Paper No. 13
Presentation Time: 6:00 PM-8:00 PM
DRESSING THE EMPEROR: THE ROLE OF THREE-DIMENSIONAL INFORMATION VISUALIZATION SOFTWARE IN THE DEVELOPMENT OF THREE-DIMENSIONAL HYDROGEOLOGIC MODELS
The goal of this research is to develop a model that describes the saturated and
unsaturated groundwater flow in Berrien County, Michigan (1,350 km2), an area containing
a complex sequence of glacio-lacustrine deposits. Stone and others (2001) mapped
the morphosequences in Berrien County at a scale of 1:24,000, which includes georeferenced
structure contours for 20 individual units. We have developed a methodology to
translate this detailed morphostratigraphy into a solid three-dimensional geologic
model, and then into a three-dimensional block of data that can be used as input
to a finite-difference groundwater-flow model. Letsinger and others (2006) describe
the process of using geographic information system software to convert the structure
contours into georeferenced raster layers that describe each unit. At this stage
of the reconstruction, only the bounding surfaces between the units are defined.
In order to stack the units in vertical space using customized computer code,
a “virtual well field” (regularized two-dimensional array of points)
samples each x-y location in each of the 20 rasterized data layers. Units that
are intersected from the top bounding surface (surface topography) to the bottom
bounding surface (bedrock surface) are then identified. The result of this step
is a vector (one-dimensional array) at each virtual well location that describes
the elevation of each morphostratigraphic unit boundary intersected at that location.
However, at this stage, the model is essentially a regularized three-dimensional
point cloud, and three-dimensional information visualization software (3DIVS)
is then utilized to generate a solid geologic model by interpolating the vertical
geologic “samples” throughout the model domain. A finite-difference
grid (“brickpile”) at the chosen resolution of the groundwater-flow
model is then generated from the solid geologic model using data-processing functions
of the 3DIVS.