1. Introduction
Detection of objects bottoming at the sea floor in shallow water is a very important problem. It is also essential in underwater exploration for protecting the underwater environment, and is a critical technology in the field of military detection.
A side scan sonar is mainly applied in conventional methods to obtain images within detection fields, and studies have been performed to recognize cylindrical targets by using image signal processing [
1,
2,
3,
4,
5]. The sonar images used in this process are composed of the intensities of sound waves scattered on the seabed surface or on the target. The resolution of these images is very low, and owing to severe noise it is impossible to detect objects during real-time processing. In addition, since frequencies higher than 100 kHz are used, the detection distance is very short, and the sonar sensors must be towed at very low speed to obtain clean images in which the detection field is relatively narrow. Meanwhile, mid-frequencies are currently used to detect sea mines at the bottom of the seabed in shallow seas. The Applied Physics Lab (APL) at the University of Washington in the United States of America conducted research on the scattering of sound waves from a 1∼2 m-long target [
6,
7]. In the study, frequencies of 1∼30 kHz are used to conduct comparative research between actual test data and simulation data on the scattering of sound waves in various cylindrical objects. Research is performed on the signal intensity reflected from the target rather than the images of the target, and characteristics on the seabed in contact with the target are modeled.
In shallow water environments with fast current such as the Yellow Sea in Korea, the detection problem is more difficult. Note that the average speed of 74.0 cm/s with the maximum speed of 172.6 cm/s has been observed near the Taean Peninsula in the Yellow Sea [
8], and its sediment consists of 85% gravel and 15% sand on average [
9]. This is a very complicated area that includes coastal fronts and swirls, substantial tides and currents, abundant sea life, and high ship traffic. These factors are changing temporally and/or spatially, and combine to create a difficult detection problem [
10,
11]. When detecting a target via active sonar, the received signal includes not only the target response but also the clutter response due to surrounding objects. Furthermore, the effect of clutter becomes stronger in the shallow water environment. It is not easy to model the channels of the clutters because of their time-varying characteristics. Studies on channel modeling in shallow water have been actively conducted [
12]. Clutter is the factor that interferes with the detection of targets [
13]. Intensive studies on reducing the influence of clutter or identifying objects and clutter have been done in various ways [
14]. In the sonar system, as the complexity of the channel structure increases, detection performance deteriorates exponentially.
Since M. Fink and his group proposed the time reversal techniques in acoustics [
15,
16,
17], research has been carried out in a variety of fields, from electromagnetism to underwater acoustics. Significant theoretical and experimental efforts have been made to improve the detection and imaging algorithms in a considerable scattering environment [
18,
19,
20,
21]. The time reversal technique requires that targets are in uniform background media [
22] in order to obtain clean images. In terms of detection, the target signal is usually covered or disturbed by the clutter signal. By capturing the received wave which radiated from the source and retransmitting the time-reversed waveform of the captured signal to the channel for reception, the energy of the wave can be focused at a specific position [
23,
24]. Note that retransmitting the time reversal signal from the received signal is a kind of matched filtering for the time-invariant components, while it is a kind of energy spreading for the time-varying components [
25]. The time domain correlation analysis according to distance and frequency shows that the time-varying characteristics of the shallow water channel become stronger as the distance becomes longer and as the frequency increases [
26]. For this reason, the time reversal technique can achieve good performance even if the scattering environment is complicated. As the time-varying property of the clutter signal becomes stronger, the detection performance improves because the time coherence of the clutter signal is decreasing while the target signal is time-invariant.
In this paper, a method is proposed to improve the detection performance using the time reversal technique in the situation where the clutter is mixed in the shallow water. By using the wave focusing effect of the time reversal technique, the peak response of the target can appear prominently. In this work, it is considered that the cylindrical object is resting on the sea floor. In this case the sea floor consists of soft sediment and there are gravel, sand, and seaweed in the current, whose scattering can cover target scattering to mask detection via active sonar. It is assumed that these clutters are time-varying and K-distributed. Therefore, when the time reversal technique is applied to the received signal from the clutter with time-varying characteristics, it is difficult to obtain a high peak response. However, for the scattering waveform of the cylindrical object considered in this work, because the time-varying characteristic of the target response is weaker than that of the reverberation by the clutter, the time reversal technique can increase the peak of the target signal.
The paper is organized as follows. The peak enhancement using the time reversal technique and the proposed method are described and the probability of detection is numerically evaluated in
Section 2.
Section 3 presents the cylindrical target model and the clutter model.
Section 4 presents the performance evaluation through computer simulation. Finally,
Section 5 concludes the paper.
2. Target Peak Enhancement Using Time Reversal Processing
2.1. Concept of the Time Reversal Scheme
In this section, the idea of the time reversal processing is introduced under the time-varying channel
. This channel represents the signal traveling path from the source to resolution cell of the sonar and back to the receiver of the sonar. This channel can be assumed to be time-varying since the channel is affected by the clutter in the resolution cell. Furthermore, for the case where the target is placed in the resolution cell, the channel is a superposition of the time-varying component due to the clutter and the time-invariant one from the target. Time reversal processing has the spatial-temporal focusing property by retransmitting a time-reversed waveform of the received signal [
27]. This process can be conceptually described as follows.
The Fourier transform
of the received signal
through the channel with its impulse response
at time
t is given by
where
is the Fourier transform of a transmission signal
. Then, the time-reversed transmission signal
at time
t is given by
where the superscript ∗ denotes complex conjugation. The received signal
for the time-reversed transmission signal
at time
is as follows:
This shows that the waveform contains the time varying spectrum of . When the channel is time-invariant , the received signal contains the power spectrum , , which means a peak.
