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WHOI-92-09t1i9!
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Intitution
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A Benthic Chamber with Electric Stirrer Mixãng
by
Wayne Dickinson and F.L Sayles
February 1992 .
Technical ReportFunding was provided by the National Science Foundation
through Grant No. OCE87-11962.
Approved for. public release; distribution unlimited.
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DOCUMENTLIBRARY
Woods Hr;:e Oceanographic
InsdLJtíDn
'--_.
WHOI.92.09
A Benthic Chamber with Electric Stirrer Mixing
by
Wayne Dickinson and F.1. Sayles
Woods Hole Oceanographic InstitutionWoods Hole, Massachusetts 02543
February 1992
Teclucal Report
Funding was provided by the National Science Foundationthrough Grant No. OCE87-11962.
Reproduction in whole or in part is permitted for any purpose of the United StatesGovernment. This report should be cited as Woods Hole Oceanog. Inst. Tech. Rept.,
WHOI-92-09.
-- ::c:,._~ni~ ..~ rr¿: c:¡ c::: ,.
c:nic:c:-
Approved for public release; distribution unlimited.
Approved for Distrbution:
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2
AcknowledgementsF. Bradsky of Warer Electrc Company provided may insights into stepper motor
characteristics, C. Peters and C. Olson assisted with the motor housing design, and J.
Goudreau performed the atomic absorption determnations and otherwise assisted in the
bounda layer experients.
This work was supported by United States National Science Foundation grt aCE
87 -11962.
3
Table of Contents
~Intruction 5
Materials and methods 5
Results and discussion 10
Conclusion 15
Biblio~phX 16
4
Abstract
Benthic chambers incorporating electrc stier mixing have been designed and
tested anij have proven reliable durng seven 18-31 day, 4300 ocean deployments. The
chambers are 21 cm diameter by 31 cm long acrlic tubes sealed with pvc lids. A stepper
motor and pressure tolerant electrnics contained within the lids ar magnetically coupled to
stirrng paddles to provide mixing within the chambers. The stirrers exhibit stable mixing
rates and uniform speeds between chambers, require less than 1/3 watt of power, and are
maitenance free. Laboratory calbration of stirng and mixing charactersitics demonstrate
that areal averaged equivalent seawater-sediment boundar layer thickness can be set to
agree with in situ measured values.
5
IntroductionBenthic chambers, used to isolate and measure chemical exchange across small
aras of water-sediment interface, are increasingly common (Smith and Teal 1973; Smith
et al. 1979; Berelson et al. 1986; Devol 1987). The chambes generay incorporate a means
to mix the isolated overlying water so that hydrodynamics within the chamber simulate
those of the external seafoor (Smith et al. 1979; Santschi et al. 1984; Berelson et al. 1986;
Devol 1987; Buchholtz-Ten Brink et al. 1989). Methods of mixing have includedcirculating water from an impeller (Smith et al. 1979; Santschi et al. 1983; James, 1974)
and use of rotating paddles or rods commonly drven by an electrc motor (Berelson et al.
1986; Devol 1987; Buchholtz-Ten Brink et al. 1989; Cahoon 1988). Studies have shown
that the rate of oxygen consumption within the chambers increases with increased stirrng
speed (Boynton et al. 1981; James, 1974) and that higher rates of consumption occur in
stired chambers as compared to un stirred ones (Hargrave, 1969). The exchange ofoxygen and other substances across the seawater-sediment interface is influenced by the
rate of diffusively mediated trsport across the thin stagnant boundar layer, the "diffusive
sublayer", separating the seawater and sediment. (Santschi et aI. 1983; Devol 1987). In
order to obtan accurate measurements of fluxes influenced by the diffusive sublayer, water
within the chamber must be ciculated at a velocity adequate to produce a sublayer thickness
similar to that outside the chamber. This velocity is dependent on rotation rate of the
stirrng paddles for a given geometry, and as a consequence, the rotation rate must beknown and constant. Diffculties in achieving constant stirng rates in some stirer designs
have been noted (Santschi et al. 1984; Buchholtz-Ten Brink et al. 1989). As par of the
development of a benthic flux instrument, we have designed and built chambersincorporatig electrc stiers that exhibit stable mixing rates adequate to produce equivalent
difusive sublayer thicknesses in agreement with reported in situ values.
