Abstract
Rainwater harvesting, consisting in collecting runoff from precipitation, has been widely developed to stop groundwater declines and even raise water tables. However, this expected environmental effect is not self-evident. We show in a simple setting that the success of this conjunctive use depends on whether the runoff rate is above a threshold value. Moreover, the bigger the storage capacity, the higher the runoff rate must be to obtain an environmentally efficient system. We also extend the model to include other hydrological parameters and ecological damages, which respectively increase and decrease the environmental efficiency of rainwater harvesting.
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Notes
For more details, see Annex 1 of the study Agricultural Technologies for Developing Countries of the European parliament.
The detailed proofs are available upon request.
For instance, water diversion in the Lower Tarim River in China induces a decline in groundwater recharge [16].
With 3 multipliers, we usually expect 23 cases. But (i) the capacity and non-negativity constraints on RW cannot both be satisfied, (ii) by our boundary conditions at least one source of water is used, (iii) if only RW is used the capacity may or may not be reached, and (iv) there is a boundary regime for which the use of GW or RW is indifferent.
This is clearly a sufficient condition. Conjunctive use may occur for higher water tables, but this allows us to refine the analysis.
Observe that this sufficient condition is independent of the runoff. This parameter can used later without additional restrictions.
For more details, see Boers and Ben-Asher [3].
We can easily compute the partial derivatives: \(\frac {\partial h_{r}}{\partial R}=-\frac {(1-\rho )\left [ P^{\prime }\left ((1-\rho )R+\rho W\right ) +\frac {C^{\prime }\left (h\right ) }{\delta }\right ] }{-C^{\prime }\left (h\right ) +\frac {(1-\rho )}{\delta }C^{\prime \prime } \left (h\right ) (R-W)}>0\) and \(\frac {\partial h_{g}}{\partial R}=-\frac {(1-\rho )\left [ P^{\prime }\left ((1-\rho ) R\right ) +\frac {C^{\prime }\left (h\right ) }{\delta }\right ] }{-C^{\prime }\left (h\right ) +\frac {(1-\rho )}{\delta } C^{\prime \prime }\left (h\right ) R}>0\).
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Acknowledgments
The authors would like to thank the advisory editor of Environmental Modeling & Assessment for helpful comments on an early version of this paper. The usual disclaimer of course applies. Support from the Labex AMSE (ANR-11-IDEX-0001-02) is gratefully acknowledged.
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Appendices
Appendix
1.1 Appendix A: The Solution to the General Problem
Let us introduce some notations used below:
1.1.1 A.1 The Problem
Let us consider the following optimal control problem:
The current value of the Hamiltonian for this problem is:
where λ(t)≥0 denotes the shadow value of the groundwater resource. Moreover, if we introduce the Lagrange multipliers μ g (t) and \(\mu _{r}^{\prime }(t)\) associated with the non-negativity constraints on w g (t) and w r (t), respectively, and the implicit price \(\mu _{W}^{\prime }(t)\) of W, the capacity constraint, the Lagrange function associated with this program is:
The Hamiltonian conditions are given by systems (CTR1) and (DYN1):
and
1.1.2 A.2 The Construction of the Steady State
Let us consider a steady state satisfying (CTR1) and (DYN1) with \(\dot {h}(t)=\dot {\lambda }(t)=0\). There are eight possible cases, since each of the three Lagrange multipliers may or may not be strictly positive. We nevertheless immediately observe that:
Remark 1
At a steady state: (i) both constrains on w g cannot be simultaneously binding since W > 0, (ii) there must be some GW consumption (i.e., μ g = 0) otherwise \(\dot {h}(t)=0\) implies that \(w_{r}=\frac {R_{\rho }}{b}=\frac {\left (1-\rho \right ) }{\left (1-\rho \right ) -\beta (1-\varepsilon )}R>R\), which is impossible since w r ≤ W < R.
Now let us observe:
Lemma 1
If the capacity constraint on RW harvesting is not binding (i.e., μ W =0) at the steady state, then K ε >C(h).