In this work, the case of detecting a cylindrical object bottoming at seafloor in shallow water is considered as shown in
Figure 1. A test of two hypotheses can be applied to this investigation. In the null hypothesis,
, the channel of shallow water is characterized only by clutter. In the alternative hypothesis
, a cylindrical target is also present. This problem can be written as follows:
where
represents the time-varying component due to the clutter while
represents the component due to the target. Note that the time-varying characteristics of the clutter and target channels are different in shallow water since the target is bottoming at the seabed. The reverberation by clutter in shallow water has the time-varying power level [
12], but the scattering by a cylindrical object is dependent on the size of the cylinder and its angles with respect to the source because the target is stationary. Therefore, the target channel
is independent of time
t. That is,
, which allows the hypotheses in Equation (
4) to be rewritten as follows:
According to the time-varying property of the clutter channel, that is, for , in case of , the expectation of may be a small value, while in case of , the expectation of may have a high value due to the time-invariance of the target channel. When the time reversal technique is applied to the signal scattered by the clutter, the focusing of the waveform does not perform well due to the time-varying characteristics. However, in the case that the time reversal technique is applied to the section where the target exists, the pulse can be focused at the target position and it has a higher value than that without the time reversal technique.
2.2. Time-Reversed Signal Implementation
The sampled signal
is given by matched filtering the received signal
at time
t. The time-reversed retransmitted signal
,
,
is given by
where
N is pulse length,
L is sample interval, and
is the unit step function. Thus, a total of
K time reversed transmission signals are used.
Figure 1 describes this implementation in Equation (
6).
2.3. Detection Performance Comparison
In this section, the proposed method is compared to the conventional matched filtering with a threshold in terms of detection probability. Since the detection problem is a binary hypothesis testing problem, the likelihood ratio test is employed. For this, the probability density function of the received signal is required. In this development, the clutter signal has the K-distribution while the target signal has a constant intensity . A sketch of the derivation for the following probability density function (pdf) is presented in the Appendix.
2.3.1. Conventional Matched Filtering
After matched filtering, the clutter signal intensity
x has the K-distribution. Thus, the conditional pdf (probability density function) under the null hypothesis
is given by
while the pdf under the alternative hypothesis
is
where
and
are the scale and shape parameters, which are dependent on the average size of the clutter and the number of the scatter in the resolution cell of the sonar, respectively.
represents the gamma function.
The likelihood ratio test with threshold
can be expressed as follows:
Then, the corresponding probability of detection is described by
with the false alarm probability
2.3.2. Time Reversal-Based Detection
It is difficult to obtain the pdf of the received signal for the retransmitted time-reversed signal in closed form. Thus, the probability of detection and the probability of false alarm are obtained by using the numerical method.
As mentioned in the earlier section, the initial return signal has the K-distributed intensity after matched filtering. Therefore, the retransmitted signal
has the K-distribution. If the time-varying property of the channel is weak, passing the retransmitted signal through the channel results in the autocorrelation of the channel. However, the real channel is time-varying while the properties do not change suddenly compared to the previous channel [
12,
28]. This deviation is modeled by Gaussian noise. Therefore, the pdf of the current channel becomes the convolution between the previous channel’s K-distributed pdf
and the Gaussian pdf
, where RV
represents the intensity of the previously received signal (i.e., the previous clutter channel) and RV
G is the deviation. Thus, the intensity of the received signal
for the retransmitted signal is the correlation of
and
, that is,
, which implies the case that there is no target, the null hypothesis
. For the case that a target exists, the alternative hypothesis
, the intensity of the received signal includes the target signal intensity
.
Figure 2 shows the probabilities of detection for the conventional and proposed schemes for various false alarm probabilities when the target-to-clutter ratio (TCR) varies from
dB to 10 dB. Note that the shape parameter
and the scale parameter
. As observed in the figure, the proposed method is better than the conventional one by about 5 dB at a probability of detection of 0.9. TCR is measured by power spectral densities of the clutter and target signals, and is defined as follows:
where
represents the band width that contains significant power.
In order to investigate the effect of the shape parameter
on the probability of detection, the probability of detection is numerically estimated as a function of the normalized target signal power with respect to the scale parameter; that is,
for the probability of false alarm
. The shape parameter
is set to 1, 5, 10 and 20 while
.
Figure 3a,b demonstrate the probabilities of detection for the time reversal-based detection and the conventional detection, respectively. As observed in the figures, the probability of detection becomes worse as the shape parameter becomes larger (
), which converges to the Rayleigh distribution.
5. Conclusions
When seabed clutter exists in the received signal, the scattering signal by the target is buried in the clutter signals, which makes accurate detection difficult. In this paper, a method using the time reversal technique is proposed to improve detection performance when the clutter environment is in shallow water. Using the wave focusing effect of the time reversal technique, the peak of the target signal can be enhanced. It is confirmed that the peak of the target buried in the clutter becomes higher when applying the time reversal technique by exploiting the time-varying characteristics of the seabed clutter. The numerical computation of the probability of detection and the false alarm probability demonstrates the improvement of the proposed method over the conventional approach. Furthermore, Monte Carlo simulation results also indicated that the proposed approach is better than the conventional one. In addition, the performance of the proposed approach was investigated in terms of the parameter of the K-distribution and the temporal coherence of the clutter channel. For a strong K-distributed channel and for a highly time-varying channel, the proposed approach shows a better probability of detection. In this study, it was observed that the time-reversal technique can improve the observability of the target peak in shallow water. Note that the kinds of time-varying clutter considered in this study were gravel, sand, and seaweed in the high-speed current. For further study, the strategy for reducing the computational complexity should be investigated for successful real-time applications.