1. Introduction
With the increasing awareness of environmental protection, the construction of high dam projects has to consider the eco-friendly regulation. Based on this background, the stilling basin with a negative step is proposed. For a high dam project, the stilling basin with a negative step is used for energy dissipation to effectively solve the problems of the fluctuating pressure of the floor, the excessive flow velocity near the bottom of the stilling basin [
1], and atomization so that the impact on the environment is smaller than the traditional energy dissipation by hydraulic jump and ski-jump energy dissipation. Therefore, it has been widely used in many hydropower projects in the world,
Table 1 gives the representative large hydropower project in the world using the stilling basin with a negative step.
The so-called stilling basin with a negative step is a stilling basin with a step set at the entrance that makes the end of the spillway higher than the bottom surface of the stilling basin. Although great progress has been made in theoretical analysis and experimental research on the hydraulic characteristics of the stilling basins with a negative step, most of the research focuses on flow pattern [
2,
3,
4], the energy dissipation mechanism [
1], flow velocity near the bottom [
5,
6], floor stability [
7], fluctuating pressure [
8,
9] and geometric parameter optimization [
10]. However, when large-flow and high-dam projects use stilling basins with a negative step, violent waves are prone to appear. If not taken seriously, this may result in incalculable damage to the entire project. In Wu’s [
11] experiment, it was discovered that the post jump waves caused by energy dissipation by hydraulic jumps can reach several meters and spread far downstream. Since the completion of the Xijin Hydropower Station [
12], both sides of the downstream banks have often been threatened by waves.Based on the results of the Xiangjiaba stilling basin hydraulic model test, Li [
13] once pointed out the stilling basin with a high negative step is prone to large-scale water surface fluctuations. In actual engineering, if this type of problem is not properly resolved, large waves may severely scour the downstream bank slopes. For instance the long-distance propagation of waves can affect downstream navigation and power generation by power plants, and wave reflection and climbing can directly affect the normal operation of the project.
The main function of the stilling pool is to dissipate water energy and to control water jumps in the stilling basin. The water flow in the hydraulic jump is violently turbulent, and a large-scale vortex structure is generated. The more uneven the flow velocity distribution in the stilling basin is, the greater the wave generated. Wu et al. [
11] studied the height, period and spectrum of waves after hydraulic jumps and deduced the relationship between the maximum wave height (
Hmax) and the length of the hydraulic jump. In addition, Dong et al. [
12] studied the water surface fluctuation characteristics of energy dissipation of surface regime, and their test results showed that the flow pattern in the stilling basin is closely related to the magnitude of wave fluctuation. Zheng et al. [
14] studied the variation law of water level in the stilling basin under different step heights and flow pattern transformation. Waves are a form of movement of water, as well as a form of the expression of energy. In the past, stilling basins were mainly used for low-head flood discharge and energy dissipation, and the wave fluctuations in the stilling basin were small and did not affect the safe operation of the project; therefore, there are few studies on wave research in stilling basins. However, a stilling basin with a negative step is mainly used in high-head and large-flow flood discharge projects, the water surface fluctuates drastically during flood discharge, and the wave problem cannot be ignored. Although there are a few studies on the waves in stilling basins and there is not enough information available for reference, at present, wave-related theories have become more mature and have played an important guiding role in ocean engineering and other fields.
According to the wave theory, waves are considered to be highly irregular and random processes in space and time [
15]. In engineering fields, people pay more attention to the basic elements of waves, including the height, period, and wavelength. At present, the zero-crossing method is commonly used to define the height and period of a wave. The wave height is the most important of the wave elements. Many scholars have studied the time-domain distribution [
16,
17], probability distribution [
18], and prediction [
19,
20] of characteristic wave heights, the wave-height statistics [
21]. Some scholars have also proposed theoretical expressions for wave height distribution. For example, Longuet-Higgins [
22] not only found that the distribution of wave heights under steady sea conditions is near the distribution of a stationary random Gaussian process but also rigorously derived the probability distribution of the maximum wave height (
Hmax). Tayfun [
23] proposed a theoretical expression for the statistical distribution of wave heights and acquired asymptotic approximations of the probability density of large wave heights on the basis of previous theories by Longuet-Higgins [
24], Naess [
25], and Vinje [
26]. The wave period is also the focus of wave research. Paolo Boccotti [
17] proved that quasi-determinism (QD) theory is valid in evaluating the probability of the period of waves in shallow and deep waters. Most scholars combine the wave period with the wave height, amplitude and other elements, such as Tayfun [
27], who deduced the theoretical formula for the simultaneous distribution of the large wave heights and periods, and the associated probability distribution for wave heights and periods are optimized by Pual Stansell [
28], who also derived an expression for the joint distribution of the wave amplitude and period. Huang [
29] studied the characteristics of roll-wave based on numerical investigation, such as wave–wave interactions, generality, and spectrum. In terms of wave propagation, Ling studies [
30] the performances of theoretical wave attenuation models in predicting wave damping caused by vegetation. Wei [
31] investigated the influence of uniform vegetation on wave attenuation through physical model experiments, while Blackmar [
32] investigated wave high attenuation in non-uniform vegetation by physical model experiments and numerical simulation. The research methods on waves are very mature, but most of the research on waves has focused on ocean waves. Few scholars have studied stilling basins on the basis of on wave theory, in particular, the waves in stilling basins with a negative step.
