
Iraq encounters climatic challenges that lead to severe rainfall shortages and compound the regional challenges that lead to reduced rates of supplying rivers. In this research, the proposed design helps obtain pure water from polluted or saline water t lower, more competitive costs that can supply nearly 80% of the Iraqi markets.
The system harvests 2 L/day of pure water by adding 5 liters of saline water, a 209% daily improvement. The system consists of 1.125 m2 of double slope single basin solar still with a tilt angle of 30°, pipes, and measurement instrumentation.
Maximum inside temperature, humidity, valuable energy, and efficiency have 77 ℃, 35%, 4.02 W/m2, and 76%, respectively. System analysis results demonstrated that the average water condensation rate per square meter is about 0.4 L/hr. Finally, the rate of pure water harvesting from this desalination system, per square meter, is about 0.282 L/m2 per day when the average intensity of solar radiation reaches 165 W/m2. Two scenarios have been suggested for the experiment. The first scenario tests the system by limiting two water levels, the first at 0.75 cm and the second at 3 cm. The second scenario includes the same design with a black cloth set in the basin demonstrates the most promising data. A wet pad regularly cools down one side of the glass to increase the water vapor condensation and production quantity by 173% to enhancing water production significantly.
Citation: Layth Abed Hasnawi Al-Rubaye, Ahmed Al-Samari, Saad Theeyab Faris, Saadoon Abdul Hafedh. Experimental investigation of improving the solar desalination system for domestic buildings: Iraq as a case of study[J]. AIMS Energy, 2022, 10(5): 1077-1099. doi: 10.3934/energy.2022051
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Iraq encounters climatic challenges that lead to severe rainfall shortages and compound the regional challenges that lead to reduced rates of supplying rivers. In this research, the proposed design helps obtain pure water from polluted or saline water t lower, more competitive costs that can supply nearly 80% of the Iraqi markets.
The system harvests 2 L/day of pure water by adding 5 liters of saline water, a 209% daily improvement. The system consists of 1.125 m2 of double slope single basin solar still with a tilt angle of 30°, pipes, and measurement instrumentation.
Maximum inside temperature, humidity, valuable energy, and efficiency have 77 ℃, 35%, 4.02 W/m2, and 76%, respectively. System analysis results demonstrated that the average water condensation rate per square meter is about 0.4 L/hr. Finally, the rate of pure water harvesting from this desalination system, per square meter, is about 0.282 L/m2 per day when the average intensity of solar radiation reaches 165 W/m2. Two scenarios have been suggested for the experiment. The first scenario tests the system by limiting two water levels, the first at 0.75 cm and the second at 3 cm. The second scenario includes the same design with a black cloth set in the basin demonstrates the most promising data. A wet pad regularly cools down one side of the glass to increase the water vapor condensation and production quantity by 173% to enhancing water production significantly.
