The General Theory of Money Quantity Determination by Professor Tim Congdon

 
The general theory of the determination
of ‘the quantity of money’
 
by Professor Tim Congdon CBE, Chairman of
the Institute of International Monetary Research
at the University of Buckingham
 
-
A presentation on the occasion of
Professor Victoria Chick’s 80
th
 birthday
 
Theories of interest rate determination
 
The rate of interest is a ‘real’ phenomenon, determined
by some combination of time-preference and the
(marginal) productivity of capital. (Ricardo, Bohm-
Bawerk, ‘the neoclassical school’)
The rate of interest is a ‘monetary’ phenomenon, with
‘the rate of interest’ determined when the demand for ‘a
monetary variable’ is equal to the supply of the same
monetary variable. (Keynes, Basil Moore, the post-
Keynesians)
Subject has a relationship with general-equilibrium
theorizing, if a very vexed relationship. The monetary
theories tend nevertheless to be expressed in
Marshallian terms, with supply-demand diagrams.
Keynes’ liquidity preference theory
Increase in M from 1 to 2 lowers bond yield, but from 2 to 3 does
not change ‘rate of interest’ in this sense
Keynes’ liquidity preference theory
 
-
Strengths
1.
The market-leader with a strong brand name.
2.
It does equilibrate the demand to hold money
with the quantity of money created by the
banking system, surely a vital condition of
macro- equilibrium.
3.
Valid if banks’ assets contain no claims on the
private sector, which is important if banks are
not lending to the private sector (for whatever
reason).
 
Keynes’ liquidity preference theory
 
-
Weaknesses
1.
A ‘general theory’? – Rate of interest is long bond yield, not money
market rate, quantity of money not distinguished from quantity of
monetary base, and only non-monetary asset is the ‘long’ bond.
2.
The ‘quantity of money’ (i.e., bank deposits) assumed to be
determined by officialdom, with money creation process
unaffected by rate of interest, and function inelastic and therefore
vertical to the quantity-of-money 
x 
axis. Realism of this
assumption is for debate.
3.
The construct in Marshallian and partial-equilibrium in character. It
takes position of money demand function to be fixed when the
quantity of money is changing, but this too is for debate. The
construct handles 
levels
 of the two variables, not 
rates of change
.
 
Basil Moore’s ‘horizontalism’
‘Money supply function’ infinitely elastic because of ‘overdrafts’, but M fixed
by intersection with ‘money demand [demand for credit] function’
In his 1988
book Moore
has diagrams
for both bank
money and the
base.
Basil Moore’s ‘horizontalism’
Money supply function’ infinitely elastic (‘overdrafts’), but M fixed by
intersection with ‘money demand [demand for credit] function’
‘Loans create deposits’ and ‘deposits make reserves’
-
Strengths
1.
Consistent with bankers’ view of their own
business and with widespread availability of
overdrafts for their corporate customers.
2.
Suggests that central banks operate not by
controlling quantity of base/reserve assets, but by
changing the money market rate, and this also has
merit of realism.
Basil Moore’s ‘horizontalism’
 
-
Weaknesses
1.
Equilibrium between M
d
 and M
s
 always achieved by
change in the money supply. Implicit flat denial that
macro outcomes can be affected by attempts to
remove excess/deficient money balances with bank
credit given.
2.
Moore in effect denies that that the notion of ‘the
demand to hold money’ has any significance. His
‘money demand function’ is not about the demand
to hold money, but is a ‘demand for bank credit’
function. Unsatisfactory if banks’ assets mostly
government securities.
Our wish list
 
Market in base money,
‘the money market’, 
with
only central bank and
commercial banks
-
Equilibrium should be on 
both
sides of the central bank
balance sheet
,
-
Demand for 
central bank
credit 
should be equal to
quantity of such credit
extended by the central banks,
and
-
Demand to hold 
base money
by commercial banks 
should
be equal to quantity of base
money created by the central
bank (and not held by non-
bank public).
 
Equilibrium in ‘money’,
in bank deposit sense,
with commercial banks and
non-bank private sector
agents (people, companies)
-
Equilibrium should be on
both sides of commercial
banks’ balance sheets
,
-
Demand for 
bank credit
should be equal to quantity
of credit extended by
commercial banks, and
-
Demand to hold 
bank
deposit money
 should be
equal to quantity of such
money created by the
banking system.
 
