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  • the Slave Geological Province (SGP) is the richest and most promising mining region

    Applied Geography 25 (2005) 287307

    www.elsevier.com/locate/apgeogE-mail address: [email protected] (P. Deadman).Multi-criteria evaluation and least cost path

    analysis for an arctic all-weather road

    David M. Atkinsona, Peter Deadmanb,*, Douglas Dudychab,Stephen Traynorc

    aDepartment of Geography, Queens University, Kingston, Ont., Canada K7L 3N6bDepartment of Geography, University of Waterloo, Waterloo, Ont., Canada N2L 3G1

    cDepartment of Indian Affairs and Northern Development, Nunavut Regional Office, P.O. Box 2200, Iqaluit,

    Nunavut, Canada X0A 0H0

    Abstract

    Increasing interest in the development of the base metal, gold, and diamond resources in the Slave

    Geological Province in Nunavut has led to the proposal that a deep-water port be constructed in

    Bathurst Inlet and connected to these mining regions by an all-weather road. In response to previous

    concerns regarding the subjectivity of existing techniques for route determination, this paper outlines

    a methodology for determining a least-cost-path for the route of an all-weather road that incorporates

    multi-criteria analysis. This methodology allows for the objective comparison of alternate scenarios

    for weighting the factors that determine the location of a roads route. The methodology is applied,

    using three alternate scenarios for road construction that are compared so as to determine the

    effectiveness and sensitivity of this approach. The strengths and limitations of this methodology are

    discussed.

    q 2005 Elsevier Ltd. All rights reserved.

    Keywords: Multi-criteria evaluation (MCE); Pair-wise comparison; Least Cost Path; Artic; Route determination;

    GIS

    Introduction

    Covering approximately 190,000 km2 within Nunavut and the Northwest Territories,0143-6228/$ - see front matter q 2005 Elsevier Ltd. All rights reserved.

    doi:10.1016/j.apgeog.2005.08.001

    * Corresponding author.

  • within Canadas north (Reynolds, 1996). Diamonds, gold, and various base metals

    comprise the majority of mineral resources in the SGP. The region currently contains two

    operating mines, while over 25 diamond, gold, or base metal mining projects are in various

    stages of exploration or development (GNWT, 1999).

    Winter roads have been used for decades throughout Northern Canada as

    supply routes for temporary access to natural resources (Hayley & Valeriote, 1994).

    The seasonal, weather-dependant nature of ice roads can limit the economic viability

    of northern projects, especially base metal mining operations. Furthermore,

    climate change scenarios indicate that the arctic will experience significant warming

    (Serreze et al., 2000) this may reduce the length of the ice road season, placing

    further economic pressures on mining operations in the region. In response to this

    problem, proposals have been developed for the construction of a deep-water port in

    Bathurst Inlet, Nunavut and an all-weather road into the mining region around

    Contwoyto Lake, Nunavut (Fig. 1). An all-weather road would solve the problems

    associated with the existing ice road and increase the economic feasibility of many

    mining operations.

    While the construction of an all-weather road through this region of the arctic could aid

    in the economic development of the region, and the Canadian arctic more broadly, it also

    raises a number of concerns regarding the impacts on the fragile environment of the

    region. Clearly, the ability to understand and incorporate many complex factors into the

    design of a route for such a road is important. Any tool capable of incorporating multiple

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307288factors into the design, selection, and evaluation of alternate routes would be useful inFig. 1. Study site.

  • support of the decision making process. This paper presents a geographic information

    system (GIS) based methodology that combines least cost path (LCP) analysis on

    a continuous surface and multi-criteria analysis (MCA) to facilitate route generation based

    on multiple environmental and economic criteria. Weights for the route criteria are

    generated though a pair-wise comparison of criteria based on three decision-making

    scenarios (Fig. 2).

    The methodology presented allows the exploration of a variety of scenarios in an

    effort to strike a balance between development and the protection of the environment.

    The ability to model the routing of such a road could not only reduce the costs of

    construction and maintenance but also allow for sensitive environmental areas to be

    avoided and protected.

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 289Fig. 2. Flow diagram of the least cost path algorithm.

  • The study of the least-cost path problem predates the development of modern GIS.

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307290Some of the earliest work came from Warntz (1957) who considered where a good must be

    transported over two broad regions, each with a different cost of transportation.

    There are a number of basic steps in finding a minimum cost path over a surface

    partitioned into regions of different resistances to movement (Collischonn & Pilar, 2000;

    Douglas, 1994) (Fig. 2):

    A friction surface is created for each evaluation criterion, where each cell in the grid isassigned a value based on the relative cost of traversing that cell.

    Multiple friction surfaces are weighted and combined to create a cost-of-passagesurface, representing the total cost associated with traversing each cell.

    A spreading function combines two separate grids representing source points anddestination points are combined with the cost-of-passage grid to calculate an

    accumulated cost surface.

