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Descriptive Test of the Hotelling Model with Data from the Rare Earths Market Esther Divovich Advisor Richard Walker Northwestern University This Version: June 6, 2011

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Descriptive Test of the Hotelling Model with Data from the

Rare Earths Market

Esther Divovich

Advisor Richard Walker

Northwestern University

This Version: June 6, 2011

Divovich 2

Acknowledgements

First and foremost, I would like to thank my thesis advisor, Professor Richard Walker, for his

accessibility, patience, and perceptive input through the various twist and turns of performing

independent research. His continued guidance not only made this thesis a possibility, but taught

me a great deal along the way. Likewise, Kathleen Murphy, the Social Science Data Services

librarian, was an invaluable resource for obtaining the necessary data sets for my analysis.

Lastly, I would like to thank all of the teachers who have given me the tools and the passion for

learning. Within this thesis, are the imprints every single teacher I’ve ever had the privilege of

learning from, ranging from my first-grade math teacher, to my highschool English teacher, and

most importantly, to all of my MMSS and Economics professors at Northwestern.

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Section 1: Introduction

The dilemma of the optimal extraction of nonrenewable resources has faced leaders,

organizations, and policy-makers consistently in the 20th

century: how much of a nonrenewable

resource to extract now, and how much to save for the future?

Harold Hotelling answered this question in 1931 with his model of the optimal extraction

of nonrenewable resources. He claimed that exhaustible resources were extracted and valued

differently than renewable resources. While real prices of sustainable commodities, such as corn

or wheat, should stay constant year to year, the real prices of nonrenewable resources rise at the

rate of interest. Since then, Hotelling’s “r-percent” rule has been expanded upon to become its

own subfield in economics.

The next immediate question to ask is: how well does Hotelling’s model hold when tested

against the data? The Hotelling model was tested extensively during the 1970’s as a result of the

oil price shocks from the OPEC embargo. After the 1970’s, however, when commodity prices

stabilized, mainstream economics has moved away from the theoretical study of Hotelling’s

model. The recent increase in real commodity prices by 286% from 1998 – 2008 alludes to the

re-emergence of this branch of economic literature.

This paper undertakes an empirical test of the Hotelling model for the rare earths market

from 1955-2009. The rare earth market is of particular interest because of the rapid growth in

technology, which has caused a surge in demand for the rare earths. In addition, while the

Hotelling model has been tested with data from nearly every major nonrenewable resource, it has

never been tested on rare earths market data.

The next section, Section 2, will deal with the theory. Section 2.1 will introduce dynamic

programming, the key theoretical fundament of Hotelling’s model. Section 2.2 will derive

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Hotelling’s basic findings using dynamic programming, and Section 2.3 will outline the

theoretical extensions to the basic model that have been developed since 1931.

Section 3 will present an empirical test of Hotelling’s model with market data on the rare

earths from 1955-2009. A review of the empirical body of literature in Section 3.1 will

differentiate between various formal and descriptive tests of the Hotelling model. Section 3.2

will outline the data. Section 3.3 will describe the methodology of the test we perform, which is a

descriptive rather than a formal test due to the unavailability of firm cost data. Section 3.4 will

present the results, which show mixed support for the Hotelling model in the rare earths data,

although the Hotelling model cannot be formally accepted or rejected due to the descriptive

nature of the test.

Section 2: Theory

2.1 Dynamic Programming

The key question that the Hotelling model seeks to answer is how a producer of a

nonrenewable resource maximizes his intertemporal profit stream over continuous time. Basic

Lagrangian optimization can no longer handle such a multi-faceted problem.1 We will abstract

from the specific application of the Hotelling model for the time being, and introduce the integral

tool of dynamic programming.2

The basic problem of dynamic programming is to maximize

(1)

subject to

(2)

1 A.K. Dixit

2 Obstfeld

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The objective function, (1), is the discounted utility function from time 0 to . The

continuously compounded discount rate is denoted, r. The constraint, , is a function of both

the flow (control) variable, q(t), and the state variable, S(t). It is a key point to distinguish

between the flow variable and the state variable. The state variable is a fixed known entity at a

certain point in time. The flow variable, however, is best known as a rate where units denote the

change in a state variable “per time.” For example, output is a state variable, whereas GDP is a

flow variable (since it is computed annually).

