For rI > 3rD it is immediate to see that ωm — 2ωsq < 0 if Dm < 4. For rI ≤ 3rD, ωm — 2ωsq
can be rearranged as
ωm — 2ωsq =
(1— ksq)2 Dsq
(1 _ k-, + 2 k3 ʌ D
2 lmn + 3 mn J Dm
(1 - ksq)2 Dsq
Suppose for a moment km = ksq and Dm = 2Dsq. Then, the expression simplifies to
k2Dsq (4ksq — 1), which is negative because ksq < 1/2. To see that this holds also for
km >ksq, we use (21) and rewrite ωm — 2ωsq as
ωm
rD
2ωsq = 'rI Dsq
rI μ 1
rD ∖2
λ Dm
D Dsq
Denote now A = (∣ — km + 3 km). Since A is decreasing in km and km > ksq for rI ≤ 3rD,
it follows ωm — 2ωsq < 0 when Dm = 2Dsq. The same holds for Dm < 2. By plotting the
expression ( DD A Dm — 1) for Dm > 2 and DD ∈ (1,3], one sees that there is a level h ∈ (2,4)
of the ratio Dm such that ωm ≤ 2ωsq if Dm ≤ h, and ωm > 2ωsq otherwise. The plot is
available from the authors upon request. Q.E.D.
Proof of Proposition 4
This proof is a generalization of that of Lemma 1. Let Dtot denote the total deposits
NDsq = Dm +(N — 2)Dc, and let Rtot denote the total reserves NRsq = Rm +(N — 2)Rc.
Applying the general formula for the distribution of a weighted sum of uniformly distributed
random variables in Bradley and Gupta (2002) to our model, we obtain the density functions
of the aggregate liquidity demands in the status quo fsq (Xsq) and after the merger fm (Xm)
as
N
fsq (Xsq ) = (N — 1)!(Dsq )N X=0 Γ1)∖ i
(Xsq—iDsq)+N-1
PN-2 hf 1 ii (N-^ X X D (i 1 'I D IN-2 I (N-^ X X iD N--2i
fm (Xm) =
i=1 (—1) i-1 (Xm — Dm — (i — 1)Dc)+ + i (Xm — iDc)+
(N — 2)!Dm(Dc)N-2
The two density functions are plotted in Figure 3. The density fsq (Xsq) is more concentrated
around the mean than fm(Xm). To verify that this is always the case, we compare the
variances of Xsq and Xm , which are given by
N
Var(Xsq)=X Ds2qV ar(δi),
i=1
35
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