1.
Introduction
Vegetation and water resources are important components of the ecosystem. In arid regions, the lack of water resources and the destruction of vegetation lead to desertification. If desertification is formed, it will seriously affect human survival and economic development. From [1], worldwide, economic losses caused by desertification are more than 40 billion dollars every year. On the other hand, in the rainforest ecosystem, abundant vegetation and water resources provide sufficient oxygen for the survival of life on earth. If the rainforest ecosystem is destroyed, life on earth will inevitably suffer the disaster. Therefore, it is of great significance to model a reasonable dynamic system and analyze its dynamic behavior. Meanwhile, studying the optimal control strategy is helpful for the reasonable and effective protection of vegetation ecology.
In the natural environment, the vegetation-water systems are usually disturbed by human activities and natural disasters, such as planting vegetation, irrigation, pruning vegetation regularly, and so on. These phenomena can be more accurately described by impulsive differential equations. Therefore, in recent years, some results were proposed on modelling impulsive vegetation systems [2,3,4,5]. In these references, only some impulse events that reduce the biomass density of vegetation were considered, such as forest fires. In vegetation restoration and protection, we mainly adopt measures, including planting and irrigation, etc. Obviously, these behaviors can increase the density of vegetation and water. However, the corresponding impulsive vegetation-water systems are rarely analyzed.
On the other hand, in ecosystem, delay is also a ubiquitous phenomenon that may cause a dramatic changes on dynamic behavior [6,7,8]. In recent years, delay has been taken into consideration in research on vegetation systems [9,10,18]. In [9], Han et al. took constant delay into the vegetation water system and studied the dynamic behavior. In [10], Wang et al. analyzed the asymptotic stability of the equilibrium and Hopf bifurcation in a constant delay vegetation ecosystem. In [11], the authors considered the delay into vegetation-water system and studied the stability and Hopf bifurcation. However, the papers mentioned all consider constant delay. In fact, in real ecology, the delay can be affected by various factors such as temperature, soil moisture content and so on. Therefore, the delay of penetration is related to time. In this paper, we consider the time-varying delay into the vegetation-water system.
In addition to impulse and delay, there are many achievements evidence that noise also plays a major role in vegetation systems [12,13]. In the real world, it is known to all that there are various environmental factors (such as organic matter, climate and so on) that can affect the ecosystem, which is manifested by fluctuating ecological material density. Recent research results support the importance of stochastic processes in ecosystems [14,15,16]. For example, Pan et al. [17] studied the near-optimal control of a stochastic vegetation-water system. Zeng et al. [18] analyzed the catastrophic regime shifts of a stochastic grazing ecosystem to explore the impact of noise on vegetation degradation. However, the stochastic process they mainly consider is Gaussian white noise in the system. The Gaussian noise is suitable to simulate non-abrupt and uniform environmental disturbances such as small-scale rainfall, temperature change, etc. It is worth noting that the phenomenon of large disturbance exists in nature, such as volcanic eruptions and earthquakes [19]. Meanwhile, there is evidence that the transition from forest to drought will not be smooth but will exhibit sudden transitions. For example, in [20,21], a large-scale, long-term experiment showed that the mortality of vegetation will increase abruptly to 226 and 462 percent in the dry season. These sudden changes may have a profound impact on the natural ecosystems and cannot be ignored [22]. The scholars have done some researches and shown that for abrupt random pulsing phenomenons can be described by the Lˊevy process [23,24]. There are several existing works on the impact of the Lˊevy process on ecosystems. For instance, Zhang et al. [25] considered the Lˊevy process into the grazing ecosystem and analyzed its impact on system dynamics. Larissa et al. [26] introduced Lˊevy process to model the Amazon vegetation ecosystem and analyzed metastability of system. However, there been no research that introduced Lˊevy process into vegetation-water system to analyze dynamic behavior.
In the last several years, the dynamic behaviors of vegetation system were extensively investigated. For example, R. Lefever and O.Lejeune [30] introduced a single-equation (vegetation biomass density) system and studied the bifurcation theory and the stability of the steady-state solution. Klausmeier et al. established a vegetation-water (soil water) system and explored the Turing instability of the system [31]. Rietkerk et al. proposed a vegetation-water (soil water and surface water) system and analyzed the stability of steady-state solution [32]. Obviously, they mainly paid attention to long-term dynamic behaviors. Noteworthy, finite-time stability plays a significant role in modeling real-life problems and arises in a wide range of applications, such as economic-controlled system, neural networks and so on [33,34,35,36,37]. In arid ecosystems, the density of vegetation and water is closely related to eco-quality. Low-level vegetation and water density means desertification. Meanwhile, because the environmental capacity is limited, the high density of vegetation and water will also harm the ecological environment. Therefore, it is of significance to study the finite-time stability of vegetation-water system.
