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IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING 1
Hydromorphological Classification Using
Synchronous Pressure and Inertial Sensing
Asko Ristolainen , Kaia Kalev, Jeffrey Andrew Tuhtan, Alar Kuusik, and Maarja Kruusmaa
Abstract— Classification of river morphology is often based
on hydromorphological units (HMUs) identified from field mea-
surements. Established survey methods rely on expert judg-
ment or collection of field point measurements. When used for
HMU classification, these methods can suffer from high errors
due to the variations in the sampling environment, causing
low repeatability. In order to expedite field data collection and
increase HMU classification accuracy, we propose a multisensory
device, the hydromast. Each hydromast provides a new source
of data to classify HMUs. The modules are inexpensive and
highly portable, consisting of a synchronous array of commodity
pressure and inertial sensors. Rapid, local changes in the flow
field are recorded with absolute and differential pressure sensors.
At the same time, slower depth-integrated flow signals are
obtained from a small damped cylindrical mast, driven by vortex-
induced vibrations. In contrast to existing passive flow measure-
ment technologies, the hydromast uses fluid–body interactions
to provide flow measurements. This allows for minimal signal
processing and simple feature extraction. An array of three
hydromasts was used to collect ten samples in three river HMUs
with shallow depths and highly turbulent flows with smooth and
rough beds. We investigated classification accuracy using single,
dual, and triple hydromast arrays with pressure, inertial, and
combined features using linear regression, a genetic algorithm,
and a neural network. Although limited in scope, the set of
spot measurements covering three HMUs showed that a single
multimodal sensor could deliver an overall classification accuracy
of 89% of the HMUs, and an increase of up to 99% was achieved
using a multimodal triple hydromast array. These preliminary
results show promise in using hydromasts for rapid and robust
HMU classification, providing a new way to collect and assess
river survey data.
Index Terms— Fluid flow measurements, hydrologic measure-
ments, water.
I. I NTRODUCTION
H
YDROMORPHOLOGICAL units (HMUs) are river
sections broken down into a series of multiscale
elements, and should ideally include both field and remote
Manuscript received April 10, 2017; revised August 21, 2017 and
November 21, 2017; accepted January 2, 2018. This work was supported by
the European Union’s Horizon 2020 Research and Innovation Program under
Grant 635568 through the frame of Lakhsmi Project. The work of J. A. Tuhtan
was supported in part by the Estonian Base Financing under Grant B53, in part
by Octavo and PUT under Grant 1690, and in part by Bioinspired flow sensing.
(Corresponding author: Asko Ristolainen.)
A. Ristolainen, K. Kalev, J. A. Tuhtan, M. Kruusmaa are with the Centre for
Biorobotics, Tallinn University of Technology, 12618 Tallinn, Estonia (e-mail:
asko.ristolainen@ttu.ee).
A. Kuusik is with the Thomas Johann Seebeck Department of Electronics,
Tallinn University of Technology, 12618 Tallinn, Estonia.
This paper has supplementary downloadable material available at
http://ieeexplore.ieee.org, provided by the author.
Color versions of one or more of the figures in this paper are available
online at http://ieeexplore.ieee.org.
Digital Object Identifier 10.1109/TGRS.2018.2795641
sensing data [1]. The reach scale divides the river longitu-
dinally into a series of subunits, and is the most commonly
investigated type of HMU as it contains salient features of the
ecological–geomorphological interface [2]. Remote sensing
can be used to efficiently collect spatial data and quan-
tify temporal effects [3]. However, HMU classification still
requires in situ measurements to supply ground truth data [4].
Once HMUs are classified, they provide essential geospatial
information for end users including regional planning, flood
control, and biodiversity assessment [5]–[7].
Current river morphological survey methodologies rely
heavily on expert opinion [8]. This sets limits on the automated
classification of HMUs, primarily due to a lack of repeatable
field data collection and assessment methods [9]. In general,
the local variables such as depth, velocity, cover type, and
bed surface condition are used as the primary features to
first classify HMUs, which can then be related to aquatic
habitats [10], [11]. More recently, local variables such as river
surface flow speed have been measured remotely with different
technologies [12]–[16].
Hauer et al. [17] found functional linkages between the
flow velocity, depth, and bottom shear stress, and developed
relations to ecological mesohabitat units using LiDAR bathym-
etry and 2-D hydrodynamic models. A hydromorphological
index of diversity using the coefficient of variation of the
velocity and water depth has also been applied using extensive
field data and hydrodynamic models to evaluate reach-scale
heterogeneity in alpine gravel-bed streams [18]. In addition,
a time-series study of reach-scale units has shown that the
classification boundaries can merge or shift depending on the
river flow rate [19]. Due to the spatial and temporal changes
occurring in rivers, it is, therefore, key that objective and
repeatable field measurement of the local variables serve as
inputs to calibrate and validate HMU classification methods.
This requires the repeated collection of field data correspond-
ing to different flow rates which are caused by seasonal
changes in the runoff.
At the reach scale, data collection of the local variables
is expensive and time consuming. This is because a plu-
rality of separate point measurements (depth, time-averaged
velocity, and sediment samples) must be collected separately
and processed before classification can be performed. The
hydromast, a simple, timesaving, field survey device that
collects local flow information using collocated synchronous
pressure and inertial data, provides a methodology to collect an
ensemble of relevant hydrodynamic data at each measurement
location. Thus, the time reduced is at least 1/3, and in the case
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