Equilibrium of central bank
credit and base money
 
Equilibrium of commercial
bank credit and the quantity of money
The ideas at work
Market in base money, ‘the
money market’
-
Identity between both sides of
the balance sheet delivered by
trick of 45 degree lines.
-
Horizontalism 
applies in
market for central bank
credit.
-
 Verticalism 
applies in inter-
bank market for base money,
= base money to hold
Note that central banks can
conduct a wide range of
operations, including auctions of
base money and last-resort loans.
Market in bank money (i.e.,
deposits), ‘quantity of money’
-
Identity between both sides of
the balance sheet delivered by
trick of 45 degree lines.
-
Horizontalism 
applies in  market
for commercial bank credit.
(Credit spread can be fixed by
bringing in bank capital.)
-
 Verticalism 
applies in quadrant
where demand to hold money is
equal to quantity of money
created by banks. 
(This
quadrant represents Keynes’
liquidity preference theory of
‘rate of interest’, which brings
us back to the textbooks.)
Horizontalism and ‘structuralism’
 
But is it entirely realistic to posit a horizontal supply curve
of bank credit? (The overdraft, and its benefits for
customers with volatile balance sheets.)
Most overdrafts specify a maximum, which – if exceeded
– cause a large step-jump in the interest margin or result
in the lending bank simply not honouring the instruction.
At an individual level, the horizontal line stops etc. At an
aggregate level, as the various overdraft maxima kick in,
the supply-of-credit curve slopes upwards to the right
beyond a certain point.
In a typical cycle, banks start to strain against capital
ceilings if loan demand is very strong, and they may
widen margins. But surely that is a shift in the supply-of-
credit curve between two or more moments in time.
Does the aggregate supply-of-credit function slope
upwards to the right? Yes, after a point, but only in
emergencies (heavy loan drawdowns in panics) , in practice
Existing four-panel/four-quadrant
treatments of the subject
 
Brunner and Meltzer 1966
A very different diagram, with
both 
base multiplier
determining deposits, 
and
earning assets determining
deposits, and the base split
between base held by banks
and non-banks. (I ignore non-
bank cash, as uninteresting.)
B & M have separate diagram
equating demand for bank
credit with supply of loans,
which introduces an interest
rate. Process of money creation
said to be ‘endogenous’.
 
Fontana 2003 (or 2004)
Again, a very different
diagram, with a. bank reserves
and deposits both having axes
and linked by base multiplier,
b. deposits also equal to bank
loans, with c. the ‘interest
rate’ equilibrating demand for
loans with loan supply,
represented by a line
horizontal to the 
x
-axis.
Equilibrium involves ‘reserve
market’, ‘credit market’ and
‘financial market’, but same
diagram used three times.
Four-panel/four-quadrant
treatments of the subject
 
What is the value of these approaches?
We can represent concisely equilibrium of
both 
the banking system (esp. determining the
quantity of money, 
broadly-defined, please
)
and 
the non-bank private sector, that both
borrows from banks and must hold the
deposits the banking system creates.
My approach enables horizontalists (‘money is
endogenous’) and verticalists (‘exogenous’)to
talk to each other! An attempt at generality
and indeed reconciliation.
Do we want a general theory of the
determination of the quantity of
money (and the rate of interest)?
 
‘Thus one concludes that money is
neither purely exogenous nor purely
endogenous. Which is the better
description depends on circumstances.’
 
- 
Victoria Chick 
Macroeconomics After Keynes
, p.
236 of the MIT Press Classic edition
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The rate of interest is influenced by time-preference, capital productivity, and monetary variables, as discussed by key economists like Keynes and Basil Moore. Keynes' Liquidity Preference Theory highlights the connection between money supply and demand. While the theory has strengths, it also faces criticisms for its assumptions and limitations, such as the inelastic money creation process and simplification of complex economic interactions. Basil Moore's horizontalism emphasizes the concept of infinitely elastic money supply.