On the other hand, as is known to all that controlling drought land and rainforest degradation have posed a huge economic burden. Because of the large affected area, it is costly to use control strategy, such as planting vegetation, rational irrigation, etc. Therefore, from the perspective of ecological economics, how to formulate optimal control strategies to balance the costs and benefits is an important and meaningful question. However, there are few papers introducing control strategies to study optimal control problems in the vegetation system.
In this paper, we propose a new vegetation-water system and analyze finite-time stability by using comparative principles. Then, we introduce the control variables into the system and analyze the optimal control of the controlled vegetation system by using the minimum principle. In summary, our main contributions are as follows:
(i) We propose an impulsive stochastic reaction-diffusion vegetation-water system driven by Lˊevy process with time-varying delay. Our model is an extension of literature [2,9,32].
(ii) The sufficient conditions for finite-time stability are given as theoretical results which reflect the effects of diffusion, impulse, delay, and noise disturbance. Compared with existing work, in the analysis of finite-time stability, our contribution is the study of system with time-varying delay and Lˊevy noise. In order to deal with time-varying delay, we use the idea of classification.
(iii) The control strategies are considered into the impulsive stochastic vegetation-water system with delay, such as planting vegetation, irrigation, applying chemicals etc. Then, the explicit expression of optimal control is obtained through the minimum principle.
The remaining structure of the paper is organized as follows: in section 2, a stochastic diffusion vegetation-water system, with varying-time delay, impulse, and Lˊevy jump is established. In section 3, we complete the proof of the existence and uniqueness of the global positive solution. Further, we analyze the finite-time stability of the system and give sufficient conditions for the establishment of stability theorem. In section 4, we analyze the optimal control problem by using the minimum principle under the vegetation-water system with control. In section 5, a numerical simulation is presented to illustrate theoretical results. In section 6, we discuss and summarize the main results of this paper.
2.
Model formulation and preparations
2.1. Model formulation
In this section, a vegetation-water system with spatial diffusion, time-varying delay, impulse, noise is proposed. Before driving our system, let us recall a classic vegetation-water system proposed by Rietkerk in [32]
here ˉu(x,t), ˉv(x,t), ˉw(x,t) represent the vegetation biomass density, soil water density and surface water density, respectively. Δ is the Laplace operator. The ∂Γ is the boundary of Γ∈R2. All parameters in model (2.1) are assumed non-negative constants and are described in Table 1. In the following, we complete the construction of the new vegetation system.
(1) Surface water evaporation
In the real world, it is ubiquity for surface water (mainly refers to rivers) to evaporate under the influence of some factors such as temperature, wind, etc. In arid regions, the problems of low rainfall and high evaporation are widespread. The evaporation of surface water can hinder the supply of soil water and further affects the growth of plants. Therefore, they may be the cause of ecological degradation. For example, in Yinchuan, China, the annual evaporation reaches 2000 mm, but the rainfall is only 200-300 mm and the desertification situation here is serious [38]. For this phenomenon, we take the loss rate of surface water into account in vegetation-water system. The system (2.1) can be transformed to
(2) Time-varying delay
The transfer of surface water to soil water is considered as a time delay process. Meanwhile, because the infiltration rate of surface water is affected by the water content of soil, we take time-varying delay into system (2.2). In Figure 1, we show the time delay from surface water to soil water. Thereby, in infiltration item of system (2.2), we replace ˉw(t) with ˉw(t−τ(t)) and get the following system
where the τ(t) is bounded, which implies that there is a constant ˉτ>0, such that 0<τ(t)≤ˉτ. Besides, we assume that 0≤˙τ(t)≤η<1. In fact, the hypothesis about ˙τ(t)≥0 fits the real situation. Because the time required for surface water to penetrate will increase with time. And when there is enough soil water, the time required surface water infiltration will tend to a fixed value ˉτ.
