ESTIMATION OF DYNAMIC INVESTMENT
FUNCTIONS IN OIL EXPLORATION
Documento 89-05
Kenneth Hendricks
Alfonso Novales
Estimation of Dynamic Investment Functions in Oil Exploration
by
Kenneth Hendricks University of British Columbia
Alfonso Novales Universidad Complutense de Madrid
Revised
September 1988
Abstract
This paper studies the dynamics of the discovery process for oil and gas pools in the province of Alberta, Canada from 1950 to 1979. A costs of adjustment, rational expectations model is specified in which current and future returns from exploration are random, and the main source of the uncertainty is the amount of discoveries. The parameters are estimated from the stochastic Euler equation using the Generalized Methods of Moments estimator proposed by Hansen (1982). We find that, at the appropriate level of aggregation, there is a stable, quantifiable relationship between exploratory investment and returns which is consistent with optimizing behavior.
*We are indebted to R. Uhler for giving us access to the data. We would also like to thank Harry Paarsch and John Kennan for helpful discussions. Financial support from NSF Grant No. SES-8409133 and the Resources for the Future, Inc. is gratefully acknowledged. This paper was written while Hendricks was visiting the Hoover Institution.
1. Introduction
Empirical models of exploration can be grouped into two categories.
The first is supply models which focus on estimating the probability law
governing the sequence of discoveries . Such models usually ignore the
economic decisions which help determine the sample of drilling outcomes. The
second is econometric models which purport to estimate the effects of economic
incentives on the flows of drilling inputs and discoveries. These usually
involve an ad hoc specification of the forces determining supply in which
measures of drilling inputs and discoveries are regressed on one-period lags
of these variables, and proxies for prices and costs. An exception is the
work by Epple (1984), who develops an optimizing, dynamic model of investment
behavior with rational expectations.
Both categories have their problems. The supply models can predict
the probability of finding at least z more reserves if k more wells are
drilled, but they cannot address the issue of whether the k wells should be
drilled and if so, at what rate. Furthermore, their failure to account for
the behavioral process which generates the data is likely to bias the
forecasts. The econometric models have yielded notoriously unreliable
estimates of supply elasticities. In his evaluation of three of these
studies, Pindyck (1975) found that estimates of supply elasticities were
highly unstable with respect to both model specification and time period. He
attributed the instability to two factors: the absence of an optimizing
framework and an inadequate specification of the dynamic structure of the
discovery process. We would add a third factor, aggregation of investment
paths and returns from diverse geographical regions.
The work by Epple (1984) addresses some of these criticisms. He
derives the firm's decision rule from a dynamic, stochastic optimization model
in which the firm chooses a contingent production plan to maximize the
expected present value of resources. The distinguishing feature of
nonrenewable resources like oil and gas is, of course, that they are
depletable. This aspect is incorporated into Epple's model through the
assumption that the costs of finding and developing new deposits in future
periods depend upon cumulative production. Thus, in choosing its current
output, the firm must take into account the effect of its decision on expected
future extraction costs. Forecasts of ultimate recovery are calculated from
the condition that expected marginal extraction costs of the last unit
produced must be equal to the resource price.
Our modelling is in the same spirit as Epple's, but the approach is
quite different. We focus on the decision of the individual firm to drill
exploratory wells in a specific area, Alberta, Canada. The optimal drilling
plan is characterized as a solution to a stochastic Euler equation which
equates the expected returns of a exploratory well to expected marginal
drilling costs. Uncertainty about returns is caused primarily by randomness
in discoveries rather than in drilling costs. The effect of depletion is
incorporated into the model through the stochastic process determining
returns: average returns are assumed to decline over time. Our objective is
to establish whether a stable, quantifiable relationship between exploratory
investment and returns exists which is consistent with optimizing behavior.
In particular, we are interested in determining whether a dynamic model is
necessary to explain the data (i.e., are there any costs of adjustment), and
how information flows from drilling activity influence expectations of current
and future returns.
The presence of nontrivial investment dynamics has important
implications for measuring the impact of changes in the economic environment.
Previous studies have generally focused on short-run measures. But this is
valid only if exploratory investment is not a dynamic process. Otherwise, the
appropriate comparison is between the time paths of investment and discoveries
that are generated by alternative economic environments. In particular, one
needs to recognize the possibility that a once-and-for-all increase in, say,
the price of oil, is likely to "tilt" the drilling profile in a region to the
present. As a result, much of the initial response in discoveries may be a
transfer from the near future to the present, and does not represent finds
that would not have occurred otherwise.
It is also important to determine the role of information in the
exploration process. If information spillovers are substantial, the
competitive allocation of resources is probably not efficient. Too much
drilling may occur in areas where discoveries have been made, and too little
in areas which are relatively unexplored. Learning may also help explain why
estimates obtained from data which aggregate returns and investments from
diverse regions are often so imprecise and unstable. The response of
investment and discoveries in a region to changes in the economic environment
may depend upon its stage of development. In that case, there is no reason to
suppose that the relationship between aggregate investment and aggregate
returns is a stable one if the vintage distribution of areas is not
stationary.
Finally, we should note that, in contrast to the previous literature,
we do not try to forecast reserves. The reason is that the model is partial
equilibrium: it predicts the supply path of drilling inputs of a
representative firm when that firm faces a fixed probability law for drilling
returns. At the industry level, this probability law is almost certain to be
endogenous, since depletion effects implies that current drilling returns
should depend upon the past history of industry drilling inputs. This
endogeneity of the returns process needs to be taken into account when making
forecasts about a region's reserves and stocks of wells.
The paper is organized as follows. In the next section, we introduce
our model of the firm's investment problem. The estimation procedure is
outlined in Section 3. Although it is possible to solve explicitly for the
decision rule under appropriate assumptions on the stochastic processes, we
have chosen instead to estimate the parameters of the objective function from
the Euler equation using the Generalized Method of Moments estimator
introduced by Hansen (1982). The main reasons for doing so are the relatively
small number of observations, and our reluctance to impose the requisite
restrictions on the stochastic process for returns. We test the model using
the restrictions implied by the theory. Previous applications of this method
include studies by Hansen and Singleton (1982) on stock returns data and by
Pindyck and Rotemberg (1983, 1984) to energy demand.
