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Description
Soils containing fragipan horizons occupy a significant land area in western Kentucky. These naturally
occurring horizons are dense and often close to the soil surface, allowing them to alter water and nutrient
distribution in a landscape. There is a need to explore management strategies to remediate shallow, fragipan
horizons to promote storage of water. The work proposed here will investigate whether inclusion of a cover
crop (ryegrass) can break up fragipan horizons and promote vertical movement of water and nutrients. Twelve
intact soil cores (7.5 cm internal diameter) will be collected from a site containing a mixture of grasses mainly
dominated by tall fescue located on the West Kentucky Research and Education Center at Princeton, KY. The
soil type is a Zanesville silt loam (fine-silty, mixed, mesic, Typic Fragiudalf) which is forming in loess over
acid sandstone residuum. Ports will be installed with depth in each soil core. Six soil cores will be seeded to
annual ryegrass and the remaining cores will serve as controls. All cores will be incubated in the greenhouse
for one growth cycle. Soil water content will be recorded daily in the ryegrass- and control soil cores using
tensiometers connected to a data logger. Soil solution will be extracted through the installed ports with depth
in all cores at 1 week, 2 weeks, 4 weeks, and 6 weeks of ryegrass growth. Several elements will be quantified
ments (silica, aluminum, iron, manganese, nitrate, nitrite, ammonium) and dissolved organic carbon species
will be quantified immediately. The purpose of following silica, aluminum, and iron is that they have been
implicated in cementing the fragipan. The behavior of nitrate, nitrite, and ammonium will useful to assess
from the standpoint of N cycling which is impacted by flow paths of water. After six weeks of growth, the
ryegrass will be carefully clipped down to the soil surface. A solution of sodium bromide (NaBr) dissolved in
Brilliant Blue FCF dye will be added to the soil surface of ryegrass-grown and control cores and leached until
two pore volumes have leached through the columns. The bromide will serve as a non-reactive solute used to
follow the movement of water. Brilliant Blue FCF dye will serve to illuminate areas of water flow paths in the
soil. The cores will then be sacrificed and soil will be characterized with depth. Digital photographs will be
collected and ImageJ will be used to estimate the area of dye-stained areas in ryegrass-treated soil and
compared with the control. This fits in well with a goal of KWRRI, to promote conservation and management
of water resources.
Status | Finished |
---|---|
Effective start/end date | 6/18/18 → 6/17/19 |
Funding
- US Geological Survey
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Projects
- 1 Finished
-
104B State Water Resources Research Institute Program 2016 - 2021
Ormsbee, L. (PI), Atwood, D. (CoI), D'Angelo, E. (CoI), Erhardt, A. (CoI), Evans, S. (CoI), Ford, W. (CoI), Fox, J. (CoI), Parris, T. (CoI), Unrine, J. (CoI), Zhu, J. (CoI), Pennell, K. (Former PI), Agouridis, C. (Former CoI), Brion, G. (Former CoI), Cagle, L. (Former CoI), Edwards, D. (Former CoI), Fryar, A. (Former CoI), Lee, B. (Former CoI), Matocha, C. (Former CoI), Munshaw, G. (Former CoI), Price, S. (Former CoI), Salmeron Cortasa, M. (Former CoI), Wang, Y. (Former CoI), Wei, Y. (Former CoI), Wendroth, O. (Former CoI) & Yost, S. (Former CoI)
3/1/16 → 12/31/21
Project: Research project