    The lowest cost line is traced down the accumulated-cost-surface from a departurepoint to a destination.

    The resulting path is considered optimal for all criteria considered (Lee & Stucky,

    1998).

    The use of least-cost path analysis for real world problems has become possible with

    the development with todays fast and powerful computers (Lee & Stucky, 1998). ThereCold region road construction

    Many of the factors influencing the routing of an all-weather haul road in the arctic are

    determined by cold region design and construction standards and techniques. Factors that

    influence the performance of an arctic all-weather road include; climate, hydrology,

    topography, geology, vegetation, material availability and suitability, and the soils

    thermal state (Schraeder, Riddle, & Slater, 1996). The continuous permafrost is a

    controlling design parameter when working in this region. The permafrost must either be

    preserved (prevented from thawing) or completely removed (McFadden & Bennett, 1991).

    Drainage is one of the most important considerations even though precipitation is low.

    Pooled water can quickly alter the thermal regime of the underlying soils, increasing the

    risk of damage to the road. The largest threat to a road embankment in cold regions is the

    stability of the underlying soils. Even if the embankment itself is stable it may suffer

    damage if its level of support from underlying soils changes. The richer the ice-content,

    the thicker the embankment design will need to be. It is desirable to obtain gravel of the

    requisite quality and quantity and keep the haul distance to a practical minimum. A good

    clean gravel embankment makes a very good foundation in a very cold environment where

    it is possible to contain the zero degrees Celsius isotherm within the embankment

    (Schraeder et al., 1996).

    Least cost path analysishave been several recent applications of least-cost path methodologies which involve:

  • Multi criteria evaluation

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 291When using least-cost path analysis to determine route alternatives, the perceived

    importance, or weight, of each criterion will directly affect the routing outcome.

    Therefore, a process to determine the relative importance of criteria is required. This

    process is known as multi-criteria evaluation (MCE). The decision about which route

    alternative to select would be defined as a multi-objective decision (Eastman, 1999). An

    objective is understood here to imply a perspective, philosophy, or motive that guides the

    construction of a specific multi-criteria decision rule. In the case of routing an arctic road,

    the objective of a mining company might be economical construction, whereas the

    objective of an environmental group would likely be environmental protection. The

    criteria they consider, and the relative importance of these criteria, will likely be quite

    different. Each party faces the challenge of assessing and clearly articulating the relative

    importance of the criteria influencing the decision.

    Multi-criteria evaluation requires the determination of the importance, or weight, of

    each criterion to the decision making process as a whole. Within the context of multi-

    spatial-criteria evaluation, Rao et al. (1991) state that a logical process for the

    development of such weights is the procedure of pair-wise comparisons developed by

    Saaty (1977). The procedure outlined by Saaty (1977, 1980) rates the importance of each

    factor, or criterion, relative to every other factor using a 9-point reciprocal scale. Fig. 3

    shows the 9-point rating scale developed by Saaty (1977).

    If, for example, we were comparing factor I with factor J and were to state that factor Iselecting the fastest path with the least slope based on elevation data (Stefanakis &

    Kavouras, 1995); selecting the best route for a pipeline based on land use and land cover

    data (Feldman, Pelletier, Walser, Smoot, & Ahl, 1996); selecting the cheapest route to

    transport commodities based on land use and topographic data (Jaga, Sundaram, &

    Natarajan, 1993). Now, the computation of least-cost paths is considered the most useful

    tool available for determining the optimal path from one or more origin points to one or

    more destination points (Lee & Stucky, 1998). The methodology for the calculation of an

    accumulated-cost surface is well documented in commercial GIS packages and in

    Collischonn and Pilar (2000); Douglas (1994), and Lee and Stucky (1998). What is lacking

    in many of the methodological discussions is how to appropriately weight and combine

    factors to create suitable cost-surfaces and how to incorporate differing weighting

    scenarios and differing points of view in the routing process.

    Often activities such as the selection of an appropriate route between two points are

    undertaken by an individual or a small group. In such a process, outcomes can be

    influenced by personal bias toward certain objectives or the inconsistent application of the

    project criteria to the route study area (Motemurro, Barnett, & Gale, 1998). Routes for

    features such as roads, railways, or pipelines are often constrained by physical,

    environmental, political, social, economic, and regulatory factors. A system that can

    optimize relationships among these factors and identify trade-offs can produce a wide

    range of alternatives (Montemurro et al., 1998).was very more important than factor J then a value of 7 would be placed in an n!n matrix

  • of ratings (where n is the number of factors being considered). The reciprocal of that rating

    would be 1/7 meaning that J is very less important than I. The number of factor

    comparisons can be determined using the following formula.

    Fig. 3. Nine point reciprocal scale developed by Saaty (1977).