The data is described in Section 4. A virtue of the data set is that
exploratory wells are distinguished from development wells, and discoveries
from revisions to initial estimates. This is important since the evidence
strongly suggests that discoveries from exploratory wells generate information
which affect drilling decisions on other prospects, but that revisions to
reserves due to development wells do not. The estimation results are
presented in Section 5, and conclusions follow in Section 6.
2. The Investment Model
We begin with a brief description of the exploration process in the
province of Alberta, Canada.
The ownership of natural resources in Canada is, for the most part,
invested in the provinces. In developing its hydrocarbon reserves, the
Alberta government has generally followed a policy of retaining public
ownership, and contracting with firms in the private sector to find and
produce the deposits. For example, in 1971, less than 12% of the total oil
and gas acreage in the province of Alberta was privately owned. The rest of
the acreage was leased by the government to oil and gas firms in a variety of
tenure arrangements.
Three types of licenses control exploration for oil and gas in
Alberta. Geophysical licenses give non-exclusive rights to conduct private
geological, seismic, magnetometer, and other types of surveys almost anywhere
in the province, including those areas subject to existing leases. The
license does not permit the drilling of test wells. Anyone can obtain a
geophysical lease, and it is renewable each year for a fee. Firms use the
surveys to identify promising areas, or prospects, over which it desires to
obtain exclusive rights to drill exploratory wells and to produce oil and gas.
Drilling and production rights are usually sold via a first price,
sealed bid auction. Initially, firms bid for a petroleum and natural gas
reservation, which gives the winner an exclusive right to drill in a specified
area. The size of the area cannot exceed 156 square miles. The term of a
reservation is four months, but it can be extended for several years with a
pledge to conduct an exploration program that meets the approval of the
government. If oil or gas is discovered, or prospects look promising, the
reservation holder would normally apply for petroleum and natural gas leases,
which confer long-term (at least 10 years) rights to produce oil and gas on
designated parts of the reservation. A lease cannot exceed eight or nine
square miles, or be less than a quarter-section. Furthermore, the reservation
holder cannot apply for more than 50% of any township subject to the
reservation, or for leases that are adjacent. This gives rise to a
"checkerboard" pattern of lease ownership. Leases not claimed by the
reservation holder are returned to the government as Crown reserves, and
subsequently sold in first-price, sealed bid auctions. The reservation holder
is required to submit cores and logs from any wells drilled, and this
information is made public one year after the application date.
The markets for land and drilling inputs into the exploration process
were competitive. For any given year in the sample period from 1946 to 1979,
the fraction of exploratory wells drilled by the top sixteen oil companies
ranged from a low of 22 per cent to a high of 40 per cent. Thus, the
individual firm's annual investment in exploratory wells was small relative to
the total number of wells drilled by the exploration industry. Wellhead
prices for the Alberta oil and gas products were clearly exogenous to the
firms, since these prices were determined by the international market, and
total output of oil and gas from Alberta was only a tiny fraction of the
volumes transacted in this market.
Wellhead prices for oil were roughly constant in nominal terms until
1973, after which they rose according to a formula imposed by the federal
government. Wellhead prices for gas increased steadily throughout the sample
period, but were generally too low prior to the 1970's to make exploration and
development of gas pools a profitable investment. Nominal drilling costs per
well were also basically constant throughout the sample period, ranging
between $70,000 to $130,000, depending upon the depth of the well. Thus, for
our sample, the main source of uncertainty in returns was the sizes of the
discoveries. Many prospects did not contain sufficient quantities of oil and
gas to make production profitable and, as a result, the cost of drilling
exploratory wells was not recovered.
We shall consider a somewhat stylized model of firm behavior. At the
beginning of each period, each firm must decide on the number of prospects it
should acquire and drill in that period, taking as given market prices of
prospects and wellhead prices of oil and gas products. Prospects not drilled
by the end of the period are returned to the government. We shall further
assume that prospects and drilling rigs are combined in fixed proportion to
produce wells. Given these assumptions, the planning problem of the
representative firm can be formulated in terms of choosing a contingent
drilling program to maximize the expected present value of discoveries :
\[E _ {t} \sum_ {j = 0} ^ {\infty} \delta^ {t + j} \left\{\left(v _ {t + j} a _ {t + j} - b _ {t + j}\right) x _ {t + j} - \alpha_ {1} x _ {t + j} - (1 / 2) \alpha_ {2} x _ {t + j} ^ {2} - (1 / 2) \alpha_ {3} \left(x _ {t + j} - x _ {t - 1 + j}\right) ^ {2} \right\}.\tag{2.1}\]
In the above notation: is the number of exploratory wells drilled
during period t, is the amount of reserves discovered per well during
period t, is the after-tax, present value price of a unit of reserves
discovered in period t, and is the cost of period t drilling inputs. The
vector of cost parameters, , is nonnegative, and the discount
parameter satisfies . The operator denotes the conditional
expectation: where y is a random variable, and is the
firm's information set at the beginning of period t. It includes, in
particular, and , for all , current and lagged prices of oil and
gas, and for i > 0. It does not include , which is random at the time
the firm drills the wells.
Define to be the dollar return per well drilled net of
drilling costs. We shall assume that the individual firm views the stochastic
process governing as lying outside of its control, and that it is of
exponential order less than . Then, differentiating (2.1) with respect to
yields the Euler equation:
\[\mathrm{E} _ {t} \left[ \pi_ {t} - \alpha_ {1} - \alpha_ {2} x _ {t} - \alpha_ {3} \left(x _ {t} - x _ {t - 1}\right) + \delta \alpha_ {3} \left(x _ {t + 1} - x _ {t}\right) \right] = 0.\tag{2.2}\]
The transversality condition is
\[\lim _ {t \rightarrow \infty} E _ {t} \delta^ {T} \left[ \pi_ {t} - \alpha_ {1} - \alpha_ {2} x _ {t} - \alpha_ {3} \left(x _ {t} - x _ {t - 1}\right) + \delta \alpha_ {3} \left(x _ {t + 1} - x _ {t}\right)\right] = 0.\tag{2.3}\]
Our assumption on ensures that equation (2.3) is satisfied. Also,
given our representative firm assumption, we shall assume that the solution to
the Euler equation is interior (i.e., for all t).
