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Organic Matter Dynamics in Kings Creek, Konza Frairie, Kansas, USA

quency characteristics of selected Pennsylvania streams. US Geological Survey Water Investigations Report 90-4160. The Kings Creek basin encompasses 1059 ha within the Konza Prairie Research Natural Area, a tallgrass prairie in the Flint Hills Uplands of eastern Kansas, USA. This region consists of ridges and valleys underlain by chert-bearing limestones alternating with softer shales of Permian age. Because of the relatively steep topography and rocky soils characteristic of the region, this grassland has never been plowed. Extensive fractures within the rocks result in numerous springs and seeps along the main channels. Elevation ranges from 338 m to 430 m. Konza Prairie was established as a research facility in 1972 after many years as a cattle ranch. The research area is subdivided into watersheds that are burned at varying frequencies. Overlaid on this design is a grazing experiment with blocks of watersheds designated as ungrazed, grazed by native ungulates (bison, Bos bison), and grazed by domestic cattle. Bison were reintroduced to Konza Prairie in 1987, and cattle grazing returned in 1992. Konza Prairie has a typical midwestern continental climate with warm, wet summers and dry, cold winters. Mean monthly air temperatures range from -2.7?C (January) to 26.6?C