Materials and methodsThe benthic chambers are 31 cm lengths of 20.8 cm i.d. x 3 mm wall cast acrylic
tube. Acrlic is inexpensive, trsparent, permitig inspection of recovered sediments and
is of low Oi permeability. Lids housing the stirrer and sampling and chemical injection
ports, are made of two PVC plates. A flat perforated baffe is secured -4cm below the lid
to break up and shed the central stiffng vortex. In operation, the plates are forced together
by a spring to provide an o-ring seal once the chamber has been implanted into thesediment. The lower plate forms an o-ring seal with the acrylic tube. (Fig. 1)
6
H
Scale
I~~:~II~L-I
Fig. 1. Schematic of chamber assembly. A-Stepper motor. B-Fluid volume compensation port. e-18
pin DIP soket with 4017 ie and resistors. D-Dnve magnet E-Driven magnet. F-PVe cup. G-Stirrngpaddles. H-Baffe. I-Acrylic baeL. J-PVe chamber plate. K-PVe lid plate. L-Ud closure spnng. M-Lidclosure piston.
7
The stier is a unipolar stepper motor (Warer Electrc, S. Benoit, IL) magnetically
coupled to 2.5 cm square PVC paddles fixed at a compound angle 45 degrees from the
vertcal to the ends of a PVC tee. The motor is drven by a single integrated circuit counter
and 4 field effect transistors (Fig. 2). that fit onto two 18 pm dip sockets cemented diectly
to the motor. Wells in the two portions of the upper lid plate form the housing for the
motor, drve circuit and drving porton of the magnetic coupling. An o-rig sealed pvc cup
isolates the motor from benthic chamber solution and provides a mount for the paddles and
drven porton of the magnetic coupling. A 50cc hospital solution bag fùled with Flourinert
FC-40 (3M Co.) is attached to the fluid filled housing to provide volume compensation for
the pressure tolerant system. A 3 conductor cable connects the housing to an external
battery and clock pulse. Figure 3 includes a photograph and schematic showing the motor,
drve circuit, pvc housing and stig paddles.
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\J1-" PARTS:
QI-Q4: BS170Diodes: In400Resistors: 1/4w carbon compositionMotor: Warer Electrc Model 13 Hybrid SteppeOpto isolater: 4N32
Fig. 2. Circuit diagr of stepper motor drve electronics
8
Fig. 3a. Photograph of stepping motor, drve, housing and stirrng paddles.
8 D
Fig. 3b. Schematic of stepper motor, drve circuit, and housing viewing motor face. A-Stepper motor.B-18 pin DIP socket with 4017 IC and resistors. C-18 pin DIP socket with FET's and diodes. D-Compression fitting port for electrcal cable. E-PVC motor enclosure
9
There are several points worth noting about the motor and drve circuit design. To
achieve the miing requirements of benthic chambers deployed in stable flow regimes, the
stiers must rotate at slow stable speeds for periods up to may weeks. In cases where the
height of enclosed water may var on different deployments, the stirrng speed must be
adjustable to achieve the desired boundar layer thickness. In addition, to extend theduration of deployment.to periods adequate for flux determnations in many pars of the
deep ocean, power required to drve the motor and electronics must be minimized. These
requiments are dificult to meet with some motors commonly used for under-sea work.
The brush commutated dc permanent magnet motor has been used in submersible
pumps, wiches and propulsion systems (Fugitt 1975; Heckman and McCracken 1979) but
is troublesome to use in oil filled pressure compensated systems requiring steady speeds.