The strength of our model is that it captures two features which we
believe are essential to understanding the exploration process. First,
current and future returns are stochastic because of the randomness in
discoveries. If learning is present, and depletion effects are anticipated,
then expectations about these returns depend upon past discoveries and
drilling efforts. Second, fluctuations in drilling activity are costly. One
interpretation of this property is that there is a fixed factor, such as the
stock of drilling rigs, which makes it costly for a firm to change its level
of drilling activity from period to period. Note that if there are no costs
of adjustment (i.e., is equal to zero), then there are no dynamics to
explain, since drilling effort in each period would depend only upon the
expected returns in that period.
The restrictive aspect of the model lies in the assumption that firms
cannot hold inventories of prospects. Each firm acquires only as many
prospects as it intends to drill in that period. This assumption has several
important implications. It means that a firm cannot delay exploration of a
prospect until after the outcomes of wells being drilled in the current period
are known. Furthermore, information from current drilling efforts about
prospects sold in subsequent periods is incorporated into the prices of these
prospects since drilling outcomes are observable. Hence, a prospect has no
informational value to its owner, and private drilling returns are determined
solely by the amount of hydrocarbons which can be produced.
The purpose of the above assumption is to rule out any incentive firms
might have to hold prospects for speculative purposes. Its necessity follows
from limitations in the available data, which identifies the location of an
exploratory well and the number of wells drilled each year, but not which firms drilled them or their lease holdings. The empirical significance of the assumption is not clear. As mentioned previously, many tenure arrangements are in fact relatively short-lived, although in most instances, they seem to be longer than the period required to drill and evaluate core samples. Consequently, it is a restrictive assumption, and we shall have to bear it in mind when interpreting the estimation results.
Finally, we should point out that the model is partial equilibrium. The probability law governing drilling returns is assumed to be exogenous to the individual firm. In a more complete model, the amount of discoveries in each period would be determined simultaneously with investment in wildcat wells, and the supply paths of both drilling inputs and discoveries would be expressed as functions of the underlying cost technology and the probability law for discoveries.
3. Estimation Strategy
The literature suggests several procedures for estimating the model. The simplest method is the approach followed by McCallum (1982) and Kennan (1979). They use realizations of future variables in the Euler equation as proxies for their conditional expectations, and treat the estimation of the resulting model as an errors in variables problem. As Hansen and Sargent (1980, 1982) point out, this method ignores a number of restrictions implied the model. A major benefit of the linear-quadratic structure is that, given suitable restrictions on the stochastic environment, one can obtain closed form solutions for the decision rule. Hansen and Sargent exploit this property in developing full information estimators for models such as ours.
The methods of Hansen and Sargent involve estimation of a relatively
large set of parameters. In addition to those in the decision rule, one must
estimate the parameters of the vector autoregressive representation of the
instrumental variables, and the parameters of the linear projections of the
forcing variable, , and the decision variable, , on the set of
instruments. We have at most 33 observations, of which we lose at least two
due to lags in the decision rule and instruments. This number seems too few
to implement with any degree of confidence the Hansen-Sargent methods. In
addition, we were somewhat reluctant to impose the requisite restrictions on
the stochastic structure.
Hansen and Singleton (1982) suggest an alternative estimation strategy
based upon the General Methods of Moments estimator proposed by Hansen (1982).
This method interprets the Euler equation as implying a set of orthogonality
conditions, which can be used to obtain estimates for the parameters, and to
test the model. As the authors note, an important benefit of this approach is
that it does not require strong a priori assumptions about the properties of
the stochastic process of the forcing variable . In particular, it permits
conditional variances of the disturbances to depend on variables in the
information set.
In describing the estimation procedure, it will be useful to express the Euler equation in the form:
\[E _ {t} \left[ x _ {t} - \beta_ {0} - \beta_ {1} x _ {t - 1} - \beta_ {2} x _ {t + 1} - \beta_ {3} \pi_ {t} \right] = 0,\tag{3.1}\]
where:
\[\beta_ {0} = - \alpha_ {1} / [ \alpha_ {2} + \alpha_ {3} (1 - \delta) ]\]
\[\beta_ {1} = \alpha_ {3} / [ \alpha_ {2} + \alpha_ {3} (1 - \delta) ]\]
\[\beta_ {2} = \delta \alpha_ {3} / [ \alpha_ {2} + \alpha_ {3} (1 - \delta) ]\]
\[\beta_ {3} = 1 / \left[ \alpha_ {2} + \alpha_ {3} (1 - \delta) \right].\]
Our strategy will be to derive an estimator for , and then
obtain estimates for from the four equations given in (3.1). Standard
errors will then be obtained using the method.
Following Hansen and Singleton (1982), we define the function
\[h \left(Y _ {t + 1}, \beta\right) = x _ {t} - \beta_ {0} - \beta_ {1} x _ {t - 1} - \beta_ {2} x _ {t + 1} - \beta_ {3} \pi_ {t},\]
where is the vector of variables in the decision rule. Deviations of from zero can be interpreted as arising from errors in expectations. Letting denote this error, the Euler condition can then be written as
\[\mathrm{h} \left(\mathrm{Y} _ {\mathrm{t+1}}, \beta\right) + \mathrm{v} _ {\mathrm{t+1}} = 0\]
or:
\[\mathrm{x} _ {\mathrm{t}} = \beta_ {0} + \beta_ {1} \mathrm{x} _ {\mathrm{t} - 1} + \beta_ {2} \mathrm{x} _ {\mathrm{t} + 1} - \beta_ {3} \pi_ {\mathrm{t}} + \mathrm{u} _ {\mathrm{t} + 1},\tag{3.2}\]
with .