(3) Impulse phenomenon
Impulsive phenomena are very common in vegetation ecosystem. For example, human behavior such as planting and felling vegetation, irrigation and so on can be described by impulse differential equations. In this subsection, we introduce the impulse into the vegetation system. The details are as follows:
(i) We define Iku as the impulse intensity that affects vegetation biomass density. It is worth noting that the planting trees, planting grass and other events correspond to Iku>0 and felling plants correspond to Iku<0. However, based on practical factors, vegetation can not be completely destroyed by impulse events. Meanwhile, the impulse intensity can not be too large. We have reason to assume that −1<Iku≤Imu, where Imu is the maximum allowable impulse on vegetation.
(ii) We define Ikv, Ikw as the impulse intensities that affects soil water density and surface water density, respectively. Irrigation, rainfall and other events correspond to Ikv>0, Ikw>0 and industrial water, drainage and other events correspond to Ikv<0, Ikw<0. However, from reality, soil water and surface water never thoroughly disappear due to impulse events and the impulse intensity can not be too large, which means that −1<Ikv≤Imv, −1<Ikw≤Imw, where Imv and Imw are the maximum allowable impulse on soil water and surface water, respectively.
Therefore, the system (2.3) rewrites as
where {tk} (k∈N) is impulsive sequence satisfies 0=t0<t1<t2<⋯<tk<⋯<t∞=∞, ϑ(x,t+k)=limt→t+kϑ(x,t) (ϑ=u,v,w). We define dm=maxk∈N{tk−tk−1}, ds=mink∈N{tk−tk−1}. x∈Γ⊂R2 is a bounded measurable set which means that there are constants bi>0, such that |xi|≤bi, where xi (i=1,2) are components of spatial variables x.
(4) Lˊevy processes
In the real world, there are physical environmental disturbances such as volcanic eruptions, sudden sandstorms, temperature surges and so on, and biological environmental disturbances such as mass migration of herbivores. It can affect the natural loss rate of species, can be modeled by the Lˊevy noise. Therefore, we let
where Li(t) is Lˊevy process which is composed of a Brownian motion with a linear drift term and a superposition of centered (independent) Poisson processes with different jump sizes ˉy∈Y. It follows from the Lˊevy-Itˆo decomposition theorem that
where ¯ai (day−1)∈R, ¯σi (day−1)≥0, Bi(t) is standard Brownian motion, ˜N(dt,dˉy)=N(dt,dˉy)−λ(dˉy)dt is a compensated Poisson process and N(dt,dˉy) is a poisson counting measure with characteristic measure λ on a measurable subset Y∈(0,∞) with λ(Y)<∞. Thus, the model becomes
where ¯l1=d+ρ1¯a1, ¯l2=b+ρ2¯a2, ¯l3=p+ρ3¯a3. Besides, we assume that Bi(t) is in dependent of N(t,dˉy). The initial value and boundary condition of system (2.5) are given as follows
where n is the out normal vector of ∂Γ; ψϑ(x,s) (ϑ=u, v, w) are bounded and continuous functions on (−ˉτ,0]×Γ.
2.2. Preparations
In order to facilitate the subsequent theoretical analysis, we implement the dimensionless processing for the system (2.5) using the method of Zelnik et.al. [12]. Therefore, we obtain the following non-dimensional vegetation-water system with time delay and impulse
where u=ˉuk2, v=ˉvk1, w=k0ˉwcgmk1, du=k0duodwocgm, dv=k0dvodwocgm, dw=1, l1=¯l1cgm, γ=k2ck1, l2=¯l2cgm, R=Rocgmk1, α=k0cgm, l3=¯l3cgm, f=f, σi=¯σicgm (i=1,2,3), ˉy=ˉycgm, t=cgmtoriginnal, x=√dwok0xoriginnal. The toriginnal and xoriginnal are the time and space variables before the dimensionless transformation processing.
Let X={(u,v,w)∈W2,2,∂(u,v,w)∂n=0on∂Ω}. Define Cb+ as a family of bounded and continuous functions. M+=L2(Γ×[0,∞),R3+) represents the set of square integrable functions defined on Γ×[0,∞), which is equipped with the norm ‖⋅‖, where ‖y(x,t)‖=(∫Γy(x,t)yT(x,t)dx)12. y(x,t)=(u(x,t),v(x,t),w(x,t)). Let (Ω, F, (Ft)0≤t≤T, P) be a complete filtered probability space with a filtration {(Ft)0≤t≤T}. E denotes the probability expectation corresponding to P. Additionally, there is a hypothesis that needs to be given.
Assumption 2.1 There is a positive constant Li such that ∫Yρiy(ρiy+2m(Γ)−2)λ(dy))<Li<+∞ (i=1,2,3), where m(Γ) is the measure of Γ.