In the past, the measurement of waves or water surfaces in stilling basins was mostly performed with point gauges or pressure measuring tubes. Due to the severe fluctuation of the water surface, the measurement results were inaccurate and random. In this study, a digital wave elevation gauge with high accuracy and frequency was used to measure waves. The measurement time met the ergodic theory of various states. The analysis method was based on wave theory, which guaranteed the reliability of the test data and test results. This paper took a hydraulic project as an example to carry out hydraulic model tests of a stilling basin with a negative step. The aim of this paper is to (1) analyze the wave height, average period, wave probability density and power spectrum; (2) obtain the relationship of different characteristics wave height and the wave height forecasting methods; (3) discuss the influence of the step heights and flow-energy ratio on the wave characteristics at the end of a stilling basin with a negative step.
3. Experimental Results
3.1. Basic Flow Patterns
To make the results more representative, a dimensionless number, the flow-energy ratio k (, where q is the unit discharge; is the water level difference between upstream and downstream,; and is the acceleration of gravity) that can represent hydraulic conditions is introduced here. d/P is the relative step height (d is the height of the step, and P is the height of the dam). In this hydraulic model test, it was observed that there are two flow patterns in the stilling basin with a negative step, namely, B-jumps and Wave-jump. The latter appears only when Q = 30 L/s and d/P = 0.0651. The two flow patterns are described below.
3.1.1. B-Jump
When a B-jump occurs, there is an anti-arc section in the spillway at the head of the hydraulic jump position, and the main flow quickly descends after passing the step, forming a local oblique submerged jet in the stilling basin. The interaction between the submerged jet and the water in the stilling pool is very strong. The main flow spreads to the surroundings, and strong shear and turbulence are formed around the main flow. The interaction between the submerged jet and the water body in the stilling pool is very strong. The main flow spreads around, and strong shear and turbulence are formed around the jet, which form a bottom roller after the step, and a large surface roller is formed in the anti-arc section of the spillway and the stilling basin. In general, B-jump can exhibit a mixed flow pattern of oblique submerged jets and submerged hydraulic jumps. When a B-jump occurs, the water surface in the stilling basin is relatively stable, and the energy dissipation rate is high. Therefore, the B-jump is the ideal flow pattern in the stilling basin with a negative step and is the flow pattern needed in the project. The wave characteristics of the B-jump flow pattern in the stilling basin with a negative step are the focus of this research.
Figure 4 shows the test photos and schematic diagrams of B-jump under some conditions.
3.1.2. Wave-Jump
When Wave-jump occurs, the main flow passes through the anti-arc section and shoots out from the top of the step. At this time, the water flow bends upwards, forming a wave, similar to a jet stream. After the main flow falls into the water, it forms a surface roller and causes violent water surface fluctuations. There is a bottom roller between the lower part of the main flow and the bottom plate. Since the incident main flow of Wave-jump first floats up and then dives into the water, higher waves occur in the stilling basin to some extent, so the water surface in the stilling basin is not stable, which has a very negative impact on downstream riverbed protection, navigation and other engineering tasks [
5]. This kind of flow pattern has also been observed in a stilling basin with a negative step and a flat floor. Scholars such as Kawagoshi [
2] and Ohtsu [
38] have carried out more research on this flow pattern.
Figure 5 shows the test photos of Wave-jump.
3.2. Wave Height
Wave height is an important indicator of wave elements and needs to be considered in engineering design.