If expectations are rational, the residual in equation (3.2) should be unpredictable, given the available information: . Furthermore, residuals are serially uncorrelated, since, letting E denote the unconditional expectations operator, for all . Finally, although not required by the estimation procedure, we shall make the simplifying assumption that the errors are conditionally homoscedastic.
The Hansen-Singleton estimator is an instrumental variables procedure which minimizes the correlation between variables known at time and the residuals of equation (3.2). Ideally, the vector of instruments is the expectation of the gradient vector conditional on the information set at time . Hansen and Singleton note that, in general, choosing the optimal instruments requires a detailed specification of the economic environment. The task is greatly simplified if one is willing to
assume that conditional expectations coincide with linear projects. We make
this assumption. Combined with the conditional homoscedsticity assumption,
the estimation procedure then reduces to two step least squares.
The estimation method uses only four of the available orthogonality
conditions to identify the parameter vector . The remaining othogonality
conditions can then be used as a specification test since, if the model and
its behavioral restrictions are correct, the sample analogues of the cross-
products of the residuals and the instruments should be close to zero. The
appropriate test statistic for the hypothesis that these restrictions are
satisfied has been derived by Hansen (1982). He has shown that the asymptotic
distribution of T times the minimized value of the objective function is chi-
square with p-r degrees of freedom, where p is the number of instruments and r
is number of orthogonality conditions actually used for identifying .
To summarize: we propose to estimate the structural parameters of our
model directly from the stochastic Euler equation using the Generalized
Instrumental Variables estimator of Hansen and Singleton. The specification
of the model will be tested by examining whether or not (1) the residuals are
serially uncorrelated, (2) the set of overidentifying restrictions are
satisfied, and (3) the coefficients and satisfy the linear restriction
for reasonable values of . We also propose to test the hypothesis
that there are no costs of adjustment (i.e., ) by estimating the
static model in which wildcat drilling is a linear function of .
4. Description of Data
The data were obtained from the study submitted by Uhler (with
Eglington) (1983) to the Economic Council of Canada on the exploration for oil
and gas deposits in the province of Alberta, Canada. An important feature of
the data set is the geographical detail of the drilling and discovery
information.
Oil and gas pools in this study were indexed by areal location and
geological horizon (depth). Horizons refer to the substrata associated with
different geological periods. The province was divided into ten areas and ten
horizons, generating one hundred possible (horizon, area) pairs. For each
(horizon, area) pair, Uhler gives annual data on changes in oil and gas
reserves separately, and on drilling activity. The sample period is basically
from 1950 to 1979. Discoveries are reported separately from revisions, and
the latter are reported by vintage. That is, annual revisions of pools
discovered in year t are listed separately from those of pools discovered in
year s, s ≠ t.
The drilling data for each (horizon, area) pair reports the number of
wells drilled annually, and the type of well: wildcat wells, which are drilled
in search of new pools, and development wells, which are drilled in pools that
have already been discovered. Wells were allocated to each category under the
assumption that the deepest horizon penetrated is the target horizon.
Since the amount of drilling in many of the (horizon, area) pairs was
quite small, Uhler (1983) reduced the number of categories to eight, mainly by
aggregating across areas within an horizon. We combined the two Lower
Devonian categories, and dropped one category from the sample due to
incomplete drilling data. (It contained virtually no oil pools, and the
number of wells drilled prior to the 1970's was quite small.) The remaining
six categories are listed in Table 1. They are ordered by depth, with the
Lower Devonian horizon representing the deepest horizon. Gas reserves are
measured in billions of cubic meters, and oil reserves are measured in
millions of cubic meters. Gas reserves in pools which contain both oil and
gas are called associated gas (AG). Reserves in gas pools are called
nonassociated gas (NAG). The Upper Cretaceous horizon includes only oil and
gas pools discovered in the central part of Alberta. The other horizons
include all pools discovered in these horizons throughout the province.
The pools in the shallower horizons tend to have a higher gas content
than oil. The exception is the Upper Cretaceous horizon, where 170 million
cubic meters of oil were discovered. This figure is somewhat misleading,
however, since most of the oil reserves, 130 million cubic meters to be
precise, are in one pool, the gigantic Pembina pool. It was discovered in
1953, and accounts for approximately 11% of Alberta's oil reserves. Most of
the remaining 89% of Alberta's oil reserves lie in the deeper Devonian
horizons.
The differences in the ratio of the number of wildcat wells to the
number of development wells across horizons reflect differences in the size
distributions of pools. When a wildcat well discovers a pool, it is usually
completed and turned into a producing well. Development wells are drilled
only if the pool is sufficiently large that more than the one well is needed
for optimal production. In the Lower Devonian and Mannville horizons, the oil
and gas pools were relatively small, and frequently did not require any
development wells. The gigantic Pembina pool, on the other hand, required a
large number of development wells and, as a result, the ratio of wildcat to
development wells in this horizon was relatively low. Many of the pools in
the Upper Devonian horizon were also quite large.
What is the appropriate geographical and geological context for the
firm's investment decision? One possibility is the horizon, on the grounds
that the presence (or absence) of hydrocarbon deposits at one location in a
horizon changes the probability of finding deposits elsewhere in that horizon.
But, even if the formation of pools in different horizons are independent
geological events, when a well is drilled to an horizon, it necessarily
produces information about every horizon that lies above the target horizon.
Therefore, all horizons in a specific area is likely to be a better
approximation to the decision environment than the individual horizon.
Unfortunately, the raw data that would permit this type of aggregation
were not available. A crude alternative is to aggregate drilling investment
in horizons where drilling occurred in approximately the same areas at the
same time. Prior to the 1970's, most of the drilling activity in the Upper
Cretaceous, Mannville, Viking, Mississippi, and Upper Devonian horizons took
place in central Alberta. In the 1970's, drilling in the Mannville, Viking,
and Mississippi horizons shifted to the southwestern part of Alberta, near the
foothills, where most of the gas pools are located. Drilling in the Lower
Devonian horizon was concentrated almost exclusively in northwestern Alberta.