Varable termnal resistance caused by commutator brushes arcing in the oil medium and
'hydroplaning' over the commutator cause the motor speed to var. For slow speeds (10-
100 rpm) used in benthic chambers, most inexpensive motors are operating near stalL. In
this condition, speed is very sensitive to changes insupply voltage and load torque as well
as brush resistace, all of which may var during the deployment. Gear motors commonly
used to provide slow speed, operate at high arature speed, making them susceptible to
brush hydroplaning and power losses due to the windage of arature rotation in fluid.Although low speed 'torque' motors are available, we found the price ranged from $700-
$100/ea for small quantities. The stepper motor used in the present design avoids thesedifficulties. It is brushless, operates at slow stable rotation speeds as low as 1 rpm for
periods of at least several weeks and is inexpensive ($30).
The specification of low power consumption applies to both the motor and drve
electronics. The stepper motor drws between 40 and 80 mA at 6v over its speed range of
1-90 rpm (Fig. 4). The drve circuit is CMOS technology and requires less than 20 uA at
6V. Exclusive use of solid electronic components i.e. integrated circuits, transistors,
resistors, permts the circuit to operate in fluid at ambient deep ocean pressure without the
need for pressure resistat housings or expensive undersea connectors.
The motor drve circuit operates by advancing the counter to energize successive
motor windings upon receipt of an external clock pulse. The motor speed is thenproportional to and has the same stabilty as the clock frequency. In our design, the clock
pulses are sent from a computer present on the benthic chamber platform, but the pulses
could easily be generated by a single integrated circuit such as the CMOS 4047. In the
latter case, motor speed could be controlled by a single potentiometer adjustment. Motor
speeds over the useable range of 1 to 90 rpm correspond to clock frequencies between
approximately 3-300 Hz.
100
E 60Q...
10
80
80
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.......¡........t........j........¡.. 0 r m .......+-........t7~..+......+mm...
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20
-50 3
i:-40
oo 50 100 150 200 250
Clock Frequency (Hz)300
Fig. 4. Motor curent and stir rpm at stepping rates from 3-300 Hz. with 5.96 volt supply. SUrrer
was operate at 5.2 x 104 KPa and 20 C. in a laboratory pressure vesseL. Voltage and clock signals weresupplied from sources external to ta. RPM was measured using an electronic counter to count pulsesfrm a 4 slot encoder. The enc'oder generated 4 counts per revoluuon of the motor shaft. For speds of 3
rpm and less, pulse were counte 3 umes for 5 minute periods and counts for each period divided by 20 togive rpm. For other spes; pulses were counted 7 umes for 1 minute periods and counts'for each perioddivided by 4 to give rpm. Curent was meaured with a digita volt meter connected between the voltagesupply and the motor circuit. Symbol size exceeds 1 sd of average rpm.
Results and discussion
As the sting mechanism is centr to performance of the benthic chamber, several
characterstics of the stier were investigated. We measured power requirements, available
torque, and speed stabilty of the stier. We also tested the effectiveness of stirrng bydetermning the equivalent boundar layer thickness at the water-solid phase interfacewithn the chamber.
The stirrers were tested at 5.2 x 1() KPa pressure and 20 C. in a laboratory
pressure vesseL. A slotted disk was fixed to the stirrer shaft as par of an optical shaft
encoder to provide a pulse frequency proportional to shaft rpm. External clock pulses
were sent to the assembly and current and rpm for each clock frequency were recorded.
The results, shown in figure 4, indicate that the device provides stable rotauon speeds over
the range 1-90 rpm under deep sea conditions of temperature and pressure. To test the
effect of varing voltage on stirrer speed, the stirrer was connected to a varable voltage
source, and clocked at 200 Hz. The stirrer was able to star up and rotate at 60 rpIT when
, operated at voltages ranging from 4.4-6.5 volts.
11
Torque charcteristics of the motor were investigated using a simple dynamometer
consistig of an elastic band, calibrated for its spring constat, having one end attached to a
pulley on the motor shaft and the other end fixed. The motor was allowed to turn until it
began to miss steps. Transition from smooth motor operation to missing steps, to stalling
occured within approximately 3 mm of elastic band travel, corresponding to a small,
(-.35 mN-m), uncertainty in the torque determinations. Motor speed was calculated fromdrve pulse frequency and the step size of 1.80. The results are shown in figure 5. The
maximum stier speed is about 90 rpm indicating that the torque required to drve thestir is about one-tenth mN-m.