We consider an ODE model for traffic flow with rough road condition. Given an index
zi(t)+ℓ≤zi+1(t), ∀t,i, |
one defines a discrete local density
ρi(t)˙=ℓzi+1(t)−zi(t). | (1.1) |
By this normalized definition, the maximum car density is
The road condition includes many factors, for example the number of lanes, quality of the road surface, surrounding situation, among other things. For simplicity of the discussion, we let
At time
˙zi(t)=k(zi(t))⋅ϕ(ρi(t)). | (1.2) |
Here
ϕ′(ρ)≤−ˆc0<0, ϕ(1)=0, ϕ(0)=1. | (1.3) |
For example, the popular Lighthill-Whitham model [18] uses,
ϕ(ρ)=1−ρ. | (1.4) |
The system of ODEs (1.2) describes the Follow-the-Leader behavior, and is referred to as the FtL model. By simple computation we obtain an equivalent system of ODEs for the local densities
˙ρi=ℓ(zi+1−zi)2[˙zi−˙zi+1]=ρ2iℓ[k(zi)ϕ(ρi)−k(zi+1)ϕ(ρi+1)]. | (1.5) |
Note that given the set
Let
Q(zi(t))=ρi(t) ∀i,t. | (1.6) |
Differentiating (1.6) in
Q′(zi)=˙ρi˙zi=ρ2iℓ⋅k(zi)ϕ(ρi)[k(zi)ϕ(ρi)−k(zi+1)ϕ(ρi+1)]. |
Using
zi+1=zi+ℓρi, ρi=Q(zi), |
and writing
Q′(x)=Q(x)2ℓk(x)ϕ(Q(x))⋅[k(x)ϕ(Q(x))−k(x♯)ϕ(Q(x♯))], x♯=x+ℓQ(x). | (1.7) |
Here
When the road condition is uniform so that
ρt+f(ρ)x=0, f(ρ)˙=Vρ⋅ϕ(ρ), | (1.8) |
as
f″≤−c0<0. | (1.9) |
This leads to the following reasonable assumption on
−ϕ″(ρ)>1ρ[2ϕ′(ρ)+c0/V]. | (1.10) |
In this simpler case where
W′(x)=W(x)2ℓ⋅ϕ(W(x))⋅[ϕ(W(x))−ϕ(W(x♯))], x♯=x+ℓW(x). | (1.11) |
Equation (1.11) is studied by the author and collaborator in [22], where we establish the existence and uniqueness (up to horizontal shifte) of the profile
limx→±∞W(x)=ρ±, |
where
0≤ρ−≤ρ∗≤ρ+≤1, f(ρ−)=f(ρ+), f′(ρ∗)=0. |
We show that the profile
In this paper we consider rough road condition, and analyze the behavior of solutions in the neighborhood of a discontinuity in
k(x)={V+,(x≥0),V−,(x<0). | (1.12) |
The ODEs for
˙ρi = {ℓ−1V−ρ2i[ϕ(ρi)−ϕ(ρi+1)],(zi<zi+1<0),ℓ−1ρ2i[V−ϕ(ρi)−V+ϕ(ρi+1)],(zi<0≤zi+1),ℓ−1V+ρ2i[ϕ(ρi)−ϕ(ρi+1)],(0≤zi<zi+1). | (1.13) |
The system of ODEs in (1.13) has discontinuous right hand side. The discontinuity occurs twice for each
The corresponding profile
Q′(x)={Q(x)2ℓϕ(Q(x))[ϕ(Q(x))−ϕ(Q(x♯))],(x♯<0 or x>0),Q(x)2ℓV−ϕ(Q(x))[V−ϕ(Q(x))−V+ϕ(Q(x♯))],(x<0<x♯), | (1.14) |
where
x♯=x+ℓ/Q(x) |
is the position for the leader of the car at
Formally, as
ρt+f(k(x),ρ)x=0, where f(k,ρ)˙=kρϕ(ρ). | (1.15) |
Here
There are various cases, with different relations between
We also show that the solution of the initial value problem with suitable initial data gives the desired stationary profile
We compare our result to the classical vanishing viscosity approach. The conservation law (1.15) can be approximated by a viscous equation
ρt+f(k(x),ρ)x=ερxx, | (1.16) |
where
ddxρε(x)=1ε[f(k(x),ρε(x))−ˉf], | (1.17) |
where
ˉf=f(V−,ρ−)=f(V+,ρ+). |
Monotone viscous profiles exist if one of the followings holds:
● We have
f(V−,ρ)>ˉf for ρ∈[ρ−,ˆρ], and f(V+,ρ)>ˉf for ρ∈[ˆρ,ρ+]. |
● We have
f(V−,ρ)<ˉf for ρ∈[ρ+,ˆρ], and f(V+,ρ)<ˉf for ρ∈[ˆρ,ρ−]. |
See [14,20,15] for more details. For other general references on scalar conservation law with discontinuous coefficient, we refer to a survey paper [1] and the references therein. Other related references on micro-macro models for traffic flow and their analysis include [2,3,9,19]. We would like to mention a recent work [8] (and the references therein), which considers the traveling waves for degenerate diffusive equations on network, where a necessary and sufficient algebraic condition is established for the existence of traveling waves.
