|

[ Newest ] [ by manufacturer ]
[ by application ] [ RFQ ] [ Rentals ]


Sequoia
products
Sequoia
Application Notes
Laser Scatterometers
Underwater
|
|
|
 |
LISST-100X
Submersible laser
scattering instrument that measures concentration and particle size spectra,
pressure and temperature
The LISST-100X
delivers the size distribution of suspended sediments in 32 logarithmically
spaced size classes. Different models of this instrument cover different
rnage of sizes.
The LISST-FLOC covers the largest
sizes, 7.5 to 1500 microns (nominal), and is intended for measuring
flocculated marine particles. These instruments can be used as laboratory
instruments, with provided accessories. The LISST-Portable is a portable
version which can be driven to a site (river, stream, highway runoff..) or
carried on an airplane.

LISST-Deep is a deep version capable of operations to 6000m.
The LISST-100X instrument is a multi-parameter system for in-situ
observations of particle size distribution and volume concentration. It also
records the optical transmission, pressure and temperature. The instrument
is fully self-contained with battery and data-logger. It can be used with
supplied programs, or in specially designed modes, e.g. event triggered
based on storms (pressure variance) or fronts (temperature front). Two
size-ranges are available: 1.25-250 microns (Type B) and 2.5-500 microns
(Type C). Standard memory size is 16MB, suitable for storing approximately
115,000 size distributions, with option to expand to 126MB, or 1,600,000
size distributions. Special versions are available for deep-ocean,
high-concentration, or low-concentration environments. At the heart of the
instrument is a collimated laser diode and a specially constructed annular
ring detector (see Application Note
L001).
Scattering at 32 angles is the primary information that is recorded. This
primary measurement is mathematically inverted to get the size distribution,
and also scaled to obtain the volume scattering function (VSF), see
Application Note L002. The size distribution is presented as concentration
(micro-l/l) in each of 32 log-spaced size bins. Optical transmission, water
depth and temperature are recorded as supporting measurements.
Parameters measured/derived
- Size distribution
- Volume scattering function (VSF)
- Optical transmission
- Pressure
- Temperature
Optical path length
- 5cm standard (1.5cm
and 2.5cm optional)
Ports
- One external analog input (0-5V)
- Two external digital I/O ports (5V logic)
Optical transmission
- 12 bit resolution
Particle size range
- 1.25 - 250 micron standard
(1.5 - 150 and 2.5 - 250 micron optional)
Resolution
- 64 size classes, log spaced
- VSF angle range: 1.70 mrad to 340 mrad
- (other ranges optional)
Data storage memory
- 512K (5000 samples)
- expandable to 2MB (20,000 samples)
Maximum sample speed
- 5 size distributions per second
Temperature-sensor range
- 5- 50°c -
resolution: 0.1°c
Pressure-sensor range
- 200 meters of water
- resolution: 5cm of water
Dimensions
- 13cm diameter
- 81 cm long
Weight in air
- 12 kg
Depth rating
- 200 meters (standard) |
|
 |
LISST-ST
Submersible laser
scattering instrument for in-situ observations of Particle Size Spectra
Settling Velocity Distribution
The LISST-ST is an extended
version of the LISST-100X, with an added Settling Tube (ST stands for
Settling Tube). This instrument is designed to perform submerged settling
experiments to obtain settling velocities of 8 size classes. With the
settling column removed, the LISST-ST may be used as a -100X, but with less
than optimal flow through the sample volume.
The LISST-ST is a submersible field instrument developed for in-situ
observation of the size-dependent settling velocity distribution of
suspended particles. It incorporates a mechanized Settling Column. In a
Settling Experiment, a water sample is drawn and trapped. The evolution of
the size distribution near the base of the settling column during the
settling experiment is interpreted to estimate settling velocities. Settling
velocities are estiamted for 8 log-spaced size classes covering the range
1.25-250 microns (Type B), or 2.5-500 microns (Type C). For details, please
see Application Note L007. The LISST-ST is designed to carry out multiple
settling experiments while submerged. A motorized mechanism operates the
doors that control exchange of water between the settling column and the
ambient environment.
This permits repeated settling experiments. A separate built-in motorized
stirrer is used to agitate and flush out settled particles after each
settling experiment.
In addition to particle size distribution histories with each settling
experiment, water pressure and temperature are also recorded.