15.0
12.5-EZ 10.0E-
7.5CD
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o 5.0l-2.5
0.01 0
. . . . . . . . . . . . .........v...........,............--... ...........n...__.....................,............,................................................,............,.......... .. .......... .. .......... .. ........... .. .......... .. ......... .. ......... .. ........--¡--¡--I---¡r--r-t-!--j-r--lrr--r-rr-i--¡-rr--rl--f - - -
torque=13.89-2.54E-03"rpm-1.67E-03"(rpm)1\2 R=.995
20 30 40 50rpm
60 70 80
Fig. 5. Motor torque at speeds from 15 to 72 rpm. The motor was operated 'wave drve' from a 6.25
volt supply. Torque was meaured using a simple dynamometer consisting of an elasuc band calibrated forits forc at varous displacements. One end of the elauc band was held stauona and the other attached toline connected to a pulley on the motor shaft. At each sped, the motor was drven unul it began to misssteps, then stal. Displacement of the elasuc band was measured and converted to force, which applied atthe radius of the pulley allowed calculauon of torque. Displacement of the elasuc band at stal ranged from3.5 cm at 72 rpm to 27.6 cm at 15 rpm. Transiuon from smooth motor operation to missing steps tostaling occured within approximately 3 mm of elastic band travel, introducing less than 0.3 mN-muncertnty in the torque values.
To test the effectiveness of stirng, experiments were performed to determne the
equivalent difusive sublayer thickness within the chamber. The thickness, z, was derived
from the rate of dissolved Cs transport between the stirred chamber solution and an
12
underlying stationar be of molecular sieve, in a fashion simar to the radiotrcer
technique of Santschi (1983). When the rate of transport across the diffusive sublayer is
much slower than sorption processes in the stationar be, the rate of transport is described
by: dCt/dt=(Ct-Cri)*D/zH (1)(Ct (t=O) = Col
where D is the molecular .diffusivity of Cs2+, Ct is the concentration of Cs2+ in thechamber at time t, Co is the initial Cs2+ concentration, Cri is the solution Cs2+concentration in the stationar bed layer, and H is the height of the column of stiedchamber solution. Cri is related to the change in Cs2+ concentration in the sti chamber
solution by: Cri=(Co - Ci) * b where: b = Mch/((KD * Me) + Ms), KD is the molecular
sieve distrbution coefficient, Mch is the mass of stired chamber solution, and Mr and Ms
are masses of the molecular sieve and solution in the stationar bed layer, respectively.
Substituting for Cri and integrating yields:
Dt/zH = 11(1 +b)*ln(((1+b)*Ct - b*Co)/Co) (2)In cases where b -c-c 1, equation 2 reduces to:
Dt/zH = In (Cr/Co) (3)
the slope of a plot ofThe equivalent thickness, z, can be calculated from
lI(1+b)*ln(((1+b)*Ct- b*Co)/Co) vs. t (Fig. 6).
The magnitude of z gives the area weighted average of sublayer thicknesses over
the entire chamber floor. It does not provide information about the sublayer thickness or
overlying water velocity at any specific site. It should be emphasized that in utilzation of
the chamber it is the average value that is of prime interest in the evaluation of fluxes., We
confied that fluid velocity near the chamber floor was fairly homogeneous by visually
following the movement of injected dye. Small upward velocity components were present
and a 2-3 cm2 patch of low velocity existed near the chamber center, but flow wasgenerally rotationally uniform over the chamber floor.
The experiments were cared out in one of the benthic chambers cemented to an
acrlic base. Approximately 50g (70 cm3) 4A 100/120 mesh molecular sieve (Alltech
Associates) was placed in the chamber, the barrel was filled with .005N NaHC03 to
stabilze pH, and the benthic chamber lid closure was fined onto the bareL. The stirrer was
tured on and the solution allowed to circulate and equilbrate overnight. The assembly
enclosed a volume of 3282 cc, with an 8.7 cm column of water overlying a 2 mm thick
bed layer of molecular sieve. A 7 ml volume of 75.1 mM CSCl2 was added to thecirculatig solution to give 16.0 uM initial Cs2+ concentrtion. Aliquots were withdrawn at
intervals over a 2-3 hour period for Cs analysis by flame atomic absorption.