Proof Lemma 1
Since \(\mu _{g}=\mu _{W}=\dot {h}=0,\) the difference between Eqs. (G W 1) and (R W 1) is:
Using (i) μ r ≥ 0 and (ii) \(\lambda =-\frac {1}{\delta }C^{\prime }\left (h\right ) w_{g}\) since \(\dot {\lambda }=0\), it follows that:
(iii) Notice that \(\frac {b}{1-\varepsilon }-a=-\frac {\rho -\varepsilon }{1-\varepsilon }<0\) since ρ > ε, and (iv) by assumption \(C^{\prime }<0,G^{\prime }>0.\) The lhs of Eq. A.4 is therefore positive and we can conclude that K ε >C(h). □
From Lemma 1, we assert :
Lemma 2
If we assume that
the RW storage capacity is always binding at a steady state.
Proof
Assume the contrary, w r < W, so that μ W = 0. Since \(\lambda =-\frac {1}{\delta }C^{\prime }\left (h\right ) w_{g}\), (R W 1) at the steady state can be written as:
Using Lemma 1, i.e., \(K_{\varepsilon }>C(h)\Leftrightarrow C^{-1}\left (K_{\varepsilon }\right ) <h\), and since \(C^{\prime \prime }\geq 0\), we deduce that:
Moreover, from system (DYN1) at steady state, we know that:
-
(i)
\(R_{\rho }-aw_{g}-bw_{r}=0\Leftrightarrow aw_{g}=R_{\rho } -bw_{r}<R_{\rho }-bW\) since we have assumed that w r < W. Moreover, b = 1−ρ−β(1−ε) and 1>ρ > ε, we can therefore say:
$$\begin{array}{@{}rcl@{}} aw_{g}&<&\left( 1-\rho\right) \left( R-W\right) +\beta(1-\varepsilon )W<R\\ &&-(1-\beta)W=R-aW. \end{array} $$(A.8) -
(ii)
The total consumption of water is \(w=\frac {R_{\rho }-bw_{r}} {a}+(1-\varepsilon )w_{r}=\frac {1}{a}\left (R_{\rho }-\left (b-a(1-\varepsilon )\right ) w_{r}\right ) \). Since b−a(1 − ε) = ε−ρ, we have \(w=\frac {1}{a}\left [ R_{\rho }+\left (\rho -\varepsilon \right ) w_{r}\right ] \). If we now remember that w r < W < R and ε < ρ < 1, we observe that:
$$ w<\frac{1}{a}\left( (1-\rho)+\left( \rho-\varepsilon\right) \right) R<\frac{R}{1-\beta}. $$(A.9)
Under assumptions \(P^{\prime }<0\) and \(C^{\prime }<0\) and items (i) and (ii), we can write condition (A.7) as:
Finally, since \(0<\frac {b}{\left (1-\varepsilon \right ) a}<1\) (see (iii) of the Proof of Lemma 1) \(C^{\prime }<0\) and \(G^{\prime }\left (0\right ) >0\), we can state that:
Given the assumption introduced in Eq. A.5, this implies that μ r < 0 which is a contradiction. □
If we now combine Remark 1 and Lemmas 1 and 2, we can say that a steady state, if it exists, verifies:
In other words, a unique steady state exists, if there exists a unique solution \(h^{\ast }\in \left [ 0,\bar {h}\right ] \) to
which verifies:
So, let us first observe:
Lemma 3
If condition (A.5) is satisfied, any solution (it is exists) to ϕ 1 (h ∗ )=0 verifies μ W >0.
Proof
Using Eq. A.12 and W < R, we get \(w<\frac {1}{a}\left (R_{\rho }+\rho W\right ) <\frac {R}{a}\) and by Eq. A.8 we know that R ρ −b W < R−a W. If we now keep in mind that \(P^{\prime }<0\) and \(C^{^{\prime }}<0\), we can deduce from condition (A.5) that:
But ϕ 1(h) is increasing in h since \(C^{\prime }<0\) and C ” ≥ 0. We deduce that the steady state \(h^{\ast }<C^{-1}\left (K_{\varepsilon }\right ) \) or C(h ∗)>K ε . We can therefore say from Eq. (A.13) that:
Since \(\frac {b}{a\left (1-\varepsilon \right ) }\in \left (0,1\right ) \), \(C^{\prime }<0\) and \(G^{\prime }\left (0\right ) >0\), we can even state:
or, in other words, that μ W >0. □
We can finally affirm that:
Proposition 10
Under condition (A.5), the path solution to optimization problem (A.1) admits a unique steady state given by Eq. A.12.