The rest of the paper is organized as follows. In section 2 we present various technical Lemmas, on specific properties for the solutions of (1.14) and (1.11). Section 3 is dedicated to the case with
For the rest of the paper, we denote the flux functions
f−(ρ)˙=V−ρϕ(ρ), f+(ρ)˙=V+ρϕ(ρ). | (2.1) |
Since the jump is stationary, the Rankine-Hugoniot condition requires
f−(ρ−)=f+(ρ+)˙=ˉf≥0. | (2.2) |
We note that the cases with
● If
● If
● If
For the rest of the discussion, we assume
f(ρ)>0, i.e. 0<ρ<1. |
We start with some definitions.
Definition 2.1. Let
zi+1−zi=ℓQ(zi), ∀i∈Z. | (2.3) |
Note that if one imposes
Definition 2.2. Given a profile
Q(zi(t))=ρi(t), ∀i∈Z, t≥0. |
The following Lemma is immediate.
Lemma 2.3. Let
Solutions of (1.7) exhibit a periodical behavior.
Lemma 2.4. (Periodicity) Let a continuous function
(a)
(b) There exist a constant period
zi(t+tp)=zi+1(t), ∀i∈Z,t≥0. | (2.4) |
Proof. We first prove that (b) implies (a). Writing
zi(0)=x, zi+1(0)=x♯=x+ℓ/Q(x), |
and using
dzdt=k(z)⋅ϕ(Q(z)) → dzk(z)⋅ϕ(Q(z))=dt, |
the time it takes for car no
tp=∫x+ℓ/Q(x)x1k(z)ϕ(Q(z))dz=constant. |
Differentiating the above equation in
(1−ℓQ′(x)/Q2(x))1k(x♯)ϕ(Q(x♯))−1k(x)ϕ(Q(x))=0, |
which easily leads to (1.7). The proof for (a) implies (b) can be obtained by reversing the order of the above arguments.
The next lemma connects the period
Lemma 2.5. (i) In the setting of Lemma 2.4, if we have
limx→∞Q(x)=ρ+, limx→−∞Q(x)=ρ−, f−(ρ−)=f+(ρ+)=ˉf, | (2.5) |
then the period is determined as
tp=ℓˉf. | (2.6) |
(ii) On the other hand, if the period
limx→∞Q(x)=ρ+, limx→−∞Q(x)=ρ−, |
then the limits must satisfy
f−(ρ−)=f+(ρ+)=ℓtp. |
The proof is for Lemma 2.5 is the same as the proof of Lemma 2.7 in [22]. We skip the details.
Next Lemma shows that the solution
Lemma 2.6. Let
x♯=x+ℓ/Q(x) |
be the position of the leader for the car at
ℓˉf−ℓf(k(x),Q(x))=∫x♯x[1k(z)ϕ(Q(z))−1k(x)ϕ(Q(x))]dz. | (2.7) |
When
ℓˉf−ℓf(V,Q(x))=1V∫x♯x[1ϕ(Q(z))−1ϕ(Q(x))]dz. | (2.8) |
Proof. The Lemma follows immediately from the periodicity property in Lemma 2.4
ℓˉf=∫x♯x1k(z)ϕ(Q(z))dz, |
and subtracting from it the identity
ℓf(V,Q(x))=1V∫x♯x1ϕ(Q(x))dz. |
Remark 2.1. Since
Lemma 2.7. Let
zi<y<zi+1 |
we have
zi+1<y♯<zi+2, where y♯=y+ℓ/Q(y). | (2.9) |
Proof. We prove by contradiction. We first assume that
y♯≤zi+1, therefore [y,y♯]⊂[zi,zi+1]. |
By the periodic property in Lemma 2.4, we have
tp=∫zi+1zi1k(z)ϕ(Q(z))dz>∫y♯y1k(z)ϕ(Q(z))dz=tp, |
a contradiction. We now assume
y♯≥zi+2 therefore [zi+1,zi+2]⊂[y,y♯]. |
But again, the periodic property in Lemma 2.4 implies
tp=∫zi+2zi+11k(z)ϕ(Q(z))dz<∫y♯y1k(z)ϕ(Q(z))dz=tp, |
again a contradiction. Thus, we conclude (2.9), completing the proof.