--~ -0.2~I 0~O -0.4
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13
o ~.. ¡ i i i ¡ i i 1 ¡ ¡ ¡ ¡:::': ~ "- : : : : : : : : :...- 40 rpm
........1.. ~;-......r..~..m..t.mm.t.......tm.....j........t.......¡........¡........1.......t........¡-. ..¡ ~1~ ¡ 'Ìl ¡ 1 ¡ ¡ ¡ ¡ ¡ _Í-gL 58 rpm ..
=rll~H~tttr:ttl~: 65 .pm -......+.......t.......¡........j.......+....~.S..,..j.......+....f..............¡..._+..~l-.. 80 rp m ..
ittttb-~~ætmtt. . . . , . . . ''' ~. .., , . . ~ .......).......l......J......l....-.J.._....l.......~.......I.......~......¡....-.l......)D...~L....~......l..m..¡........L.......¡ ¡ ¡ 1 1 1 ¡ 1 ¡ ¡ ~ "10 ¡....1 ¡ ¡ l.;......Lm...l........Lmm.L.......L..m.L.......L....mL......L..m..Lm:..l.~..L....:l_mmO-..:...l........L..m..L.....
¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡"'xj . p . r"'q i..n._n:....n..+n....n~.n.n...~.n.n..;....nn~........-:........~.........;.....n.:........+........;........~....~........;.........;.......__~._......
! ¡ i ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ ¡ , ~X ¡ q ,
o 4000 8000time
12000(see)
16000
Fig. 6. Modellng of the Cs2+ concentrations for the chamber uptae experiments used to
estimate diffusive sublayer thickness. The slope of the plots are proportonal to equivalent boundalayer thcknes. Shown are data from severa of the exPerimenta runs.
Separte experiments were conducted at 8 sting speeds in the range 40-80 rpm.
The rates of Cs2+ removal from the stied chamber solution were at least 60 to 100 times
lower than rates measured in well shaken batch experiments, indicating the sorption rate is
rapid compared to transport across the diffusive sublayer. The value of b (eq. 2) was
small and corresponded to a maximum Crl/C t value of .06 or less throughout allexperiments. Figure 7 summarzes the effect of stirer speed on diffusive sublayer
thickness. The minimum thickness practical for the geometr we use is approximately
300um (i.e. stirrng at 80-90 rpm). This permts us to extend our coverage beyond the
rage reported for the oceans of roughly 500 to 1500um (Santschi et al. 1983; Anderson et
al. 1989). There is about a 5 percent change indiffusive layer thickness per 10 percent
change in sting speed at 60 rpm. Since varation in sting speed is less than 2 percent
(Figu 4), errors in flux estimates resulting from uncertnities in sting speed contrbute, very little to reported flux uncertainities of 15-20 percent (Bender et aI., 1989; Berelson et
al., 1987; Deyol, 1987).
600
-E:i- 500 '
tntnCD
C.:u.-..l-
400
300
20030
14
. . . .~-:~=t=::=!::=1::::::+-TS~~.~:;~.:.~:~.~~;~::.~:~~~~J:._nn.nn..tn.n"__._"in"d.u...~...n......n~....n.....nt.....nn.....~...n........l.............~.............~.n..........f.............r............: : : : : : : : : : :......_.....1..........._.~..............¡..........n.r........._..t........._..1.........n..~.............~...............r............t..............t............
:::::::::::::::::::::::::P:::::¡:;::::::¡:::::::::::::r::::::::::r:::::::::::¡:~::::::~::i::::::::::::r::::::::::r::::::::::::r::::::::::.....m.....¡.....'...m.¡.m..m....¡..........~............,;m......................;.............,.............,.............,;..............m......m: : : :..: : : : : : :: : : : ~ ..: : :': : :mmm....¡............¡-..........¡............ì.........¡.....-i..¡..:........¡..........¡.............j.............¡.......m..¡...........