Moreover, almost all of the drilling in this area was targeted to the Lower
Devonian horizon, since other horizons in this area contained few oil or gas
pools. On the basis of these facts, we separated the Lower Devonian horizon
from all other horizons, and aggregated the latter into one category, called
Agg\LoDev. This classification represents our base case.
Our measure of exploratory drilling effort is the number of wildcat
wells. We regard expenditures on development wells as part of the cost of
developing the pool. Accordingly, the amount of oil and gas discovered by a
wildcat well drilled in year t is given by the average size of pools
discovered in that year, where size is measured by cumulative production.
Revisions to initial estimates of discoveries are assumed to reflect reporting
lags, and to add no new information about the prospect. We examine the
validity of these assumptions in the appendix, and find that they are strongly
supported by the data.
Annual prices for developed and undeveloped reserves of an "average"
pool in Alberta were computed using annual data on wellhead prices for oil and
gas, development costs, and taxes. The formula which Uhler used to calculate
the expected price of reserves in each year is based upon the following
assumptions: a fifteen year production life, a constant rate of production,
and price expectations which were static up to 1973 , and consistent with the
government-controlled growth rate in prices after 1973. The price shock of
1973 was assumed to be unanticipated. After deducting various operating
costs, taxes, and royalties from the wellhead price (measured in nominal
dollars), the flow of expected net returns were discounted back to the date of
discovery at the nominal rate of interest to yield a price for developed
reserves. The price of undeveloped reserves was obtained by deducting
development costs, which were assumed to occur in the first year of the
production period.
Drilling costs were obtained from the Annual Report on exploration
expenditures by Alberta Department of Energy and Natural Resources.
The empirical definitions of the variables introduced in Section 2 are
listed in the top panel of Table 2. All dollar figures are expressed in
millions of 1965 dollars. The gross return from a wildcat well is defined as
the sum of oil and gas revenues, although in most horizons, and for most of
the sample period, oil revenues was the main component. The net return is
calculated by deducting exploratory drilling costs. It does not net out
geophysical and land acquisition costs, since these data were available only
for Alberta as a whole, and not for the individual horizons. Means and
standard deviations for annual wildcat drilling, net returns, and profits are
reported in the bottom panel of Table 2 for each horizon, and for each of the
aggregates.
5. Estimation Results
The model was estimated by two step least squares. Instrumental
variables for and were constructed using as instruments one lag each of
discoveries, discoveries per well, and wildcat drilling, and contemporaneous
values of wildcat drilling, oil prices, and gas prices. The standard errors
for were calculated using a consistent estimate of the asymptotic
covariance matrix under heteroskedasticity, proposed by White (1982).
Standard errors for were derived using the covariance matrix A·Σ·A, where A
is the Jacobian of the mapping between and .
Table 3 gives the estimation results for the base case. The estimates
in column U correspond to the model with no restriction on the coefficients.
The estimates in column R are obtained under the restriction and a
value for . T, gives the chi-squared statistic which tests the
validity of this hypothesis. gives the chi-squared statistic for the
overidentifying restrictions of the dynamic model, and gives this statistic
for the restriction , which yields the static model. The numbers
which appear in parentheses after the chi-squared statistics are their
marginal significance levels.
The specification tests indicate that our model is consistent with the
data. The overidentifying restrictions are not rejected in either of the two
equations, although the marginal significance levels are not very high. The
linear restriction on the coefficients (i.e., ) was satisfied at
conventional significance levels. The first order autoregressions for the
residuals in each of the two equations revealed no evidence of serial
correlation. We checked the simple and partial autocorrelation functions of
the residuals, and did not find any contrary evidence. Of course, one should
remember that the sample size is small, so the confidence intervals for the
autocorrelations are quite wide (i.e., the tests surely have low power).
Most of the coefficients of the restricted model are significant at
conventional confidence levels, have the correct sign, and are stable across
the two classifications. Furthermore, the magnitudes of the associated cost
parameters do not appear to be implausible. The parameter can be
interpreted as average geophysical costs and land acquisition costs per well
over the sample period. For the province as a whole, these costs ranged
between $400,000 to $1 million per well during the sample period, which does
not differ too greatly from the point estimates of $1.2 and $1.5 million in
the Agg/LoDev and Lower Devonian horizons, respectively. The cost of
adjustment parameter is estimated to be about $15,000 to $28,000 per well,
which also seems plausible. However, the estimates for are consistently
negative, although not significantly different from zero.
The statistics for the set of overidentifying restrictions in the
static version of the model indicate that the null hypothesis of no costs of
adjustment (i.e., ) is overwhelmingly rejected in both the Lower
Devonian horizons and the unit called Agg/LoDev. Thus, the instantaneous
response in exploratory drilling to the discovery of a large pool, or an
unexpected rise in oil prices, can differ substantially from the long-term
response.
A striking result that deserves emphasis is the similarity of the
estimates across the two regions. In Figures 2 and 3, we have depicted the
actual drilling paths for the Agg/LoDev horizons and the Lower Devonian
horizons, respectively. The pattern of drilling activity in the latter case
was clearly quite different from that in the non-Lower Devonian horizons, even
after one accounts for differences in scale. Nevertheless, the same model is
capable of explaining both patterns.
Furthermore, the model performs well. The dashed lines in Figures 2
and 3 depict the predicted drilling paths for the two regions. The overall
fit in both cases is quite good. In the Agg/LoDev case, the model just misses
the spike in 1973, but it adjusts to it in a short period of time. In the
Lower Devonian case, the model captures quite well the turning points in 1960,
1964, and 1974.
Alternative Classifications of Pools
Table 4 reports the results of the restricted model when it is
estimated by horizon. As expected, the model does quite poorly in horizons
other than the Lower Devonian. The specification tests reveal inconsistencies
between the model and the data. The overidentifying restrictions are rejected
at the 5% significance level in the Upper Cretaceous and Mississippi horizons.
Support for the linear constraint is relatively weak in the Upper Cretaceous,
Viking and Upper Devonian horizons. Also, there is evidence of serial
correlation in the residuals for the Mississippi and Upper Devonian horizons.
