physical limnology weta151 l6b instruments. 9/14/2015 wets150 timo huttula 2...
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Physical limnologyWETA151
L6b
Instruments
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04/21/23WETS150 Timo Huttula
2
ConductivityTemperatureDepth-probe
12 16 20 24läm pötila [°C ]
16
12
8
4
0
syvy
ys [m
]
Profiili 25
Profiili 24
Profiili 26
Profiili EXT2
Profiili EXT3
24-7-2003 P ro fi i l it 25 , 24 , 26 , E X T 2, E X T 3
0 2 4 6 8 10abs 440nm [m -1 ]
16
12
8
4
0
syvy
ys [m
]
Profiili 25
Profiili 24
Profiili 26
Profiili EXT2
Profiili EXT3
24-7-2003 P ro fi i l it 25 , 24 , 26 , E X T 2, E X T 3
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04/21/23 WETS150 Timo Huttula 3
Drogues; history
• Ancient: Anything floating with current has been used• Operational network along Finnish coast from 1910 to 2nd World
War on light house ships• After the war around the world (wood pieces, apples, post cards,
flow crosses and cylinders)• Positioning from shore by eye, triangle measurement, radars• Satellite buoys 15 years in seas• Since 10 years GPS provided new possibilities
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04/21/23 WETS150 Timo Huttula 4
A droque at the depth of 5 m in Lake Issyk-Kul
.IAA.pdf
p-.109
• A drogue consists of:– Cylinder : diameter of 60 cm,
height 100 cm
– Cross: A4 size (21*29 cm)
– Rope: 2-3 mm
– Buoy: Diameter about 10-15 cm, shape: ball or double cone
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Drogue measurement
• In simplest way: – You need droques, a boat and manual GPS
– in one vertical you can follow a large group of drogues
– in horizontal direction 300-500 m spacing is practical
– waves and darkness are problem
– lights and radar reflectors
• Accuracy: GPS with 12 channels gives about 6 m drifting distance of 60 m gives 10 % accuracy for droque measurement
• How long time for a measurement? – Let’s expect a water velocity of 5 cm/s
– time=distance/velocity
– For 60m travel you need time=(60 m)/(0.05 m/s)=1200 s = 10 min
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04/21/23 WETS150 Timo Huttula 6
Drogue measurement, 2
• In simplest form: boat and manual GPS– in one vertical you can follow a large group of drogues– in horizontal direction 300-500 m spacing is practical– waves and darkness are problem– lights and radar reflectors
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Datasheet drog1.xls
JY/BIO1
Measurement: Current with droques Site:
Date Buoy Depth Start Start Start Start Start Stop Stop Stop Stop Stop Distance Direction Velcocity
identificationm Lat Lon Lat Lon time Lat Lon Lat Lon time km deg cm/s
61 xx.xxx N 23 xx.xxx E61.xxxxx 25.xxxxx xx.xx 61 xx.xxx N23 xx.xxx E61.xxxxx 23.xxxxx
25.7.2001 Plus 0.25 29.10 44.489 61.48495 23.74148 13:02 29.197 44.224 61.4866 23.7371 15:04 #NAME? #NAME? #NAME?
25.7.2001 Minus 4.5 29.10 44.489 61.48495 23.74148 13:02 29.144 44.041 61.4857 23.734 15:04 #NAME? #NAME? #NAME?
Datasheet for drogue measurement
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04/21/23 WETS150 Timo Huttula 8
A drogue with GPS buoy
A result from lake Jyväsjärvi at 14.9.2002. Wind was blowing weakly from north. Two drogues were placed at the depth of 0,7-2,7 m. They were connected to the automatic GPS buoy.
