The team is also testing Iron Reduction in Sediment (IRIS)
probes to see if these might be a simple and cost-effective way to monitor
redox changes on the broader landscape when collection of subsurface water
samples may not be practical. These
probes consist of PVC coated with a ferrihydrite paint (photo 2). Under reducing conditions iron on these
probes will partially dissolve. The
amount of dissolution can be quantified by image analysis and related in a
semi-quantitative fashion to redox conditions in the sediment. IRIS probes have been approved by the EPA for
demonstrating the presence of reducing soils for wetlands delineation. We are
deploying these probes adjacent to our rhizon arrays so that we can compare out
chemical results (a snapshot in time) to the time integrated signals provided
by the IRIS probes, which will be pulled in September. Image analysis will employ LANL’s GENIE
technology.
In addition to synoptic survey activities, Liz Miller of
LANL has also joined the team to perform a high-resolution differential GPS
survey of troughs and flooded low-centered polygons to fill in gaps in LIDAR
data. This data will provide sub-centimeter
elevation profiles for improved hydrologic modeling of the site (photo 3).
After rigorous days in the field, field team leader Heikoop
was particularly impressed that his younger colleagues decided rooms in the
Herman House should be segregated based on age with no doubt as to which room
he belonged. He also wants to thank
Cathy Wilson for arranging to have high caliber athletes, including a champion
ironwoman and world-class skier on the trip for him to keep pace with. Fortunately everyone has provided plenty of
calorie replenishment back home at ‘camp’ with their array of culinary talents.
Photo 1: Rhizon array in ancient DTLB.
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Photo 2: Mike Hudak holding IRIS probes prior to deployment
in a young DTLB to the south of the BEO.
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Photo 3: Liz Miller performing high-resolution GPS
surveying.
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