  • Money Quantity Determination
  • Interest Rate Theories
  • Keynesian Economics
  • Liquidity Preference Theory
  • Monetary Policy

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  1. The general theory of the determination of the quantity of money by Professor Tim Congdon CBE, Chairman of the Institute of International Monetary Research at the University of Buckingham - A presentation on the occasion of Professor Victoria Chick s 80thbirthday

  2. Theories of interest rate determination The rate of interest is a real phenomenon, determined by some combination of time-preference and the (marginal) productivity of capital. (Ricardo, Bohm- Bawerk, the neoclassical school ) The rate of interest is a monetary phenomenon, with the rate of interest determined when the demand for a monetary variable is equal to the supply of the same monetary variable. (Keynes, Basil Moore, the post- Keynesians) Subject has a relationship with general-equilibrium theorizing, if a very vexed relationship. The monetary theories tend nevertheless to be expressed in Marshallian terms, with supply-demand diagrams.

  3. Keynes liquidity preference theory Increase in M from 1 to 2 lowers bond yield, but from 2 to 3 does not change rate of interest in this sense 'Rate of interest', in sense of the long bond yield Money supply function 1 2 3 Demand-to-hold -money function The quantity of money, in the sense of broadly-defined money (bank deposits)

  4. Keynes liquidity preference theory - Strengths 1. The market-leader with a strong brand name. 2. It does equilibrate the demand to hold money with the quantity of money created by the banking system, surely a vital condition of macro- equilibrium. 3. Valid if banks assets contain no claims on the private sector, which is important if banks are not lending to the private sector (for whatever reason).

  5. Keynes liquidity preference theory - Weaknesses 1. A general theory ? Rate of interest is long bond yield, not money market rate, quantity of money not distinguished from quantity of monetary base, and only non-monetary asset is the long bond. 2. The quantity of money (i.e., bank deposits) assumed to be determined by officialdom, with money creation process unaffected by rate of interest, and function inelastic and therefore vertical to the quantity-of-money x axis. Realism of this assumption is for debate. 3. The construct in Marshallian and partial-equilibrium in character. It takes position of money demand function to be fixed when the quantity of money is changing, but this too is for debate. The construct handles levels of the two variables, not rates of change.

  6. Basil Moores horizontalism Money supply function infinitely elastic because of overdrafts , but M fixed by intersection with money demand [demand for credit] function 'Rate of interest', in the sense of a rate relevant to bank credit 'Demand for money function', meanng 'demand for credit' Money supply function, taken to be an infinitely elastic supply of bank credit at any interest rate 1 2 In his 1988 book Moore has diagrams for both bank money and the base. The quantity of money, in the sense of broadly-defined money (bank deposits), which approximates quantity of bank loans

  7. Basil Moores horizontalism Money supply function infinitely elastic ( overdrafts ), but M fixed by intersection with money demand [demand for credit] function Loans create deposits and deposits make reserves - Strengths 1. Consistent with bankers view of their own business and with widespread availability of overdrafts for their corporate customers. 2. Suggests that central banks operate not by controlling quantity of base/reserve assets, but by changing the money market rate, and this also has merit of realism.

  8. Basil Moores horizontalism - Weaknesses 1. Equilibrium between Md and Ms always achieved by change in the money supply. Implicit flat denial that macro outcomes can be affected by attempts to remove excess/deficient money balances with bank credit given. 2. Moore in effect denies that that the notion of the demand to hold money has any significance. His money demand function is not about the demand to hold money, but is a demand for bank credit function. Unsatisfactory if banks assets mostly government securities.

  9. Our wish list Market in base money, the money market , with only central bank and commercial banks - Equilibrium should be on both sides of the central bank balance sheet, - Demand for central bank credit should be equal to quantity of such credit extended by the central banks, and - Demand to hold base money by commercial banks should be equal to quantity of base money created by the central bank (and not held by non- bank public). Equilibrium in money , in bank deposit sense, with commercial banks and non-bank private sector agents (people, companies) - Equilibrium should be on both sides of commercial banks balance sheets, - Demand for bank credit should be equal to quantity of credit extended by commercial banks, and - Demand to hold bank deposit money should be equal to quantity of such money created by the banking system.