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307292Comparisons ZnnK1

    2(1)

    Let us suppose that there are three (3) criteria A, B, and C. In this case three (3)

    comparisons are required to complete a 3!3 matrix Y, according to the previous formula.The three statements, and the resulting comparison matrix based on Saatys 9-point scale,

    are shown in Fig. 4.

    Saaty (1977) has shown that the principal eigenvector of the comparison matrix

    represents a best-fit set of weights. In pair-wise comparison, consistency within

    comparisons is important. Saaty (1980), states that a consistency ratio (CR) of 0.10 or

    less is considered acceptable. The CR value is the probability that the weights are random.

    The principal eigenvector corresponding to matrix Y is seen in vector W shown in Fig. 5

    along with the consistency ratio.

    In a general sense, a GIS model can be thought of as the process of combining a set of

    input maps with a function to produce an output map (Bonham-Carter, 1994). For this

    paper, the combination of factors represents the creation of the cost surface for least-cost

    path analysis. There are a number of models for combining maps together including

    Boolean operations, index overlay, and fuzzy logic. The Boolean model takes a strict

    binary (true or false) approach to a problem, while the greatest disadvantage of the index

    overlay is its linear additive nature. Both Eastman (1999); Bonham-Carter (1994),

    suggest that a fuzzy logic approach is in many ways similar to the index overlay methodFig. 4. Criteria comparison statements, and the resulting reciprocal matrix.

  • D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 293but offers a more flexible set of combination options and improves on the linear additive

    nature of the index overlay model.

    In classical set theory, set membership is defined as true or false, 1 or 0. Membership in

    a fuzzy set is expressed on a continuous scale from 1 (full membership) to 0 (full non-

    membership). Fuzzy membership values can be applied to categorical, ordinal, or interval

    variables. As long as fuzzy membership values lie within the range of 0 and 1 there are no

    practical constraints on the choice of fuzzy membership values (Bonham-Carter, 1994).

    Yager (1977) established that raising a fuzzy set by the power of its weighted eigenvalue,

    derived from Saatys pair-wise comparison technique for developing criteria weights, was

    a good method for adjusting fuzzy sets to reflect their relative importance prior to

    combining fuzzy membership functions. Yager (1977); Bonham-Carter (1994), and

    Zimmerman and Zysno (1980) all show that fuzzy sets provide very useful tools to

    investigate multi-criteria decision problems. One reason for this is that fuzzy sets provide a

    mathematical structure for manipulating and evaluating vague ideas that can become very

    complex (Yager, 1977). What is important is that the idea of comparing the criteria as to

    their importance incorporates an ability to account for trade-offs between criteria.

    Furthermore, the power of each criterion that is included in the model corresponds to a

    hierarchical structure in the sense that various experts can evaluate each fuzzy set and then

    these can be combined to create a result based on all criteria.

    As an example of a fuzzy membership we can examine the degree of membership in the

    set defined as suitable locations for a road. Let us consider a siting of a road in relation to

    a stream, where it is more desirable to be further from the stream to a maximum of 60 m;

    the stream is defined as 010 m. The fuzzy values for positions start to rise above 0.0

    immediately at the stream boundary (10m) and approach a value of 1.0 at the 60 m mark.

    Further distance does not increase the value since the distance is far enough to not affect

    the stream or the road. Such a membership function might be expressed as in Fig. 6 along

    with its accompanying graphical representation of that linear function.

    In this example, X is the distance in meters and x(x) is the fuzzy membership function.The ordered pairs (X, x(x)) are known as the fuzzy set (Bonham-Carter, 1994). According

    Fig. 5. Eigenvector produced from the comparison matrix with consistency ratio.to Bonham-Carter (1994), the shape of fuzzy membership function need not be linear; it

    can take any analytical or arbitrary shape appropriate to the problem, and can be expressed

    as a continuous surface, lists, or tables of numbers. One must be aware that when

    discretisizing continuous data some data may be lost in the generalization.

    Previously we developed a set of weights for three criteria A, B, and C (Fig. 4). Let us

    now assign a fuzzy membership value to each of those criteria. Within each criterion there

    are four classes, each of which has an assigned fuzzy value (Table 1). These values are

    derived from an example given in Yager (1977).

  • D.M. Atkinson et al. / Applied Geography 25 (2005) 287307294Yager (1977) states that the first step is that the unit eigenvector W needs to be scaled.

    The reason for this is that if all the criteria were equal then the there would be no effect on

    the fuzzy values entering the decision function. Each fuzzy set is then raised by the power

    Fig. 6. Fuzzy membership function and graph for stream data.of its scaled eigenvalue. The scaled values for the three criteria are shown in Table 1. This

    scaling procedure means that important criteria are exponentially weighted heavy forcing

    them into the decision process while small values tend to make the membership value

    smaller which effectively takes them out of the process (Yager, 1977).