In equation (2), S(0) is the initial quantity of the state variable at time zero. The key to

solving this problem, as we will see later, is that the maximized value of (1) depends solely on

S(0), the predetermined initial value of the state variable. The dot over S(t) denotes a time

derivative, such that

.

The flow variable is also known as the control variable because it is the variable under

the control of the entity maximizing the objective function, (1). This is why we will eventually

differentiate (1) with respect to q(t) in order to obtain the optimal path. The optimal path, ,

is the solution the problem. In real-life applications, it can represent a household’s decision of

how much to consume, or in the case of Hotelling’s model, how much a firm will choose to

extract of an exhaustible resource.

The first step to solving this problem involves assuming that there exists a maximized

value function, , which is the lifetime utility a producer gains from following the optimal

extraction path. The value function is the answer to the question: if the producer picks the

optimal extraction path, , what is the maximum level of utility he will gain? Thus, with the

defined terms and

, the maximized value function can be written as,

(3)

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where the maximized value of (1) depends solely on S(0). Hence, this problem is stationary – it

does not change with the passage of time. This implies that at any time onward to T, a new

decision maker would make the same optimal choice path because S(0) would be the same for

both decision makers. Another common term for stationarity is “dynamic consistency” because

dynamically (over time) the solution is consistent. As a result, (3) can be rewritten as

+ for all T (4)

Since the value function is the solution to our optimization problem, we know that

(5)

By the assumption of dynamic consistency, the maximized value function holds for all

so we can take

, which results in,

(6)

where the constraint is ]. This is equivalent to

0 = (7)

Let us define the first two terms of the maximized function as the Hamiltonian equation,

H = (8)

Maximizing the Hamiltonian with respect to the control variable (extraction) will give us the

static efficiency condition for solving the producer’s intertemporal problem,

: (9)

The static efficiency condition says that at each (static) point in time, the marginal benefit

is directly offset by the marginal cost, , which is the potential value at a

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future point in time. This marginal cost is the user cost (shadow cost) of the

constraint .

Since q(S) and it is the solution to the Hamiltonian, then it automatically satisfies the

original equation (7). If we substitute back into (7), we can further optimize to solve for the

dynamic efficiency condition,

0 = (10)

By envelope theorem, we know that

(11)

where

(12)

Substituting (12) into (11) gives us the optimized function

(13)

Let us denote the user cost,

Also, by definition, the term =

Thus, (13) can be rewritten as

(14)

which gives us the dynamic efficiency condition,

(15)

or

(16)

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The tool of dynamic programming has given us two necessary conditions, static and

dynamic, in order to solve continuous time maximization. In the next section, we will apply this

critical tool to the problem of solving a producer’s optimal extraction path of a non-renewable

resource.

2.2 Hotelling’s Model

Hotelling developed the basic model for the optimal extraction rate of a nonrenewable

resource by a firm extracting from a known resource stock. The basic model assumes a perfectly

competitive market, although the general structure can accommodate the case of a monopoly as

well.

A producer attempts to maximize his discounted profit stream, which is modeled by the

objective function, J,

(17)

where r is the discount rate the firm faces and his profit is defined by the benefit gained from

selling the resource minus the cost. The functions depend on the control and state variables, q(t)

and S(t). The control variable, q(t), is the rate of extraction the producer chooses at each point in

time. The state variable, S(t), is the amount of the stock remaining at time t.

However, the producer is also subject to the following constraints,

(18)

(19)

(20)

(21)

With the tool of dynamic programming, we are able to define the Hamiltonian equation,

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H = (22)

where is the shadow price on the resource constraint.

Maximizing the Hamiltonian with respect to the control variable (extraction) will give us

the static efficiency condition for solving the producer’s intertemporal problem,

: (23)

In the Hotelling model, the static efficiency condition says that at each (static) point in

time, the producer’s marginal utility, , from extracting and selling the nonrenewable

resource is directly offset by the producer’s potential utility from extracting at a future point in

time. Also from dynamic programming we know that the dynamic efficiency condition is

(24)

or

(25)

Equation (26) is the famous “r-percent rule”, that the marginal value of the nonrenewable

resource will increase at the rate of interest.

2.3 Literature Review of the Theory: Extensions to Hotelling’s Model

In the dynamic world of extracting nonrenewable resources, the basic assumptions on the

cost function may not be sufficient to account for real life complications. Such complications

include exploration, uncertainty about the size of reserves, durability effects (recycling and

stockpiling), imperfect competition, taxation effects, stock effect, and technical changes.3 For the

sake of this review, however, we will focus on three major extensions to the Hotelling model:

depletion (stock effect), exploration, and technical advances.