Proof
It simply remains to show that ϕ 1(h) = 0 admits a unique solution \(h^{\ast }\in \left [ 0,\bar {h}\right ] \). This is immediate since (i) \(\phi _{1}^{\prime }>0\) because \(C^{\prime }<0\) and C” ≥ 0, (ii) \(\lim _{h\rightarrow 0}\phi _{1}(h)=-\infty \) because \(\lim _{h\rightarrow 0}C(h)=\infty \) and (iii) \(\lim _{h\rightarrow \bar {h}}\phi _{1}(h)>0\). However, this last point is less obvious. So let us first observe that \(\lim _{h\rightarrow \bar {h}}\phi _{1}(h)=P\left (\frac {1} {a}\left (R_{\rho }+(\rho -\varepsilon )W\right ) \right ) -aG^{\prime }\left (0\right )\) since we have assumed that \(C(\bar {h})=C^{\prime }(\bar {h})=0\). Now remark that \(\frac {1}{a}\left (R_{\rho }+(\rho -\varepsilon )W\right ) <\frac {R}{1-\beta }\) since W < R and use condition (A.5) in order to obtain:
(remember \(C^{\prime }<0\) and R−a W > 0). □
1.1.3 A.3 The Local Saddle Point Property
Let us return to the systems (CTR1) and (DYN1) and set μ g = 0, and μ r = 0. Since μ W >0 at the steady state, we can choose a neighborhood around the steady state such that μ W (t)>0 and therefore set w r (t) = W. In this case, equation (G W 1) becomes:
Moreover, \(\partial _{w_{g}}\phi _{2}=P^{\prime }-\left (\frac {a}{sA}\right )^{2}G"<0\) by our assumptions. We can therefore apply the implicit function theorem around the steady state and build \(w_{g}(t)=\phi _{3}\left (h(t),\lambda (t)\right ) >0\). We even know that:
It follows that the dynamics of the system is locally given by:
It remains to verify that the Jacobian J of this two dimensional system has a positive trace T r(J) and a negative determinant \(\det (J)\). By computation, we obtain:
We can therefore say, under our assumptions, that :
Appendix B: The Study of the Threshold
Let us introduce the system:
with \({\Gamma }=G^{\prime }\left (0\right ) \). The first equation gives us the stationary water table without RWH while the second includes this option. So if we solves this system in h and ρ, we obtain the threshold value, \(\bar {\rho }\) for which the stationary water table h is the same without or with rainwater harvesting. Moreover, this threshold can then be linked to the different parameters \(\left (W,R,\varepsilon ,\beta ,{\Gamma }\right ) \).
1.1 B.1 Existence of a Threshold
Let us observe that for any admissible \(\left (W,R,\varepsilon ,\beta ,{\Gamma },s,A\right ) \), ∀{i = 4,5}, (i) ∂ h ϕ i >0 since \(C^{\prime }<0\) and C”≥ 0, (ii) \(\lim _{h\rightarrow 0}\phi _{i} =-\infty \) since \(\lim _{h\rightarrow 0}C(h)=-\infty \) and (iii) \(\lim _{h\rightarrow \bar {h}}\phi _{i}>0\) (apply the same argument as in the proof of Proposition 10). We can therefore, by the implicit function theorem, define two continuous functions \(h_{g}\left (\rho \right ) \) and \(h_{r}\left (\rho \right ) \) which respectively solve in h, ϕ 4(ρ, h;R, β,Γ)=0 and ϕ 5(ρ, h;W, R, ε, β,Γ)=0. It remains now to study \(\left (h_{g}\left (\rho \right ) -h_{r}\left (\rho \right ) \right ) \) since the threshold solves \(h_{g}\left (\bar {\rho }\right ) -h_{r}\left (\bar {\rho }\right ) =0\).