Remark 2.1 The assumption 2.1 implies that the intensity of random noise is constrained, which follows the biological background.
3.
Main results
In this section, the positivity, existence and uniqueness of the global solution of system (2.6) is analyzed by a method similar to [39,40]. Then, we study the finite-time stability of vegetation-water system. In the end, we introduce control variables into the vegetation-water system and study the optimal control of the control system.
3.1. Existence and uniqueness of positive solutions
Theorem 3.1 For any given initial data (ψu(x,s),ψv(x,s),ψw(x,s))∈Cb+, there is a unique global positive solution (u(x,t),v(x,t),w(x,t)) of system (2.6) on t≥0 almost surely, which means the solution will remain in M+ with probability 1.
The proof of Theorem 3.1 is given in Appendix.
3.2. Finite-time stability
Definition 3.2 Given positive number T, B1, B2 with B1<B2, system is said to be finite-time stabile with respect to (T,B1,B2), if any t∈[0,T],
where y(x,t)=(u(x,t),v(x,t),w(x,t)).
Remark 3.3 Definition 3.2 implies that when the initial value of the state variable is within a given limit, it does not exceed the given threshold in a finite time. The image of finite-time stability is displayed in Figure 2.
In the following, we give the theorem of finite-time stability of impulsive stochastic reaction-diffusion system with time-varying delay. We present some parallel sufficient conditions of finite-time stability of the system. These conditions reflect the influence of random disturbance and spatial diffusion on finite-time stability. Before proposing the theorem, assign
Theorem 3.4 The system (2.6) is finite-time stable with respect to (T,B1,B2) if one of the following condition holds:
C1:0<θ<1, K3≠0, c1θ≤−K4e−c2ˉτ<0, −lnθ≤ω,
C2:0<θ<1, K3≠0, −K4e−c1ˉτ≤c2θ≤0, (c1+K4θ(1−η)e−c2ˉτ)T+K4θ(1−η)e−c2ˉτˉτ−lnθ≤ω,
C3:0<θ<1, K3>0, c1>0, (K4+c1)T−lnθ≤ω,
C4:θ≥1,K3>0, c3>0, (K4+c3)T≤ω,
C5:θ≥1,K3<0, c3>0, (K4+c4)T≤ω,
C6:θ≥1,K3<0, c3<0, (c4+K41−ηe−c4ˉτ)T+K4ˉτ1−ηe−c4ˉτ≤ω.
Proof. For a given number B1, letting sup−ˉτ≤s≤0∫Γu2(x,s)+v2(x,s)+w2(x,s)dx≤B1. Set
An application of Itˆo formula yields that
By using some basic inequalities and applying of Green identity (lemma 2, [41]), we have
where K2=m(Γ), K4=α(1+f), K3=max{1+ρ21σ21+L1−l1−2du∑2i=1b−2i,α(1+f)+ρ22σ22+L2−l2−2dv∑2i=1b−2i,R2+α(1+f)+ρ23σ23+L3−l3−2dw∑2i=1b−2i}.
For t=tk, one can derive that
where θ=max{(1+Iku)2,(1+Ikv)2,(1+Ikw)2}. Taking expectation on Eq.(3.1), Eq.(3.2), we get
Next, we choose b(t) satisfies
It follows from comparison lemma [42] that
According to the method of variation of constant on (3.3), we have
for t≥0. Noting that
Therefore, a direct computation gives that
Hence, based on (3.4), for t≥0, there is
In the following, we continue our analysis under two situations.
Situation1: 0<θ<1.
Case C1−1: K3>0.
Take a continuous function h(λ)=K4e−λˉτ−θ(λ−lnθdm−K3). We have h(−∞)=+∞, h(0)=K4+θ(K3+lnθdm). Form C1, we can know θ(lnθdm+K3)<−K4e−(lnθdm+K3)ˉτ. Therefore, we can easily yield that h(0)=θ(lnθdm+K3)+K4<0. Besides, ˙h(λ)=−ˉτK4e−λˉτ−θ<0. Therefore, there is at least one number λ1<0 such that K4e−λ1ˉτ=θ(λ1−lnθdm−K3). It is clearly that
In the following, we prove the inequality
If the inequality is not true, there is a t∗ such that
and
However, it follows from (3.4) that
It contradicts (3.7), so (3.6) holds. Furthermore, we have
Based on C1, we have −lnθ≤lnB2−ln(B1+K2K3) for K3>0. This implies that EV(t)≤B2. It shows the desired result.