3 Slade and Thille

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In order to model the role of depletion, the intuitive logic is that extraction costs depend

not only on the current extraction, q(t), but also on the remaining stock of reserves, S(t). This is

due to the fact that the cheapest, most readily available resources are extracted first, followed

sequentially by less economic reserves deeper in the ground that are more difficult to extract. For

minerals, this is known as declining ore quality. While the static efficiency condition remains

unchanged, the dynamic efficiency condition becomes,

(26)

Another real-life complication of the Hotelling model that alters the cost function is

exploration. Exploration is an added cost, but the benefits of discoveries lower cost because they

increase the stock of cumulative discoveries, D. The rate of change of discoveries is

where e is the exploratory effort at cost . The constraint on the objective function with

exploration becomes,

(27)

and the new static efficiency condition is,

(28)

The role of technical advancement has also been modeled as a realistic extension to the

general Hotelling model. Technical innovation lowers marginal cost such that the new cost

function becomes C(q,S,T). The static efficiency condition is,

(29)

where is the rate at which marginal costs fall due to changes in technology.

All three of these theoretical extensions predict that the marginal cost function is U-

shaped. Initially, the marginal cost of production is extremely high until efficient technology is

established. Over time, this drop in cost is offset by the diminishing rate of technological

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advances, at which point the marginal cost of production continues to rise as the resource grows

in scarcity. For the case of depletion, stock effect is initially minimal. A U-shaped cost function

is formed over time when ore quality decreases and extraction is more costly. Similarly,

discoveries of reserves are far more common in the first stages of production of a nonrenewable

resource. In the later stages, exploration becomes more expensive as the rate of discoveries

diminishes.

The theory presented in this section will serve as the foundation for the next section,

where we will test the theory of the Hotelling model empirically.

Section 3: Empirical Test of the Hotelling Model on Rare Earths Market Data, 1955 – 2009

3.1 Literature Review of Empirical Tests

Empirical tests of the Hotelling model can be divided into two broad categories:

descriptive and formal tests. Formal tests derive an appropriate cost function (such as the ones

outlined in the previous section) and test the Hotelling model with the appropriate data.

Specifically, cost data must be available to perform such a test. However, due to the proprietary

nature of cost data and the difficulty in obtaining it, formal tests are limited. These tests lead to

more conclusive results but also restrict the cost function to one specific form. Descriptive tests,

however, do not commit to a specific functional form. Rather, descriptive tests study the role of

market prices in the market equilibrium. They use market data to assess which of these models

are consistent.

The first to empirically assess the validity of the Hotelling model were Barnett and Morse

(1963), who used a descriptive approach. They concluded that the observed fall in mineral-

commodity prices over time indicated that scarcity was not a concern. Further descriptive tests

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were then undertaken by Heal and Barrow (1980), who compared metal price movements to

interest rates, but found that changes in interest rates, not interest rate levels, predicted prices.

Other descriptive studies found evidence that price paths are U-shaped, as was predicted

by the various theoretical extensions included in Section 2.3. One example of such a study was

performed by Slade (1982), who found that quadratic trends revealed upturns of real prices in

mineral commodities in the 1970’s, which she attributes to technical change.

Formal tests have had mixed results. Stollery (1983) obtains cost data from INCO, the

Canadian firm that is a monopolistic force in the world nickel industry. He concludes that the

Hotelling model is congruent with the data and a discount rate of 15%. In contrast to this

conclusion, Farrow (1985), rejects the hypothesis that proprietary data from a mining firm was

consistent with the theoretical Hotelling model. Although other structural have been performed,

such as those of Halvorsen and Smith (1984, 1991) and Young (1992), among others, evidence

in support of the Hotelling model from both formal and descriptive tests has been mixed and

varies based on the type of nonrenewable resource data tested.

3.2 Rare Earths Market Data, 1955-2009

As seen in the previous section, the Hotelling model has been tested both descriptively

and formally with market data from nonrenewable resources such as oil, copper, tin, and

numerous others. However, a test of the Hotelling model has never been performed with data

from the rare earths market. This section will present the data used, both historical and

quantitative, in order to perform such a test. Section 3.2.1 will give a general background of the

rare earths and their uses. Section 3.2.2 will describe the empirical data set utilized in testing the

Hotelling model. Section 3.2.3 will summarize the historical market trends taking place in the

rare earths market from 1955-2009.