Additional evidence for rejecting the model as a plausible explanation
of drilling behavior in non-Lower Devonian horizons is provided by the
parameter estimates themselves. The estimates for and are generally not
significantly different from zero, and in several instances, they have the
wrong sign. The implied estimates for are implausibly large in the Upper
Cretaceous and Upper Devonian horizons, and have the opposite signs to that
expected in the other three non-Lower Devonian horizons. The estimates for ,
and frequently have the wrong sign, although in most instances, they are
not significantly different from zero.
These results indicate that firms did not choose their drilling
programs to maximize the present value of discoveries within an horizon. Our
interpretation of this negative conclusion, in conjunction with the positive
conclusion obtained for the base case, is that the horizon was not the
geographical context in which firms were making their investment decisions.
Rather, the appropriate geographical context is one which aggregates different
horizons in a region.
6. Concluding Remarks
In this paper we have formulated and estimated a dynamic model of
exploratory drilling with rational expectations. The results provide some
important insights about the nature of the exploration process, which are
likely to be useful for policy-makers. In particular, we would emphasise the
following implications.
First, the data strongly rejects the hypothesis of a static model of
drilling behavior. This puts into question short-run measures of the impact
of changes in the economic environment on drilling and discovery rates. Most
of the initial response in discoveries may simply represent transfers from
future periods to the current period as the drilling profile is "tilted"
toward the present. Furthermore, they do not provide a measure of discoveries
that would not have been made if prices had not increased. The correct
approach to evaluating the impact of price and other policy changes is to
recognize that alternative economic environments generate different paths of
investment and discoveries, and to compare these paths.
Second, the data provides evidence that firms do not regard drilling
returns as a sequence of independent random variables. Instead, they use the
information from past realizations of returns and drilling efforts to forecast
current and future values of returns. Furthermore, their forecasts appear to
be consistent with the underlying probability law. The structure of this
probability law and the firm's response to drilling outcomes indicates that
information spillovers are likely to be an important determinant of drilling
behavior. This raises several issues, which could not be addressed at the
current level of aggregation, but could be studied if firm data were
available. How important are "bandwagon" effects in determining the
geographical pattern of drilling? What is the impact of different tenure
arrangements on rates of exploration?
Third, classifying pools and wells according to the informational
context in which drilling decisions are taken is important for obtaining
precise and stable estimates of the decision rule. In the Alberta basin, this
implied a classification that was based more on geographical than on
geological criteria. It is also apparent that aggregating investments from
regions which are in different stages of development, or have different
probability laws for returns, is in general not a good idea, since the
underlying probability laws and the expectations mechanism determining
investment behavior are region-specific.
Our costs-of-adjustment interpretation of the dynamics is subject to
an important caveat. It was derived under the assumption that the tenure of
prospects was equal to the drilling period. The presence of information
spillovers indicates that this assumption is crucial. Otherwise, firms have
an incentive to behave strategically, and delay drilling marginal prospects
until after drilling outcomes on prospects that are currently being drilled
are observed. As a descriptive matter, there is some reason to believe that
this assumption is not correct. Consequently, some of the dynamics detected
in the data may reflect the desire of firms to delay in order to learn more.
If so, the disaggregation of pools and wells must be extended to firms as well
as location. This is clearly the next step in the research.
Kaufman et. al. (1975, 1981), Meisner and Demirmen (1981) are good examples.
Three examples of this literature are Erickson and Spann (1971), Khazzoom (1971), and MacAvoy and Pindyck (1973).
See Hendricks and Kovenock (1989) for a theoretical analysis of the efficiency issue.
These restrictions did not apply for those parts of the province designated as Block 'A' areas. In these areas, a firm did not have to surrender any of the leases covered by the initial permit to the government.
It can be shown that this maximization problem is equivalent to maximizing the present value of production if output in period t is assumed to be proportional to stock of reserves in period t.
Nominal prices were essentially constant during this period.
In most cases, a comparison of to the covariance matrix obtained under the assumption of conditional homosckedasticity indicated that some heterosckedasticity was present.
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APPENDIX
In this appendix, we examine the hypothesis that development wells are primarily investments in production, and that revisions to initial estimates do not represent new information about reserves. In our evaluation, we ignore gas pools because, for most of the sample period, gas prices were too low to make exploration for gas a profitable investment. Gas pools tended to be produced only if it was discovered as a byproduct of the search for oil pools, after the costs of drilling had been sunk.
Let denote the initial estimate of the amount of oil reserves discovered in period t, and let represent the period s revision of oil reserve estimates for these pools, s > t. Final reserves of vintage t oil pools are given by:
\[Z _ {t} = \Sigma_ {s \geq t} ^ {T} Z _ {s, t},\]
where T is equal to 1981, the last year for which reserve data are available. Total changes in oil reserves in period t due to development drilling are given by:
\[R _ {t} = \sum_ {s = 0} ^ {t - 1} z _ {t, s}\]
The Viking horizon contained virtually no oil pools. In the Upper Cretaceous, Mannville, and Mississippi horizons, oil pools were generally quite small, and the values of were frequently zero. (The correlation coefficients between initial and final reserve estimates in these pools are 0.75, 0.97, and 1.00 respectively.) Yet, in many of these years, substantial numbers of development wells were drilled. In the Devonian horizons, the oil pools were much larger, and final reserve estimates were often four to eight times as large as initial reserve estimates. However, even in these cases, the revisions exhibited a predictable pattern. The correlation coefficients between initial and final reserves for the Upper Devonian horizon and the two Lower Devonian categories are 0.94, 0.97, and 0.95 respectively. This evidence supports our hypothesis.
If discoveries from wildcat drilling represent new information, and revisions of initial reserve estimates represent anticipated information, then the former should be an important determinant of wildcat drilling, and the
latter should not. To test this implication, we regressed the number of wildcat wells drilled in period t, , on two lags of itself and one lag of each of the following variables: annual discoveries, , annual discoveries per wildcat well, , annual revisions in reserves, , and annual revisions per development well, . If our hypothesis is correct, the set of coefficients on the lagged discovery variables should be significantly different from zero, and the coefficients on the lagged revision variables should not.
