Water Canyon/Canyon de Valle investigation was conducted by Glorieta Geoscience, Inc., in collaboration with Los Alamos National Laboratory during 2010-2011 to assess contaminant inventory in post-1942 sediments. Characterization of post-1942 sediments using hand-dug pot holes, dendrochronology and measurement of cross sections following post-fire floods.
1 of 35
Download to read offline
More Related Content
Post-Fire Sediment Transport and Erosion in the Water Canyon and Canon de Valle Watershed, Jamez Mountains, NM
1. Post-Fire Sediment Transport and Erosion
in the Water Canyon and Ca単on de Valle
Watershed, Jemez Mountains, NM
DRAKOS, Paul, RENEAU, Steven, SCHULTZ-FELLENZ, Emily, RIESTERER,
Jim, KELLEY, Rick, MILLER, Elizabeth, GOETZE, Phillip, and
CHAMBERLAIN, Paul
GLORIETA GEOSCIENCE INC
3. Water Canyon/Ca単on de Valle investigation
conducted 2010-2011 to assess contaminant
inventory in post-1942 sediments
1:200 scale mapping in 25+ reaches
Characterization of post-1942 sediments using hand-dug pot
holes (identified based on presence of exotic clasts, buried
soils, bedrock, etc.)
Dendrochronology utilized to provided supplemental
information to constrain the age of flood deposits
Reworked ash from 1977 La Mesa fire and 2000 Cerro
Grande fire preserved in situ within sediment deposits
provides additional age control
Measurement of cross sections following post-fire floods on
8/3/11 and 8/21/11
8/21/11 flood est. ~3000 cfs in CDV, larger than 8/3/11 flood
GLORIETA GEOSCIENCE INC
4. Extent of 1977 La Mesa fire within Water Canyon/
Ca単on de Valle Watershed
5. Extent of 2000 Cerro Grande fire within Water Canyon/Ca単on de
Valle Watershed and maximum post-fire discharge (6/2000)
740 cfs
840 cfs
274 cfs
6. Extent of 2011 Las Conchas fire within Water Canyon/Ca単on de
Valle Watershed, and estimated discharge from 8/21/2011 flood
~3000 cfs (estimated)
1600+ cfs (estimated)
3500 cfs (est.)
7. Sediment delivery after Cerro Grande wildfire
(Reneau et al., 2007)
Over 90% of ash delivered to LA Canyon reservoir in
the first year after the fire
Slurries dominated by ash flow (suspended sediment)
follow first convective storm after the wildfire
Sediment transport rates declined after first year, but
remained above pre-fire levels five years after the fire
Significant increase in erosion rates in the first year
following the fire
Rapid decline in fine-grained sediment transport,
whereas coarse-grained sediment transport is
prolonged (bedload transport during snowmelt runoff)
Post-fire sediment is primarily deposited within first
two years after the fire
8. Preservation of in situ ash in post-1942 sediment deposits
Cerro Grande muck deposit
(June 2000)
16. Cross sections in Reaches WA-2 and WA-3 showing post-1942
sediment deposition and post-Las Conchas fire muck deposits
23 of 58 cm post-fire sed (f1s)
CG ashy si-fs
10 of 10 cm
post-fire sed (f2)
~58 of 123 cm
~58 of 123 cm post-fire sed (f1)
post-fire sed (c2)
CG ashy si
CG ashy si LM(?) ashy vfs
CG ashy si at base
LM deposit at base
17 of 127 cm post-fire sed (c3)
18. Cross sections in Reach CDV-1E showing post-1942 sediment
deposition and post-Las Conchas fire muck deposits and erosion
measured after floods on 8/3/11 (left) and 8/21/11 (right)
> 50% (+/-75%) of post 1942 sediment deposits are post-fire seds
CG muck
at base
CG ashy si
19. Cross sections in Reach
CDV-2W showing post-
1942 sediment
deposition and post-Las
Conchas fire muck
deposits and erosion
measured after flood
on 8/21/11
Note in lower cross section
Some channel incision but
most post-1942 sediments
remain in place.
CG muck
CG ashy si+vfs
GLORIETA GEOSCIENCE INC
20. Cross sections in Reach CDV-2W showing post-1942
sediment deposition and post-Las Conchas fire muck
deposits and erosion measured after flood on 8/21/11
Note erosion of
c2 sediments
next to channel,
preservation of
c3/f1 deposits on
higher surface,
deposition of
muck from
8/3/11 and
coarse sediment
from 8/21/11
flood.
23. Cross sections in Reach CDV-3 showing post-1942 sediment deposition
and post-Las Conchas fire muck deposits measured after flood on
8/3/11; upstream (left) and downstream (right); post-fire sediment
<20% of total post-1942 deposition
27. Cross sections in Reach WA-5 showing post-1942 sediment
deposition and post-Las Conchas fire muck deposits and erosion
measured after floods on 8/3/11 (left) and 8/21/11 (right)
GLORIETA GEOSCIENCE INC
29. Coarse sediment deposits in Ca単on de Valle from August 21,
2011, flood. Gravel bar adjacent to channel in reach CDV-1E.
30. Coarse sediment deposits in Ca単on de Valle from 8/21/2011
flood. ~2 to 4 m wide gravel deposit buries 0.5m wide
channel in Reach CDV-2W
31. Scour hole in reach CDV-1E demonstrating channel erosion
in Ca単on de Valle from August 21, 2011, flood.
32. Water Canyon fan deposit at Rio Grande (left) and
detail showing ~10 cm thick L.C. muck deposit (right)
Water Canyon Fan
Coarse (ms-cs) sediment
from 8/21/11 flood?
Muck from
8/3/11 flood?
Photos taken 11/30/11
Post-Las Conchas sediment deposits along Rio Grande
33. Conclusions
First post-Las Conchas fire flood on 8/3/11 deposited muck layer
(ashy silt) with a maximum thickness of 22 cm at cross section
locations
Some erosion also occurred
Second post-Las Conchas fire flood on 8/21/11 was larger
discharge event. Coarser-grained sediment deposits up to 50 cm
thick at cross section locations were observed in both overbank
and channel settings.
Considerable scour and bank widening also observed during
second flood event.
Total post-fire related sediment deposits from LM, CG, and LC
fires at randomly selected cross sections ranges from up < 20% to
75%, shows a general down-stream attenuation trend
Post-LC muck and coarser-grained sediment deposits observed at
mouth of Water Canyon at Rio Grande.
GLORIETA GEOSCIENCE INC
34. Pending Investigation (2012)
Systematic assessment of post-Las Conchas erosion and
deposition in reaches investigated in 2010/2011
Reoccupy and resurvey cross sections to quantify post-Las
Conchas fire erosion and deposition at specific locations
GLORIETA GEOSCIENCE INC