  10. Equilibrium of central bank credit and base money Determination of quantity of central bank credit and the central bank rate ('discount rate', etc.) Central bank rate, r r Banks' demand-for-central-bank-credit function r 1 Horizontal supply schedule 3 2 1 R 1 45 degrees Central bank credit, quantity Inter-bank rate, R Monetary base, held by banks, qty. Banks' demand-to-hold- base function 3 4 5 Central bank capital, etc. , plus , in the real world, non-bank public's note holding Vertical supply schedule Determination of quantity of banks' cash reserves and the inter-bank rate

  11. Equilibrium of commercial bank credit and the quantity of money Determination of quantity of commercial bank credit and the bank lending rate Bank lending rate, r r Non-banks' demand-for-bank-credit function r 1 Horizontal 'overdraft' supply schedule 3 2 1 'The rate of interest', in Keynes' sense, R R 1 45 degrees Commercial bank credit, quantity Quantity of money, broadly-defined Demand-to-hold- money function 3 4 5 Banks' capital and other non- monetary liabilities Vertical supply schedule Determination of quantity of money and Keynes' 'rate of interest'

  12. The ideas at work Market in base money, the money market - Identity between both sides of the balance sheet delivered by trick of 45 degree lines. - Horizontalism applies in market for central bank credit. - Verticalism applies in inter- bank market for base money, = base money to hold Note that central banks can conduct a wide range of operations, including auctions of base money and last-resort loans. Market in bank money (i.e., deposits), quantity of money - Identity between both sides of the balance sheet delivered by trick of 45 degree lines. - Horizontalism applies in market for commercial bank credit. (Credit spread can be fixed by bringing in bank capital.) - Verticalism applies in quadrant where demand to hold money is equal to quantity of money created by banks. (This quadrant represents Keynes liquidity preference theory of rate of interest , which brings us back to the textbooks.)

  13. Horizontalism and structuralism But is it entirely realistic to posit a horizontal supply curve of bank credit? (The overdraft, and its benefits for customers with volatile balance sheets.) Most overdrafts specify a maximum, which if exceeded cause a large step-jump in the interest margin or result in the lending bank simply not honouring the instruction. At an individual level, the horizontal line stops etc. At an aggregate level, as the various overdraft maxima kick in, the supply-of-credit curve slopes upwards to the right beyond a certain point. In a typical cycle, banks start to strain against capital ceilings if loan demand is very strong, and they may widen margins. But surely that is a shift in the supply-of- credit curve between two or more moments in time.

  14. Does the aggregate supply-of-credit function slope upwards to the right? Yes, after a point, but only in emergencies (heavy loan drawdowns in panics) , in practice Rate of interest', in sense of cost of bank loans Supply-of-bank-credit function Demand-for-bank-credit function x Quantity of bank loans/Quantity of money

  15. Existing four-panel/four-quadrant treatments of the subject Brunner and Meltzer 1966 A very different diagram, with both base multiplier determining deposits, and earning assets determining deposits, and the base split between base held by banks and non-banks. (I ignore non- bank cash, as uninteresting.) B & M have separate diagram equating demand for bank credit with supply of loans, which introduces an interest rate. Process of money creation said to be endogenous . Fontana 2003 (or 2004) Again, a very different diagram, with a. bank reserves and deposits both having axes and linked by base multiplier, b. deposits also equal to bank loans, with c. the interest rate equilibrating demand for loans with loan supply, represented by a line horizontal to the x-axis. Equilibrium involves reserve market , credit market and financial market , but same diagram used three times.

  16. Four-panel/four-quadrant treatments of the subject What is the value of these approaches? We can represent concisely equilibrium of both the banking system (esp. determining the quantity of money, broadly-defined, please) and the non-bank private sector, that both borrows from banks and must hold the deposits the banking system creates. My approach enables horizontalists ( money is endogenous ) and verticalists ( exogenous )to talk to each other! An attempt at generality and indeed reconciliation.

  17. Do we want a general theory of the determination of the quantity of money (and the rate of interest)? Thus one concludes that money is neither purely exogenous nor purely endogenous. Which is the better description depends on circumstances. - Victoria Chick Macroeconomics After Keynes, p. 236 of the MIT Press Classic edition

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