We now establish the invariant regions
Lemma 2.8. Let
limx→∞Q(x)=ρ+, where ˉf=f+(ρ+). |
Let
I=[y,y♯] where y♯=y+ℓ/Q(y)≤0. |
Then, the followings hold.
(a) If
(b) If
In both cases, we have
limx→−∞Q(x)=ρ−. |
Proof. We only prove (a), while the proof for (b) is similar. The proof is achieved by contradiction. Suppose that
Q(ˉy)=ρ−, Q(x)>ρ− for x>ˉy. | (2.10) |
Now (2.8) implies that the "average" value of
Q(ˆy)=ˆρ, Q(x)<ˆρ for x>ˆy. |
Again, this contradicts (2.8), proving (a).
To prove the asymptotic limit as
Mk˙=maxx∈Ik1ϕ(Q(x)), k≤−2, |
and let
1ϕ(Q(yk))=Mk, k≤−2. |
We claim that
Mk+1−Mk≥O(1)⋅(Q(yk)−ρ−), for k<−2, | (2.11) |
which implies that
limk→−∞Mk=1ϕ(ρ−) and limx→−∞Q(x)=ρ−. |
Indeed, if
yk=zk+1, Mk=1/ϕ(Q(zk+1)). |
Now, (2.8) gives
ℓˉf−ℓf−(Q(zk))≤zk+1−zkV−⋅[1ϕ(Q(zk+1))−1ϕ(Q(zk))]=ℓ(Mk−Mk−1)V−Q(zk), |
which implies
Mk−Mk−1≥V−Q(zk)(1f−(ρ−)−1f−(Q(zk)))=O(1)⋅(Q(yk−1)−ρ−). |
Now consider the case where
Furthermore, applying (2.8) on
ℓf−(ρ−)−ℓf−(Q(yk))=1V−∫y♯kyk[1ϕ(Q(z))−1ϕ(Q(yk))]dz<1V−⋅ℓQ(yk)⋅[1ϕ(Q(y′k+1))−Mk]. |
Since
Mk+1−Mk>V−Q(yk)[1f−(ρ−)−1f−(Q(yk))]=O(1)⋅[Q(yk)−ρ−], |
completing the proof.
Lemma 2.9. (Ordering of the profiles) Assume that there exist multiple profiles that solve the equation (1.14) with asymptotes
Proof. We prove by contradiction. Assume that there exist two profiles
Q1(y)=Q2(y), Q1(x)>Q2(x) for x>y. |
Let
y♯˙=y+ℓQ1(y)=y+ℓQ2(y) |
be the position of the leader for the car at
tp,1=∫y♯y1k(x)ϕ(Q1(x))dx > ∫y♯y1k(x)ϕ(Q2(x))dx=tp,2. |
Since both profiles
In this section we consider the case where the speed limit has a downward jump at
0<ˉf≤f+(ρ∗), where f′−(ρ∗)=f′+(ρ∗)=0, |
and let
f−(ρ−1)=f−(ρ−2)=f+(ρ+1)=f+(ρ+2)=ˉf, and ρ−1<ρ+1≤ρ∗≤ρ+2<ρ−2. | (3.1) |
See Figure 2 for an illustration. Note that we may have
There are 4 possible combinations of
1A.
1B.
1C.
1D.
