Publication | Closed Access
Geologic Nitrogen in Pleistocene Loess of Nebraska
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1976
Year
EngineeringLand DegradationEarth SciencePaleoenvironmental ChangeNo 3 −Quaternary ResearchGeochronologySoil FertilityFertilizer UseBiogeochemistryGeologic NitrogenSoil ScienceNo 3GeographyGeologyEnvironmental GeologyNutrient CycleGeochemistryQuaternary PeriodNutrient Management
Abstract Research into the relationship between fertilizer use and water quality in Nebraska has resulted in the discovery of large quantities of geologic nitrate within the deep loess mantle of southwestern and central Nebraska. The NO 3 − is first encountered at a depth of about 7 m and continues to an unknown depth in excess of 30 m. Nitrate‐N values of 25 to 45 ppm characterize the N zone, but values to 87 ppm have been recorded. The NO 3 − exists only under the leveler uplands of the region; however, it is on this plain that rapid development of irrigation is taking place and it has been shown that the NO 3 − has been leached from beneath older irrigation sites on the plain.