Case C1−2: K3<0.
From (3.4), we have
Based on C1, we can obtain θ(lnθdm)<−K4e−(lnθdm)ˉτ<0. By the same discussion as in C1−1, we obtain that
where λ2 is the root of equation h(λ)=K4e−λˉτ−θ(λ−lnθdm) and λ2<0. C1 implies that −lnθ≤lnB2−ln(B1−K2K3) for K3<0. This means that
It is the desired result.
Case C2−1: K3>0.
Contrary to C1-1, we consider −K4e−(lnθdm+K3)ˉτ≤θ(lnθdm+K3)≤0. Assign
Form (3.5), 0≤η<1 and Gronwall inequality [43], one has
Then, there is
C2 gives that ((lnθdm+K3)+K4θ(1−η)e−(lnθdm+K3)ˉτ)T+K4ˉτθ(1−η)e−(lnθdm+K3)ˉτ−lnθ≤lnB2−ln(B1+K2K3). Therefore, we obtain EV(t)≤B2. It means that the system (2.6) is finite-time stability under condition C1.
Case C2−2: K3<0.
Contrary to C1-2, we consider −K4e−(lnθdm)ˉτ≤θ(lnθdm). In this case, choosing
Similar discussion as in C2−1, one obtains
Further, we can compute that
In view of C2, one can calculate that (lnθdm+K4(1−η)θe−(lnθdm)ˉτ)T+K4ˉτ(1−η)θe−(lnθdm)ˉτ−lnθ≤lnB2−ln(B1−K2K3). Therefore, EV(t)≤B2.
Case C3−1: K3>0.
Contrary to the above case, we consider K3+lnθdm>0. Let f(t) satisfy the following equation
where ˜f=sup−ˉτ<s<0f(s). By virtue of (3.5) and (3.13), we derive 0≤b(t)≤f(t) for t≥−ˉτ. Before the following proof, setting
It is obvious that A1∪A2=(0,ˉτ]. For t∈A1, one can obtain
For t∈A2∪(ˉτ,T], a direct calculation leads that
This implies that f(t)≥f(t−τ(t)) when t>0. Then, in light of (3.13), we can deduce the following inequality
The Gronwall inequalities [43] gives that
That is to say
By virtue of C3, one can see that (K4+lnθdm+K3)T−lnθ≤lnB2−ln(B1+K2K3). This implies that EV(t)≤B2. Then we can obtain the required statement.
Situation 2: θ≥1.
In this situation, one can calculate that
and
It is clear that inequalities (3.15) and (3.5) have the same form and properties. We can use the same method as the discussions in Situation 1, and yield the desired result. For the sake of simplicity, we omit the details.
Remark 3.5 In the theorem 3.4, we have dealt with sufficient conditions that are more stringent than the actual situation. For example, in C1, we show the system 2.6 is finite-time stable when the condition c1θ≤−K4e−c2ˉτ<0 holds. In fact, in our proof, we put forward that the system 2.6 is finite time stable under the condition c1θ≤−K4e−c1ˉτ<0. It is clearly that −K4e−c2ˉτ<−K4e−c1ˉτ.
Remark 3.6 For an ecosystem, the initial material (vegetation and water) density B1 can be estimated. Similarly, the desired maximum density B2 of vegetation and water can also be given. In addition, the desired time T to keep the density of plants and water between B1 and B2 can also be given. Therefore, we can judge whether the system is finite-time stable through the relationship between the parameters.
4.
Optimal control strategies
Desertification can bring great economic losses. We need to adopt some control strategies to increase the amount of vegetation and water density. There are many strategies for the management of vegetation systems such as replanting, irrigation, and so on. The cost of strategy is inevitable. It is easy to think that the way to save costs is the search for optimal control. In the following, we mainly use the principle of minimum value to find the optimal control in the vegetation system.
Consider (u(x,t),v(x,t),w(x,t))∈X where X is defined in preparations. We define a control function set as U=U1⋃U2={πi=πi(x,t) where (x,t)∈Γ×{t|[0,T]−{tk, (k∈N)}}|i=1,2,3}⋃{πi=πi(x,tk) where x∈Γ, tk∈[0,T] and k∈{1,⋯N}|i=4,5,6} where the meaning of πi are listed as follows:
(a) π1 indicates that the planting strategy is used to increase vegetation density.