Since \(\rho \in \left [ \varepsilon ,1-\beta \left (1-\varepsilon \right ) \right ] \), let us first observe that \(\left (h_{g}\left (\rho \right ) -h_{r}\left (\rho \right ) \right )_{\rho =\varepsilon }>0\). To verify this point, let us observe that, for ρ = ε, h g and h r respectively solve:
This implies:
It is straightforward that the right-hand side of Eq. (B.4) is positive, so that:
Finally, since \(C^{\prime }<0\) and C ” ≥ 0, we deduce that \(h_{g}\left (\varepsilon \right ) >h_{r}\left (\varepsilon \right ) \).
Second, observe that \(\left (h_{g}\left (\rho \right ) -h_{r}\left (\rho \right ) \right )_{\rho =1-\beta \left (1-\varepsilon \right ) }<0.\) In this case, the quantities h g and h r solve:
Since \(P\left (\frac {\beta \left (1-\varepsilon \right ) }{1-\beta }R\right ) >P\left (\frac {\beta \left (1-\varepsilon \right ) }{1-\beta }R+\left (1-\varepsilon \right ) W\right ) \) (remember that \(P^{\prime }<0\)), we can write:
Since \(C\left (h\right ) -\frac {\beta \left (1-\varepsilon \right ) }{\delta sA}C^{\prime }\left (h\right ) R\) is decreasing in h, we conclude that \(h_{g}\left (1-\beta \left (1-\varepsilon \right ) \right ) <h_{r}\left (1-\beta \left (1-\varepsilon \right ) \right ) \).
Finally by continuity, we can affirm that there exists at least one \(\bar {\rho }\in \left [ \varepsilon ,1-\beta \left (1-\varepsilon \right ) \right ] \) such that \(h_{g}\left (\bar {\rho }\right ) -h_{r}\left (\bar {\rho }\right ) =0\).
1.2 B.2 Uniqueness of the Threshold
Since this threshold and the associated water table are also obtained as a solution to system (B.1) for a given set \(\left (W,R,\varepsilon ,\beta ,{\Gamma }\right ) \) of parameters, we can use the Gale-Nikaido theorem (see Gale-Nikaido [11] or Mas-Colell [22]) which states that if every principal minor of \(\partial _{\rho ,h}\left (\phi _{i=4,5}\right ) \) is positive and the domain \(K=\left [ 0,\bar {h}\right ] \times \left [ 0,1\right ] \) of the function is a rectangle, the solution, if it exists, is unique. Let us verify this point.
Concerning the principal minors of order 1, we notice that:
-
(i)
\(-R\left (\frac {1}{a}P_{g}^{\prime }+\frac {1}{\delta sA} C^{\prime }\right ) >0\) since \(C^{\prime }<0\) and \(P^{\prime }<0\);
-
(ii)
\(-C^{\prime }+\frac {R_{\rho }-bW}{\delta sA}C">0\) since \(C^{\prime }<0\), C ” ≥ 0 and R ρ −b W = (1−ρ)(R−W) + β(1−ε)W > 0;
It therefore remains to compute the determinant of \(\partial _{\rho ,h}\left (\phi _{i=4,5}\right ) \). This quantity is given by:
since \(C^{\prime },P_{g}^{\prime },P_{r}^{\prime }<0,C"\geq 0\) and because P ” > 0, \(P^{\prime }\left (\frac {1}{a}R_{\rho }\right ) <P^{\prime }\left (\frac {1}{a}\left (R_{\rho }+(\rho -\varepsilon )W\right ) \right ) \), i.e. \(P_{g}^{\prime }-P_{r}^{\prime }<0\).