The estimation results for the base case, which are reported in Table A1, support the hypothesis. The F-statistics which tests the null hypothesis that the intertemporal correlations between wildcat drilling and the reserve revision variables are not significantly different from zero are equal to 0.689 for Lower Devonian and 0.162 for Agg\LoD. These figures indicate that the hypothesis can be maintained at the 99% confidence level. By contrast, the intertemporal correlations between wildcat drilling and the discovery variables are significantly different from zero at conventional significance levels.
We also estimated the equations on horizon data to verify that the results did not depend on our form of aggregation. The estimates for the Upper Cretaceous, Mannville, Mississippi and Upper Devonian horizons are reported in Table A2. (The Viking horizon was omitted since it contained virtually no oil pools.) Once again, there is no evidence that the reserve revision variables have any marginal explanatory power. Note that the evidence for a feedback effect of discoveries onto wildcat drilling is much weaker at this level of aggregation. The intertemporal correlations between the lagged discovery variables and wildcat drilling are generally not significantly different from zero at the 95% confidence level. One explanation of this result is that the horizon is not the appropriate decision environment.
TABLE 1 Cumulative Stocks of Wells and Reserves By Horizon
| Category | Expl. Period | Total NAG | Total AG | Total Oil | Wildcat Wells | Devel. Wells |
| Upper Cretaceous | 1953–79 | 53.9 | 0 | 170.4 | 1319 | 5733 |
| Viking* | 1950–79 | 88.7 | 24.3 | 11.8 | 1855 | 2970 |
| Mannville* | 1950–79 | 363.8 | 26.0 | 68.8 | 12733 | 12828 |
| Mississippi* | 1950–79 | 472.6 | 79.8 | 46.6 | 2427 | 2325 |
| Upper Devonian | 1947–79 | 252.2 | 111.1 | 553.0 | 4788 | 6326 |
| Lower Devonian | 1957–79 | 90.2 | 45.3 | 355.5 | 2816 | 2988 |
* Exploration in the Viking, Mississippi, and Mannville horizons began in the 1940's. However, 1950 is the first year for which annual data are available.
Means and Standard Deviations of Wildcat Drilling and Returns*
| Category | $x_t$ | $π_t$ | $π_t x_t$ |
| 1. Lower Devonian | 122.4(58.03) | .8000(2.279) | 47.373(80.06) |
| 2. Agg\Lower Devonian | 762.9(603.5) | .2339(.6811) | 66.119(201.2) |
| Mississippi | 80.90(74.11) | .2733(.7267) | 6.2403(18.25) |
| Mannville | 424.4(441.8) | -.03667(.0801) | -17.999(50.41) |
| Viking | 61.8(58.3) | -.0474(.0961) | -2.6701(5.680) |
| Upper Devonian | 151.7(48.2) | .3458(.9885) | 61.368(164.02) |
| Upper Cretaceous | 48.9(18.5) | 19.093(98.79) | 21.311(99.197) |
| 3. All Horizons | 856.7(632.1) | .2991(.6748) | 102.438(204.843) |
*Standard deviations are displayed in parantheses.
Instrumental Variable Estimates (2SLS) of Cost Parameters Base Case
| Indep. Variable | Agg\LD | Lower Devonian | ||
| U | R | U | R | |
| Constant | -57.54(-1.78) | -60.51(-1.90) | -29.2(-1.62) | -29.5(-1.64) |
| $x_{t-1}$ | 0.49(4.00) | 0.56(18.0) | 0.49(2.73) | 0.61(9.43) |
| $x_{t+1}$ | 0.59(5.45) | 0.53(18.0) | 0.71(3.60) | 0.58(9.43) |
| $\pi$ | 29.64(0.96) | 38.10(1.40) | 12.93(0.63) | 21.5(1.30) |
| $\alpha_1$ | 1.59(1.59) | 1.37(1.83) | ||
| $\alpha_2$ | -.0023(.135) | -.0086(-.86) | ||
| $\alpha_3$ | .0146(1.39) | .028(1.40) | ||
| $\delta$ | .95 | .95 | ||
| $R^2$ | 0.91 | 0.89 | 0.75 | 0.75 |
| SEE | 184.5 | 203.3 | 30.6 | 29.8 |
| Q | 8.16 (.881) | 9.45 (.801) | 3.54 (.968) | 4.71 (.91) |
| $T_1$ | .33 (.56) | .52 (.47) | ||
| $T_2$ | 8.81 (.18) | 9.09 (.17) | ||
| $T_3$ | 1465 (.00) | 234 (.00) | ||
| Period | 1950 - 79 | 1957 - 79 | ||
* t-statistics for the coefficients are displayed in parantheses. Q denotes the Box-Pierce statistic for serial correlation of any order. The number in parenthesis after the value of Q is its marginal significance level. T₁ is the chi-squared statistic for the hypothesis that β₂ = δ·β₁. T₂ is the chi-squared statistic for the overidentifying restrictions of the dynamic model, and T₃ is the statistic for the restriction that β₁ = β₂ = 0 (i.e., the static model). The numbers which appear in parenthesis after the chi-squared statistics are their marginal significance levels.