Figure 6 shows the variation in relative wave height
H1/100/
h2 (
h2 is the water depth after the jump) along the stilling basin with a negative step. The abscissa in the figure is the relative position
x/
L,
x is the distance between the wave elevation gauge and the starting point of the stilling basin, and
L is the length of the stilling basin. The figure shows that under different discharges, the
H1/100/
h2 in the stilling basin shows a gradual attenuation trend as the propagation distance increases. Except W-jump, the
H1/100/
h2 in the standard stilling basin (TP0) is smaller than that in the stilling basin with a negative step (TP1~TP3). With increasing discharge, the degree of fluctuation along the stilling basin gradually increases, and the attenuation speed of the wave height gradually increases along the stilling basin. At the same section position, as the discharge increases,
H1/100/
h2 increases to varying degrees. When
and
, the concentration of
H1/100/
h2 ranges from 0.05 to 0.45.
In addition, under the same discharge conditions, with increasing relative step height d/P, the H1/100/h2 of the same section position shows a decreasing trend. However, TP3 (d/P = 0.0650, Q = 30 L/s) in the figure shows an inconsistent trend. Since the flow pattern in the stilling pool is a Wave-jump, the water flow does not dive to the bottom after entering the stilling basin but forms a wave upward, which causes the overall wave height in the stilling basin to be too large, and the main impact range is x/L < 0.4706. By comparison, it is found that Q = 50 L/s; when the relative step height increases from d/P = 0 to d/P = 0.0651, the maximum reduction in H1/100/h2 is 39.08%, which shows that the height of the step has the most obvious impact on the wave height of H1/100 at this time.
3.3. Average Period
The average period
T (the total time divided by the number of wave height) of the wave is the ratio of the total time to the number of waves, which represents the average speed of the fluctuations.
Figure 7 shows the variation in the average period of waves in different stilling basins with a negative step under different discharge conditions. From the figure, we can obtain the following conclusions:
(1) There is no obvious relationship between the average wave period and the step height. Dong and Lai [
12] also mentioned in their wave research that water surface fluctuation is relatively complicated and that the conventional average period calculation is not enough to reveal an accurate trend; in-depth research and analysis are needed;
(2) In the B-jump flow pattern, the trend of the average period variation along the stilling basin with a negative step is consistent; generally, it increases first and then decreases along the flow direction when the Q ≥ 50 L/s;
(3) As the discharge increases, the self-similarity (coincidence of the curve) of the average period along the flow direction increases because as the discharge increases, the impact of the step height on the waves decreases;
(4) In this study ( and ), the average period of the waves in the stilling basin with a negative step is concentrated in the range of 0.33~0.71 s.
3.4. Wave Probability Density
The probability density of waves can be calculated by the following formula:
where
is the probability density function;
is the expectation;
is the standard deviation; and
is the variance. In the normal distribution,
describes the position of the central tendency, and σ represents the shape parameter. Here, the probability density of the stilling basin with a negative step is analyzed with discharge
Q = 70 L/s as an example.
Figure 8 shows the probability density distribution of the measured values of waves for four test plans (TP0~TP3) when the discharge
Q = 70 L/s. The figure shows the following:
(1) The probability density distribution along the flow direction of different stilling basins with a negative step shows strong similarity due to the same flow pattern in the stilling basin with a negative step (B-jump), the same causes of wave formation and the same form of propagation occurring.
(2) As the relative position x/L increases, the probability density distribution shape gradually develops from “short-fat” to ”thin-tall”, and tends to y-axis symmetry, that is, decreases and the mean value gradually tends to zero along the flow direction, because the water is viscous, the wave energy is dissipated during the propagation process, the reduction in wave energy causes the degree of fluctuation to decrease, and the degree of wave dispersion decreases along the flow direction. The amplitude of the wave gradually moves closer to the average along the flow direction, and the up and down fluctuations tend to stabilize.
(3) The data from
Figure 7 show that in the same discharge conditions, with the increase of relative height of step
d/
P, the
of the same position show a decrease trend, namely the shape of the probability density distribution is more and more tall. This occurs because the distance from the bottom to main flow on the rise with the increase of step height, making the main flow friction and mix with the surrounding water more, the energy dissipation is higher, so the wave energy generated by water at the surface is less, and it fluctuates less.
To further study the extent of wave surface fluctuations, the skewness coefficient
Sk and kurtosis coefficient
Ku are introduced to test the normality of the wave data. The calculation formulas of the skewness coefficient
Sk and kurtosis coefficient
Ku are:
where
is the wave surface height and
is the mean value of the
. The skewness coefficient (
Sk) is an indicator used to measure the asymmetry of the probability distribution of a random signal, and the kurtosis coefficient (
Ku) is an indicator used to measure the steepness or smoothness of the data distribution. For the standard normal distribution,
Sk = 0, and
Ku = 3.