1.3 B.3 Comparative Statics
Let us denote by θ one of the following parameters {W, R, β, ε,Γ, s, A} and let us compute \(\frac {\partial \rho } {\partial \theta }\). It we differentiate system (B.1) with respect to \(\left (h,\rho ,\theta \right ) \) and solve the system, we know by the Cramer rule that:
From Eq. B.8, we know that the denominator D is positive. It follows that the sign of \(\frac {\partial \rho }{\partial \theta }\) is simply given by its numerator N. Moreover, a simple exercise of computation shows that :
and
we can therefore identify, after computation, the effects on the threshold of the following parameters:
-
(i) The storage capacity, \(\frac {\partial \rho }{\partial W}\).
$$\begin{array}{@{}rcl@{}} &&{}sign~\left( \frac{\partial\rho}{\partial W}\right) =sign~\left( \left( \frac{\rho-\varepsilon}{a}P_{r}^{\prime}-\frac{b}{\delta}C^{\prime}\right) \underset{>0\text{ since }C^{\prime}<0\text{, }C">0}{\underbrace{\left( -C^{\prime}+\frac{R_{\rho}}{\delta sA}C"\right) }}\right)\\&& {}=sign~\left( \frac{\rho-\varepsilon}{a}P_{r}^{\prime}-\frac{b}{\delta sA}C^{\prime }\right). \end{array} $$(B.12)Let us now observe that the computation of the difference of the two equations (see Eq. (B.1)) which define the threshold gives:
$$ P\left( \frac{1}{a}R_{\rho}\right) -P\left( \frac{1}{a}\left( R_{\rho }+(\rho-\varepsilon)W\right) \right) +\frac{bW}{\delta sA}C^{\prime}=0 $$(B.13)and the convexity of the inverse demand gives:
$$ P\left( \frac{1}{a}R_{\rho}\right) -P\left( \frac{1}{a}\left( R_{\rho }+(\rho-\varepsilon)W\right) \right) >-\frac{\left( \rho-\varepsilon \right) W}{a}P_{r}^{\prime}. $$(B.14)These two last equations immediately show that \(\left (\frac {\left (\rho -\varepsilon \right ) }{a}P_{r}^{\prime }-\frac {b}{\delta sA}C^{\prime }\right ) >0\) hence that \(\frac {\partial \rho }{\partial W}>0.\)
-
(ii) The evaporation rate, \( \frac {\partial \rho }{\partial \varepsilon }\).
$$ sign\left( \frac{\partial\rho}{\partial\varepsilon}\right) =sign\left( -W\left( \frac{1}{a}P_{r}^{\prime}+\frac{\beta}{\delta}C^{\prime}\right) \left( -C^{\prime}+\frac{R_{\rho}}{\delta}C"\right) \right) >0 $$(B.15)since \(P_{r}^{\prime }<0\), \(C^{\prime }<0\) and C ” > 0.
-
(iii) The marginal ecosystem damage, \(\frac {\partial \rho }{\partial {\Gamma }}\).
$$ sign\left( \frac{\partial\rho}{\partial{\Gamma}}\right) =sign\left( -\frac{abW}{\delta\left( sA\right)^{2}}C"\right) \leq0. $$(B.16) -
(iv) The recharge, \(\frac {\partial \rho }{\partial R}\). Since \(\partial _{h}\phi _{5}=\partial _{h}\phi _{4}+\frac {bW}{\delta sA}C^{\prime \prime }(h)\) and \(\left (\frac {1-\rho }{a}\right ) >0\), a routine computation gives:
$$ sign\left( \frac{\partial\rho}{\partial R}\right) =sign\left( \underset{>0}{\underbrace{\partial_{h}\phi_{4}}}\underset{\geq0\text{ (since }P"\geq0\text{)}}{\underbrace{\left( -P_{g}^{\prime}+P_{r}^{\prime}\right) }}+\underset{\geq0}{\underbrace{\frac{bW}{\delta sA}C^{\prime\prime}} }\underset{<0}{\underbrace{\left( P_{g}^{\prime}+\frac{a}{\delta sA}C^{\prime}\right) }}\right). $$(B.17)This quantity is clearly ambiguous. For instance if the demand is linear, we have \(P_{r}^{\prime }-P_{g}^{\prime }=0\) and \(\frac {\partial \rho }{\partial R} <0\). But if the unit pumping cost is linear in h so that C ” = 0, we observe \(\frac {\partial \rho }{\partial R}>0\). Finally in the Gisser-Sánchez case (i.e., C ” = 0 and P linear), it is immediate that \(\frac {\partial \rho }{\partial R}=0.\)
-
(v) The return flow, \(\frac {\partial \rho }{\partial \beta }\).