The LISST-ST is a fully autonomous, battery operated, self-contained unit.
It is engineered for low power consumption and built to withstand the rigors
of field deployment. Easy to program features permit flexibility in duration
of experiments, and in operating modes.
Parameters measured/derived
- Size distribution
- Settling velocity distribution
- Pressure
- Temperature
Optical path length
- 5cm standard (1.5cm
and 2.5cm optional)
Particle size range
- 1.25 - 250 micron standard
(1.5 - 150 and 2.5 - 250 micron optional)
Resolution
- 64 size classes, log spaced
Data storage memory
- 512K (5000 samples)
- expandable to 2MB (20,000 samples)
Maximum sample speed
- 5 size distributions per second
Temperature-sensor range
- 5- 50°c -
resolution: 0.1°c
Pressure-sensor range
- 200 meters of water
- resolution: 5cm of water
Dimensions
- 13cm diameter
- 85 cm long
Weight in air
- 16kg
Depth rating
- 200 meters (standard) |
|
 |
LISST-SL:
Easy estimates of riverine sediment fluxes
The LISST-SL is an
isokinetic version of the LISST-100X developed for river sediment
monitoring. It senses river velocity and adjusts intake velocity to match.
Optics and electronics are enclosed. Data are stored on a bridge-top Topside
box.
Sequoia Scientific, Inc. announcesthe first
advanced technology laser diffraction system for measuring
sedimentproperties in rivers and streams. The streamlined body is a minimum
drag shape.Twin fins below the body orient the LISST-SL facing upstream
before insertion.A propeller on top of the body measures river velocity. The
system employsactive control of the intake pump that matches river velocity
to intakevelocity making the sample acquisition isokinetic. Diffracted light
is measuredin an enclosed electro-optics test section. Data are transmitted
up the USGSB-reel to a ‘topside’ Control Box. The detailed size distribution
and volumeconcentration is recovered after data processing. Depth, velocity,
andtemperature are stored with each sample. With the included depth data,
thesystem is capable of delivering sediment flux in the river. |
|
| |
Software
|
Radiance
distribution
|
 |
HydroLight
A radiative transfer numerical model that computes radiance
distributions and derived quantities for natural water bodies.
The HYDROLIGHT radiative transfer numerical model computes radiance
distributions and related quantities (irradiances, reflectances, diffuse
attenuation functions, etc.) in the ocean. Users can specify the water
absorption and scattering properties, the sky conditions, and the bottom
boundary conditions in various ways: by selection of built-in defaults, by
reading in user-supplied data (such as WETLabs® ac-9 data), or by writing
their own Fortran subroutines to define their input. HYDROLIGHT then
computes the in-water light field and other quantities of interest to
optical oceanographers, such as the water-leaving radiance and
remote-sensing reflectance. Output is presented as ASCII printout, as Excel®
spreadsheets, or as digital files designed for plotting and analysis using
IDL®. HYDROLIGHT is used in various ways:
As a predictive tool
What will the oceanic light field be at some time in the future?
Given a prediction of water absorption and scattering properties, HYDROLIGHT
can use that information to predict the corresponding light field.
HYDROLIGHT can even become the optics component of a coupled
biological-physical-optical ecosystem model.
As a data analysis tool
What was the ambient light field when the data were taken?
For example, when imaging an underwater object in the daytime, the ambient
daylight may contribute noise (in this case, path radiance) to the signal of
interest (the light propagating from the target to the sensor). HYDROLIGHT
can compute the ambient daylight field so that it can be subtracted from the
total signal received at the sensor to improve the signal-to-noise ratio of
the detected signal.
As a system design tool
How would a proposed system perform under different environmental
conditions?
HYDROLIGHT can serve as a controlled environment to predict what the light
field received by a sensor would be under a wide range of conditions. Such
control of the environment and of simulated noise cannot be obtained in the
field, which is best used for final testing and evaluation of sensors that
were first designed using numerical simulations.
As a teaching tool
How can someone new to the field of optical oceanography most quickly build
up "intuition" or a "working knowledge" about the marine optical
environment? The best way to gain such knowledge is of course to spend 20
years working as an optical oceanographer. The next best way is to use
HYDROLIGHT to study how oceanic light fields depend on various environmental
parameters.
|
|
Top of Page |
|