The calculation results of the skewness coefficient (
Sk) and kurtosis coefficient (
Ku) are shown in
Figure 9. The figure shows that for both a standard stilling basin and a stilling basin with a negative step, the larger the relative position
x/
L is, the closer the probability distribution of the waves is to the normal distribution (
Sk = 0,
Ku = 3). This occurs because the wave generation is the strong turbulence formed after the incident main flow enters the stilling basin; the continuous generation of vortices complicates the water surface fluctuations; the farther the relative position is, the more energy the water flow into the stilling basin can dissipate; and irregularly moving water surface fluctuations are continuously adjusted along the flow direction, making the water flow close to a nonuniform gradual flow, so the dispersion degree of the wave relative to the average value is smaller. A study by Dong [
12] et al. found that the wave probability density is more skewed approaching the nose sill and is close to the normal distribution far from the nose sill. The main reason for this is that there is a roller area near the nose sill, so the data have a large degree of dispersion. Sun [
39] also mentioned in his paper that the probability density distribution of waves is closer to a normal distribution as the distance from the step increases; when the discharge increases,
Sk and
Ku both tend to increase because when the discharge increases, the turbulence of the water entering the basin increases, resulting in more violent water surface fluctuations and poor stability.
The figure also shows that there are no obvious differences between the standard stilling basin (TP0) and stilling basin with a negative step (TP1~TP3). When and , the skewness coefficient (Sk) of the wave probability distribution is in the range of 0.0062~0.7535, and the kurtosis coefficient (Ku) is 2.8531~4.7516.
3.5. Power Spectrum
The frequency-domain properties are usually represented by spectra, which can describe the internal structure of waves.
Figure 10 shows the time-domain process and power spectrum of the wave signal at
Q = 30 L/s and relative position
x/
L = 0.047 in the stilling basin with a negative step (TP3).
Figure 10a shows that the wave signal in the stilling basin with a negative step is a typical random process signal. The result of
Figure 10b shows that the wave signal in the stilling pool is in the low-frequency narrowband noise spectrum [
40]. The frequency band is narrow, and the wave energy is concentrated in the low-frequency area (
f < 10 Hz).
The frequency with the highest spectral density is called the dominant frequency (also known as the dominant frequency or peak frequency) and is denoted as
. In water conservancy projects, it is generally believed that when the main frequency is equal to or close to the natural frequency of the hydraulic structure in the water, resonance is likely to occur, leading to the destruction of the hydraulic structure. Therefore, it is necessary to obtain the distribution relationship of
through the spectrum analysis method. The distribution of the
of waves in the stilling basin with a negative step is shown in
Figure 11. From the figure, we can obtain the following:
(1) The along the stilling basin with a negative step shows a trend of first increasing and then decreasing, and the maximum value of appears in the range of 0.20 < x/L < 0.45.
(2) The correlation between the of the wave and the step height is weak, and the values along the flow direction of the standard stilling basin (TP0) and the stilling basin with a negative step (TP1~TP3) are not very different.
(3) When and , the wave energy is mainly concentrated in the low-frequency band, and is less than 2.5 Hz.
5. Conclusions
In this study, the waves in a stilling basin with a negative step were studied through hydraulic model tests. Based on wave theory, the trends of wave height and other elements along the flow direction were analyzed, and the effects of the flow-energy ratio k and relative step height (d/P) on the wave characteristics were discussed. The following conclusions were drawn:
(1) Two typical flow patterns in the stilling basin with a negative step are observed in the experiment, B-jumps and Wave-jump. The Wave-jump has a greater influence on the wave characteristics than the B-jump. For both Wave-jump and B-jumps, the H1/100/h2 increase with discharge and decrease with relative step height d/P. There is no obvious relationship between the average wave period and the step height, but the change in the average period shows a trend of first increasing and then decreasing along the flow direction when Q ≥ 50 L/s.
(2) The probability density distribution of the wave gradually tends to the standard normal distribution as the relative position x/L increases. The dominant frequencies of the wave in the stilling basin with a negative step are all less than 2.5 Hz.
(3) According to the experimental data, the conversion relationships between different wave heights are obtained. Based on the theorem and regression analysis, the empirical calculation formula for the relative characteristic wave height is obtained. The dimensionless standard deviation at the end of the stilling basin with a negative step is linearly related to the flow-energy ratio k. For the B-jump, shows a good linear relationship with the relative step height d/P.