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Q2 Z2,(Q2) Z2(Q2) - Institute for Water Resources - U.S. Army

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(4.26)<br />

(4.27)<br />

(4.28)<br />

(4.29)<br />

(4.30)<br />

(4.31)<br />

(4.32)<br />

-b 2 Q 2<br />

T l • g l + h l M<br />

4 ■ g 2 + h 2 M<br />

T 3<br />

g 3 + h 3 M<br />

In this <strong>for</strong>mulation we see that equations (4.26), (4.27) and (4.28)<br />

are each a self-contained sub-set of order zero and may be estimated<br />

separately and independently. 1<br />

Equations (4.22) through (4.25) then constitute a derived struc-<br />

ture of the first order. Using (4.26), (4.27) and (4.28) to eliminate<br />

the rate variables, they become<br />

. Q1 <strong>Q2</strong> + . (13 " c m a+ YA<br />

-b 1 Q 1<br />

+ T c • (al + gl )<br />

+ T c ■ (82 + g 2 )<br />

-b 3 Q 3 + T c ■ (a 3 + g 3 )<br />

+ (c1 + h 1 ) M<br />

• + (c 2 + h 2 ) M<br />

+ (c3 + h3) M<br />

The following sections deal with our empirical investigations of<br />

these two sets of estimating equations.<br />

Empirical Results -- The Rate Equations<br />

Having derived the estimating equations, we now turn to our em-<br />

pirical work. In this section we shall deal with equations (4.26),<br />

(4.27) and (4.28), the transport rate equations. The following section<br />

contains our discussion of the demand equations. As stated previously,<br />

1. The terminology and procedure is taken from H. A. Simon, "Causal<br />

Ordering and Identifiability," Chapter III of W. C. Hood and T. C.<br />

Koopmans, Studies in Econometric Method, Cowles Commission Monograph<br />

No. 14, Wiley, New York, 1952.<br />

82

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