Order this information in Print

Order this information on CD-ROM

Download in PDF Format

     

Click here to make tpub.com your Home Page

Page Title: PRODUCTION CALCULATIONS (cont.)
Back | Up | Next

Click here for a printable version

Google


Web
www.tpub.com

Home


   
Information Categories
.... Administration
Advancement
Aerographer
Automotive
Aviation
Combat
Construction
Diving
Draftsman
Engineering
Electronics
Food and Cooking
Math
Medical
Music
Nuclear Fundamentals
Photography
Religion
USMC
   
Products
  Educational CD-ROM's
Printed Manuals
Downloadable Books
   

 

ERDC TN-DOER-I5
August 2000
ρw
= the density of the water
V = the flow velocity in the pipe
A = the area of the dredge pipe
The solids flow rate in the dredge pipe is defined as:
af
a f a  Af
ρs - ρw
Mt =
ρm V
(2)
ρm - ρw
with ρm the sediment mineral density. The load in a dredge hopper can be defined in terms of
volume of in situ materials or weight of sediments in the hopper. The volume of in situ material is
computed by the following expression:
b
g
ρ - ρw
VOL = h
(3)
VOLh
ρi - ρw
with the solids load in a dredge hopper computed by:
b gb
g
ρh - ρw
M=
ρm  VOLh
(4)
ρm - ρw
with VOLh the hopper volume and ρh the average density of the material in the hopper, calculated
by dividing the weight of the material in the hopper as measured by the draft sensors located in the
hull of the vessel, by the volume of material in the hopper as measured by the water level sensors
mounted above the hopper.
The data reduction equations for the in-line production meter contain a total of six variables; the
density of the waterw), the sediment mineral densitym), the in situ density of the sediments
i), the velocity as measured by the flow meter (V), the slurry density measured by the nuclear
density gauges), and the pipe diameter (D).
The data reduction equations for the hopper production monitoring system contain a total of five
variables; the density of the waterw), the sediment mineral densitym), the in situ density of the
sediments (ρi), and the average density of the material in the hopper, ρh. As mentioned before, this
average density measurement is calculated by the weight of the material in the hopper (Wh) divided
by the volume of the material in the hopper (VOLh).
Each of the previously mentioned variables have some error associated with their values. This error
may be associated with changing physical conditions in the dredging environment such as water
temperature and salinity levels and variations in the mineral and organic content of the sediments,
or measurement error inherent in the instrumentation. The error contributed by each variable will
propagate through the production equations into the final production calculation.
3

Privacy Statement - Press Release - Copyright Information. - Contact Us - Support Integrated Publishing

Integrated Publishing, Inc. - A (SDVOSB) Service Disabled Veteran Owned Small Business