(b) π2 is the strategy of applying aquasorb which can reduce the infiltration and loss of soil water [44].
(c) π3 is the use of chemical substances such as Hexadecanol, Octadecanol, Cetyl and Stearyl alcohols strategy which can inhibit the evaporation of surface water [45,46,47].
(d) The control strategy of πi (i=4,5,6) can be explained by human control or government intervention.
Due to the limitation of technology or cost, each control strategy πi has an upper bound πmax. A vegetation model with control strategy can be given as
The conditions of initial value and boundary are the same as system (4.1). The set X is admissible trajectories is given by
and the admissible control set U is given by
We consider the objective function
It is worth noting that Qi (i=1,2⋯6) are the weight constants for control strategies, Pi (ˉPi) (i=1,2,3) are positive weight constant of vegetation, soil water, surface water, respectively. 12Qiπ2i (i=1,2,⋯6) is the cost of control strategies. The square of the control variables means that the cost of strategies is gradually increasing [48]. Our goal is to obtain the most plants and the lowest cost of corresponding control strategy. Therefore, optimal control problem is equivalent to finding the optimal control U∗ in the allowable control set U and determining the corresponding vector function (u∗,v∗,w∗)∈X to satisfy the objective function:
Further, we introduce adjoint equation and Hamiltonian function [49,50,51,52]
Theorem 4.1 The optimal control problem (4.2) with fixed time T admits a unique optimal solution (u∗,v∗,w∗) associated with an optimal control U(x,t) for (x,t)∈Γ×[0,T]. Moreover, there are adjoint functions pi(⋅,⋅) (i=1,2,3) such as
where ς(t) is introduced to take into account the function dependence of the time-varying delay τ(t) on time; if s=t−τ(t), 0≤t≤T, is solved for t, ς(t) is given by t=s+ς(s). Additionally, the χ[a,b](t) is a characteristic function defined by
Furthermore,
where
The proof is omitted. Interested readers can see the reference [49].
5.
Numerical examples
In this section, numerical simulations are given to illustrate our theoretical results. We select the parameters from the Table 2.
5.1. Finite-time stability
In this section, we discuss that the system is finite time stable when the sufficient conditions are satisfied. We take Γ=[−0.25,0.25], d=0.1, k0=0.05, Ro=3, ρi=0.3, ai=0.5, σi=0.9 (i=1,2,3). Then, one can obtain the m=1, L1=L2=L3=0.09, K2=0.500, K3=0.7809≠0, K4=0.12. Letting B1=1.44, B2=8.41, T=4, (u0(x,t),v0(x,t),w0(x,t)=(0.9,0.9,1) where t∈(−ˉτ,0) and taking Iu=Iv=Iw=−0.2, we can get c1=−0.3348, θ=0.64∈(0,1) and y(0)=1.144 by simple calculation. We set the impulse sequence tk={0.4,0.8,1.2,1.6,2,2.4,2.8,3.2,3.6,4,4.4}. Therefore, dm=0.4, ds=0.4. Additionally, we choose
and noise (Figure 3(a)). Through calculation, we have ˉτ=110f=1/2, η=5fπ4=π/4. For noise, we choose a α stable Lˊevy process which is randomly generated and shown in Figure 3(a). A directly calculation shows c1θ=−0.2143<−K4e−c2ˉτ=−0.2096<−K4ec1ˉτ=−0.1419<0, and −ln(θ)=0.4463<ln(B2)−ln(B1+K2K3)=2.8619. Therefore, the condition C1 is holds. From Figure 4, we can know ‖y(x,0)‖=1.144<√B1=1.2<maxΓ×[0,T]‖y(x,t)‖=2.8814<√B2=2.9, which means the system (2.6) is finite-time stable.
(1) The role of impulse
In this section, we consider the impact of impulses on finite-time stability. Obviously, from sufficient conditions, we can find that the finite time stability of system (2.6) can be effected by impulse. In order to intuitively indicate the effect of the impulses through numerical simulation, we keep the system parameters, time delay function τ(t) and noise (Figure 3 (a)) unchanged and show the variation of the finite-time stability of the system (2.6) under different impulse intensities. Therefore, we choose Iu=Iv=Iw=0.