    Zimmermann (1985) discusses a variety of fuzzy logic combinations such as the fuzzy

    algebraic product, the fuzzy algebraic sum and the fuzzy gamma operator. The fuzzy

    Table 1

    Fuzzy values, and scaled fuzzy values, assigned to each criterias four subclasses

    Fuzzy Values Criteria

    Class A B C

    1 0.5 0.5 0.2

    2 0.7 0.4 0.1

    3 0.3 0.8 0.6

    4 0.6 0.4 0.9

    Scaled fuzzy values Criteria

    Class A0.48 B1.77 C0.75

    1 0.72 0.29 0.3

    2 0.84 0.2 0.03

    3 0.56 0.67 0.2

    4 0.78 0.2 0.92

  • degree of increasive or decreasiveness that is desired for a given solution. An

    increasive solution includes more trade-offs creating more possible solutions, though

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 295they may not be ideal, while a decresive solution remains more rigid to the rule

    structure. In the case of selecting a y value for least-cost path analysis a low value

    (yZ0) can result in a path that has effectively removed the distance element to therouting and relies more on cell weights to determine the route. This could result in a

    very sinuous path. Selecting a high y (yZ1) could result in a path that minimizes thedistance between two points and produce a straight path that ignores factors other than

    distance.

    Methods

    The study area for this project is a large section of the Barren lands within the

    boundaries 65678N, and 1061128W. Previously proposed routes for an all-weather roadrun from the proposed port at Bathurst inlet to the area around Contwoyto lake (Fig. 1).

    The regions climate is classified as arctic tundra. The entire region is underlain with

    continuous permafrost (Natural Resources Canada, 1995), with an active thaw layer of

    about 0.51 m (Judge, Taylor, Burgess, & Allen, 1981).

    The methodology utilizes a GIS to prepare, weight, and combine construction

    factors. Actual construction costs are not included in this model as those values were

    unobtainable, and the assignment of monetary costs to environmental factors is beyond

    the scope of this paper. Instead a multi-criteria decision making methodology of pair-

    wise comparisons is used to determine factor weights for three scenarios, an

    environmentally sensitive scenario, a strict engineering scenario, and a comprehensive

    scenario. These scenarios are based on subjective knowledge driven concepts. A

    detailed description of the weighting methods along with any assumptions made will bealgebraic product combines fuzzy memberships through multiplication. This model is

    decreasive since the output value is always less than or equal to the smallest fuzzy

    membership. The fuzzy algebraic sum is complementary to the algebraic product. Unlike

    the algebraic product, the algebraic sum is always greater than or equal to the largest

    contributing fuzzy membership value. This creates an increasive effect although the output

    is limited to a maximum value of 1.0. The final combination operator is, in essence, a

    combination of the previous operators. The Gamma operation utilizes the algebraic sum

    and the algebraic product in the following formula

    Gamma Z Algebraic sumyAlgebraic product1Ky (2)The y is a parameter chosen in the range (0,1). When the y is 1, the combination is

    the same as the algebraic sum, while when y is 0 the combination is the same as the

    algebraic product (Bonham-Carter, 1994; Zimmerman & Zysno, 1980). According to

    Bonham-Carter (1994), a judicious choice of y produces output values that ensure a

    flexible compromise between the increasive fuzzy algebraic sum and the decreasive

    effects of the fuzzy algebraic product. The selection of y is arbitrary and based onoutlined.

  • Construction factors

    The ultimate purpose of this methodology is to combine spatial data from diverse

    sources, in order to create a cost-of-passage surface that can be analyzed through least-cost

    path analysis to generate route alternatives, based on a series of factor scenarios. One of

    the initial steps is to identify the input factors that can be generated from the available data.

    Though there are many factors that can influence the routing of a cold region road, this

    methodology only examines factors for which spatial data were collected or readily

    available. Cost factors for this methodology will be classified into two categories,

    engineering factors, and environmental factors. Each category has what could be viewed

    as a set of objectives, accompanying those objectives are spatial data inputs that would

    accomplish them. Table 2 outlines both the engineering and environmental objectives and

    their associated spatial data.

    For a least-cost path algorithm to be applied, the vector data were converted to

    raster format with a cell size of 20 m. This resolution was considered an acceptable

    trade-off between processing time, with increased number of cells, and the detail for

    small landscape features. Extensive pre-processing for each factor was required to

    prepare it for inclusion in a least-cost path analysis. For further discussion, see

    Atkinson (2003)

    Table 2

    Scenario criteria and associated data processing

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307296Engineering goals Spatial data Data source Pre-processing

    Avoid bodies of water Lake locations NTS 1:250 K Boolean Clip 20, 40,

    60 m

    Minimize stream

    crossing

    Stream buffers NTS 1:250 K Boolean Clip 20, 40,

    60 m

    Maximize construction

    on low ice content

    surficial material

    Surficial Material

    Classifications

    Satellite derived

    classifications

    (Orazietti, 2003)

