously entrained in the water column, and mostly consist of clay and silt, with varying amounts of sand during high-energy Size: 1MB.
TWI 3-C3. Computation of fluvial-sediment discharge, by George Porterfield. 66 pages. TWI 4-A1. Some statistical tools in hydrology, by H. Riggs. 39 pages. discharge-weighting sampler designed to provide a representative sample of the average suspended- (Porterfield, ). Samples collected during 2 or more consecutive days usually were combined for analysis.
During critical sampling periods such as George,Computation\of fluvial-sediment discharge: U.S. ~eolo~ical SurveyFile Size: 1MB. Book 5, Chapter C1. 58 pp. Porterfield, George. Computation of fluvial-sediment discharge. In: Techniques of Water-Resources Investigations of the United States Geological Survey.
Chapter C3. Field methods of measurement of fluvial sediment, by H.P. Guy and V.W. Norman. 59 pages. Computation of fluvial-sediment discharge, by George Porterfield.Fluvial-sediment discharge to the oceans from the conterminous United States on *FREE* shipping on qualifying offers.
Fluvial-sediment discharge to Manufacturer: [U.S. Geological Survey].deployment. Porterfield, George,Computation of fluvial‐sediment discharge: U.S. Geological Survey Techniques of Water‐Resources Investigations, book 3, chap.
C3, 66 p. The of turbidity in streams, lakes, and estuaries is often proportional to SSC. The site‐specific relation is illustrated when turbidity and SSC are plotted on a scatter.