As shown in
Figure 1, a coordinate system
is set on the water surface, with the
-axis pointing right and the
-axis pointing upward. The origin of the coordinates falls at the intersection of the first plate and the undisturbed free surface. There are
vertical thin plates numbered from left to right. The draft of the
th plate is
. The depth of water is
. The distance between
th plate and the first plate is
. The progressive waves advance along the negative
-axis direction. The flow field is divided into
regions for the convenience of analysis. The velocity potential of the flow field in each region is denoted as
. Assuming that the propagation time of progressive waves is long enough and the flow field is already stable, the velocity potential can be written as:
2.1. Definite Problem for the Transmission and Reflection of Water Waves
The velocity potential
satisfies the following definite conditions:
The separation variable method is adopted to solve the definite problem shown by Equation (3), and the detail is given in
Appendix A. The general solution for the velocity potential in each flow field region has the expression:
where
are unknowns that should be solved using the rest boundary conditions.
In Equation (4), the first and second terms on the right hand side represent the potential of far-field waves spreading along the negative and positive -axis direction, respectively. The third and fourth terms represent the potential of near-field waves spreading along the positive and negative -axis direction, respectively.
The velocity potentials in different regions are discussed as follows.
2.1.1. Region 1
In region 1 there only exist the first three terms on the right hand side of Equation (4), i.e.:
The first term is the potential of progressive waves, and the second and third ones are the potential of the far-field and near-field reflection waves, respectively.
The progressive waves corresponding to the incident potential
can be written as:
In Equation (6),
is the amplitude of progressive waves. There exists relation between the incident potential and the elevation of the free surface:
i.e.:
Combining Equations (5) and (8), the incident potential can be obtained:
The far-field reflection wave has the expression:
where
is the far-field reflection coefficient, which should be between 0 and 1. Thereby, the velocity potential of the far-field reflection wave can be written as:
Analogously, one can obtain the near-field reflection wave:
where
is the near-field reflection coefficient.
For the convenience of writing, the following substitutions are made:
Substituting Equations (13) and (14) into Equations (9), (11), and (12), and then substituting the resulting equations into Equation (5), one obtains:
2.1.2. Region
In region
, there exist far-field and near-field transmitted waves originating from the right plate (
th plate) and spreading toward the negative
-axis direction, as well as far-field and near-field reflection waves originating from the left plate (
th plate) and spreading toward the positive
-axis direction. Therefore, there should exist four terms in the expression of the velocity potential, which can be written as:
where
are the far-field and near-field transmission coefficients, respectively;
are the far-field and near-field reflection coefficients, respectively.
2.1.3. Region
In region
, there only exist far-field and near-field transmitted waves originating from the right plate (
th plate) and spreading toward the negative
-axis direction. Thus the velocity potential in region
should have the following expression:
where
are the far-field and near-field transmission coefficients, respectively.
2.2. Velocity Potential in Flow Fields
The coefficients in Equations (15)–(17) are unknown, and they need to be solved according to the remaining boundary conditions. The first boundary condition is:
which means that the flow velocities from the two neighbouring domains are the same on their adjacent boundary.
Taking the derivative of Equations (15)–(17) with respect to
, and then taking Equation (18) into account, one obtains:
Substituting Equation (19) into Equations (15)–(17) yields:
In addition, there still exist two sets of boundary conditions. One of them is that the thin plates are impenetrable, so the fluid velocity on the surface of plates is 0. The other is that the velocity potential is the same on the adjacent boundaries of each pair of the neighbouring regions. These boundary conditions can be written as (
):
Substituting Equation (20) into Equation (21) leads to (
):
To obtain the coefficients
and
(
), one should eliminate variables
from Equation (22). To this end, the following steps are carried out. Multiplying Equation (22) by
, then multiplying Equation (22b), (22d), and (22f) by
, then integrating the resulting equations over the domain of definition, finally adding the resulting Equation (22a) to (22b), (22c) to (22d), and (22e) to (22f), respectively, one obtains (
):
with:
From Equations (23)–(29) one can obtain coefficients and (). In the calculation, the value of and could be truncated to limited numbers. Once all coefficients are solved, the velocity potentials in any region can be obtained using Equation (20).
Within the framework of potential flows, the wave energy should be conserved [
8], i.e., the following condition should be satisfied:
In Equation (30), the coefficients
and
related to near-field waves are not included due to the fact that they do not contribute to the wave energy propagation [
8]. Therefore, the transmission coefficient
at the last plate (see Equation (19c)) is sufficient to reveal the characteristics of progressive waves under multiple vertical thin plates.