    Clipped to study area

    Maximize proximity to

    aggregate sources to

    minimize haul distance

    Esker and rock locations

    and Haul costs

    Esker databaseb

    (WKSS, 1999)

    Spreading function for

    haul costs

    Maintain low grade

    (Slope)

    Slope maps NTS 1:250K DEM

    Avoid bodies of water Lake locations NTS 1:250K Boolean clip 20, 40,

    60 m

    Avoid stream crossing Stream buffers NTS 1:250K Boolean clip 20, 40,

    60 m

    Avoid sensitive soils Surficial material

    classifications

    Satellite derived

    classifications

    (Orazietti, 2003)

    Clipped to study area

    Avoid sensitive wildlife

    and cultural sites

    Wolf den and archaeo-

    logical site buffers

    Esker database

    (WKSS, 1999)

    Spreading funciton

    2501000 m

  • Factor weightings

    For reasons outlined previously, each factor will be defined in terms of a fuzzy

    membership function. Traditionally, fuzzy membership functions are expressed on a

    continuous scale from 1 (full membership) to 0 (full non-membership). Fuzzy map values

    are defined according to a given spatial locations degree of membership in a set. In this

    methodology the values for each factor map are assigned a fuzzy membership value based

    on their degree of membership in the set suitable for a road. For example, the fuzzy set

    for surficial material is based on the suitability of different materials for road construction.

    Rock provides a solid base for a road so has a high degree of membership in the set

    suitable for a road while deep till requires a thicker roadbed to protect the underlying

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 297permafrost so has a lower degree of membership in the suitable for a road set. For the

    least cost path analysis, the polarity of the fuzzy membership function is reversed so that

    values closer to 0 indicate stronger membership in the suitable for a road set. This is

    necessary because the least cost path algorithm interprets the cell values as costs.

    Reversing the polarity of the fuzzy membership function assigns lower cost values to cells

    that are more suitable for a road.

    The fuzzy values reflect the degree of membership in the suitable for a road set and

    are based on information gathered through a literature review of expert knowledge.

    Subjective judgment was required to translate qualitative information from the literature

    into quantitative fuzzy membership values.

    A detailed discussion of how the costs for each factor were developed is beyond the

    scope of this paper. However, the considerations surrounding each factor are briefly

    discussed below. The surficial material factor is based on the fact that lower ice content

    materials, such as rock and thin till, do not require a thick road base and are less prone to

    permafrost degradation. For this reason they are better materials to build a road on and thus

    given a fuzzy value closer to zero. Table 3 summarizes the attribute values and

    corresponding fuzzy membership values for this criterion.

    The maximum slope for the road is 8%. This methodology does not account for cut and

    fill construction techniques and is looking to find the route that follows the lowest natural

    slope. For this reason it was decided to eliminate all areas of slope greater than 10%.

    Table 3

    Attribute data and fuzzy values for the surficial material factor

    Surficial material

    Legend Class Fuzzy

    Unknown water 1 0.9

    Gravel 2 0.1

    Organic 3 0.7

    Rock 4 0.1

    T1 5 0.1

    T2 6 0.3

    T3 7 0.5

    Unknown/cloud 8 0.4

    Bridge 9 0.1

  • from the stream) was used to determine the decreasing fuzzy values to a maximum of 60m

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307298after which a fuzzy value of 0.1 was assigned to all distances greater than 60 m.

    mx ZK0:0075x C1:05 (4)For the Archaeological and Wolf Den sites it was decided that areas within 250 m of the

    site were to be eliminated from analysis to insure that no route would enter such an area.

    Using a distance function and the following formula the fuzzy values were determined to

    the maximum distance of 1 km after which the lowest value of 0.1 was assigned

    mx ZK0:0008x C0:9 (5)Construction of a road in this region depends upon access to local aggregate sources.

    Access to these sources will most likely require the further construction of access roads to

    link the main road construction with the aggregate source. The designs of these access

    roads also form an interesting least-cost path problem that is not within the scope of this

    paper. Some understanding of haul cost is required to ensure that the main road is

    constructed to minimize haul distances. The esker and rock haul distance factor was

    created using a cost surface and a spreading function. Further details on the creation of this

    factor can be found in Atkinson (2003).

    Least cost path scenarios

    To outline how this methodology allows the factors discussed above to be combined in

    different ways, three decision scenarios were examined. Each scenario placed a differing

    level of importance on the different factors. The scenarios result in different factor weights

    and thus generate three cost-of-passage surfaces and least cost paths. The three scenarios

    were developed to approximate an engineering based approach to routing a cold-region

    road, an approach where more importance was given to environmental factors, and finally

    an approach representing a compromise between the engineering and environmental

    scenarios. Within each scenario factors deemed unnecessary to the location of a road were

    given a weight of zero. The non-zero weight factors were weighted using Saatys paired

    comparison technique. The comparisons were made using IDRISI 32s WEIGHT moduleContinuous fuzzy values were derived by processing the slope data with the following

    linear equation where x is the percent slope.

    mx Z 0:099x (3)Steep regions, with a slope between 9 and 10% were given the highest values of 0.89

    and 0.99 this creates the possibility that some slopes in this range may be crossed by the

    path but the higher value will limit them.