We denote by
W(0)=ρ∗, limx→−∞W(x)=ρ+1, limx→+∞W(x)=ρ+2. | (3.2) |
Note that any horizontal shifts of
We also recall Lemma 2.5 in [22], where the following is proved:
● As
● As
We discuss each sub-case in detail in the rest of this section.
Since here
ρ+1<Q(0)≤ρ+. |
Once
Theorem 3.1. (Well posedness of the initial value problems) Let
Proof. The proof takes a couple of steps.
Step 1. In the
Along
Q′(0±) is bounded. | (3.3) |
This is easily verified from (1.14), since
Along the curve
h′(x)=ℓ/x2=h(x)2/ℓ. |
Let
Q′(y±)<h′(y). | (3.4) |
Indeed, from (1.14) we have
Q′(y−)=h(y)2ℓ⋅ϕ(h(y))[ϕ(h(y))−ϕ(Q(0))] = h′(y)[1−ϕ(Q(0))ϕ(h(y))],Q′(y+)=h(y)2ℓV−ϕ(h(y))[V−ϕ(h(y))−V+ϕ(Q(0))] = h′(y)[1−V−ϕ(Q(0))V+ϕ(h(y))]. |
Thus (3.4) holds since
Step 2. Once the transversality properties (3.3)-(3.4) are established, the existence and uniqueness of the solution for
Ik=[−kℓ,−(k−1)ℓ], for k=1,2,3,⋯. |
Consider
x♯=x+ℓ/Q(x)>0. |
We have an ODE with discontinuous right hand side, with
Q′(x)=Q(x)2ℓ⋅V−ϕ(Q(x))[V−ϕ(Q(x))−V+ϕ(Q(x♯))] | (3.5) |
where
Q′(ˆx)=Q2(ˆx)ℓϕ(Q(ˆx))[ϕ(Q(ˆx))−ϕ(ρ+)]=0, where ρ+=limx→∞Q(x). |
To prove the upper bound, we claim that
Q′(y)=0, Q′(x)≥0 for x>y. |
Since
Q(y)<Q(y♯), y♯=y+ℓ/Q(y)>0. | (3.6) |
Now (3.5) and
V−ϕ(Q(y))−V+ϕ(Q(y♯))=0. |
Since
Q(y)>Q(y♯), |
a contradiction to (3.6).
Step 3. We iterate the argument in Step 2 for
Q′(x)=Q(x)2ℓ⋅ϕ(Q(x))[ϕ(Q(x))−ϕ(Q(x♯))], x♯=x+ℓ/Q(x)<0. | (3.7) |
The same argument follows. This proves the existence and uniqueness of a monotone solution
Next Corollary establishes the existence of infinitely many monotone profiles
Corollary 3.2. Let
V−>V+, 0<ρ−≤ρ∗≤ρ+<1, f−(ρ−)=f+(ρ+). |
There exist infinitely many monotone profiles
limx→−∞Q(x)=ρ−, limx→+∞Q(x)=ρ+. | (3.8) |
Moreover, these profiles never intersect with each other, and
ρ+1<Q(0)≤ρ+. | (3.9) |
Proof. In Theorem 3.1 we show that there exist many profiles
tp=ℓˉf, where ˉf=f+(ρ+). |
By part (ⅱ) of Lemma 2.5 the limit at
The non-intersecting property of the profiles follows from Lemma 2.9.
