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Iowa Daily Erosion Project 2: Real time 
soil and water resource inventory
Brian K. Gelder, PhD
Associate Scientist
Iowa State University
D. James, D. Herzmann, R. Cruse, J. Laflen, W. 
Kraszewski, J. Opsomer, D. Flanagan, J. Frankenberger
Iowa Daily Erosion Project
• Our mission:
To help farmers, land managers, and the public 
better understand the dynamics and magnitude of 
runoff and soil erosion through daily estimation of 
these processes on agricultural areas and 
dissemination of the estimates via the web
These estimates are made using WEPP, the Water 
Erosion Prediction Project model, a mechanistic 
model designed for agricultural and forest plots.
• Township 
level data
– Soils
– Slopes
– Manage
ment
NEXRAD 
Precip
data
Iowa Daily Erosion Project 1
• Estimating
– Sheet and rill erosion 
– Soil moisture 
– Runoff
– Rainfall
• On 18,000 hillslopes
– 6‐20 per township
• Weather from NEXRAD/ 
Iowa Mesonet
• Slope, soils, and 
management 
information from 1997 
USDA Natural Resource 
Inventory (NRI)
– Extrapolated to present
• Estimates aggregated to 
township level
• Debuted in 2003
Iowa Daily Erosion Project 2
• IDEP continues to function, but
– Rotations are out of date (1994‐97)
– Hillslopes are simple, uniform slope
– Actual locations not known
• Impossible to assess current accuracy
• Township structure not ideal for water issues
• Research in remote sensing makes it possible to 
generate all model inputs
– Run at HUC12 watershed scale on approximately 250 
flowpaths per watershed
• 1700 HUC12 watersheds, each approximately 100 km2
NEXRAD 
Precip
LiDAR
Slopes
SSURGO 
Soils
Remote 
Management
Iowa Daily Erosion Project 2
• New Interface
– Similar to Google Earth, Bing Maps
• Selectable basemaps, overlays, data layers
• Transition to remotely sensed inputs
– Rainfall – 1x1 km 5 minute NEXRAD
• Upgraded from 4x4 km 15 minute NEXRAD
– Management – Remote sensing of crops/residue cover
– Hillslope profile – LiDAR derived 
– Soils – SSURGO derived
• Enables field and watershed monitoring comparisons 
for estimating model accuracy and precision
– Eventually stream delivery and channel erosion
IDEP 2 Rainfall
• Upgrade to Level II
NEXRAD radar data
from the NWS and UI
– 1 x 1 km rainfall
– Every 5 minutes
• Previously
– 4 x 4 km rainfall
– Every 15 minutes
• Improved wind, temp,
and solar spatial
resolution
IDEP 2 Management
• Estimates are currently made on 
agricultural land parcels greater 
than 10 acres
• To accurately delineate 
agricultural land we began with 
pre‐2008 publically available 
USDA FSA Common Land Units
• A CLU has
– Permanent, contiguous boundary
– Common land cover & 
management
– Common owner
– Common producer
• Does not represent crop 
boundaries
• Aerially truthed to 2009 field 
boundaries
IDEP 2 
Management
• To obtain crop 
rotations we use 
USDA NASS 
Cropland Data 
Layer
– Annual map of 
crop cover
– Based on Landsat 
& other images
– Does not delineate 
common 
management 
practices
2011
20092008
2010
20132012
IDEP 2 
Management
2011
20092008
2010
20132012
For each 2009 field boundary the 
majority land cover and fraction is 
calculated for each year from 
2008‐2013 and the pattern is 
assigned to one of nine major 
rotation types and extrapolated to 
the current year.
+
IDEP 2 Management
2008‐2013 Crop Rotations
IDEP 2 Management
• Remotely sensed residue 
cover estimates will come 
from Landsat TM and 
ETM+ sensor
• Soil and residue reflect 
differently in middle 
infrared
• Index relationship can 
define tillage intensity
• Index uses crop cover 
from previous step to 
improve estimates
IDEP 2 Management
Post Fall Residue Polygons NDTI = Band 5 – Band 7
Band 5 + Band 7
IDEP 2 Management
• Determining residue cover (RC)
– Identify and download all imagery 
from the Landsat archive over Iowa 
from October 15 to June 15 from 2000‐
01 to 2011‐12
– Use Fmask, an automated process for 
classifying imagery into snow, cloud, 
cloud shadow, water, and clear sky 
pixels
– Visually inspect Fmask results to find 
any missed clouds and create 
additional cloud/shadow masks if 
needed
– Calculate Normalized Difference Tillage 
Index (NDTI) value to estimate RC
IDEP 2 Management
• Steps to determine residue cover (RC)
– Utilize date, crop, growing crop (and 
potentially soil) adjusted NDTI values to 
calculate residue cover
• 100% NDTI value decreases with time
• 100% decreases from corn ‐> beans
• 0% ‐ consistent across date & crop
• Growing crop increases values
• No till class may be needed
– Utilizing all available imagery minimum 
residue cover for each field is estimated in 
two time periods
• After fall tillage (before March 15)
• After planting (before June  15)
– Based on residue cover estimates, corn 
and soybean tillage practices are assigned 
to 1 of 4 possible regimes
• No‐till
• Mulch‐till (2 levels) 
• Conventional tillage
y = 507.95x - 23.333
R² = 0.8063
0
10
20
30
40
50
60
70
0.000 0.050 0.100 0.150 0.200
AVG_RCPLAN
NDTI_Corn
y = 165.95x + 0.0596
R² = 0.1142
0
10
20
30
40
50
60
70
0.000 0.050 0.100 0.150 0.200
AVG_RCPLAN
NDTI_Soybean
IDEP 2 Hillslope Profiles
• LiDAR topographic data
can better predict water
flow across the landscape
but LiDAR is not perfect –
– Doesn’t always flow
• Roads/railroads create digital
dams
• Areas of no returns (water,
heavy trees) create errors
– Enforcement is needed to
get water to the channels
or depressions and not
back up in fields
Fill Depth at 3 m Resolution
Best Connection(s)
Remaining Fill Depth
IDEP 2 Hillslopes (Cont.)
• Once surface is enforced 
further processing begins
– Too many flowpaths to run 
them all
• Random sampling
– Stratify HUC12s into 
subcatchments
• Using Douglas‐Peuker constant 
drop stream analysis
• 100‐250 subcatchments per 
HUC12
– Select 1 ag flowpath per 
subcatchment
Catchments and Channels
Field Level Flowpaths
Field Level Flowpaths and Soils
HUC12 Framework
IDEP2 Rainfall
IDEP2 Erosion
IDEP2 Runoff
Questions?
• Acknowledgements:
– Iowa State University Agronomy Department 
Endowment
– USDA Agricultural Research Service
– Environmental Defense Fund
IDEP 2 Management
June 1 2011 Residue Cover Index

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