Instrumental Variable Estimates (2SLS) of Cost Parameters Classification of Pools by Geological Horizon
| Indep. Variable | Upper Cretaceous | Viking | Mississippi | Mannville | Upper Devonian | Lower Devonian |
| Constant | -15.0(-1.63) | -4.7(-.84) | -3.2(-.60) | 9.8(.29) | -85.6(-1.91) | -29.5(18.0) |
| $x_{t-1}$ | .66(7.01) | .53(8.26) | .54(16.6) | .55(19.7) | .82(4.99) | 0.61(.06) |
| $x_{t+1}$ | .63(7.01) | .50(8.26) | .51(16.6) | .52(19.7) | .78(4.99) | 0.58(.06) |
| $\pi$ | 1.26(.49) | -53.6(-1.54) | -1.8(-.25) | 970.5(1.82) | -.73(-.21) | 21.5(16.6) |
| $\alpha_1$ | 11.9(.64) | -0.087(-.97) | -1.76(.19) | -.01(.33) | 38.6(1.08) | 1.37(1.83) |
| $\alpha_2$ | -0.23(.38) | .0005(.25) | .03(.27) | -.00006(1.50) | -.27(.67) | -.0086(-.86) |
| $\alpha_3$ | 0.53(.52) | -.01(1.67) | -.30(.25) | .0005(1.67) | .38(1.00) | .028(1.40) |
| $\delta$ | .95 | .95 | .95 | .95 | .95 | .95 |
| $R^2$ | 0.63 | 0.68 | 0.96 | 0.94 | 0.57 | 0.75 |
| SEE | 9.0 | 35.8 | 14.8 | 110.6 | 35.1 | 29.8 |
| Q | 19.4 (.08) | 16.2 (.30) | 17.4 (.23) | 7.51 (.91) | 9.79 (.78) | 2.32 |
| $T_1$ | 5.0 (.03) | 1.02 (.31) | 5.7 (.46) | .08 (.78) | .002 (.96) | .52 (.47) |
| $T_2$ | 17.4 (.01) | 10.4 (.11) | 6.9 (.01) | 4.2 (.65) | 9.3 (.16) | 9.09 (.17) |
| $T_3$ | 104 (.00) | 657 (.00) | 963 (.00) | 1065 (.00) | 36.9 (.00) | 234 (.00) |
| Period | 1953-79 | 1950-79 | 1950-79 | 1950-79 | 1950-79 | 1957-79 |
t-statistics for the coefficients are reported in parantheses. Q denotes the Box-Pierce statistic for serial correlation of any order. The number in paranthesis after the value of Q is its marginal significance level. is the chi-squared statistic for the hypothesis . is the chi-squared statistic for the overidentifying restrictions of the dynamic model, and is the statistic for the restriction . The numbers which appear in paranthesis after the chi-squared statistics are their marginal significance levels.
\[\underline {{A 1}} ^ {*}\]
Feedback Effects of Discoveries and Reserve Revisions on Wildcat Drilling Base Case
| Independent Variable | Agg\LoDev Horizons | Lower Devonian Horizons | ||
| Constant | 92.6(1.40) | 97.7(1.24) | 49.6(2.32) | 31.3(1.10) |
| $x_{t-1}$ | 1.18(5.92) | 1.18(5.62) | .604(2.26) | .669(2.28) |
| $x_{t-2}$ | -.116(-.49) | -.104(-.42) | -.046(-.194) | -.019(-.063) |
| $Z_{t-1}$ | -34.8(-3.41) | -37.2(-3.26) | 2.43(2.07) | 2.16(1.77) |
| $a_{t-1}$ | 11826.3(3.35) | 12628.7(3.21) | -186.1(-1.72) | -167.8(-1.50) |
| $R_{t-1}$ | 3.83(0.56) | .702(.976) | ||
| $r_{t-1}$ | -3287.8(-.56) | -14.2(-.196) | ||
| $R^2$ | .921 | .922 | .698 | .725 |
| Q | 12.8(.54) | 13.6(4.8) | 8.73(.56) | 7.70(.65) |
| SEE | 185.1 | 192.3 | 33.0 | 33.7 |
| Period | 1950–79 | 1959–79 | ||
t-statistics for the coefficients are displayed in parantheses. Q denotes the Box-Pierce statistic for serial correlation of any order. The number of lags used in the computations is . The number in parenthesis below the value of Q is its marginal significance level. Marginal levels below .05 means that the null hypothesis of no serial correlation is rejected at the 95% confidence level.
TABLE A2* Feedback Effects of Discoveries and Reserve Revisions on Wildcat Drilling Individual Horizons
| Independent Variable | Upper Cretaceous | Mannville | Mississippi | Upper Devonian | ||||
| Constant | 24.3(2.14) | 24.7(2.03) | 80.5(1.56) | 59.1(1.05) | 9.87(1.35) | 8.63(.95) | 98.0(2.68) | 109.6(2.26) |
| $x_{t-1}$ | 1.03(5.36) | 1.06(4.75) | 1.39(5.14) | 1.35(4.83) | 1.11(5.31) | 1.12(5.06) | 1.04(4.29) | 1.07(4.26) |
| $x_{t-2}$ | -.453(-2.25) | -.478(-1.97) | -.42(-1.53) | -.32(-1.06) | -.135(-.60) | -.143(-.61) | -.733(-3.09) | -.818(-2.44) |
| $Z_{t-1}$ | -8.39(-1.61) | -8.93(-1.59) | -42.7(-1.02) | -97.1(-1.51) | -4.03(-1.53) | -4.13(-1.48) | -4.93(-1.08) | -5.36(-.95) |
| $a_{t-1}$ | 262.7(1.59) | 280.8(1.58) | 4016.3(.70) | 8311.2(.85) | 61.9(1.22) | 64.3(1.01) | 971.5(1.13) | 1025.6(.94) |
| $R_{t-1}$ | -.023(-.10) | -77.5(-1.13) | .384(.373) | .591(.37) | ||||
| $r_{t-1}$ | -7.58(-.18) | 9002.1(.75) | -3.88(-.21) | -144.6(-.73) | ||||
| $R^2$ | .597 | .601 | .911 | .916 | .925 | .926 | .564 | .582 |
| Q | 10.98(.53) | 10.48(.57) | 7.01(.93) | 6.14(.96) | 8.77(.85) | 7.36(.91) | 8.26(.87) | 8.70(.84) |
| SEE | 11.06 | 11.60 | 144.5 | 146.8 | 22.04 | 22.98 | 34.9 | 35.9 |
| Period | 1953–79 | 1950–79 | 1950–79 | 1950–79 | ||||
t-statistics for the coefficients are displayed in parantheses. Q denotes the Box-Pierce statistic for serial correlation of any order. The number of lags used in the computations is . The number in paranthesis below the value of Q is its marginal significance level.

FIGURE 2
