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        ---- Utilize components of the “SoLIM” approach to help assist 
        in the development and evaluation of a computer generated-landscape model 
        that captures existing soils and environmental knowledge, creates data 
        layers for input into a GIS, and produces raster and vector maps suitable 
        for used in soil survey, as well as providing the potential for the use 
        of “fuzzy soil logic” in the development of “soilscape-based” 
        soil interpretations. 
         
        ---- Evaluate these procedures and products as to their applications with 
        the National Cooperative Soil Survey, as well as within the National Park 
        Service and the Natural Resources Conservation Service. In particular, 
        assess the adoption of these techniques for mapping soil resources over 
        areas that are not easily accessible for field observation. 
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       SoLIM 
        stands for “Soil Land Inference Model”. It is a fuzzy inference 
        scheme for estimating and representing the spatial distribution of soil 
        types in a landscape. There are four key components included in this framework: 
        (1) Soil-Landscape model: The knowledge on the relationships between the 
        soil series and their surrounding environmental variables can be obtained 
        from soil experts using a set of knowledge acquisition techniques. 
        (2) GIS Database: The soil formation environmental database of an area 
        can be characterized and represented using GIS and RS techniques. 
        (3) Inference Engine: A set of computer programs under fuzzy logic used 
        to estimate and predict the spatial distribution of soil types in a landscape 
        based on Soil-Landscape model and GIS database. 
        (4) Fuzzy Representation: A Similarity Vector Model to represent soil 
        as continuum. 
         
         
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      Our 
        study area is three quadrangles in the Great Smoky Mountains National 
        Park, which straddles the boundary between North Carolina State and Tennessee 
        State. In phase I, we worked on Mt. Guyot quadrangle and in phase II, 
        we worked on Mt. LeConte quadrangle and Clingmans Dome quadrangle. 
       
           
        
          
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      Results: 
        Three soil information products were provided: fuzzy membership maps of 
        individual soil types (series), raster soil series maps, and conventional 
        soil polygon maps. 
        ---- Fuzzy Membership Maps 
        Fuzzy membership maps showing the spatial gradation of soils and preserving 
        the intermediate nature (between types nature) of soils. This preservation 
        would assist in soil interpretation. The images show the membership variation 
        of Anakeesta (Right Upper) and Sylco (Right Lower) respectively. Anakeesta 
        occupies most ridge top areas and slopes areas above frigid line while 
        Sylco occupies most ridge top areas and slopes areas below frigid line. 
        The membership maps show a realistic gradation of the two soil types when 
        one travels from high elevation to low elevation position. 
        
      ---- 
        Raster Soil Maps 
        Conventional soil type maps can be produced through harden process from 
        the fuzzy membership maps derived from the SoLIM approach.  
       
           
        
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        Polygon Soil Maps (with the minimum mapping size of 1 hectare) 
        Conventional soil polygon like maps can also be created from the fuzzy 
        representation. We know that it is inevitable for a soil polygon to include 
        some small soil bodies which are different from what the soil polygon 
        is labeled to be. These inclusions can be reported per soil polygon basis 
        which is a great improvement over the conventional approach to reporting 
        inclusions (often lumped into a mapping unit). 
          
         
      Evaluation: 
        ---- Accuracy for model develop area – Mt. Guyot: 30 meter resolution 
        - 96.43% (54 out of 56); 10 meter resolution – 98.21% (55 out of 
        56)  
        ---- Accuracy for extrapolated areas – Mt. Le Conte: 30 meter resolution 
        - 92.68% (38 out of 41); 10 meter resolution– 92.68% (38 out of 
        41) 
        ---- Accuracy for extrapolated areas – Clingmans Dome: 30 meter 
        resolution - 97.67% (42 out of 43) 
       
        
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      University 
        of Wisconsin - Madison 
        A-Xing Zhu and James 
        Burt, principal investigators, provide leadership in applying 
        and evaluating the SoLIM approach in the study area; 
        Rongxun Wang, project assistant, 
        do soil inference 
         
        Natural Resources Conservation Service 
        Darwin Newton and Roy 
        Vick, provide administrative leadership respectively for 
        the states of Tenne4ssee and North Carolina; 
        Anthony Khiel and Doug 
        Thomas, serve as the local NRCS project coordinator; 
        Berman Hudson and Sheryl 
        Kunickis, provide guidance and support from  
        the national NCSS perspective and oversee partial funding of the proejct 
        from the NRCS persepetive 
         
        National Park Service 
        Pete Biggam, serve as project 
        coordinator from the NPS; 
        Mike Jenkins, serve as the 
        local contact representing GRSM 
       
        
          
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     last 
      updated: March 8, 2004 | 
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