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3.2.1 General Background

The rare earths elements are the relatively abundant group of 17 chemical elements in the

periodic table, specifically the 15 lanthanides along with scandium and yttrium. Although the

actual elements are abundant in the earths crust, the reason these resources are considered “rare”

is the scarcity of their concentrated, economically exploitable reserves, which are known as rare

earth minerals.

The principal rare earth minerals are bastnäsite, monazite, loparite, and the lateritic ion-

adsorption clays. The extraction of these minerals is the first step to a ten-day process in which

the actual rare earth elements are separated from one another. Rare earth producers require

significant capital and technological expertise, as well as licensing for mines which can be very

costly due the environmental impacts on the surrounding area.

The uses of the rare earths are extremely diverse, ranging from everyday devices

(computer memory, DVD's, rechargeable batteries, cell phones, magnets, fluorescent lighting) to

critical defense applications and medical devices. Recently, demand for rare earths has

dramatically increased due the heightened production of high-tech products and various political

factors. This makes the optimal extraction of rare earths an important area of study.

3.2.2 Empirical Data

Data on rare earth prices and production is available from the U.S. Geological Survey

(USGS) website which provides Historical Statistics for Mineral and Material Commodities in

the United States. Price data is reported in real terms as well as nominal. Data on interest rates

was found on the Federal Reserve website. The rate used in analysis was the 3-month Treasury

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bill secondary market rate, on a discount basis, from 1954-2009. Also, data on the annual CPI

(Consumer Price Index) was obtained from the Bureau of Labor Statistics website from 1955-

2009.

3.2.3 Historical Research on the Rare Earths Market

Historical research on the rare earths market was conducted with data from the Bureau of

Mines Minerals Yearbook, which outlined in detail the major events in the rare earths market

during the years in question. Knowledge in the historical events of the market will be utilized

later to see if the empirical test performed is congruent with reality. In specific, the roles of

depletion, exploration, and technology (which were the three theoretical extensions reviewed in

the literature review of the theory) will be summarized.

Technology – Technological advancement in the rare earths industry was most pronounced in the

late 1950’s and early 1960’s when efficient separation techniques for the rare earth elements

were developed. The concentrated, pure form of the rare earth elements are extremely difficult to

separate from the minerals and from one another due to their small ionic size. Thus,

technological advances are central in the production of rare earths, which require complex

separating technology such as ion exchange, fractional crystallization, and liquid-liquid

extraction.

In the late 1950’s, intensive research was published by the Bureau of Mines describing

solvent extraction, ion exchange, and other methods of rare earth extraction. At this point, the

price of rare earths metals began to drop due to “advances in extraction and separation

technology, rapid expansion of procession facilities, and competition among major producers”.

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By the early 1960's, the methods of solvent extraction and ion exchange were well-

researched; however these findings were still being applied to the industrial setting, specifically

for the separation of bastnäsite. For example, in 1962, the mill at Mountain Pass, California was

able to expand production of high-grade bastnäsite concentrate through improved efficiency.

In 1961, techniques using liquid-liquid extraction were presented at the Second Rare-

Earth Conference in the US. Likewise, Russian scientists used rapid liquid-liquid extraction on a

semi-industrial scale. Most technological advances continued until the mid-1960's, at which

point separation techniques were well-established and enabled research to focus on the properties

of rare earths and their numerous applications.

Some research did occur in the 1970's, mostly focusing on the separation of Yttrium and

overall cost efficiency. However technological discovery was pretty minimal until 1988 when

China was able to improve the recovery rate of rare earths such that the operating cost of

recovery was lowered by over 80%.4 Afterward, research efforts temporarily heightened in the

late 1980’s due to China’s entry in the world market, but quickly subsided. Since then,

technological advances regarding the uses of rare earths have dominated over improvements in

separation technology.

Exploration – In the rare earths market, exploration for the minerals of bastnäsite, monazite,

xenotime, and rare-earths bearing clay was rarely conducted specifically for the rare earths.

Rather, most mineral sand deposits were found in search for ilmenite and other titanium

minerals. Also, because many of the rare earths are naturally radioactive, many discoveries were

made during exploration for uranium and thorium. Once located however, there are substantial

4 Rare Earths Minerals and Metals, Mineral Yearbook 1988.

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costs in determining if the ore is economically extractable. This often involves constructing a

pilot plant in order to understand if the grade and purity of the minerals are economical.