$$\begin{array}{@{}rcl@{}} &&sign\left( \frac{\partial\rho}{\partial\beta}\right) =sign\left( \partial_{h}\phi_{4}\left[ \frac{R_{\rho}}{a^{2}}\left( -P_{g}^{\prime }+P_{r}^{\prime}\right)\right.\right.\\ &&\left.+\frac{(\rho-\varepsilon)W}{a^{2}}P_{r}^{\prime }+\frac{(1-\varepsilon)W}{\delta sA}C^{\prime}\right]\\&&\left. +\frac{bW}{\delta sA}\left( \frac{R_{\rho}}{a^{2}}P_{g}^{\prime}+{\Gamma}\right) C^{\prime \prime}\right). \end{array} $$(B.18)This quantity is again ambiguous. To illustrate this point let us assume that C ” = 0 so that \(C^{\prime }=-c_{0}\) a constant with c 0>0. If we add that P(w) is linear (the Gisser-Sánchez case) then \(sign\left (\frac {\partial \rho }{\partial \beta }\right ) =sign\left (\frac {(\rho -\varepsilon )W}{a^{2}}P_{r}^{\prime }-\frac {(1-\varepsilon )W}{\delta sA}c_{0}\right ) <0\). If we now introduce an iso-elastic demand P(w) = w −α with a > 1, then
$$\begin{array}{@{}rcl@{}} &&sign\left( \frac{\partial\rho}{\partial\beta}\right) =sign\left( \alpha\underset{\equiv d>0}{\underbrace{\left( \left( \frac{R_{\rho}} {a}\right)^{-\alpha}-\left( \frac{R_{\rho}+(\rho-\varepsilon)W}{a}\right)^{-\alpha}\right) }}\right.\\&&{\kern90pt}\left.-\underset{\equiv n>0}{\underbrace{a\frac{(1-\varepsilon )W}{\delta sA}c_{0}}}\vphantom{\underset{\equiv d>0}{\underbrace{\left( \left( \frac{R_{\rho}} {a}\right)^{-\alpha}-\left( \frac{R_{\rho}+(\rho-\varepsilon)W}{a}\right)^{-\alpha}\right) }}}\right) \end{array} $$(B.19)so if \(\alpha >\max \left \{ \frac {n}{d},1\right \} \) then \(\frac {\partial \rho }{\partial \beta }>0\).
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(vi) The storativity coefficient, \(\frac {\partial \rho }{\partial s}\). A routine computation gives:
$$ sign\left( \frac{\partial\rho}{\partial s}\right) =sign\left( \frac{\Gamma}{s}C"-(C^{\prime})^{2}\right). $$(B.20)If the marginal damage of the aquifer is not considered, i.e. Γ=0, or if marginal pumping cost is linear in h, we have\(\frac {\partial \rho }{\partial s}<0\). Otherwise, this quantity may be unsigned especially if the marginal environmental damage Γ is high.
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(vii) The area of the aquifer, \(\frac {\partial \rho }{\partial A}\). Since A and s work in the same way on the threshold, we can say that \(sign\left (\frac {\partial \rho }{\partial A}\right ) =sign\left (\frac {\Gamma }{A}C"-(C^{\prime })^{2}\right ) \) and we can apply the same comments as in (vi).
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Stahn, H., Tomini, A. On the Environmental Efficiency of Water Storage: the Case of a Conjunctive use of Ground and Rainwater. Environ Model Assess 21, 691–706 (2016). https://doi.org/10.1007/s10666-016-9509-3
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DOI: https://doi.org/10.1007/s10666-016-9509-3