    The stream distance factor acknowledges that crossing streams is necessary in road

    construction but the ideal is to minimize crossings and approach them at right angles if

    possible. Furthermore, if a stream is not to be crossed, the road should travel at least 60 m

    away to minimize disturbances or contamination. The stream location was given a fuzzy

    value of 0.9 away from that the following linear formula (where x is the distance awaywhich also output the eigenvalues for each factor along with the consistency ratio. As

  • Table 4

    Comparison matrix with eigenvalues and scaled map weights for the (a) engineering scenario (b) environmental scenario and (c) compromise scenario cost factors

    (a) Surficial Esker Dist Rock Slope Streams Eigen vector Eigen!5

    Surficial 1 0.4714 2.357

    Esker Dist 1/3 1 0.2303 1.1515

    Rock 1/4 12 1 0.1549 0.7745

    Slope 1/4 1/3 1/3 1 0.099 0.495

    Streams 1/7 1/5 1/3 1/4 1 0.0444 0.222

    Wolf site N/A 0

    Arc site N/A 0

    Consistency 0.06 Sum 1 5

    (b) Surficial Esker Dist Rock Slope Streams Wolf Arch Eigen vector Eigen!7

    Surficial 1 0.1491 1.04

    Esker dist 1/5 1 0.0573 0.40

    Rock 1/6 1/2 1 0.0436 0.31

    Slope 1/3 1/2 1/2 1 0.0556 0.39

    Streams 2 4 5 2 1 0.2046 1.43

    Wolf site 3 5 6 3 1 1 0.2449 1.71

    Arc site 3 5 6 3 1 1 1 0.2449 1.71

    Consistency 0.07 Sum 1 7

    (c) Surficial Esker Dist Rock Slope Streams Wolf Arch Eigen vector Eigen!7

    Surficial 1 0.3119 2.1833

    Esker dist 1/3 1 0.1831 1.2817

    Rock 1/4 12 1 0.1376 0.9632

    Slope 1/3 12 1/2 1 0.1269 0.8883

    Streams 1/3 1/3 1/2 1/3 1 0.0883 0.6181

    Wolf site 1/2 1/2 1/2 1/2 1/2 1 0.0761 0.5327

    Arc site 1/2 1/2 1/2 1/2 1/2 1 1 0.0761 0.5327

    Consistency 0.07 Sum 1 7

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  • previously mentioned, the eigenvalues were multiplied by the number of non-zero-weight

    factors to obtain scaled eigenvalues which then were used to exponentially weight each

    factors fuzzy value (Yager, 1977). The location of water bodies was included in each

    scenario as a Boolean clip to the surficial material dataset. Each scenario had a hard rule

    for the distance from a lake that the road could be located. The lake locations along with a

    20, 60, and 40 m buffer were classed as a no-data barrier for the engineering,

    environmental, and comprehensive scenarios, respectively. This Boolean operation is

    analogous to a group requiring that specific land parcels be off limits to development.

    For the Engineering scenario only five factors were evaluated with non-zero-weights.

    These factors are surficial material, esker distance, rock distance, slope, and streams. Wolf

    surfaces. A YZ0.7 is slightly increasive but generates outputs that lie slightly above the

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307300initial rage of values. This value is a good balance between the routing factors and desire to

    minimize the total distance of the route. A cost surface was generated for each scenario

    representing the combined frictions of the weighted factors for each cell within the study

    area. These final cost surfaces were then used to generate paths.

    The accumulated-cost-surface (ACS) was generated by treating the proposed port as the

    destination location and then using a spreading function to sum the costs of movement

    away from that destination. To generate paths from the ACS, all that was required was

    Table 5

    Scenario weights for each input factor

    Factor Engineering weight Environmental weight Comprehensive weight

    Surficial 2.357 1.04 2.1833

    Esker dist 1.1515 0.40 1.2817

    Rock 0.7745 0.31 0.9632

    Slope 0.495 0.39 0.8883

    Streams 0.222 1.43 0.6181

    Wolf site 0 1.71 0.5327

    Arc 0 1.71 0.5327

    Sum 5 7 7den sites and Archaeological sites were given a weight of zero. Ten comparisons are made

    using the 9-point scale discussed previously. The Environmental scenario evaluated seven

    non-zero factors: surficial material, esker distance, rock distance, slope, streams, wolf den

    sites and Archaeological sites. The final scenario, the comprehensive scenario, also

    considered all seven factors as non-zero weights in the factor comparisons. Twenty-one

    comparisons are made using Saatys scale. The matricies of comparison values for each

    scenario are shown in Table 4.