Exploration can be divided into the search for heavy minerals and light minerals. Heavy

minerals such as monazite and xenotime survive continued erosion, generally through river and

sea currents, and form economic heavy-mineral deposits. Light minerals, such as bastnäsite are

formed when molten magma intrudes the earths crust at points of weakness and crystallizes. If

this occurs at or near the surface at a sufficient grade it may be economic. Exploration techniques

employed to locate the rare earths, as well as other minerals, include surface and airborne

reconnaissance with magnetometric and radiometric equipment.

From the years of 1955-2009, there were significant discoveries that decreased the

marginal cost of rare earth production (due to increased stock). The first large discovery took

place in 1961 in Argentina, followed in 1965 by a very large rare-earth monazite discovery in

Malawi as well as in South-West Africa in 1969. In the 1970’s, discoveries were made in

Western Australia, Burundi, India, and Brazil.

In 1980, one of the largest discoveries of rare earths to date took place in the Bayan Obo

mining region of Mainland China, which increased world reserves nearly two-fold. This was

followed by numerous discoveries in Canada: in 1982, a substantial discovery of yttrium-

beryllium-zirconium deposit was found near Strange Lake in Quebec, and in 1984, yttrium-

beryllium deposits were also discovered at Thor Lake, in the Northwest Territories of Canada.

Discoveries in the late 1980’s were made in Germany, Venezuela, Zaire, Gabon, Sri Lanka, and

Western Australia. Specifically in Australia, the discovery Mount Weld, one of the richest grade

rare earth deposits in the world, contained reserves of 15.4 million tons grading at 11.2% REO.

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World reserves were dramatically revised upward in 1991 from 62 million tons of

contained REO to 85 million tons of contained REO due to additional data on the

Commonwealth of Independent States, which reported 21.4 million tons. China’s share of world

reserves, which was thought to be 78%, dropped to 50%. In 1992, another revision of C.I.S. data

caused world reserves to be revised upward to 100 million tons of contained REO, such that

China’s reserves dropped to 43%.

Since then, reserves have stayed fairly constant although discoveries were made in

northern Mozambique, New South Whales (Australia), and India.

Stock Effect – Stock effect (decreasing ore quality over time) has not historically been a large

issue for rare earths producers. In some cases, however, it has been apparent. Beginning in the

1970’s, Australia’s production of monazite decreased by 12.6% because of leaner monazite

contents of the ore. Similarly, India’s production decreased in 1979-1980 due to lower

concentrations in mineral sands, requiring them to install new technology to provide higher feed

grades. With the rise of China as the main producer of rare earths, low-grade ores may become a

problem for Chinese producers in the future.

3.3 Methodology

The data presented on the rare earths market from 1955 – 2009 will be used to

empirically test the validity of the general Hotelling model. Due to the proprietary nature of cost

data for the rare earths market, cost data was unavailable. As a result, the Hotelling model cannot

be formally accepted or rejected because a formal model on the cost function cannot be

performed. However, the descriptive test described below will still be able to provide interesting

results.

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In order to test the Hotelling model without the availability of cost data for rare earths

market, we will first make the assumption that the theoretical Hotelling model holds. Another

way to re-write the general equation of the Hotelling model is,

(30)

In the above equation, we have data on nominal prices, , as well as data on nominal

interest rates, , from 1955 – 2009. Data is nominal due to the underlying theory of rational

expectations. The expected rise in price is equivalent to the expected rise in interest rate.

We will use this available data to empirically fit the “best-case” marginal cost function,

. This approach was used by Ellis and Halvorsen (2002), who estimate the functional form of

market power in a monopoly industry. This analysis was done as a component of their empirical

test on the Hotelling model. In specific, they restrict their function to a polynomial function and

use the assumption that the Hotelling model holds in order to estimate the appropriate

coefficients on the polynomial. After we obtain the estimated time path of marginal cost, we will

compare it with the historical data of what actually happened.

In addition to the assumption that the Hotelling model holds, however, this test also

makes an assumption on the nature of the rare earths industry. More specifically, we are

assuming that the rare earths market is perfectly competitive. This enables us to use price data,

, as a proxy for the benefit of extracting a nonrenewable resources where the benefit is

defined as the area under the demand curve. Without this assumption we would have to replace

price data, , with another proxy for benefit. For example, if the market were a monopolistic,

we would have to obtain data on marginal revenue, , which would be extremely difficult.