Sample profiles of
V−=2, V+=1, ℓ=0.2, ϕ(ρ)=1−ρ, ˉf=3/16. |
As comparison, we also illustrate the stationary viscous profiles. For this sub-case there exist infinitely many stationary monotone viscous profiles that satisfy the ODE (1.17). For each value of
We have shown that for each given
D˙={(x,y) : Q♭(x)<y≤Q♯(x), x∈R}. | (3.10) |
Clearly all profiles of
Since all the profiles in
Q(x,y)(x)=y. |
For any point
Ψ(x,y)˙=Q(x,y)(0), (x,y)∈D. | (3.11) |
Theorem 3.3. Consider the setting of Corollary 3.2 and let
(zi(0),ρi(0))∈D, ∀i∈Z. | (3.12) |
Let
(zi(t),ρi(t))∈D, ∀t>0, ∀i∈Z. | (3.13) |
Denote
Ψi(t)=Ψ(zi(t),ρi(t)), i∈Z, |
and define the total variation
TV{Ψi(t)}˙=∑i|Ψi(t)−Ψi+1(t)|. |
Then, we have
limt→∞TV{Ψi(t)}=0, i.e., limt→∞Ψi(t)=˜Ψ, ∀i∈Z. | (3.14) |
Thus, asymptotically the points
Proof. We first assume (3.13) and prove (3.14). Fix a time
(ⅰ) If
(ⅱ) If
We prove (ⅰ) while (ⅱ) can be proved in an entirely similar way. Let
ρm+1(τ)<ˆQ(zm+1(τ)). | (3.15) |
It suffices to show that
˙ρm(τ)˙zm(τ)<ˆQ′(zm(τ)), | (3.16) |
indicating that the point
ˆQ′(zm)=ˆQ2(zm)ℓk(zm)ϕ(ˆQ(zm))[k(zm)ϕ(ˆQ(zm))−k(zm+1)ϕ(ˆQ(zm+1))]. | (3.17) |
On the other hand, (1.2) and (1.5) give
˙ρm(τ)˙zm(τ)=ρ2mℓk(zm)ϕ(ρm)[k(zm)ϕ(ρm)−k(zm+1)ϕ(ρm+1)]. | (3.18) |
Since
We now prove (3.13). We consider the upper bound
ρi(τ)=Q♯(zi(τ)), ∀i. |
It suffices to show that, if there exist an index
ρm(τ)=Q♯(zm(τ)), ρm+1(τ)≤Q♯(zm+1(τ)), |
then
˙ρm(τ)˙zm(τ)≤(Q♯)′(zm(τ)), | (3.19) |
The proof for (3.19) is entirely similar to that of (3.16), replacing
Numerical approximations are computed for the solutions of the FtL model with the following "Riemann initial data",
zi(0)={iℓ/ρ+,i≥x0,iℓ/ρ−,i<x0, ρi(0)={ρ+,i≥x0,ρ−,i<x0. | (3.20) |
The simulations are carried out for
2−ℓˉf≤t≤2, |
together with the car positions at
x0=0, x0=0.3ℓ/ρ−, and x0=0.6ℓ/ρ−. |
Even though the initial data points
All numerical simulations in this paper are carried out using SciLab. The source codes are available from the author's web-site, see [21].
Since
Theorem 3.4. Let
Q(x)=ρ+ for x≥0, limx→−∞Q(x)=ρ−. |
A typical plot of
Instability. Since
f′−(ρ−)>0, f′+(ρ−)>0, |
therefore information travels to the right.
Since
Q(x)≡ρ− for x<0. |
Now consider the value
V−ϕ(Q(−ℓ/ρ−))=V+ϕ(Q(0+)) → Q(0+)<Q(−ℓ/ρ−)=Q(0−). |
This implies that
Theorem 3.5. Let
We remark that for this sub-case there exists a unique viscous profile for this case, see Figure 5 plot (2). We also plot the solution of the FtL model with this "Riemann data", see Figure 5 plot (3). Observe that the solution is highly oscillatory on
Since both
Theorem 3.6. Let
For this sub-case there are no monotone viscous profiles either. In Figure 6 we plot numerical simulation result for the FtL model, with "Riemann initial data". We observe oscillatory behavior on
In this section we study the case where the speed limit has an upward jump at
0<ρ+1<ρ−1≤ρ∗≤ρ−2<ρ+2. |
We have the following 4 sub-cases:
● Case 2A:
● Case 2B:
● Case 2C:
● Case 2D:
Here both
Theorem 4.1. Let
limx→∞W(x)=ρ+, ρ+1≤W(0)≤ρ−2. | (4.1) |
Then the initial value problem has a unique solution
Furthermore, such a solution satisfies also
limx→−∞Q(x)=ρ−, where ρ−<ρ∗, f−(ρ−)=f+(ρ+). | (4.2) |
Piecing together
limx→∞Q(x)=ρ+, limx→−∞Q(x)=ρ−. | (4.3) |
Varying the
Proof. This Theorem is the counter part of Theorem 3.1 and Corollary 3.2 for Case 1A, but the proof here is much more involving due to the lack of monotonicity. See Figure 8.
