Using GIS Techniques to Identify and Delineate Karst ... · Types of elevation data National...
Transcript of Using GIS Techniques to Identify and Delineate Karst ... · Types of elevation data National...
Geohazards Impacting Transportation in the Appalachian Region – 11th Annual Technical Forum
Chattanooga, TN – August 4, 2011
Using GIS Techniques to Identify and Delineate Karst Features in Tennessee
Background
Karst features (such as sinkholes) present challenges to the planning and construction of roads and
other public works natural-resources management topographic/hydrologic analysis
Approximately 2/3 of Tennessee is in karst terrain
Problem
Hand-delineation from maps is inefficient for large areas
Automated techniques using digital elevation data can be used, but it is not straightforward Digital elevation data are never “perfect” Digital filters must be used to control the detection of
false positives and false negatives
GIS Karst Delineation
Needs: Digital Elevation Model (DEM)
GRID format – array of cells with elevation values
Hydrography vector format – like a polyline shapefile
Types of elevation data
National Elevation Dataset (NED) Derived from USGS 1:24k topos State-wide
State base-map data Mass points and breaklines
1:4800 rural, 1:1200 in some urban areas Needs thorough QAQC Inconsistent quality across TN
Best data are in West TN (no karst) LiDAR
Best data available Very limited availability
Hydrography Data
High-resolution National Hydrography Dataset (NHD) Primary data source is blue lines from 1:24k
topo maps Proposed local-resolution (TN State base
map) NHD Primary data source is 1:1,200-4,800 imagery
(same as State base map elevation data)
GIS definitions – depressions vs. sinks
GIS Sink – area where surficial flow direction cannot be resolved
GIS Depression – area that must be filled in order to contribute flow to runoff
sinks
depression
GIS Definitions – Depressions vs. Sinks
Depressions and sinkholes
For this analysis and this talk, sinkholes and depressions are synonymous
This terrain analysis method will delineate depressions - areas with some amount of internal drainage
Delineation of depressions - hurdles
All digital data have limitations DEMs
Have some amount of error associated with elevations Elevations are averaged for each cell Tend to have some erroneous small depressions Roads and bridges tend to build artificial dams Discrepancies in depression density between datasets
We must accept a reasonable definition of a “true” depression to weed out “false” depressions
Delineation of depressions - hurdles
Hydrography Huge datasets such as NHD have line work errors
and connectivity errors
Proposed local-res NHD - highly and inconsistently dense Needed to weed out drainage ditches, etc.
Chose only streams that existed in high-res NHD Result was local-res (1:1,200-4,800) line work at high-
res (1:24k) density
Delineation of depressions – Process
Goal is to create a “hydrologically correct” DEM Must have a process that leaves “true” depressions
in DEM and eliminates “false” depressions Steps
1. DEM manipulation and delineation of preliminary depressions
2. Evaluation of depressions3. “True” depression enforcement/delineation and
delineation of watersheds4. Calculation of depression characteristics
DEM Manipulation and preliminary depression delineation
• Hydrography enforcement (“burning”)• Allows for more accurate basin delineation
and correctly routes flow across the landscape
• Fill DEM enforced with hydrography• Gives us a DEM with no depressions
• Subtracting “burned” from “filled” DEM delineates preliminary (first cut) depressions
Hydrography Enforcement
Hydrography Enforcement
Unfilled DEM
Filled DEM
filled area
Evaluation of depressions
Identify depressions with “true” depression characteristics
• Must...• Be > 60 ft (2 cells) away from a connected stream• Be larger than 1 cell (900 sq ft)• Contain a 10-ft contour with an area > 1 cellOr• Include or comprise a disconnected stream
Hydrography Enforcement
60-foot buffer around stream
Tiny depressions must go
Must contain a 10-ft contour
sinking streams must stay
Evaluation of depressions
3. Identify depressions with “true” depression characteristics
• Must...• Be > 60 ft (2 cells) away from a connected stream• Be larger than 1 cell (900 sq ft)• Contain a 10-ft contour with an area > 1 cell,Or• Include or comprise a disconnected stream
The depressions that meet these criteria are our “true”depressions.
“True” depression enforcement and delineation
Fill DEM except areas where true depressions exist
Create grid of “true” depressions
Create watershed for each new depression
Calculation of depression characteristics
Depth characteristics Fill elevation Area characteristics Storage characteristics
raw DEM
depression fill elevation grid
deptharea
volume(storage)
Outcomes
State-wide (eastern 2/3) data set of karst features derived from best elevation data available
Statistical analysis of karst features to understand differences in different physiographic/geologic settings
A tool to aid in the design of roads and other structures built in karst areas of TN
Questions and Comments