::::::::::::E::::::~::!:::::::::::::j:::::::::~:!:::::::::::E:~::::::E::::::l~=:::f:::i::r¿::::::::E::::::::I::::::::::¡ ¡ i ¡ ¡ ¡ ¡ ¡ ¡.. ¡
~~-.-.:~::E~i-.::¡~~f:-.I-.::!~:~!-.-.
40 50 9060rpm
70 80
Fig. 7. The effect of sting sped on equivalent difusive sublayer thickness.
The real test of chamber operation has come from deployment for extended periods
in the deep sea. Thee of the chambers have been built and installed as par of our free
vehicle benthic lander. The lander has been deployed 7 times at a depth of 4300 meters,
each tie for a period of 18 to 31 days. In all but one case, the stiers in all chambers
have been operating prior to and following the deployments. On the 31 day deployment,
one stier was not sting on recover due to low battery voltage.
Consumed capacity durng a deployment was evaluated for several stier batteries
to estiate the average curnt drawn by the stiers during the deployment and thereby the
average sting speed (Fig. 4). We measured the amp-hrs required to fully recharge the
batteries following the deployments and found that a capacity equivalent to 50-54 in for
the durtion of deployment had been consumed from each battery. While the consumed
battery capacity represents only the integrated curent over the durtion of deployment, it is
consistent with the measured current of 53 in (6.2V, 2 degrees C., 5.2 x 1() KPa)
corresponding to the set speed of 60 rpm.
15
ConclusionWe feel the chamber design is a versatile solution to many problems encountered in
benthtc chamber operation. It exhibits mixing rates adequate to establish an equivalent
diffusive sublayer thickness that lies within the range of reported ocean values. The speed
stabilty and low power requirements of the stig mechanism wil maintain stable mixing
rates over deployments up to 1 month. Simple speed control allows the rate of mixing to
be adapted to chambers of different volumes. A single clock can be used to drve several
stiers thereby assuring uniform speeds in each chamber. The small size and pressure
balanced design allow the sting mechanism to be integrated within the chamber lid and
avoids the need for expensive pressure cases and undersea connectors. Magnetic coupling
to the stirng paddles prevents leakage of electronic fluid into the chamber and avoids
torque loss from bushing type shaft seals. Four 'D' cell alkaline batteries wil furnish
sufficient power for short chamber incubation periods up to a week, common fordeployments in coastal waters. Finally, the chambers have proven very durable. Nodamage to the acrylic tube or lids has occurred in seven deployments and inspection of the
stirrers after 75 days of operation revealed no wear, fluid decomposition, or seawaterleakage. Routine maintenance consists solely of rinsing the chamber and exposed stirrng
paddes and coupling magnet with fresh water following recovery.
16
REFERENCESAnderson, R., M. Fleisher, P.H. Santschi. 1990. Measurements of diffusive sublayer
thicknesses in the ocean by alabaster dissolution, and their implications for themeasurements of benthic fluxes. EOS 71(2): 124.
Bender, M., R Jahnke, R Weiss, W. Marin, D.T. Heggie, J. Orchado, and T. Sowers.
1989. Organc carbon oxidation and benthic nitrogen and silca dynamcs in San Clemente
Basin, a contiental borderland site. Geochim. Cosmochim. Acta 53: 685-697.
Berelson, W.M, D.E. Hammond, K.L. Smith, RA. Jahnke, A.H. Devol, K.R. Hinga,
G.T. Rowe, F. Sayles. 1986. In Situ benthic flux measurement devices: bottom landertechnology. Mar. Tech. Soc. J. 21: 26-32.
Berelson, W.M., D.E. Hammond, and K.S. Johnson. 1987. Benthic fluxes and thecycling of biogenic silca and carbon in two southern California borderland basins.
Geochim. Cosmochim. Acta 51: 1345-1363.
Boynton, W.R., W.M. Kemp, G.C. Osborne, K.R. Kaumeyer, and M.C. Jenkins.1981. Influence of water circulation rate on in situ measurements of benthic community
respiration. Mar. BioI. 65: 185-190.