Let the initial data be given on
zk+ℓQ(zk)=zk+1, ∀k∈Z. |
We also denote the intervals
Ik˙=(zk,zk+1), for k∈Z. |
Throughout the rest of the proof, we use the simplified notations, for any index
Qk=Q(zk), ϕk=ϕ(Q(zk)). | (4.4) |
The proof takes several steps.
Step 1. Assume that
ρ−≤Q0≤ρ−2. | (4.5) |
We claim that
Q′(0−)>0. | (4.6) |
Indeed, since
1ϕ1−1ϕ0>Q0V+[1ˉf−1f+(Q0)]. | (4.7) |
By using
1V+ϕ1−1V−ϕ0=1V+[1ϕ1−1ϕ0]+1V+ϕ0−1V−ϕ0 >Q0[1ˉf−1f+(Q0)]+1V+ϕ0−1V−ϕ0 ≥ 0. | (4.8) |
Equation (1.14) leads to
Q′(0−)=Q20V+ϕ1ℓ[1V+ϕ1−1V−ϕ0]>0, |
proving (4.6).
Step 2. We claim that on the interval
V−ϕ(Q(y1))=V+ϕ(Q(y♯1)). | (4.9) |
Moreover, there exists a point
y1<y2<0, Q(y2)<Q(y1), Q′(y2)<0. |
Let
Q(y♯2)>Q(y♯1) ⇒ ϕ(Q(y♯2))<ϕ(Q(y♯1)). | (4.10) |
On the other hand, by (1.14) and
V+ϕ(Q(y♯2))>V−ϕ(Q(y2))>V−ϕ(Q(y1))=V+ϕ(Q(y♯1)), |
a contradiction to (4.10).
Step 3. We now show that, if (4.5) holds, then
Q−1<Q0. | (4.11) |
Indeed, we know that there are no local maxima on
Q(y)=Q(0)=Q0, Q(x)<Q0 for x∈(y,0). |
Let
∫y♯y[1k(z)ϕ(Q(z))−1V−ϕ(Q(y))]dz = ∫y♯y[1k(z)ϕ(Q(z))−1V−ϕ0]dz=ℓˉf−ℓf−(Q(y)) = ℓˉf−ℓf−(Q0)˙=γ ≥ 0, |
which gives
γ=∫0y[1V−ϕ(Q(z))−1V−ϕ0]dz+∫y♯0[1V+ϕ(Q(z))−1V−ϕ0]dz. |
Since the first integrand on the right hand side is strictly negative, we get
∫y♯0[1V+ϕ(Q(z))−1V−ϕ0]dz>γ. | (4.12) |
But (4.12) is not possible. Indeed, since
1V+ϕ(Q0)−1V−ϕ(Q0)<0, ∫z10[1V+ϕ(Q(z))−1V−ϕ(Q0)]dz=γ, |
one reaches
∫x0[1V+ϕ(Q(z))−1V−ϕ(Q0)]dz<γ, for any x∈(0,z1), |
a contradiction to (4.12).