Through simple calculations, we can get θ=1, c3=0.7809>, K2=0.5, K3=0.7809>0, K4=0.12 and (K4+c3)T=4.0541>ln(B2)+ln(B1+K2/K3)=1.3969. Therefore, the conditions of theorem 3.4 is not satisfied. The results of the numerical simulation of Iu=Iv=Iw=0 are shown in Figure 5. We can find y(1.9154)=4.0297>√B2=2.9 which means system (2.6) is not finite time stable. Comparing with the results of Iu=Iv=Iw=−0.2 which are shown in Figure 4, we can know that the impulse can affect the finite-time stability.
(2) The role of time delay
Time delay does affect the finite-time stability of system (2.6). For example, in details, the larger ˉτ plays an opposite role in satisfying the inequality c1θ≤−K4e−c2ˉτ in C1. Retaining the system parameters, the impulse intensity and noise (Figure 3 (a)) unchanged, we choose τ2(t)=ˉτ2=4.5.
Through a direct calculation, it can be known that η=0, θ=0.64<1, K2=0.5, K3=0.7809>0, K4=0.12, c1=−0.3348 and (c1+K4/θ/(1−η)exp(−c1ˉτ))T+K4ˉτ/θ/(1−η)exp(−c1ˉτ)−ln(θ)=6.5531>ln(B2)+ln(B1+K2/K3)=1.3969, which means the conditions of theorem 3.4 is not satisfied. Further, from Figure 6, we find ‖y(3.3980)‖=4.0454>2.9=√B2 which implies the system is not finite-time stable. Compared with ˉτ=1/2 in Figure 4, the change of delay affects the finite-time stability.
(3) The role of noise
It is essential to analyze the impact of environmental noise. For comparison, we choose ρi=0 and ρi=0.5 (i=1,2,3) to carry out numerical simulation. The time delay function τ(t), noise path as Figure 3(a) and system parameters except ρi (i=1,2,3) are also unchanged.
When ρi=0 (i=1,2,3), we have −ln(θ)=0.4463<ln(B2)−ln(B1+K2K3)=1.3918 which means the system is finite time stable. Meanwhile, through calculation, when ρi=0.5 (i=1,2,3), the sufficient condition for finite-time stability also is not satisfied. The results of the numerical simulation are shown in Figures 7 and 8. Comparing with the ρi=0.3 (i=1,2,3) in Figure 4, we can observe that noise intensity does affect the finite-time stability.
(4) The role of diffusion
In this section we mainly analyze the impact of the diffusion on finite-time stability. In the ecological environment, different types of plants have different diffusion intensities. The vegetation structure of the area can be changed through human planting, etc. However, the diffusion strength of water is fixed and not easily changed. Therefore, we adjust the diffusion coefficient of vegetation to analyze the impact of diffusion. We choose duo=10 (m2/d) while keeping all other parameters unchanged.
Through calculation, it can be obtain that du=0.1, θ=0.64<1, K2=0.5, K3=−0.0991 and −ln(θ)=0.4463>ln(B2)−ln(B1+K2K3)=0.2599. This is obvious that the conditions of theorem 3.4 is not hold. The results of the numerical simulation are shown in Figure 9 which confirmed the analysis. Comparing with the results of duo=0.1 (m2/d) which are shown in Figure 4, we know that diffusion can affect the finite-time stability.''
5.2. Optimal control
In this section, we mainly show optimal control through numerical simulation. We choose t∈[0,300], x∈[−5,5], d=0.35, b=0.5, z=0.7, ai=0.2, σi=0.2, ρi=0.1, qi=0.2, ri=0.2, Pi=1, ˉPi=1, Qi=1 (i=1,2,4,5,6), Q3=5, Iku=Ikv=Ikw=0.2 where i=1,2,3. We set the impulse sequence tk={25,50,75,100,125,150,175,200,225,250,275} and choose noise (Figure 3 (b)). Other parameters can be found in Table 2. Because of technical limitations, we set the maximum value of the control variable π1∈(0,0.3), π2∈(0,0.4), π3∈(0,0.5), π4∈(0,2), π5∈(0,2), π6∈(0,2).
From (4.1), (4.3), (4.5), we can get the numerical solution of optimal control which are shown in Figures 9 and 10. Meanwhile, under optimal control, state trajectories of vegetation-water system is shown in Figure 11 (a). For comparison, we give state trajectories of vegetation-water system without control, which is shown in Figure 11(b). Obviously, the biomass density of vegetation has increased significantly under control. From the view of ecology, this is beneficial to the ecological environment.
6.