This assumption of a perfectly competitive industry is reasonable for the rare earths

market. From 1955-1990, the rare earths market has been extremely competitive and divided

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amongst numerous producing countries. The years where perfect competition may be an issue

occurred from 1990-2009, when China began its ascent as a major producer of rare earths.

China’s production grew dramatically from producing 30% of world rare earths in 1990, to

currently producing nearly 95%.

At first glance, China’s monopoly power would contradict our assumption of a perfectly

competitive industry. However, due to the decentralization of production (historically it has been

controlled by the individual localities rather than the central government) rare-earth producers

have struggled to maintain profitability. Competition between local governments has resulted in

overproduction and has deflated prices. In addition, illegal smuggling of rare-earths has also

decreased prices, limiting the profit of individual firms.5 Since 2007, the Chinese government

has been struggling to centralize production in order to preserve their resources and improve

profitability, but the given the scope of the data set from 1955-2009 and the lack of tangible

results thus far, this fact has little effect on the assumption that the rare earths market resembles a

perfectly competitive industry.

Now that the major assumptions have been made, we can define the marginal cost

function of rare earth production, , as a function of time. We will perform two separate tests.

The first test will include a wide variety of functional forms including a constant, a linear time

argument, quadratic time argument, a cubed time argument, a square root time argument, and a

logarithmic time argument. The “best-case” result would mirror the time path of marginal cost

from 1955-2009. In order to account for the nominal terms, and , we deflate each variable

by the .

Test 1:

(31)

5 USGS, “China’s Rare-Earth Industry”

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The second test enables us to model environmental cost, which is not a cost included in

the marginal cost function. This is because environmental costs began at a specific point in time,

marking a structural shift rather than a continuous process. In 1988, the radioactive byproduct of

rare earth production, thorium, became far more costly to process, ship, and dispose of. Costs

have only increased since then and are continuing to rise. Thus, a dummy variable for the years

after 1988, as well as an interaction term with this dummy variable, were included in the second

test to proxy for the structural shift in environmental costs.

Test 2:

(32)

By substituting and (the derivative of with respect to time) of each test into

(30) and rearranging terms (see Appendix I for algebraic calculations), we can simplify the

equation into the empirically testable forms shown in (33) and (34). This involves generating the

variables and , such that

running the OLS regressions below (with the constant withheld) will yield the appropriate

coefficients for the time path of marginal cost,

Test 1: (33)

Test 2:

(34)

3.4 Results

Before analyzing the results, it is important to once again highlight that the descriptive

test performed does not have the power to formally accept or reject the Hotelling model for the

rare earths market. Nonetheless, analyzing the "best-case" marginal time paths in conjunction

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with the historical research of the rare earth market from 1955-2009 will deliver meaningful

conclusions.

The “best-case” marginal cost function for each test had a positive initial marginal cost in

the constant term, the most statistically significant coefficients, and the highest . The

functional form for Test 1 that performed best with respect to the data is reported below, along

with Graph 1.1 and Graph 1.2,

(Test 1)

Graph 1.1: Best-Fit Functional Form, 1955-2009

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Best-Fit Functional Form, 1955-2009

MC(t)=381278+41623t-253050(t)^.5

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Graph 1.2: Best-Fit Functional Form, 1960-1970

As is seen by the results of Test 1, the "best-case" marginal cost function is negative in

the mid-1960's when marginal cost is at its minimum. This is inconsistent with the definition of

marginal cost, which is a powerful result because this marginal cost function is the “best-case”

scenario. Given we are assuming the Hotelling model holds, such an unrealistic result can be

seen weakly as a contradiction of the Hotelling model.

However, the results for Test II did not have these contradictory results. The "best-fit"

functional form of Test 2, along with Graph 2.1, Graph 2.2, Graph 2.3 are reported below,

(Test 2)

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Best-Fit Functional Form, 1960-1970

MC(t)=381278+41623t-253050(t)^.5

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Graph 2.1: Best-Fit Functional Form with Structural Break, 1955-2009

Graph 2.2: Best-Fit Functional Form with Structural Break, 1987-1989

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Time in Years (1955-2009)

Best-Fit Functional Form with Structural Break, 1955-2009

MC(t)=40912.3+10.8t^3-20762.2 ln t+19899post1988-425post1988t

320000

340000

360000

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Time in Years (1987-1989)

Best-Fit Functional Form with Structural Break, 1987-1989

MC(t)

Divovich 24

Graph 2.3: Best-Fit Functional Form with Structural Break, 1960-1970

The structural break in 1988 is hardly apparent in Graph 2.1. A closer look at the

structural break is seen in Graph 2.2, which shows that during 1988 marginal cost increased if

the Hotelling model holds true. Given the increase in environmental costs, this seems reasonable.