Step 4. We now have that, for the initial value problem with initial data
0<Q(z−1)<ρ−2. | (4.13) |
We now claim that there exists a unique solution
limx→−∞Q(x)=ρ−. | (4.14) |
Indeed, if
Mk=max{maxx∈Ik1ϕ(Q(x)),1ϕ(ρ−)}. |
Then, we have, for some index
Mk=1ϕ(Q(yk))>1ϕ(ρ−), where yk∈Ik and Q′(yk)=0. |
Let
Mk+1−Mk≥V−Q(yk)[1f−(ρ−)−1f−(Q(yk))]=O(1)⋅(Q(yk)−ρ−). |
Thus, we conclude that
limk→−∞Q(yk)=ρ−, and limk→−∞Mk=1ϕ(ρ−). |
Therefore on
Q(x)≤E♯(x), limx→−∞E♯(x)=ρ−. | (4.15) |
A symmetrical argument for the local minima below
E♭(x)<ρ−, limx→−∞E♭(x)=ρ−. | (4.16) |
The result (4.14) follows from a squeezing argument. Finally, the uniqueness of the solution follows from the transversality properties (3.3)-(3.4), see [4].
Piecing together the solution
Step 5. Denote by
0<Q♯(z−1)<Q♯(0)=ρ−2. |
We now relax the condition (4.5) on
0<Q(z−1)<ρ−2. |
By Step 4, such a profile satisfies the boundary condition (4.14), completing the proof.
Remark 4.1. We remark on the bound (4.1), in particular the upper bound
Q′(0−)=ρ2+ℓV−ϕ(ρ+)(V−V+)ϕ(ρ+)<0. |
Then, on the interval
With the upper bound
Sample profiles of
Local Stability of the Profiles. Let
Again, numerical simulations are performed for the FtL model for Case 2A, and we plot the solutions with "Riemann initial data" (3.20). See Figure 8 plot (4). We see the clear convergence to a certain profile for each choice of initial data.
This is similar to Case 1B. Since
In Figure 9 we plot the profile
This is the corresponding sub-case as for Case 1C. With the same argument, one concludes that there doesn't exist any profile
For this case, we have neither the profile
We perform numerical simulation to obtain approximate solution for the FtL model, with "Riemann" initial data
ρi(0)={ρR,i≥0,ρL,i<0, zi(0)={iℓ/ρR,i≥0,iℓ/ρL,i<0, z0(0)=0. |
We choose values of
f−(ρL)≠f+(ρR). |
We use
ϕ(ρ)=1−ρ, (V−,V+)=(2,1), ρL=0.6, ρR=0.7, ℓ=0.01. |
The flux functions
ρt+f(k(x),ρ)x=ερxx, |
using the same Riemann data, with
The vanishing viscosity limit solution for the conservation law (1.15) consists of a shock with negative speed from L to M, and a stationary jump from M to R. The solution of the FtL model captures this main feature. However, due to the instability of the path M-R (where the left state is unstable), we observe oscillations behind the stationary jump at
In this paper we derive a discontinuous delay differential equation for the stationary traveling wave profile for an ODE model of traffic flow, where the road condition is discontinuous. For various cases, we obtain results on the existence, uniqueness and local stability of the profiles.
These results offer alternative approximate solutions to the scalar conservation law with discontinuous flux, as a counter part to the classical vanishing viscosity approach. The stabilizing effect of the viscosity is not entirely present in the FtL model, where oscillations are observed behind the discontinuity in the road condition. This is caused by the "directional" influence in real life traffic, where the drivers adjust their behavior only according to situations ahead of them, not what is behind. Heuristically, this fact contributes to the "lack of viscosity" behind the jump at
The natural followup work is to investigate the convergence of solutions of the FtL model, under suitable assumptions, to some entropy admissible solution of the scalar conservation law with discontinuous flux. We expect this to be a challenging task, due to the non-monotone profiles and oscillations behind the jump in the road condition.
One may criticize the FtL model used here of being too simple, especially around the jump in the road condition, where the drivers change their speeds suddenly as they cross
The author is grateful to an anonymous referee for careful reading of the first manuscript and detailed comments, which led to the improvement of the manuscript.
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