    Least cost path modeling

    All spatial data analysis was undertaken using ArcGIS. The factor grids were

    exponentially weighted using the weights shown in Table 5, and the fuzzy product and

    fuzzy sum of the resulting weighted grids were calculated. The fuzzy product and fuzzy

    sum grids were combined in a Gamma operation (YZ0.7) to produce the final cost

  • a starting location, in this case Lupin Mine, to then trace a least-cost line back to the

    destination.

    Results

    Three routes were created through the least-cost path analysis, one for each weighting

    scenario. Fig. 7 shows the northern sections of the study area with the three generated

    routes and a fourth route that was proposed by the Government of the Northwest

    Territories (GNWT) in 1999. The GNWT route, known as Route I, was determined

    through an air photo analysis. The figure shows the locations and size of esker deposits,

    wolf dens. Archaeological sites have been omitted from the map due to protective

    legislation.

    Within this route there are three areas where variation in route location occurs. These

    three areas (1, 2, and 3) will be used to better compare these routes. Area 1 can be seen in

    Fig. 8, area 2 in Fig. 9 and area 3 in Fig. 10.

    Within area 1 the study area is rather confining for the routes. All three routes follow

    very similar paths from Lupin west and then north towards the Contwoyto lake crossing

    point. Aggregate sources are scarce in this area and so do not influence the path of the

    route. There is a cluster of archaeological sites in the northern section. The Engineering

    route bisects this cluster while the Comprehensive route travels around the cluster to

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 301Fig. 7. Least-cost paths from the proposed port on Bathurst inlet to Lupin mine.

  • D.M. Atkinson et al. / Applied Geography 25 (2005) 287307302the west. Route I, the GNWT route, follows a similar route to the LCP routes, though it

    takes a much wider curve around the western Contwoyto bay, and, like the Engineering

    Route, bisects the cluster of Archaeological sites.

    Area 2 shows much more variation in route location. There are only a few

    archaeological sites or wolf dens in the data for this area; they are located in the north,

    and so have little effect on the LCP routes. The Engineering route is pulled further south in

    this area by the aggregate deposits, then curves north again meeting up with the

    comprehensive route. Route I takes northern course, coming close to some archaeological

    sites, but is further from some larger aggregate deposits.

    Area three has the LCP routes again following a very similar path, yet it is quite

    different from route I. The LCP routes travel in a steady northeast route towards the port,

    while route I travels due east quite a distance then curves north. Again this area does not

    show many Archaeological sites, however there are a few Wolf dens near the port. Route I

    appears to run closer to some esker deposits in the eastern portions of the area, yet they are

    mostly small eskers that would not provide much aggregate.

    Stream crossings

    The number of stream crossings on a route can directly affect the cost of construction as

    well as the environment. The engineering route crosses the most streams with 93

    Fig. 8. Lupin least-cost paths in sub-area 1.

  • D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 303crossings, while the environmental route, which had streams with a larger criteria weight

    from the scenario comparisons, crosses far fewer at 77. The Comprehensive route crosses

    82, which is very similar to Route I, which crosses 84.

    Aggregate volume

    The volume of aggregate required to construct a given route is dependant upon the

    underlying surficial material. The LCP routes and Route I have been examined in terms

    of their underlying surficial geology. Route I values have been taken from Orazietti

    (2003) who analysed all proposed routes in terms of aggregate. All routes are very

    close in overall length, including Route I, approximately 300 km in length. The lengths

    of road segments for each surficial geology type do vary. The largest difference is that

    Route I has 23% of its route traveling over thick, ice-rich till and 7% on organic soils

    which require thicker embankments to stabilize the underlying permafrost, compared to

    2% and 1% respectively for the LCP routes. The majorities of LCP routes are on thin

    till veneer (54%) and rock (30%), which require much less aggregate to prevent

    permafrost degradation. These lengths make a significant impact on the volume of

    aggregate required to construct the routes, when these least cost paths are compared to

    previously proposed routes in terms of aggregate requirements there is a 20% reduction

    in the required aggregate.

    Fig. 9. Lupin least-cost paths in sub-area 2.

  • D.M. Atkinson et al. / Applied Geography 25 (2005) 287307304Discussion

    Criteria evaluation

    Schraeder et al. (1996), and McFadden and Bennett (1991) all illustrate the importance

    of construction factors. What is not stated is the quantified importance of each of these

    factors, although certain criteria are emphasized. Personal bias toward certain objectives

    and inconsistencys can often result when criteria importance is guided by an individual or

    a small group (Montemurro et al., 1998).

