-III111,I~IIIIIIIIIII-ITechnischeUniversiteit DelftFaculteit der Civiele TechniekVakgroep Waterbouwkunde
IIpump and entered the beaker again. An outline of this set-up is given in flgure 2.3.2. The influenceof a varying flow velocity on the reading of the
IIIIperformance of the sensors was observed. However, if the maximum concentration was 0.2 kg-m?the 5 mm sensor gave the best results and was the most
IIIIThe transmitter uses a pulsed-dc technique to energize the flux-producing coils of the flow tube. Theflow tube is grounded with wires to the flang
II3.2 TestsIIThe performance of the flowmeter was compared to the performance of an orifice plate under thesame conditions in June 1990. For this purp
IIIIIwater (concentration490kg-m") was injected at position B (see figure 3.2.1) in such a way that thetotal average flow rate was not changed. T
II5.Electromag~etic velocity meterIIIMeasuring the flow velocity of a suspension of saline water and China Clay makes high demandsupon the device used
II5.2ExperiencesIPrior to using an E.M.S., the sensor is placed in a stagnant fluid identical to the fluid in which themeasurement will be made. The X
IITable 5.2.1Comparison of velocity measurements.IAverage velocityAverage velocityPosition of sensor(distance/time)(logged data)[cm-s"][cm-s"
III6.2 Instructions for useIWhen the gauge has been kept dry for a long period, it should be cleaned and the electrodes shouldbe placed under water fo
IIThe best straight line ( V=aH + b) was calculated using a least squares approximation [2]. Theslope(a)and its standard deviation(u,.)are shown in ta
IIIIIIIIIIIIIIIIIIIIInstruments used in the research onCohesive SedimentsP.J. de Witreport DO.8-92August 1992Hydromechanies SectienHydraulic and Geote
IIIIIIIIIIIIIIIIIIII0.5006..--1,,°5..2*=511.11.41~,~~ r'''ten,.o.."- -J--tt=J==~=========:3g ~IZFIII..I(uf.mie.LEI.e"fca,conn
IIIIn the Hydromechanics Laboratory four of these pore-pressure meters are present; three with a rangeof 75 mbar and one with a range of 350 mbar. Eve
IIIn the same cross-sectiçn a wave gauge was instalied. The data ofthe different devices were recordedon a personal computer by means of a data-acquis
IIIUsing the experimental data the wave number k = 211"L -t can be estimated and the pressureamplitudeftcan then be calculated.From the results p
IIIIIIIIII1IIIIIIIsediment and the temperature. Therefore the instrument should be calibrated with exactly the samepore water and sediment. In order t
IIIIIIIIIIIIIIIIIIIIvibrations. To determine the weight of a sample as accurate as possible the balances should becalibrated.Ifthe balance is unloaded
IIIfor half an h?ur at100°C.From now on the filter should only be touched carefully by asmooth-tip forceps.Ill. Remove filter from oven and place it i
IIIr-_JI=::;----TPCC.",I ••• 1...-..:---- Venl Poru~'----C...,IF~----Go'htSupponPlotefunncl $(tmtiNo. 8 StoPP<l'IIIIFigureJO
IIII13. References.II[3]II[4][5]IIIII[6][7][8][9][10]III[11][12][13]II[14][15]II[1] Battjes, J.A., 1990,Short period waves,(in Dutch), Delft Universit
IIIIIIIIIIIIIIIIIIII[16][17][18][19][20][21]Nalge Company, 1988,Nalgene™Vacuum Manifold.Sartorius,Sartorius Industry IB 16000S,IB 31000 P, IB3I, Insta
IIIITable of contentsAbstract...III1. Introduction... 1II2. Oslim
IIIIIIIIIIIIIIIIIIII
IIII10. Filtration... 2010.1 Filtration procedure 2010.2 Specifications filters and apparatus used . . . . .
IIIAbstractIIA research program was started to study the behaviour of cohesive sediments at the Delft Universityof Technology in 1989. As part ofthis
I2.1 DescriptionAn Oslim comprises of a sensor and a signal processor. The sensor housing is made of brass andcontains an infrared LED (Light Emitting
III-ee-e-e-e..LICIIT DEAMILlGIiT UEAMIIIIIFigure 1.1.1The Oslim sensor.IIIamount of adsorbed light and the sediment concentration. The analog output o
III- Pump the suspension with the maximal concentration to be measured through the sensor.Adjust the output reading to 10.0 Vdc with the "SPAN&qu
IIIconcentrations. A description of these tests will be given in the next sections.IIIIIIoMAGNETIC STIRRERIoIIIFigure 2.3.2Ouüine of experimenta/ set-
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