Most importantly, allowing for this structural shift kept the marginal cost function positive, as

seen in Graph 2.3.

Both Test I and Test II predict U-shaped marginal cost functions, which are consistent

with the theoretical and empirical literature to date. Likewise, both cost functions are at a

minimum around year 1964 (for Test 1 the minimum is at the start of 1964, while for Test 2 the

minimum is between 1963 and 1964).

Is this compatible with what actually took place in the rare earths market? As was

described earlier, technological advances were at their peak in the late 1950's and early 1960's

when the major separating technologies were being developed. By 1964, such technologies were

well-developed and were being successfully applied on an industrial scale. After the mid-1960's,

0

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1960 1961 1962 1963 1964 1965 1966 1967 1968 1969 1970

Time (1960-1970)

Best-Fit Functional Form with Structural Break, 1960-1970

MC(t)=40912.3+10.8t^3-20762.2 ln t+19899post1988-425post1988t

Divovich 25

however, technological developments that decreased the marginal cost of rare earth production

were scarce. While discoveries of rare earths have been fairly constant over time and stock effect

has been minimal, technological change has been, arguably, the most important factor embedded

in the marginal cost of production.

Section 4: Conclusion

With the key theoretical tool of dynamic programming, along with data on the rare earths

market from 1955-2009, we were able to derive the basic Hotelling model and perform a

descriptive test on the rare earths market. We were unable to formally prove or disprove the

Hotelling model due to lack of cost data, however, we were able to derive the “best-case” time

path of marginal cost from 1955 – 2009. Results were in line with the current theoretical and

empirical literature that predicts U-shaped cost curves. In addition, the minimum point of the

cost curve, in year 1964, was aligned with the technological advances in the rare earths market,

lending credibility to the Hotelling model for this market. However, without allowing a structural

shift for increased environmental costs, the Hotelling model was not consistent with the data.

Future tests should seek cost data in order to generate a formal test of the Hotelling model in the

rare earths market. The optimal extraction of this nonrenewable resource is an economically and

politically viable area of interest for future research.

Divovich 26

References

Agbeyegbe, T. "Interest Rates and Metal Price Movements: Further Evidence." Journal of

Environmental Economics and Management (1989): 184-92. Print.

Barnett HJ, Morse C. 1963. Scarcity and Growth, Baltimore: Johns Hopkins University Press

Dixit, Avinash K. Optimization in Economic Theory. London: Oxford UP, 1976. Print.

Ellis, Gregory, and Robert Halvorsen. "Estimation of Market Estimation of Market Power in a

Nonrenewable Resource Industry." The Journal of Political Economy 110.4 (2002): 883-

99. Print.

Farrow, Scott. "Testing the Efficiency of Extraction from a Stock Resource." Journal of Political

Economy 93.3 (1985): 452-87. Print.

Halvorsen, Robert, and Tim R. Smith. "On Measuring Natural Resource Scarcity." Journal of

Political Economy 92.5 (1984): 954-64. Print.

Heal, Geoffrey, and Michael Barrow. "The Relationship Between Interest Rates and Metal Price

Movements." Review of Economic Studies (1980): 161-81. Print.

Krautkraemer, Jeffrey A. "Nonrenewable Resource Scarcity." Journal of Economic Literature

XXXVI.December (1998): 2065-107. Print.

Obstfeld, Maurice. "Dynamic Optimization in Continuous-time Economic Models (A Guide for

the Perplexed)." University of California at Berkeley (1992).

Slade, M. "Trends in Natural-resource Commodity Prices: An Analysis of the Time Domain."

Journal of Environmental Economics and Management 9.2 (1982): 122-37. Print.

Stollery, K. "Mineral Depletion with Cost as the Extraction Limit: A Model Applied to the

Behavior of Prices in the Nickel Industry." Journal of Environmental Economics and

Management 10.2 (1983): 151-65. Print.

Divovich 27

Appendix 1

Below is the algebraic restructuring which enables us to test the Hotelling model

empirically and find the coefficients of marginal cost with respect to time,