Buchholtz-Ten Brink M.R., G. Gust, and D. Chavis. 1989. Calibration andperformance of a stied benthic chamber. Deep Sea Res. 36: 1083-1 10 1.
Cahoon, L.B. 1988. Use of a whirling cup rotor to stir benthic chambers. Hydrobiologia
160: 193-198.
Devol, A.H. 1987. Verification of flux measurements made with in situ benthicchambers. Deep Sea Res. 34: 1007-1025.
Fugitt, Bruce R 1975. Design and operation of two remotely manned undersea vehicles.
In Oceans '75' Conf. Record, IEEE/MTS publication 75 CHO 995-1 OEC. 870-876.
Hargrave, B.T. 1969. Similarty of oxygen uptake by benthic communities. Limnoi.
Oceanogr. 14: 801-805.
Heckman, P. and H. McCracken. 1979. An untethered unmanned submersible. InOceans '79' Conf. Record, IEEE/MTS publication 78CHI478-70EC,I, 733-737.
James, A. 1974. The measurement of benthal respiration. Wat. Res. 8: 955-959.
Santschi, Peter H., U.P. Nyffeler, A. Azevedo, W.S. Broecker. 1983. Estimates of the
resistace to chemical transport posed by the deep-sea boundar layer. Limnòl. oceanogr.
28: 899-912.
Santschi, P.H., J.P. Nyffeler, P. O'Hara, M. Buchholtz, and W.S. Broecker. 1984.
Radiotracer uptake on the sea floor: Results from the MANOP chamber deployments in the
Eastern Pacific. Deep Sea Res. 31: 451-468.
17
Smith, K.L. and J.M. TeaL. 1973. Deep-sea benthic community respiration: An in situ
study at 1850 meters. Science. 179: 282-283.
Smith, K.L., G.A. White, and M.B. Laver. 1979. Oxygen uptake and nutrient exchange
of sedments measured in situ using a free vehicle grab respirometer. Deep Sea Res. 26:
337-346.
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REPORT DOCUMENTATION 11. REPORT NO.PAGE WHOI-92-092. 3. Recipient's Accession No.
4. Title and SubtitleA Benthic Chamber with Electric Stirrer Mixing
S. Repo DateFebruar 1992
6.
7. Author(s) Wayne Dickinson and F.L Sayles
9. Performing Organization Name and Address
8. Performing Organization Rept. No.
WHOI-92-0910. ProjectlaskIork Unit No.
Woods Hole Oceanographic InstitutionWoods Hole, Massachusetts 02543
11. Contract(C) or Grant(G) No.
(C) OCE87-11962
(G)
National Science Foundation
13. Type of Report & Period Covered
Technical Report12. Sponsoring Organization Name and Address
14.
1 S. Supplementary Notes
This report should be cited as: Woods Hole Oceanog. Inst. Tech. Rept., WHOI-92-09.
16. Abstract (Limit: 200 words)
Benthic chambers incOlporating electrc stirer mixing have been designed and tested and have proven reliable during seven 18-31day, 4300m ocean deployments. The chambers ar 21 cm diameter by 31 cm long acrlic tubes sealed with pvc lids. A steppermotor and presslUe tolerat electronics contaned within uie lids are magnetically coupled to stirng paddles to provide mixingwithin the chambers. The stiers exhibit stable mixing rates and unifonn speeds between chambers, require less than 1/3 watt ofpower, and are maintenance free. Laboratory calibration of sting mid mixing chaacteristics demonstrate uiat areal averaged
equivalent seawater-sediment boundar layer thickness can be set to agree WÏul in situ measured values.
17. Document Analysis a. Descriptorsbenthic chaberssubmersible motorsbounda layer
b. Identifiers/Open-Ended Terms
c. COSATI Field/Group
18. Availabilty Statement
Approved for public release; distribution unlimited.
19. Security Class (This Report)
UNCLASSIFIED21. No. of Pages
1720. Security Class (This Page) 22. Price
(See ANSI-Z39.18) See Instructions on Reverse OPTIONAL FORM 272 (4-77)
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