Conclusions
The desertification phenomenon caused by the destruction of the ecological environment by human beings is becoming more and more serious. Severe desertification may cause a food crisis and bring the disaster. Therefore, it is necessary for us to study the dynamics of vegetation-water system in arid areas and consider control strategies. In this paper, we propose a vegetation-water system with delay, impulse and noise. Through the proof, we show that the system has a unique global positive solution. Different from the analysis of the long-term dynamic behavior, we give the sufficient conditions for the finite-time stability of the system. It is worth noting that what we analyze is the finite-time stability of the system with time-varying delay. Some simulations are provided to support the theoretical results. Furthermore, we considered several control strategies and formulated an optimal control strategy to increase the density of vegetation. Through numerical algorithm, the numerical path for optimal control is given.
It is well-known that the initial values and parameters can affect the dynamic behavior of the system [54,55]. Obviously, this phenomenon can also be observed from the conditions of Theorem 3.4. For example, from C2, we can find that delay has a negative impact on the finite-time stability. As the delay increases, the system may lose finite-time stability, which is shown in Figure 6. The effect of diffusion coefficients du, dv, dw, noise intensities σi, Li (i=1,2,3) and impulse intensities Iu, Iv, Iw on the finite-time stability also can be obtained from Theorem 3.4 via similar discussion. Furthermore, through the analysis, we naturally raise a question. Whether changes in parameters can cause more complex dynamics of the system, such as the change of basins of attraction [54] and the generation of branching phenomena [55]. These will also be our further investigation.
Acknowledgments
The authors thank the editor and referees for their careful reading and valuable comments. The research was supported in part by the National Natural Science Foundation of China (No. 12161068) and Ningxia Natural Science Foundation (No. 2020AAC03065).
Conflict of interest
The authors declare there is no conflict of interest.
Appendix
The proof of Theorem 3.1 is as follows
Proof Considering the following stochastic partial differential equation without impulse:
with initial value (X(0),Y(0),Z(0))=(u(0),v(0),w(0)), where Aϑ (ϑ=u,v,w) can be defined by
Clearly, Aϑ (ϑ=u,v,w) is left-continuous, bounded and 1-periodic when t≥0. Next, we explain that system (2.6) and system (6.1) are equivalent. Let (u(x,t),v(x,t),w(x,t))=(Au(t)X(x,t),Av(t)Y(x,t),Aw(t)Z(x,t)). It can be easily checked that (X(x,t),Y(x,t),Z(x,t)) are continuous on (k,k+1)∈[0,∞), k∈N. For t≠tk, one can compute
For k, we have
This means that u(x,k+)=(1+Iku)u(x,k) for t=tk. Similarly, we can derive that
In this way, we have shown that the system (6.1) without impulse is equivalent to system (2.6). Therefore, in the following, we just need to analyze the solution of system (6.1).
Obviously, the coefficients of the system conforming to the local Lipschitz continuous, for any given initial data (X(x,s), Y(x,s), Z(x,s))∈C(Γ×[−ˉτ,0]; R3+), the system (6.1) has a unique maximal local solution (X(x,t),Y(x,t),Z(x,t))) on Γ×[−ˉτ,τe), where τe is explosion time. Make k0>0 be sufficiently large number for
Define the stopping time
for each k≥k0, k∈N. We set inf ∅=∞ (usually ∅ is the empty set). We can easily know that τk is increasing as k→∞. Besides, we set limk→∞τk=τ∞, whence τ∞<τe. Hence, if we can show that τ∞=∞, then τe=∞ and the solution of system (6.1) is positive.
Define a C2(R+;R) function
For 0≤t<τk∧T, Applying Itˆo formula to V(t) leads to
Through some simple calculations and Holder inequality, we can get
Assign
In view of the partial integral formula, some basic inequalities and hypothesis (H1), we deduce that
where
Therefore, we can know that
Integrating bosh sides of (6.5) from 0 to t1∧τk and taking expectations gives that
where C1=V(0)+E∫0−ˉτK1−η(∫ΓZ2(x,s)dx)ds+KT<∞, K1=max{K,K+K1−η}. Further, we can drive that
For ∀ t1∈[0,T], (6.6) holds, then, it follows from Gronwall inequalities [43] that
for any k≥k0. Particularly,
Define
Thus, (6.8) implies that
However, we can easily see that
Letting k→∞ in (6.9), one can deduce that P(τ∞≤T)=0, that is
For the arbitrariness of T, we must have τ∞=∞. Then, the system (6.1) has a unique global positive solution. Therefore, we complete the proof.
Algorithm
where