    The criteria for the methodology were selected criteria based on the engineering

    literature, environmental principles, and the availability of spatial data. A mathematical

    structure for manipulating, evaluating and combining, road routing criteria is provided

    through the use of Saatys multi-criteria evaluation (MCE) method of pair-wise

    comparisons, along with the methods of weighting and combining fuzzy sets presented

    by Bonham-Carter (1994); Yager (1977). What has been illustrated is the idea that

    comparing the criteria, as to their importance in selecting a route, incorporates an ability to

    account for trade-offs. Second, the weight of each criterion corresponds to a hierarchical

    structure, in the sense that each fuzzy set can be evaluated by various experts, and these

    can then be combined to create the resulting cost surface and thus that experts least-cost

    path. The criteria comparisons and thus weights that were generated through the three

    Fig. 10. Lupin least-cost paths in sub-area.

  • scenarios, engineering, environmental, and comprehensive, were based on subjective

    decisions derived from the knowledge base within the literature. Although the actual

    weightings for a given scenario may be inaccurate, due to the subjective nature of the

    comparisons, the use of differing scenarios, which took different views, compensates for

    this. What is important is that this methodology of MCE provides a mathematical structure

    to ensure that criteria are evaluated equally across the study area and not subjectively

    within the study area.

    Route determination: LCP versus traditional approaches

    The traditional methodology that was used to produce the previously proposed routes is

    that of Terrain Unit Mapping using non-digital black and white air photos and maps

    (GNWT, 1999). Terrain units were evaluated by strictly using these data sources, no

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307 305fieldwork was undertaken. The GNWT routes were determined based on the criteria

    outlined in Table 6.

    The methodology for the previously proposed routes was subjective and qualitative.

    The use of a GIS and most importantly LCP analysis provides a methodology for a less

    subjective and more quantitative analysis. The power of GIS and LCP comes not only

    from the ability to store geographic data, but also from the ability to analyze it more

    efficiently and more conveniently than is possible with paper maps (ESRI, 2000). The LCP

    analysis combines and analyzes all of the spatial criteria to produce a cost surface for the

    entire study area. The LCP analysis examines a variety of data over a large area relatively

    quickly and is consistent in its evaluation of criteria to find the least-cost path based on the

    given data.

    Strengths and limitations

    A prime strength of this methodology is that it can be applied to routing applications for

    a variety of study areas and differing criteria can be compared and weighted to produce

    alternative routes. What is needed to apply this methodology to other locations

    Table 6

    Route selection criteria outlined by the GNWT

    Criteria Implications

    Topography Route selection should have little to no right-of-way excavation; embankment

    construction should average 0.51.5 m in thickness

    Bedrock surface Route location should follow glacier-smooth surfaces with micro relief of 1.0 m

    Lakes Vertical and horizontal alignment considerations

    River crossings Route should minimize river crossings and locate crossings that are narrows and

    on suitable foundation conditions

    Wet organic terrain Route locations should avoid seasonally wet or permanent organic terrain

    wherever practical

    Granular borrow sites Route location should consider location, volume and composition of potential

    sources (i.e. esker complexes)

    Permafrost Not considered a major factor in route location as entire area is a zone of

    permafrost

  • many factors as possible; there is a gap in available data for the region. Some examples of

    missing data, that may have proved useful include, snowdrift data, caribou migration data,

    D.M. Atkinson et al. / Applied Geography 25 (2005) 287307306and more detailed wildlife studies. An additional factor, that was not included, that could

    play a role in the routing of this all-weather road is the locations of known mineral deposits

    and their potential for development. This data was not available but could create a heavily

    weighted factor that could pull the road in the direction of the potential mine.

    The scale of the data is another limitation. At the time of the project computer-

    processing power did not permit data at a finer scale. At the resolution that these grids were

    created their file size was rather large requiring several gigabytes of storage to allow for

    the data management and processing. If data at a larger scale was available, the file size

    may be prohibitively large, and inhibit processing.

    Other challenges exist with the pair-wise comparisons and determination of fuzzy

    values. The comparisons that were used in this project were based on subjective,

    knowledge-based judgments, but may not represent the opinions of an expert although the

    methodology permits the flexibility of using expert opinion. Another issue may be how to

    compare criteria that cannot easily be compared. Physical properties of a factor are

    difficult to compare to emotions or ideologies.

    This project has contributed to our understanding of how pair-wise comparisons and

    fuzzy data sets can be used within a GIS and LCP analysis to determine possible routings

    of an arctic all-weather road. Ideally the methodology will provide a framework for further

    research and provide alternatives to the previously proposed routes. With some further

    refinement, the methodology could be used by developers and decision makers with

    increased expert knowledge to create other routing alternatives. As better data becomes

    available, along with increased digital storage and processing capabilities, improved

    routes can be generated for this project and other routing applications.

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    Multi-criteria evaluation and least cost path analysis for an arctic all-weather roadIntroductionCold region road constructionLeast cost path analysisMulti criteria evaluationMethodsConstruction factorsFactor weightingsLeast cost path scenariosLeast cost path modeling

    ResultsStream crossingsAggregate volume

    DiscussionCriteria evaluationRoute determination: LCP versus traditional approachesStrengths and limitations

    References