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04/21/23 WETS150 Timo Huttula 9
+/- of drogues
• +++ very inexpensive, major cost is the cost of GPS (about 300 USD)
• +++ practical and easy to use• ++ good learning and teaching tool• -- laborious for long term measurements
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04/21/23 WETS150 Timo Huttula 10
Moored current meters
• For collecting time series of currents• Velocity measured on basis of propeller or impeller
revolutions• Available for more than 30 years• Recording capacity 2…12 months • Moderate cost• Buoy – rope- meter (1)-…meter (n)- anchor• Deployment with surface buoy or subsurface buoy• Representative sites: bathymetric survey, tentative
model application, current mapping with ADCP• Not on navigational routes• Risk of loss
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04/21/23 WETS150 Timo Huttula 11
Statistical analysis of currents
• Cartesian components direction information included• Filtering important time scales• Auto correlation and spectral analysis principal periods of
oscillation• Cross correlation is there any correlation between currents at
different sites??• Regression analysis factors causing currents
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04/21/23 WETS150 Timo Huttula 12
Lake Karhijärvi 7.7. - 16.8.1993
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04/21/23 WETS150 Timo Huttula 13
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04/21/23 WETS150 Timo Huttula 14
+/- of Aanderaa and Endeco propeller RCM
• + inexpensive• ++ durable and rugged• +++ widely used• -- not possible to measure near boundaries except
Endeco near surface• -need several instruments to cover the vertical and
horizontal variation of currents
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04/21/23 WETS150 Timo Huttula 15
Ultrasonic current meter UCM50
• Travelling time of acoustic pulses depends on the velocity of water
• Three pairs of sensors, with 3 MHz piezometric transducer/receivers
• In each pair the pulses are sent from both sides exactly at the same time
• The 3D current vector is obtained
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04/21/23 WETS150 Timo Huttula 16
+/- of UCM
• ++ Very accurate and sensitive meter• +++ Can measure near boundaries• + Basic measurements are easily done• -- Not very dependable in operation • - Needs calibration• - Small producer
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04/21/23 WETS150 Timo Huttula 17
Acoustic Doppler Current Profilers; History
• 1982, First model by RD Instruments, Self contained• 1983, Vessel mounted version• 1986, five 75-1200 kHz, SC, VM and direct reading• In Finland since 1987 R/V Aranda (VM) and 1989 R/V Muikku• 1991, RDI BB-generation • 1995, RDI, Workhorse• 1997, SonnTek• 1998, Norrtek
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04/21/23 WETS150 Timo Huttula 18
ADCP is a radar, 1
• Four beams. Angle 200 • Measures the floating velocity of particles• Reflectors are mostly zooplankton
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04/21/23 WETS150 Timo Huttula 19
ADCP is a radar, 2
• Sends pulses (= pings) about 10-20 times in second• Integrates over certain volume (eq. 1 m thickness), width of the
samples is O(1 m)• Movement of instrument platform has to extracted (bottom tracking
or GPS can be used) • Accuracy depends on integration time
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04/21/23 WETS150 Timo Huttula 20
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04/21/23 WETS150 Timo Huttula 21
Sound velocity
• Absorption of energy is dependent on density• Long waves decay less than short waves • Water density is mainly dependent on temperature and salinity• Reflections from density boundaries
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04/21/23 WETS150 Timo Huttula 23
Acoustic Doppler current profiler, RDI Workhorse
IAA.pdf p. 18, p.69
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04/21/23 WETS150 Timo Huttula 24
Contaminated layer near boundaries in ADCP measurements
Also near transducer surface an off-set is left. It’s thickness is about one layer thickness
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04/21/23 WETS150 Timo Huttula 25
+/- of ADCP
• +++ Collects lot of data• + Fairly good software• + Quite easy to use,• --Tuning and data interpretation is demanding• - Older ADCP’s: for seas • ++New products • ++Costs are coming down
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04/21/23 WETS150 Timo Huttula 26
Turbidity meters
Transmissometer model BTG
Scattering meter model D&A OBS3+
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04/21/23 WETS150 Timo Huttula 27
Radiometers
•Likor 1800 UW spektro radiometer
• WetLab’s AC-9 absorption and scattering meter
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04/21/23 WETS150 Timo Huttula 28
Flow through instrument set up in
a boat
http://www.luode.net/
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04/21/23 WETS150 Timo Huttula 2924.00 24.04 24.08 24.12
longitude [°E]
59.26
59.28
59.3
59.32
59.34
59.36
59.38
lati
tud
e [
°N]
0
4
8
12
16
20
m odelled spim [m g/l] 4th of October
24.00 24.04 24.08 24.12
longitude [°E]
59.26
59.28
59.3
59.32
59.34
59.36
59.38la
titu
de
[°N
]
0
4
8
12
16
20
watersam ple spim [m g/l] 4th of October
24.00 24.04 24.08 24.12
longitude [°E]
59.26
59.28
59.3
59.32
59.34
59.36
59.38la
titu
de
[°N
]
0
4
8
12
16
20
m odelled spim [m g/l] 26th of Novem ber
Turbidity of surface
waters during
dredging
This figure is based on standard water sampling and laboratory analyses
Figures based on flow through measurements
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04/21/23 WETS150 Timo Huttula 30
Reflection measurements
• Measurements– Above water surface sensors are not affected by biofouling – Sensors are not so expensive as submerged or flow through
meters– Accuracy is not very high– Large set of possible applications
• Monitoring diffuse loads• Calibration of satellite images• Monitoring dam infiltration